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Lichens and associated fungi from Glacier Bay National Park, Alaska

Published online by Cambridge University Press:  11 May 2020

Toby Spribille
Department of Biological Sciences, CW405, University of Alberta, Edmonton, Alberta T6G 2R3, Canada Department of Plant Sciences, Institute of Biology, University of Graz, NAWI Graz, Holteigasse 6, 8010 Graz, Austria Division of Biological Sciences, University of Montana, 32 Campus Drive, Missoula, Montana 59812, USA
Alan M. Fryday
Herbarium, Department of Plant Biology, Michigan State University, East Lansing, Michigan 48824, USA
Sergio Pérez-Ortega
Real Jardín Botánico (CSIC), Departamento de Micología, Calle Claudio Moyano 1, E-28014 Madrid, Spain
Måns Svensson
Museum of Evolution, Uppsala University, Norbyvägen 16, SE-75236 Uppsala, Sweden
Tor Tønsberg
Department of Natural History, University Museum of Bergen Allégt. 41, P.O. Box 7800, N-5020 Bergen, Norway
Stefan Ekman
Museum of Evolution, Uppsala University, Norbyvägen 16, SE-75236 Uppsala, Sweden
Håkon Holien
Faculty of Bioscience and Aquaculture, Nord University, Box 2501, NO-7729 Steinkjer, Norway NTNU University Museum, Norwegian University of Science and Technology, NO-7491 Trondheim, Norway
Philipp Resl
Faculty of Biology, Department I, Systematic Botany and Mycology, University of Munich (LMU), Menzinger Straße 67, 80638 München, Germany
Kevin Schneider
Institute of Biodiversity, Animal Health and Comparative Medicine, College of Medical, Veterinary and Life Sciences, University of Glasgow, Glasgow G12 8QQ, UK
Edith Stabentheiner
Department of Plant Sciences, Institute of Biology, University of Graz, NAWI Graz, Holteigasse 6, 8010 Graz, Austria
Holger Thüs
Botany Department, State Museum of Natural History Stuttgart, Rosenstein 1, 70191 Stuttgart, Germany Natural History Museum, Cromwell Road, London SW7 5BD, UK
Jan Vondrák
Institute of Botany of the Czech Academy of Sciences, Zámek 1, 252 43 Průhonice, Czech Republic Department of Botany, Faculty of Science, University of South Bohemia, Branišovská 1760, CZ-370 05 České Budějovice, Czech Republic
Lewis Sharman
Glacier Bay National Park & Preserve, P.O. Box 140, Gustavus, Alaska 99826, USA
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Lichens are widely acknowledged to be a key component of high latitude ecosystems. However, the time investment needed for full inventories and the lack of taxonomic identification resources for crustose lichen and lichenicolous fungal diversity have hampered efforts to fully gauge the depth of species richness in these ecosystems. Using a combination of classical field inventory and extensive deployment of chemical and molecular analysis, we assessed the diversity of lichens and associated fungi in Glacier Bay National Park, Alaska (USA), a mixed landscape of coastal boreal rainforest and early successional low elevation habitats deglaciated after the Little Ice Age. We collected nearly 5000 specimens and found a total of 947 taxa, including 831 taxa of lichen-forming and 96 taxa of lichenicolous fungi together with 20 taxa of saprotrophic fungi typically included in lichen studies. A total of 98 species (10.3% of those detected) could not be assigned to known species and of those, two genera and 27 species are described here as new to science: Atrophysma cyanomelanos gen. et sp. nov., Bacidina circumpulla, Biatora marmorea, Carneothele sphagnicola gen. et sp. nov., Cirrenalia lichenicola, Corticifraga nephromatis, Fuscidea muskeg, Fuscopannaria dillmaniae, Halecania athallina, Hydropunctaria alaskana, Lambiella aliphatica, Lecania hydrophobica, Lecanora viridipruinosa, Lecidea griseomarginata, L. streveleri, Miriquidica gyrizans, Niesslia peltigerae, Ochrolechia cooperi, Placynthium glaciale, Porpidia seakensis, Rhizocarpon haidense, Sagiolechia phaeospora, Sclerococcum fissurinae, Spilonema maritimum, Thelocarpon immersum, Toensbergia blastidiata and Xenonectriella nephromatis. An additional 71 ‘known unknown’ species are cursorily described. Four new combinations are made: Lepra subvelata (G. K. Merr.) T. Sprib., Ochrolechia minuta (Degel.) T. Sprib., Steineropsis laceratula (Hue) T. Sprib. & Ekman and Toensbergia geminipara (Th. Fr.) T. Sprib. & Resl. Thirty-eight taxa are new to North America and 93 additional taxa new to Alaska. We use four to eight DNA loci to validate the placement of ten of the new species in the orders Baeomycetales, Ostropales, Lecanorales, Peltigerales, Pertusariales and the broader class Lecanoromycetes with maximum likelihood analyses. We present a total of 280 new fungal DNA sequences. The lichen inventory from Glacier Bay National Park represents the second largest number of lichens and associated fungi documented from an area of comparable size and the largest to date in North America. Coming from almost 60°N, these results again underline the potential for high lichen diversity in high latitude ecosystems.

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This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (, which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright © British Lichen Society 2020

Table of Contents

  • Introduction

  • The present study

  • Materials and Methods

  • Study area

  • Climate

  • Glaciation and vegetation history

  • Stratification of study area into target sampling units

  • Specimen analysis

  • Molecular data

  • Phylogenetic trees

  • Species delimitation and nomenclature

  • Presentation of species data

  • Comparison between sectors and national parks

  • Results and Discussion

  • Comparison of sectors within GLBA

  • Lichen diversity in the national parks of the greater Gulf of Alaska region

  • Phylogenetic trees

  • Descriptions of New Genera and Species

  • Atrophysma T. Sprib.

  • Atrophysma cyanomelanos T. Sprib.

  • Bacidina circumpulla S. Ekman

  • Biatora marmorea T. Sprib.

  • Carneothele Fryday, T. Sprib. & M. Svenss.

  • Carneothele sphagnicola Fryday, M. Svenss. & Holien

  • Cirrenalia lichenicola Pérez-Ort.

  • Corticifraga nephromatis Pérez-Ort.

  • Fuscidea muskeg Tønsberg & M. Zahradn.

  • Fuscopannaria dillmaniae T. Sprib.

  • Halecania athallina Fryday

  • Hydropunctaria alaskana Thüs & Pérez-Ort.

  • Lambiella aliphatica T. Sprib. & Resl

  • Lecania hydrophobica T. Sprib. & Fryday

  • Lecanora viridipruinosa M. Svenss. & T. Sprib.

  • Lecidea griseomarginata Fryday

  • Lecidea streveleri T. Sprib.

  • Miriquidica gyrizans Fryday

  • Niesslia peltigerae Pérez-Ort.

  • Ochrolechia cooperi T. Sprib.

  • Placynthium glaciale Fryday & T. Sprib.

  • Porpidia seakensis Fryday

  • Rhizocarpon haidense Brodo & Fryday

  • Sagiolechia phaeospora Fryday & T. Sprib.

  • Sclerococcum fissurinae Pérez-Ort.

  • Spilonema maritimum T. Sprib. & Fryday

  • Thelocarpon immersum Fryday

  • Toensbergia blastidiata T. Sprib. & Tønsberg

  • Xenonectriella nephromatis Pérez-Ort.

  • Other Species Treated in Detail

  • Absconditella rosea Kalb & Aptroot

  • Lecanora alaskensis H. Magn.

  • Lecanora leptacina Sommerf.

  • Lepra subvelata (G. K. Merr.) T. Sprib. and similar taxa

  • Ochrolechia xanthostoma (Sommerf.) K. Schmitz & Lumbsch and similar taxa

  • Steineropsis alaskana T. Sprib. & Muggia

  • Steineropsis laceratula (Hue) T. Sprib. & S. Ekman

  • Known Unknowns

  • Catalogue of All Named Taxa Found

  • Acknowledgements

  • References


The landscapes of south-east Alaska are best known for their most striking macrofeatures: snow-capped mountains, misty saltwater fjords and dark coniferous rainforests. Closer examination reveals that the texture of nearly every terrestrial feature in south-east Alaska is, in one way or another, determined at a much smaller scale. Zooming from the landscape view into the canopies of the coastal rainforests and the tapestry of their outcrops and boulder fields reveals a Russian doll of nested ecosystems, one within another, within another. At the scale of an ecosystem a human can hold in her hand, it is fungi and bryophytes that form the building blocks of the multicellular canopy, supporting yet another set of nested dolls of microbial and invertebrate life in their peaks and ravines. It is at this scale, where fungi, algae and bacterial biofilms meet in a permanently wet, cold milieu, that the south-east Alaskan temperate rainforest exhibits peak biodiversity.

Lichens, s’éixwani to the Tlingit (Edwards Reference Edwards2009), the indigenous people of south-east Alaska, played a role in traditional food and garment dyeing for the residents of these fjords for thousands of years. In Glacier Bay, the subject of the present paper, lichens are featured in place names and play an outsized role in the recent vegetation history. When the first European collections of lichens were made here, in the framework of the Harriman Expedition (Cummings Reference Cummings, Cardot, Cummings, Evans, Peck, Thériot and Trelease1904), Glacier Bay had only recently undergone a massive glacial retreat of over 80 km as a result of saltwater glacial erosion. Only a few years later, the American ecologist William Skinner Cooper arrived in Glacier Bay and began a series of studies that shaped the textbook description of plant succession (Cooper Reference Cooper1923), now the longest-running primary succession plot series in the world (Buma et al. Reference Buma, Bisbing, Krapek and Wright2017). Despite its fame in plant ecology, Glacier Bay was neglected by lichen researchers in the 20th century. Far fewer collectors have worked here compared to other localities in Alaska, for example, the Juneau region (Krog Reference Krog1968), Sitka or the north end of the Lynn Canal (see e.g. Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010). Between the 1899 Harriman Expedition and the beginning of the present study, we could reconstruct the activity of 17 different collectors or groups of collectors, based on specimens in US, Canadian and Swedish herbaria (Supplementary Material Table S1, available online). Most collected specimens of common macrolichens, with a few notable exceptions. By the end of the 20th century, the recently deglaciated tundra-like pavements visited during the Harriman Expedition had grown into mature forest (Buma et al. Reference Buma, Bisbing, Krapek and Wright2017).

Since the 1990s, attention has been increasingly focused on south-east Alaska as a biodiversity hotspot in conjunction with controversy over commercial logging in the Tongass National Forest (Durbin Reference Durbin1999). In parallel, ecologists have begun to draw attention to the forests of south-east Alaska as a global archetype of ‘temperate rainforest’ (DellaSala et al. Reference DellaSala, Moola, Alaback, Paquet, Schoen, Noss and Della Sala2011), highlighted to a significant extent by characteristic lichen assemblages (Goward & Spribille Reference Goward and Spribille2005). While some research was conducted on south-east Alaska's lichens in the 1960s (McCullough Reference McCullough1965; Krog Reference Krog1968), lichens gained significance here from the 1990s onwards, with their use in air quality monitoring (Geiser et al. Reference Geiser, Derr and Dillman1994; Derr et al. Reference Derr, McCune and Geiser2007; Derr Reference Derr2010), the characterization of ecological indicator species (Dillman Reference Dillman2004; Root et al. Reference Root, McCune and Jovan2014), the drafting of a first lichen list for all of south-east Alaska (Geiser et al. Reference Geiser, Dillman, Derr, Stensvold, Glenn, Harris, Dirig and Cole1998) and the first steps to manage National Forest lands for rare and ‘sensitive’ lichens. Considerable work has been carried out in coastal temperate rainforest areas to the south, especially by I. M. Brodo on Haida Gwaii (e.g. Brodo Reference Brodo1995, Reference Brodo2010; Brodo & Ahti Reference Brodo and Ahti1996; Brodo & Santesson Reference Brodo and Santesson1997; Brodo & Wirth Reference Brodo, Wirth, Glenn, Harris, Dirig and Cole1998). Systematic and phylogeographic studies have suggested that outer coastal rainforests bordering the north-eastern Pacific Ocean may have provided Pleistocene refugia to epiphytic lichens (Printzen et al. Reference Printzen, Ekman and Tønsberg2003) and, for some taxa, a hotbed of speciation (Brodo Reference Brodo1995; Jørgensen Reference Jørgensen2005).

Cruise ship tourism has gradually increased since its onset in the late 1960s and concerns about air quality have led to the introduction of lichen-based biomonitoring in Glacier Bay and elsewhere in south-east Alaska. In recent years, c. 400 000 people have visited Glacier Bay annually on cruise ships, constituting over 95% of all visitors (Nemeth & Apgar Reference Nemeth and Apgar2010). A cruise ship may spend 9–12 hours in Glacier Bay, with delays in the lower bay to pick up Park rangers and berthing time in front of glaciers in the upper West Arm. Output of pollutants in Glacier Bay has been estimated at 780 mol km−2 h−1 for SO2 in a single season under reported cruise speeds (Mölders et al. Reference Mölders, Gende and Pirhalla2013). Air quality monitoring plots based on lichen community and collection protocols were established as a baseline for the first time in 2008 at Bartlett Cove (at Park Headquarters near Gustavus) and Blue Mouse Cove in the West Arm of Glacier Bay. Monitoring included throughfall deposition analysis and direct measurement of heavy metal concentrations in lichen thalli using inductively coupled plasma mass spectrometry (ICP-MS; Schirokauer et al. Reference Schirokauer, Geiser, Bytnerowicz, Fenn and Dillman2014). Air quality monitoring relies on two approaches in this ongoing long-term study: 1) the propensity of lichens to accumulate heavy metals that can then be quantified using an ICP-MS element analysis protocol; 2) the indicator value of species assemblages rated for sensitivity to nitrogen enrichment and SO2. Results to date record an elevated amount of lithium at the Blue Mouse Cove site and elevated N values (c. 90% above regional reference thresholds), both attributed to natural factors such as geology and proximity to seawater (Schirokauer et al. Reference Schirokauer, Geiser, Bytnerowicz, Fenn and Dillman2014). However, lichen compositional data were well within the range of reference sites on the adjacent Tongass National Forest (Schirokauer et al. Reference Schirokauer, Geiser, Bytnerowicz, Fenn and Dillman2014).

Several factors make compositional analysis of lichens for air quality monitoring relatively difficult with the knowledge we have to date. First, our baseline knowledge of the lichens has been, until now, rudimentary. As much as 10% of the lichen species in south-east Alaska have yet to be given scientific names (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010; present study). Second, achieving meaningful levels of biological species monitoring requires factoring in the successional dynamics and high geological and climatic heterogeneity of Glacier Bay itself. Species composition shifts may be as likely to be related to these natural abiotic factors as they are to external stressors such as increased pollutant deposition. Partitioning the signal for natural and anthropogenic factors benefits from increased resolution in lichen taxonomy.

The present study

The documentation of over 750 lichens and associated fungi in the nearby Klondike Gold Rush National Historical Park (KLGO; Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) suggested that lichen richness in SE Alaska was even greater than previously estimated. It raised several questions relevant to understanding both regional species richness patterns and the behaviour of meta-regional lichen species assemblages: 1) is such richness generally to be expected in coastal Alaska, or was KLGO exceptionally rich? 2) How specific is regional species composition (i.e. how much ‘turnover’ in species would there be from one fjord to another)? 3) On a gradient from inland to outer coast (increasing oceanicity), how does lichen richness change? These questions were at the core of a proposal funded in 2011 by the US National Park Service to replicate the KLGO study c. 80 km to the SSW in Glacier Bay National Park (hereafter referred to by its US National Park Service acronym, GLBA, and not equivalent to ‘Glacier Bay’, which refers to the bay itself). We hypothesized that the high species numbers we detected in KLGO were not unique, but that the infrequency with which such results are reported was rather a reflection of the large investment in effort required to name species in a poorly studied region. We also hypothesized that GLBA would have more species owing to its larger size and greater geological diversity but would largely overlap with the KLGO species pool. Answering questions 1 and 2 above would be possible with an inventory that replicated the style and intensity of the KLGO study; answering question 3 might be more difficult, as many factors covary with climate while, independently, richness can be influenced by geological parent material. We expected this to be the case in GLBA as it is geologically complex, straddling no fewer than three tectonostratigraphic terranes (Perry et al. Reference Perry, Garver and Ridgway2009).

Sixty-nine species of lichens had been recorded for GLBA at the time we began our study in 2011 (Bennett & Wetmore Reference Bennett and Wetmore2005). We had two objectives: 1) to acquire a baseline inventory of species in GLBA to support future ecological and monitoring studies; 2) to develop a georeferenced species occurrence database on species pool and turnover (a) along a deglaciation gradient and (b) between geographical sectors and nearby areas (such as KLGO). While imperfect, the resulting data set allows us to make inferences about species richness patterns fjord-to-fjord as well as local and regional gradients. Our results are aggregated into two parts: A) a condensed summary of the species inventory results and caveats, and how these inform our understanding of regional species turnover in SE Alaska; B) a full list of the taxa discovered, including 29 taxonomic novelties (two genera, 27 species) and 71 known unknowns, species which we recognize but the taxonomy of which cannot be resolved at this time.

Materials and Methods

Study area

Glacier Bay National Park and Preserve (Fig. 1) is one of the largest national parks in the United States, at 10 849 km2 including 10 616 km2 in the National Park proper and 233 km2 in the Preserve, located in the delta of the Alsek River to the north-west of the park and administered by the park. The current study is concerned only with the National Park and within GLBA with terrestrial and intertidal habitats not currently covered by glaciers. The non-glacier terrestrial land base of GLBA, and thus the study area, currently encompasses c. 6023 km2. Almost the entire study area is inaccessible by road, the exceptions being the park headquarters area at Bartlett Cove and an access road to the city water supply intake for the town of Gustavus, on Falls Creek. Except for sampling sites in the Bartlett Cove, Tower Road, Gustavus, Falls Creek and Excursion Ridge areas, all sites surveyed were accessed by boat. Landing accessibility, weather and boat scheduling were major factors in planning our sampling.

Fig. 1. A, Alaska and the north-east Pacific showing US national parks in which major lichen inventories have been conducted in the last ten years (outlined); B, Glacier Bay National Park, showing sample sites (black circles) and subdivisions into sectors referred to in the text (separated by black lines). Geographical sectors are indicated as follows (see text for more details): DUN = Dundas, EA = East Arm, EX = Excursion Ridge, GB = Glacier Bay, GUS = Gustavus, WA = West Arm.


The Glacier Bay area is dominated by a wet, maritime climate with moderate temperature fluctuations and low overall annual temperature. We generated a Walter-Lieth climate diagram (Fig. 2) with data from NOAA (2000) using the R package climatol v3.1.2 ( The mean monthly temperature at Bartlett Cove is 5.3 °C, which is similar to Skagway (5.1 °C) near KLGO, with freezing temperatures common from November to March. The outer, coastal parts of GLBA however are much warmer, with Cape Spencer registering only 70 freezing days per winter over a six-year period (Loewe Reference Loewe and Mirsky1966). The annual precipitation at Bartlett Cove is 1770 mm, nearly three times that of Skagway (666 mm; NOAA 2000) but still considerably less than on Haida Gwaii, British Columbia (2140–2523 mm; Brodo Reference Brodo1995). Variation in precipitation within GLBA is likely to be large. Outside of the long-term sampling at Bartlett Cove, data for Cape Spencer, on the outer coast and near one of our sampling sites in the present study, indicate annual precipitation of 2860 mm, and at Yakutat, which is on the coast 150 km to the north, 3330 mm (Loewe Reference Loewe and Mirsky1966). Values over 2000 mm are probably widespread in Glacier Bay, especially in mountain areas and to the west of the Fairweather Mountains. Preliminary data support the impression that the West Arm might lie in a rain shadow, receive less rain and snow than the East Arm or the main part of Glacier Bay, and be c. 1 °C colder than the rest of Glacier Bay (Kopczynski et al. Reference Kopczynski, Bigl, Lawson and Finnegan2003; Finnegan et al. Reference Finnegan, Lawson, Kopczynski, Piatt and Gende2007). Short-term data from climate measurements over several summers at Casement Glacier in the East Arm indicate values similar to those at Gustavus (Loewe Reference Loewe and Mirsky1966).

Fig. 2. Thirty-year monthly normals of precipitation and temperature near sea level from the station at Glacier Bay (NOAA 2000). Walter-Lieth diagram indicating temperature (°C) on left y-axis and precipitation (mm) on right y-axis (with daily maximum average temperature of the warmest month and daily minimum average temperature of the coldest month in black along left margin), as well as mean annual temperature and precipitation (top right, black).

Glaciation and vegetation history

The history of deglaciation and post-glacial primary succession in Glacier Bay are well documented in a series of detailed studies beginning with the classical work of Cooper (Reference Cooper1923). Though much of the area of Glacier Bay was covered in ice during the Pleistocene, the latest glaciation peaked in the Little Ice Age (c. 1300 to 1870 C.E.) and rapidly receded in the early part of the 19th century. By the late 19th century, ice had retreated to near the mouth of the East Arm and the area now known as Muir Point. Glacial retreat proceeded with greater speed in the West Arm than in the East Arm and many studies on succession, including those on vegetation (e.g. Chapin et al. Reference Chapin, Walker, Fastie and Sharman1994) and stream invertebrate community development (e.g. Milner et al. Reference Milner, Knudsen, Soiseth, Robertson, Schell, Phillips and Magnusson2000), give special attention to the spectacular chronosequence offered in the East Arm. Boggs et al. (Reference Boggs, Klein, Grunblatt, Streveler and Koltun2008, Reference Boggs, Klein, Grunblatt, Boucher, Koltun, Sturdy and Streveler2010) provide fine-scale baseline descriptions of current land cover classes and plant associations for the entire park and preserve complex. Cooper (Reference Cooper1923) mentioned the presence of abundant Stereocaulon alpinum in early successional stages but otherwise lichens have not been treated at the species level in the cited studies.

Stratification of study area into target sampling units

Following a reconnaissance in September 2011, the 2012 sampling season was laid out to obtain reference species lists for six main geographical sectors (Fig. 1) overlaid with specific abiotic criteria. The geographical targets were A) four main areas glaciated in the Little Ice Age: West Arm Glacier Bay (WA), East Arm Glacier Bay to Muir Point (EA), the main part of Glacier Bay including Geikie Inlet (GB), and the glaciated Gustavus area from Bartlett Cove to the base of Excursion Ridge (GUS); B) two areas not glaciated since the end of the Pleistocene: Excursion Ridge and unglaciated Falls Creek down to the Bear Track Inn (EX) and the Dundas to Taylor Bay area parallel to Icy Straits (DUN). Further potential sampling sectors, such as the outer coast, Deception Hills and the Alsek River outwash plain, were not sampled due to logistical constraints.

The study area harbours large habitat diversity (examples in Fig. 3). For the purposes of lichen sampling, this habitat diversity could be classified in terms of vertical zones (near sea level, mountain slopes to 600 m, subalpine/alpine) and geological parent material (acidic rocks including granite, intermediate pH rocks including argillites, high pH rocks including limestones, and ultramafic rocks including gabbro). If only these seven coarse categories were applied, without reference to topographic aspect and plant community succession, we would have 42 geographical sector/habitat envelopes to survey. Because surveying with this level of stratification was logistically prohibitive, we opted to focus on as many different habitats in as many sectors as was feasible within the allocated sampling period, and given boat time, safety and access constraints. The resulting sampling was biased towards low elevations for all sectors, except EX and DUN, and gave mixed results for major bedrock types. We did not explicitly sample each sector based on surface age since deglaciation, though this is also critical to species composition and was used locally as a sampling criterion in sectors WA and EA. Other factors were considered on a site-by-site basis, such as making an inventory of possible phorophyte substrata (bark of available tree and shrub species). Historical specimens from Glacier Bay in herbaria were not systematically surveyed as the majority of these were of common species and had imprecise locality information; only noteworthy records were checked.

Fig. 3. GLBA landscapes. A, terminus of Riggs Glacier (East Arm) in 2014; B, recently deglaciated Dryas mats with numerous Stereocaulon species just east of the terminus of Muir Glacier (East Arm) in 2014; C, alder thicket along a jeep trail at Tower Road near the park entrance (Gustavus sector; M. Svensson); D, Pinus contorta muskeg in the Falls Creek area, not glaciated during the Little Ice Age (included in the Excursion Ridge sector); E, Picea sitchensis rainforest near Bartlett Cove (Gustavus sector); F, alpine meadows and heaths on Excursion Ridge, the richest locality studied for lichens and associated fungi.

Sampling followed an ‘observational feedback’ approach (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) and was delimited by neither fixed sampling times nor plots; maximization of species capture within the time we could spend at a site was the sole field objective. GPS waypoint data (Supplementary Material Table S2, available online) were gathered using WGS84 Datum in digital degrees. A total of 349 waypoints were recorded on multiple GPS devices carried by individual researchers. Following deduplication and imposing a 200 × 200 m grid, this translates to 103 unique sites surveyed.

Specimen analysis

Specimens were examined in the laboratory under a dissecting microscope and pre-sorted for light microscopy or chemical analysis. Specimens were examined with dissecting and compound microscopes with a polarizing light filter and Nomarksi differential interference contrast. The presence or absence of birefringent crystals is noted as POL+/POL−, respectively. Thallus and ascomatal sections were prepared in water and treated with 10% potassium hydroxide (KOH), household bleach (NaOCl, shortened to C according to lichenological convention), para-phenylenediamine (C₆H₄(NH₂)₂, abbreviated to PD), nitric acid (HNO3; 1% unless otherwise indicated), 1% hydrochloric acid (HCl), Lugol's solution (reported by its full name when referring to the solution, or abbreviated to I when reported as a spot test) or lactophenol cotton blue (LCB; Merck). Pigments are described according to Meyer & Printzen (Reference Meyer and Printzen2000). Images of specimens analyzed by TS and AMF were captured with an Olympus XC50 camera mounted on an Olympus SZX16 dissecting microscope; microphotograph images were captured on a Zeiss Axioskop light microscope. In several cases, images were stacked using CombineZM freeware ( Specimens were mounted in water for photographing unless otherwise specified. Scanning electron microscopy was carried out using an FEI XL-30 scanning electron microscope on gold sputtercoated, dry thalli affixed to aluminium stubs. Ascospore measurements are provided for new taxa as (smallest absolute measurement–) smallest mean – largest mean (–largest absolute measurement) or minimum value – arithmetic mean value ± standard deviation – maximum value; s in this case denotes sample standard deviation, n denotes sample size; in Hydropunctaria alaskana the measurements are (minimum–) [median − 1 s] – [median + 1 s] (–maximum). Figures in the main species catalogue reflect informal measurements of several ascospores.

Secondary metabolite analysis was carried out using thin-layer chromatography (TLC) techniques for lichens described by Culberson (Reference Culberson1972), Culberson et al. (Reference Culberson, Culberson and Johnson1981) and Culberson & Johnson (Reference Culberson and Johnson1982). All analyses employed glass plates (Macherey-Nagel 821 030) to visualize fatty acids. Fatty acids were identified by vertically dipping the fully developed and dried plates into a tank of tap water (in Bergen after application with a fine H2O mister) and noting hydrophobic spots in the first 5–10 s while dripping off. Common substances are reported in the text by their acid names and several are abbreviated as follows: atranorin (atr), fumarprotocetraric acid (fpc), protocetraric acid (pc). The presence of satellite substances is denoted with the abbreviation ‘sats’.

Unless otherwise stated, voucher specimens collected for this project are deposited in the herbarium of Michigan State University (MSC). Due to the changing application of National Park Service rules on the deposition of specimens, vouchers that were previously cited as being deposited in other herbaria, especially GZU, by Spribille et al. (Reference Spribille, Tønsberg, Stabentheiner and Muggia2014a, Reference Spribille, Resl, Ahti, Pérez-Ortega, Mayrhofer and Lumbschb) and Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015, cited in their Supplementary Materials) have been transferred to MSC, except for vouchers that were collected outside the formal park boundaries.

Molecular data

Molecular (DNA) analysis was carried out on selected specimens using a standardized laboratory pipeline. Ascomata or thallus fragments were pulverized in 1.5 ml Eppendorf tubes using a Retsch cell grinder with a single 3 mm steel bead after freezing at −80 °C. We extracted genomic DNA using the Qiagen DNeasy Plant Mini Kit following the manufacturer's instructions. In the case of sparse material, we used the QIAmp DNA Investigator Kit. We eluted raw nucleic acids in 50–75 μl of elution buffer without RNAse and used the samples undiluted for subsequent PCR reactions. For most samples, we sequenced the internal transcribed spacer (ITS rDNA; internal transcribed spacer regions 1 and 2 as well as the embedded 5.8S region of the ribosomal rDNA) as it is the single most sequenced locus in fungi and widely used as a barcode (Schoch et al. Reference Schoch, Seifert, Huhndorf, Robert, Spouge, Levesque, Chen and Fungal2012). Primers and annealing temperatures follow those outlined in Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015). PCR was performed using PuReTaq Ready-To-Go PCR beads (GE Healthcare, Chicago) or the KAPA 3G Plant PCR Kit (KAPA Biosystems). PCR products were sequenced by Microsynth (Switzerland). Newly acquired sequences are listed in Table 1 and for all DNA isolates from which no new sequences are published, in Supplementary Material Table S3 (available online).

Table 1. Voucher information and NCBI GenBank Accession numbers for all specimens from which DNA sequences are newly generated for this study. Voucher information and sequence accession numbers for specimens from which no newly generated data are provided here can be found in Supplementary Material Table S3 (available online). A dash (–) indicates no data, an asterisk (*) indicates that the voucher does not appear in any tree in the present paper. GenBank Accessions beginning with letters other than ‘MN’ or ‘MT’ represent sequences generated in other studies.

Phylogenetic trees

Phylogenetic analyses were used strictly to place newly described or remarkable species in larger groups, not to test species delimitations. We amplified DNA sequences from a total of 136 specimens for this study, including 83 collected in GLBA and adjacent areas (Table 1). We also used gene data from over 440 voucher specimens extracted for previous studies, as well as published genome projects available on the Joint Genome Institute MycoCosm website ( Depending on the species, we included up to eight fungal loci, including ribosomal loci of the nucleus (ITS, 18S, 28S) and mitochondrion (12S) and nuclear protein-coding loci (Mcm7, RPB1, RPB2, EF1a). For newly generated sequences, primers, PCR conditions and locus abbreviations follow Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015) and Schneider et al. (Reference Schneider, Resl, Westberg and Spribille2015). The decision on how many loci to sequence was informed by the available ‘background’ data in the NCBI nt database (‘GenBank’) for the larger taxonomic group in question. We assembled a private database of DNA sequences from GenBank and added an identifier code to each sequence to indicate the voucher it was derived from (typically a letter followed by three or four numbers, such as X123). Sequences from multiple loci, but one voucher, can thus be tied together and automatically called up for use in a tree. We combined this with MAFFT v7 (Katoh & Standley Reference Katoh and Standley2013) alignment and automated concatenation in the python-based phyloscripts pipeline (Resl Reference Resl2015). Concatenation of DNA specimen data from different specimen vouchers was thereby eliminated. Automated concatenation based on an identifier code enabled quick testing of taxon samples for phylogenetic analysis. We included multiple samples of a taxon or group of closely related taxa if they had a ‘bridging’ locus in common, as this increased the number of loci represented for the resulting clade.

We further screened sequences with BLAST searches against the NCBI nt database to identify potential sequences from non-target fungi, even from already published sequence data. Based on this, we removed seven sequences from our data set: Lecania atrynoides 28S (AY756352) is identical to Bryobilimbia hypnorum; Candelariella terrigena mitochondrial 12S (DQ986884) appears to derive from a member of Gyalectales close to Porina; and Micarea (Leimonis) erratica 18S (KJ766742), 28S (KJ766591) and mitochondrial 12S (KJ766425) belong to an unknown member of Lecideales, not M. erratica (which is represented by other sequences in NCBI nt). Lecanora achroa 28S sequence JN939502 (Zhao et al. Reference Zhao, Leavitt, Zhao, Zhang, Arup, Grube, Pérez-Ortega, Printzen, Śliwa and Kraichak2015) is a chimeric duplicate sequence of itself following ~position 651; because of uncertainty regarding the sequence identity, the entire sequence from this locus was deleted. Similarly, sequence HM576929 deposited by Zhao et al. (Reference Zhao, Leavitt, Zhao, Zhang, Arup, Grube, Pérez-Ortega, Printzen, Śliwa and Kraichak2015) as Rhizoplaca shushanii Mcm7 protein in fact derives from the β-tubulin locus and was therefore not used. Major data sources and their underlying voucher specimens are listed in Table 1 and Supplementary Table S3 (available online).

Upon data set selection, we visually examined each alignment. For three sequences (P172, P173, T764) we removed several hundred base pairs from the 3′ end of the 28S sequence that was unalignable due to long introns and c. 150 bp of Ramalina dilacerata KP794953 due to poor quality. For the Lecanorales alignment, MAFFT failed to align a major 28S intron starting at position 932 of Ramboldia arandensis DQ431919; 24 of the 116 taxa in the 28S Lecanorales alignment possessed this homologous intron, the only section of any alignment that could not be handled by MAFFT and required manual adjustment. We then trimmed all sites from the alignment present in 10% or fewer sequences and subjected the trimmed alignment to a partition search using PartitionFinder v1.1.1 (Lanfear et al. Reference Lanfear, Calcott, Ho and Guindon2012, Reference Lanfear, Frandsen, Wright, Senfeld and Calcott2016; v2.1.1 for the Ostropales/Gyalectales and Sticta data sets), using linked branch lengths, all available models, a ‘greedy’ search scheme, and the Bayesian Information Criterion for evaluating best model fit. The alignments were then used for maximum likelihood analyses using RAxML-HPC v8.0.0 (v.7.2.8 for Pertusariales) with 1000 bootstrap replicates and the GTRGAMMA model of nucleotide substitution for each partition (Stamatakis Reference Stamatakis2014).

Species delimitation and nomenclature

As in the KLGO study, we based species identification more on systematic observation than on the a priori use of keys, that is, we sorted specimens into ‘morphospecies’ based on chemical and morphological characters in statu symbiotico and only then looked for applicable names in a global literature set. We continue to track ‘phantom phenotypes’ (Spribille Reference Spribille2018), distinct lichen symbiotic outcomes that may not be supported at the present time by DNA data from a small number of fungal gene loci. The reasons for this can be exemplified by the members of the Bryoria implexa group. Based on five gene loci and 18 microsatellite markers, Boluda et al. (Reference Boluda, Rico, Divakar, Nadyeina, Myllys, McMullin, Zamora, Scheidegger and Hawksworth2018) concluded that historically recognized members of this group are formed by one fungal species and thus, according to the International Code of Nomenclature for Algae, Fungi and Plants (Turland et al. Reference Turland, Wiersema, Barrie, Greuter, Hawksworth, Herendeen, Knapp, Kusber, Li and Marhold2018), the oldest valid name of this fungus should be used for all these lichens. We consider such a move premature, and the null hypothesis of genetic distinctness of these putative species impossible to reject at the current time, for the following three reasons. First, the existence of distinct multistate phenotypes, especially those that have been tracked with little controversy for over a century, is in itself evidence for genetically encoded biological phenomena; second, the biological basis for the formation of the phenotypes has neither been explained nor, to our knowledge, studied; third, the absence of evidence must not be confused with evidence of absence, in this case of phylogenetic signal in the ascomycete genome. Five loci represent less than 0.05% of the 10 000+ protein-coding genes that can be expected on a lecanoromycete genome (compare Armaleo et al. Reference Armaleo, Müller, Lutzoni, Andrésson, Blanc, Bode, Collart, Dal Grande, Dietrich and Grigoriev2019).

Nomenclature of lichens and lichen-associated fungi largely follows Esslinger (Reference Esslinger2019) and Diederich et al. (Reference Diederich, Lawrey and Ertz2018), though two special cases merit comment: 1) we accept the need for segregate genera of Caloplaca and Xanthoria in Teloschistaceae, as outlined by Arup et al. (Reference Arup, Søchting and Frödén2013), but retain Caloplaca here in the broad sense with segregate names in parentheses since a) the combinations have not been made for approximately half of the taxa found in GLBA, and b) the names are not familiar to many users and we wish to avoid the confusion caused by moving closely related taxa to different parts of the main list; 2) we agree with Esslinger (Reference Esslinger2019) and do not follow the circumscription of cetrarioid genera derived from ‘temporal banding’ (Kraichak et al. Reference Kraichak, Crespo, Divakar, Leavitt and Lumbsch2017), for two reasons. First, temporal banding assumes that rates of phenotype evolution are linearly linked to rates of molecular evolution, but this is obviously not true across the tree of life or we would see as much phenotypic diversity in protists as we do in mammals (though extant members of both are at an equal distance to the most recent common ancestor in evolution). Second, unlike species, which are biological entities, genera are groupings of species that are alike from the human point of view, in recent years informed by what we have learned about common descent (monophyly). No imperative exists for these groupings to be equally old, nor does there exist a consensus on whether such an imperative would be desirable. Numerous other arguments against the adoption of temporal banding have been advanced by Lücking (Reference Lücking2019). Our approach may be conservative, but it does not preclude rigorous hypothesis testing and the exploration of alternative nomenclatural solutions in the future.

Nomenclature of vascular plants follows Flora of North America (online treatments: with the exception of Cupressus nootkatensis (D. Don) Spach, which follows Gadek et al. (Reference Gadek, Alpers, Heslewood and Quinn2000).

Presentation of species data

Not all collections could be confidently assigned to a known species. The reasons for this are often complex and the story behind each ‘problem species’ reveals the challenges of working in poorly studied regions, as well as the interconnectedness of local taxonomic issues to broader global-level systematics. Replicating our approach in KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010), we present species in a hierarchical fashion here to allow the reader to navigate the results from the standpoint of their relative novelty and certainty. The results are presented in three groups: 1) taxa for which we have invested considerable effort to resolve their underlying systematic relationships, including species new to science; 2) ‘known unknowns’, putative species which we can characterize but for which we can neither find unambiguously applicable names nor assert with confidence that they are new species, or for which material is insufficient for a formal description; 3) lichen-forming and lichenicolous fungi for which we are more or less certain we can apply existing names (but see below). Unlike ‘known unknowns’, these latter species can be connected to a species name, even if this is done with caveats. Communicating to land managers, funders and other scientists the distinction between these types of taxonomic problems and the work they require is essential to building an appreciation of the role of systematics in the lichen inventory of poorly studied regions. We also consider it essential to report species of uncertain status, so the biodiversity of an area can be properly recorded, and other lichenologists can be alerted to their existence. We also hope this flags specimens from our study area to be included in other research, either current or in the future.

The list of taxa with names also includes some species for which the application of a name is uncertain. These are denoted with ‘cf.’ (for confer, the Latin imperative to compare) in cases where further studies, especially comparison with type material, would be advantageous; or ‘aff.’ (Latin: ex affinitatis) in cases where we or consulted experts have performed such studies and conclude that the species in question is in close affinity with, but not identical to, the type material. Of fungi, we exclude only yeast-forming microfungi associated with the lichen cortex, several of which have been detected in macrolichen samples from GLBA (Spribille et al. Reference Spribille, Tuovinen, Resl, Vanderpool, Wolinski, Aime, Schneider, Stabentheiner, Toome-Heller and Thor2016), because surveying for these species requires special techniques and is beyond the scope of the present study.

After the species name, a brief summary of its observed ecological and elevational range in GLBA is provided, followed by an abbreviated list of specimens seen. Sector abbreviations are as noted above and waypoints are listed in Supplementary Material Table S2 (available online). Collection numbers reflect individual collectors based on initials: F = A. Fryday, M = M. Svensson, P = S. Pérez-Ortega, S = T. Spribille and T = T. Tønsberg. Records presented in the main and known unknown lists in square brackets (e.g. […]), denote localities outside the formal GLBA boundaries (most are within a few hundred metres of the formal park boundary). New species for Alaska are denoted with an asterisk (*) and for North America by a double asterisk (**); a hash symbol (#) denotes putatively lichenicolous fungi and a plus sign (+) putative saprobic fungi (we refer to these as ‘putative’ because our knowledge of their nutritional mode is derived from observations of fertile structures, not the whole mycelium or yeast stages).

Comparison between sectors and national parks

To compare lichen composition of different areas, we constructed Venn diagrams using the R packages venn ( and VennDiagram (Chen & Boutros Reference Chen and Boutros2011). We used species lists from McCune et al. (Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018) for Katmai and Lake Clark National Parks and Preserves, and Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) for Klondike Gold Rush National Historical Park. Species lists were synonymized based on comparison of the application of names in the four studies and final reported numbers differ slightly from those in the original publications owing to deduplication of names in McCune et al. (Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018) and follow-up studies since Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010). The underlying matrix is presented in Supplementary Material Table S4 (available online). Maps to show park locations were generated using QGIS 3.10 (, based on shapefiles downloaded from and

Results and Discussion

We found a total of 947 species from the 4741 specimens collected. Ninety-eight could not be assigned to any named species. Of these 98, we have enough data to describe 27 as new to science. The remaining 71 species are reported as ‘known unknowns’. Of the 947 species reported, 831 are lichens, 96 are assumed non-mutualistic lichen-associated (lichenicolous) fungi and 20 are assumed non-mutualistic saprotrophic fungi. Thirty-eight previously described taxa are reported here for North America for the first time, and an additional 93 taxa are new reports for Alaska. The addition of 158 named taxa (27 + 38 + 93) to the known lichens and lichen-associated fungi of Alaska represents approximately a 9% increase in the collective Alaskan lichen-associated biota, which until now was estimated to contain c. 1750 taxa (unpublished data). All but 11 species (indicated in the main list in brackets) were found within the official GLBA boundaries, the others occurring on lands near the town of Gustavus. The survey accomplishes our twin goals of establishing a baseline inventory for GLBA and providing a georeferenced occurrence database for every species, which we analyze below at the level of park sectors. The number of lichen and associated fungal taxa we recorded in GLBA exceeds that of any US national park in the review of Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) or published since, and for the total number of taxa in study areas under 10 000 km2 worldwide, it is second only to the 1061 taxa found in Parc national des Cévennes, France (Roux et al. Reference Roux, Coste, Bricaud, Bauvet and Masson2008), an area with decades of study investment.

Comparison of sectors within GLBA

Individual sectors of GLBA differ greatly in their species composition (Fig. 4A; Supplementary material Table S4A, available online). The richest sector is Excursion Ridge with 438 taxa, followed by Gustavus and Dundas (both with 326), West Arm (248), Glacier Bay (232) and East Arm (189). Only 14 taxa were found in all sectors. The Excursion Ridge and Dundas sectors, which escaped glaciation in the Little Ice Age, together harbour 615 species, while all four glaciated sectors together harbour 607. If the Gustavus sector is instead lumped in with the unglaciated sectors, the first number climbs to 750 and the remaining unglaciated sectors drop to 452. This explains why parts of the Venn diagram (Fig. 4A) that exclude these three sectors, and display species found only in one or more of the remaining sectors, contain so few species. Excursion Ridge harbours the greatest number of unique species (i.e. species found only in one sector) with 198, while Glacier Bay (43) and East Arm (40) harbour the fewest. Collectively, the two unglaciated sectors hold 339 species not found in any glaciated sector, whilst glaciated sectors harbour 331 species not found in any unglaciated sector; again, the first number rises to 494 species if the Gustavus sector is instead lumped in with the unglaciated sectors, whilst the remaining glaciated sectors minus Gustavus have only 196 species. Why the Glacier Bay, West Arm and East Arm sectors harbour so few unique species, individually and collectively, cannot be directly determined from our data. These sectors account for the most recently deglaciated surfaces in GLBA but at the same time they were also the most remote and difficult to access during this survey. In contrast to the other three glaciated sectors, the Gustavas sector shares a long boundary with the unglaciated Excursion Ridge sector. Such proximity, providing easier opportunities for recolonization, could help explain the much higher species richness of the Gustavus sector compared to other glaciated sectors. That being said, the Gustavus sector was also easier to access.

Fig. 4. A, Venn diagram of species occurrence within the six sectors of GLBA. Numbers do not add up to 947 because one species (Melanohalea olivacea) could not be assigned to any one sector due to a lack of site data. All species of lichens and lichen-associated fungi, including ‘known unknowns’, are included in this diagram. Where a number is absent from a segment, the value is zero; B, occurrence of named lichen species across four national parks and preserves in the Gulf of Alaska region (lichen-associated fungi and ‘known unknowns’ not included). Data is based on the present paper (Supplementary Material Table S4A & B, available online), Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) and McCune et al. (Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018).

While numbers per sector will increase with further surveys, so too should the number of singleton species (those represented by only one specimen); we suspect the dissimilarity recorded between the sectors is real. However, results are skewed based on the kinds of sites that were accessible. The argillite outcrops of Excursion Ridge contained by far the richest sites found anywhere in GLBA. The sampling of such a site elsewhere in GLBA, if accessible, could lead to a significant rearrangement in the Venn diagram. We hypothesize that many factors (glacial history, vegetation succession and associated substratum availability and geological bedrock) drive richness patterns but inclusion of diverse sites within a sector would certainly affect the perceived richness distribution. Though our study was not designed to detect the impacts of air quality, we do not suspect a role for cruise ship emissions in the observed richness patterns. Cruise ship exhaust, to the extent it was observed, appears to linger in narrow passages of the West Arm in elevational belts well above sea level, sites inaccessible during the present survey.

Lichen diversity in the national parks of the greater Gulf of Alaska region

Three other national parks in the greater Gulf of Alaska region (Fig. 1A) have been intensively surveyed for lichens in recent years: Klondike Gold Rush National Historical Park (KLGO: Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) and Katmai and Lake Clark National Parks and Preserves (McCune et al. Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018). Our collated lists of lichens and associated fungi from those parks, including revisions undertaken since (for KLGO), give total numbers of 757 (KLGO), 589 (Katmai) and 722 species (Lake Clark; lists in Supplementary Material Table S4B, available online). A four-way comparison of these national parks (Fig. 4B) provides an overview of the known collective lichen species pool and the species turnover along a 1000 km segment of the mountain chain that borders the Gulf of Alaska from Cook Inlet to the Icy Straits. A cumulative 1341 named lichen taxa occur in the four parks (GLBA 773, KLGO 604, Katmai 568 and Lake Clark 691; Fig. 4B). Comparisons for lichenicolous fungi and saprobic fungi and ‘known unknown’ lichens are not included above or in Fig. 4B because the first two groups were not specifically targeted in surveys of Katmai or Lake Clark (lichenicolous fungi: Katmai 9, Lake Clark 6; saprobic fungi: Katmai 2, Lake Clark 7) and the latter group is comparable only between GLBA and KLGO (though 10 ‘known unknown’ lichen species were reported from Katmai and 18 from Lake Clark). The cumulative number of lichenicolous fungal species in GLBA and KLGO is 147, and for ‘known unknown’ lichens 111 (all summary data in Supplementary Material Table S4B, available online).

Many taxa (617/46% of the 1341 named taxa) are found in only one park. GLBA has by far the highest number (248 taxa) followed by Lake Clark (160 taxa). This might reflect the relatively southern position of GLBA at the edge of the large temperate rainforest formation of south-east Alaska, and the position of Lake Clark on the opposite end of the northwest-southeast gradient. By contrast, only 192 (14%) of named taxa are found in all four parks (Fig. 4B). The large percentage of singletons—taxa found in only one park—underlines the importance of these protected areas in providing non-redundant habitat for lichen species. It also raises the question of how many species occur in natural landscapes of the Gulf of Alaska region that are not under any current form of protection.

Phylogenetic trees

We obtained 280 new DNA sequences from the ascomycete fungal symbiont for specimens used in this study, most of them from specimens collected in GLBA (Table 1). A total of 223 were used in calculating phylogenetic trees together with previously published data. We calculated seven phylogenetic trees to provide context for placement of new species and ‘known unknowns’ when DNA data could be acquired. The taxon sample of each tree was designed to allow the exploration of placement of a sequence set across a broad cross-section of fungal evolution. In some cases, these are the first phylogenetic analyses to incorporate previously published, disparate data sets, and as a result, some new patterns emerge. Relationships specific to newly described species or ‘known unknowns’ are discussed under the treatments of those species but we highlight some of the broad patterns here, except for the Hydropunctaria tree which is discussed under the description of Hydropunctaria alaskana.

The broadest evolutionary taxon sample includes representatives of the entire class Lecanoromycetes with Eurotiomycetes as an outgroup (Fig. 5) based on eight loci. This provides context for five of the remaining phylogenetic trees (Figs 6–10) as well as several clades not treated in those analyses. The overall topology largely recapitulates known relationships but provides for the placement of two species placed here in the hitherto monotypic genus Toensbergia (Sporastatiaceae), a relationship that had not been suspected based on morphological data.

Fig. 5. Majority-rule consensus tree of the class Lecanoromycetes, showing the placement of two new species (in bold) using selected voucher specimens and eight loci. Dots and dashes to the right of tip names indicate presence and absence of loci, respectively, in the following order: ITS, 18S, 28S, mtSSU, Mcm7, RPB1, RPB2, EF1a. Values indicate percent bootstrap support. Alphanumeric codes in brackets are identifiers unique to this study. Voucher information and GenBank Accession numbers are outlined in Table 1 and Supplementary Material Table S3 (available online).

Fig. 6. Majority-rule consensus tree of the order Pertusariales (subclass Ostropomycetidae) based on eight loci. Dots and dashes to the right of tip names indicate presence and absence of loci, respectively, in the following order: ITS, 18S, 28S, mtSSU, Mcm7, RPB1, RPB2, EF1a. Values indicate percent bootstrap support. Novel taxa are in bold. Alphanumeric codes in brackets are identifiers unique to this study. Voucher information and GenBank Accession numbers are outlined in Table 1 and Supplementary Material Table S3 (available online).

Fig. 7. Majority-rule consensus tree of the orders Ostropales and Gyalectales (subclass Ostropomycetidae) showing placement of two new species (in bold) based on eight loci. Dots and dashes to the right of tip names indicate presence and absence of loci, respectively, in the following order: ITS, 18S, 28S, mtSSU, Mcm7, RPB1, RPB2, EF1a. Values indicate percent bootstrap support. Alphanumeric codes in brackets are identifiers unique to this study. Voucher information and GenBank Accession numbers are outlined in Table 1 and Supplementary Material Table S3 (available online).

Fig. 8. Majority-rule consensus tree of the order Baeomycetales (subclass Ostropomycetidae) based on eight loci. Dots and dashes to the right of tip names indicate presence and absence of loci, respectively, in the following order: ITS, 18S, 28S, mtSSU, Mcm7, RPB1, RPB2, EF1a. Values indicate percent bootstrap support. Novel taxa are in bold. Alphanumeric codes in brackets are identifiers unique to this study. Voucher information and GenBank Accession numbers are outlined in Table 1 and Supplementary Material Table S3 (available online).

Fig. 9. Majority-rule consensus tree of the suborder Collematineae (order Peltigerales) showing placement (in bold) of four new species and a ‘known unknown’ based on four loci. Dots and dashes to the right of tip names indicate presence and absence of loci, respectively, in the following order: ITS, 28S, mtSSU, Mcm7. Values indicate percent bootstrap support. Alphanumeric codes in brackets are identifiers unique to this study. Voucher information and GenBank Accession numbers are outlined in Table 1 and Supplementary Material Table S3 (available online).

Fig. 10. Majority-rule consensus tree of the order Lecanorales (subclass Lecanoromycetidae) showing placement (in bold) of three new species and several ‘known unknowns’ or previously poorly understood taxa, based on five loci. Dots and dashes to the right of tip names indicate presence and absence of loci, respectively, in the following order: ITS, 18S, 28S, mtSSU, Mcm7. Values indicate percent bootstrap support. Alphanumeric codes in brackets are identifiers unique to this study. Voucher information and GenBank Accession numbers are outlined in Table 1 and Supplementary Material Table S3 (available online).

An eight-locus phylogenetic tree of Pertusariales (Fig. 6) includes representatives of major genera that have been previously sampled, as well as representatives of the main groups within the genus Ochrolechia. This analysis places a sterile ‘known unknown’ in the Lepra-Varicellaria clade (Varicellaria sp. S38337) and another sterile sample in Ochrolechia (Ochrolechia sp. S38864). It places the newly described Ochrolechia cooperi relative to other species in that genus, provides evidence for the close relationship of the putatively undescribed Ochrolechia sp. S38011 to the alectoronic acid-containing species of Ochrolechia with closed ascomata (O. subplicans, O. xanthostoma), and finally provides evidence for the monophyly of that species group and its position within, not outside of, Ochrolechia as currently circumscribed.

An eight-locus phylogenetic tree (Fig. 7) of the clade of Ostropomycetidae circumscribed as the order Ostropales s. lat. includes many of the species sampled by Baloch et al. (Reference Baloch, Lücking, Lumbsch and Wedin2010), augmented with data from Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015), Schneider et al. (Reference Schneider, Resl and Spribille2016) and new data. It places Absconditella rosea in the Absconditella clade (as opposed to Cryptodiscus) and the new species Sagiolechia phaeospora in a clade with S. protuberans and S. rhexoblephara. The expanded locus and taxon sampling recovers reciprocal monophyly of a clade of predominantly saprotrophic genera that include Ostropa barbara on the one hand, and a clade of mainly lichen-forming groups including the well-studied families Graphidaceae, Gyalectaceae and Porinaceae on the other. The second clade encompasses many of the same genera placed in Gyalectaceae and the order Gyalectales (Hawksworth & Eriksson Reference Hawksworth and Eriksson1986; see also the overview by Gagarina Reference Gagarina2015) as well as the Graphidales. The split we found is better resolved than in previous studies (Kauff & Lutzoni Reference Kauff and Lutzoni2002; Baloch et al. Reference Baloch, Lücking, Lumbsch and Wedin2010) and could be taken as support for the recognition of a single order including the families Coenogoniaceae, Graphidaceae, Gyalectaceae, Porinaceae and Phlyctidaceae, and the Odontotrema clade of Ostropaceae. Our analysis provides a larger sample of Ostropales and Gyalectales than the recently published five-locus data set of Kraichak et al. (Reference Kraichak, Huang, Nelsen, Leavitt and Lumbsch2018), but we recover a broadly similar topology. Kraichak et al. (Reference Kraichak, Huang, Nelsen, Leavitt and Lumbsch2018) included a considerably larger taxon sample of Diploschistaceae, Fissurinaceae, Graphidaceae and Thelotremataceae, which they recognize as constituting an order of their own (Graphidales).

An eight-locus phylogenetic tree of Baeomycetales (Fig. 8) relies heavily on data generated by Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015, Reference Resl, Fernández-Mendoza, Mayrhofer and Spribille2018) and Schneider et al. (Reference Schneider, Resl and Spribille2016) and recovers almost the same topology as the first study. It places the newly described Lambiella aliphatica as well as a previously unpublished sequence from a Chilean specimen of the otherwise Australasian Lambiella hepaticola and ‘known unknowns’ from genera Placopsis and Trapeliopsis.

A five-locus phylogenetic tree of the Peltigerales suborder Collematineae (Fig. 9) relies heavily on data from Ekman et al. (Reference Ekman, Wedin, Lindblom and Jørgensen2014) but is expanded to include newly generated, as well as published, sequences from Coccocarpiaceae and Placynthiaceae (Spribille & Muggia Reference Spribille and Muggia2013; Spribille et al. Reference Spribille, Tønsberg, Stabentheiner and Muggia2014a). The tree places the newly described Spilonema maritimum in a monophyletic clade with Coccocarpia and Spilonema, suggesting that more work is needed on the relationships between the lecanoromycete mycobionts in those lichens. The newly described Placynthium glaciale is recovered within a strongly supported Placynthium clade despite its muriform ascospores, a first for that genus. The sampling also enables us to place the new genus Atrophysma as a distinct clade among previously sampled members of Pannariaceae and the newly described Fuscopannaria dillmaniae in the genus Fuscopannaria.

The final lecanoromycete tree is of the order Lecanorales and is based on five loci (Fig. 10). To construct this tree, we screened GenBank for sequences from Lecanoraceae, Malmideaceae, Pilocarpaceae and Ramalinaceae and chose taxa that, either alone or in combination with multiple replicates of the same or closely related taxa, covered as many of the five loci as possible. The objective was to build a topology that covered phylogenetic structure in all the main groups of Lecanorales and explored the relationships of several sequence sets we recovered from GLBA. The taxon sample, especially for Lecanoraceae, relied heavily on published sequences from Zhao et al. (Reference Zhao, Leavitt, Zhao, Zhang, Arup, Grube, Pérez-Ortega, Printzen, Śliwa and Kraichak2015). Because of our interest in the placement of the Lecidea albofuscescens group and a suspected relationship with Malmideaceae, we included as much multilocus data from that family as was available. Despite the lacunose sequence coverage, we recovered the Malmideaceae as a well-supported, monophyletic clade including L. albofuscescens as well as Lecidea malmeana, a polysporous species collected in GLBA. Of species that have been previously reported to belong to Malmideaceae, only Kalbionora (Sodamuk et al. Reference Sodamuk, Boonpragob, Mongkolsuk, Tehler, Leavitt and Lumbsch2017) was not recovered within this clade, instead grouping in an unsupported relationship with the outgroup Rhizocarpon. We refrain from undertaking any nomenclatural changes because of poor internal support within Malmideaceae, and ongoing studies.

Also in Lecanorales, the newly described species Lecania hydrophobica, Biatora marmorea and Miriquidica gyrizans grouped with Lecania baeomma and the genera Biatora and Miriquidica, respectively, as expected based on morphological analyses (Fig. 10). Zhao et al. (Reference Zhao, Leavitt, Zhao, Zhang, Arup, Grube, Pérez-Ortega, Printzen, Śliwa and Kraichak2015) did not include the recently described genus Palicella in their Lecanoraceae analyses, but in our topology, the species referred here are recovered as a strongly supported monophyletic group within a poorly supported Lecanoraceae. Our analysis confirms the recent result of Kondratyuk et al. (Reference Kondratyuk, Lőkös, Jang, Hur and Farkas2019), in that even the narrow Palicella clade encompasses a saxicolous taxon (Palicella anakeestiicola S.Y. Kondr. et al.) and is sister to a clade of saxicolous species with similar chemistry and pigments, until now called the Lecanora formosa group. One of our newly described species, Lecanora viridipruinosa, and one ‘known unknown’ (Lecanora sp. F10122) resolve within this group. We refrain from making any new combinations because we could not find accessions with enough loci to represent the Lecanora varia group, an important group of species with an older genus name (Straminella Choisy), and thus cannot eliminate the possibility that some or more of these species may be assignable there. Another ‘known unknown’, Lecanora sp. S38412, resolves within a supported clade referable to Lecanora s. str., in proximity to Lecanora gangaleoides, as expected by morphochemical analysis. Lecanora leptacina is recovered on its own branch in a clade that includes the Lecanora polytropa group, Myriolecis (now treated in part as Polyozosia; Kondratyuk et al. Reference Kondratyuk, Lőkös, Jang, Hur and Farkas2019), Protoparmeliopsis and Rhizoplaca. Finally, a new sequence set from Myriolecis schofieldii resolves as expected within that clade, as well as a recently published sequence of Lecanora poliophaea (Kistenich et al. Reference Kistenich, Timdal, Bendiksby and Ekman2018).

A further 57 DNA sequences were generated for species not included in any phylogenetic analysis here, in most cases because we were unsuccessful in obtaining multiple loci and no meaningful analysis could be conducted with a single locus in conjunction with published data. We publish the sequences (Table 1) because single locus data published here might match up against future sequences from multilocus and barcoding data sets.

Descriptions of New Genera and Species

Atrophysma T. Sprib. gen. nov.

MycoBank No.: MB 830090

A cyanolichen with minutely coralloid, finger-like lobes over a black hypothallus, similar to Placynthium but ascospores are simple, similar to Leciophysma but with dark blue-black pigments in the apothecium; asci lacking an amyloid apical tube.

Type: Atrophysma cyanomelanos T. Sprib. (below).


The genus name comes from atra (black), a reference to its colour impression in the field, and –physma, thought to derive from the Greek verb physao, to blow up or distend, and the suffix –ma, indicating a completed action (Verdon Reference Verdon1992).

Atrophysma cyanomelanos T. Sprib. sp. nov.

MycoBank No.: MB 830091

A cyanolichen with minutely coralloid, finger-like lobes over a black hypothallus, black apothecia, internally with a black pigment, reversibly HNO3+ mauve, KOH+ remaining blackish but weakly greenish tinged, and simple ascospores, 11.0–16.0 × 7.1–8.1 μm, frequently with a warted gelatinous epispore.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, ridgetop, 58.46503°N, 135.55757°W, 903 m, saxicolous on argillite slabs on alpine ridgetop covered by deep snow much of the year, 1 August 2012, Spribille 39425 (MSC—holotype; NY—isotype).

(Fig. 11)

Fig. 11. Atrophysma cyanomelanos (holotype). A & B, habit; C, habit with SEM; D, broken thallus lobe with SEM; E, broken thallus lobe in brightfield microscopy; F, ascoma section (composite image); G, ascus stained in Lugol's solution. Scales: A = 1 mm; B & C = 0.5 mm; D & F = 50 μm; E & G = 10 μm.

Thallus a sprawling crust up to 7 cm diam., becoming confluent with adjacent thalli, olivaceous brown, consisting of minute coralloid fingers 70–150 μm diam.; hypothallus present as a black base to the coralloid fingers, but not extending beyond the perimeter of the main thallus, coloured with the same pigment as the apothecia (see below); individual lobes consisting of tightly packed Nostoc-like cyanobacterial cells with fungal hyphae sheathed in a gelatinous cortex-like layer, a cellular cortex lacking.

Ascomata apothecia, round, sometimes flexuose, single or grouped, (0.25–)0.5–0.6(–1.3) mm diam., often absent; disc flat to more often convex, jet black, matt, sometimes hollowed out (herbivory?) leaving concave shells; proper margin prominent, receding with age but not disappearing, matt. Excipulum 60–90 μm wide laterally, to 40 μm wide basally, composed of radiating, anastomosing hyphae that widen towards the tips, up to 8–9 μm diam. with lumina to 3–5 μm, streaked with black pigments externally, POL+ crystals not seen. Hymenium (60–)70–90 μm tall, hazy reddish brown, I+ wine red before KOH treatment, uppermost part (‘epihymenium’) lacking crystals, heavily black-pigmented, the pigment reversibly HNO3+ mauve, KOH+ remaining blackish but weakly greenish tinged, similar to the ascomatal pigments in Farnoldia and the hypothallus pigments in Placynthium; paraphyses mostly simple, 2–4 μm wide at midpoint, not widened apically, moniliform. Hypothecium to 200 μm thick, hyaline or light reddish brown, grading in the lowermost 50–150 μm to deep brown, I+ wine red. Asci 8-spored, widely flask-shaped, lightly amyloid externally, I− internally, lacking an amyloid apical tube or tholus; ascospores simple, broadly ellipsoid, (10–)11.0–16.0(–19) × (5.5–)7.1–8.1(–9.5) μm, frequently with a warted gelatinous epispore (n = 60, from six specimens).

Pycnidia not observed.


No secondary substances detected.


From kyanos (blue) and melas (black), referring to the characteristic contrasting colours of the ascomata and thallus upon close examination.


On rock, apparently preferring weakly calcareous rock (in GLBA, argillite) in subalpine and alpine habitats.


We first encountered this species working in KLGO and tentatively assigned it, as a ‘known unknown’, to the genus Santessoniella Henssen (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010, as Santessoniella sp. 24535). The GLBA material is much richer and gave us a broader basis for morphological as well as DNA analysis but placing the new species into an existing genus proved impossible. Ekman et al. (Reference Ekman, Wedin, Lindblom and Jørgensen2014) showed that Santessoniella as circumscribed by Henssen (Reference Henssen1997) is polyphyletic and its characteristic thallus morphology evolved independently. In addition, the type of the genus, S. polychidioides (Zahlbr.) Henssen, has been recovered within Psoroma Ach. ex Michx. with moderate support, suggesting that the former genus will be lost to synonymy. We also suspected a relationship to Leciophysma Th. Fr., but species of that genus have a distinct I+ apical tube in the ascus (such as in L. saximontana (T. Sprib. et al.) P. M. Jørg. et al., a species initially described in Santessoniella but later placed in Leciophysma; Spribille et al. Reference Spribille, Jørgensen, Schultz and Houde2007; Ekman et al. Reference Ekman, Wedin, Lindblom and Jørgensen2014). We also know of no species of Pannariaceae with the black pigments of this species, which recall those in Placynthiaceae. We considered a possible placement in the latter family but no Placynthiaceae are known to have simple ascospores. Multilocus DNA sampling from the apothecia of the new species placed it in the Pannariaceae (Fig. 9). A continued discussion of species formerly placed in Santessoniella can be found under the treatment of Fuscopannaria dillmaniae later in this paper.

We observed a wide variation in ascospore sizes within the limited material available to us, so much so that we initially suspected we might have two species. To at least cursorily test this, we sequenced ITS rDNA from both a specimen with large ascospores and one with small (the type) and found no difference between the two.

Atrophysma cyanomelanos is currently known only from Alaska. We have also seen a specimen from the Brooks Range in northern Alaska (below).

Additional specimens examined

USA: Alaska: Klondike Gold Rush National Historical Park, 2007, Spribille 24535 (KLGO); west side of White Pass, 2008, Spribille 26967 (KLGO, L853), 26968 (KLGO, voucher L947); Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, 58.46274°N, 135.55288°W, 919 m, saxicolous on soft argillite, 2012, Spribille 38414 (MSC); ibid., 58.46222°N, 135.55954°W, 883 m, small rock in tundra, 2012, Spribille 38770 (MSC); ibid., 58°27.810′N, 135°33.485′W, 2012, Svensson 2660 (MSC); ibid., 58.46503°N, 135.55757°W, 2012, Spribille 39435 (MSC); ibid., 58.46469°N, 135.55736°W, 918 m, saxicolous, 2012, Fryday 10338 (MSC, topotype); ibid., Spribille 39384 (MSC), 39388 (MSC), 39402 (NY; DNA voucher 1346); Gates of the Arctic National Park, northern Brooks Range, Summit Lake, 68.0495226°N, 150.5257256°W, 1140 m, saxicolous on sandstone/quartzite cobbles, 2012, T. Wheeler 4271 (hb. Wheeler).

Bacidina circumpulla S. Ekman sp. nov.

MycoBank No.: MB 830092

Thallus of ± placodioid, pale greyish, yellowish or brownish squamules that never form goniocysts or soralia. Apothecia biatorine, mostly flat, with a pinkish, beige, ±brown, greyish to almost black and often piebald disc and a ± greyish black and slightly shiny margin. Proper exciple thin, paraplectenchymatous, diffusely reddish brown and/or dirty green in at least the uppermost part. Hymenium colourless in lower part, diffusely and unevenly reddish brown and dirty green in upper part and in scattered vertical streaks. Hypothecium colourless to pale yellowish. Ascospores straight, curved to shallowly helical, acicular, mostly with 3–5 thin septa.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Queen Inlet, shoreline, 58.88500°N, 136.50838°W, 0–5 m, on rotting driftwood log, 19 July 2012, Svensson 2540 (NY—holotype; MSC—isotype).

(Fig. 12)

Fig. 12. Bacidina circumpulla. A, part of thallus with pale and medium dark apothecia (holotype); B, thallus with dark-pigmented apothecia (Fryday 10017); C, section of relatively pale apothecium, with brown pigment in upper part of proper exciple and irregularly in hymenium (holotype); D, section of dark apothecium with more pigment in exciple and hymenium, including some green pigment in upper part of exciple (mixed with the brown) (holotype). Scales: A & B = 0.5 mm; C & D = 50 μm.

Thallus crustose, consisting of firm, ±placodioid, discrete, contiguous, or overlapping, sometimes imbricate, squamules. Squamules up to 350 μm wide, adnate and flattened or somewhat raised when overlapping, pale greyish, yellowish, or brownish, matt, not forming goniocysts or soralia. Prothallus thin and endosubstratal, whitish, present along edge of thallus or lacking. Photobiont chlorococcoid, cells rounded to ellipsoidal, 8–18 μm long, single or in clusters.

Apothecia scattered over thallus or aggregated, biatorine, broadly sessile, 0.2–0.4–0.7 mm diam. (s = 0.1, n = 40), flat, remaining so or becoming convex with age, without pruina, often strikingly variable in colour within the same thallus; disc dirty pinkish or pale beige to dark reddish or olive-brown to dark pinkish grey to almost black, often piebald; proper margin with dark pigment (appearing greyish black) in a ring around the paler disc, otherwise with colours similar to the disc, somewhat shiny, distinct and raised in young apothecia, soon level with the disc, ±persistent or later partially excluded in convex apothecia. Proper exciple 30–35 μm thick, without crystals, paraplectenchymatous, diffusely reddish brown and/or dirty green in at least the uppermost part, in dark apothecia with reddish brown pigment also along the edge and in the innermost part bordering the hypothecium, otherwise ±colourless, composed of radiating, dichotomously branched hyphae with moderately gelatinized walls; cell lumina in upper part of exciple narrowly ellipsoid (up to 9 μm long and 3 μm wide), wider and ±ellipsoid in lower part (up to 14 μm long and 6 μm wide), sometimes somewhat expanding terminally. Hymenium 49–54–59 μm tall (s = 3, n = 20), colourless in lower part, diffusely and unevenly reddish brown and dirty green in upper part and in scattered vertical streaks, pigment mostly concentrated around groups of paraphyses and young asci; paraphyses fairly abundant, in approximately equal proportion to number of asci, 1.5–2.3 μm wide in mid-hymenium, unbranched or sparingly branched in upper part; apices ±clavate, 2.3–3.6–5.4 μm wide (s = 0.8, n = 70), without gelatinous cap or internal pigment. Hypothecium colourless to pale yellowish. Asci clavate, 8-spored, approximately of Bacidia type sensu Hafellner (Reference Hafellner1984); young spore mass not forming ocular chamber, apex above young spore mass staining dark blue in IKI with a widely and bluntly conical axial body staining pale blue; ascospores colourless, without perispore or ornamentation, acicular, straight, curved or shallowly helical, 26–37–54 μm long (s = 6, n = 70), 1.6–2.2–3.1 μm wide (s = 0.3, n = 70), with (0–)3–5(–7) thin septa.

Pycnidia scattered, immersed in thallus with protruding ostiole, globose, unpigmented except for a dark ring of reddish brown pigment around the ostiole, 60–100 μm diam., unilocular; conidiophores lining inside of cavity, terminated by cylindrical to narrowly clavate conidiogenous cells, 3.5–6.0 × 1.5–2.3 μm. Conidia acrogenously formed, filiform, curved (but not hooked), non-septate, 7–13 × 0.7–1.0 μm.


All spot tests negative. No substances detected by HPTLC (Arup et al. Reference Arup, Ekman, Lindblom and Mattsson1993).


Laurocerasi-brown (reddish brown in H2O, KOH+ purplish, N+ orange-red) in proper exciple, hymenium and pycnidial wall, Bagliettoana-green (green in H2O, KOH− then HCl+ purple, HNO3+ purple) in hymenium and uppermost part of proper exciple (Meyer & Printzen Reference Meyer and Printzen2000), and possibly sometimes small amounts of Rubella-orange (yellow to orange in H2O, KOH+ intensifying, HNO3+ intensifying) in hypothecium (Ekman Reference Ekman1996).


The epithet circumpulla (nominative singular circumpullus) alludes to the shiny black ring formed by pigment in the uppermost part of the apothecial margin, surrounding the often paler disc.


Known from two localities in the western United States and Canada: one in inland British Columbia and one in GLBA. At the first locality, it was found overgrowing a decaying polypore in a swamp and at the other locality the exposed, soft wood of a log near the seashore.


Bacidina circumpulla is readily distinguished from all other species of the genus by its thallus, resembling a flattened miniature version of Bilimbia lobulata (Sommerf.) Hafellner & Coppins, and the apothecia that are superficially similar to the apothecia of Cliostomum griffithii (Sm.) Coppins, including the striking colour variation even within the same thallus. Unlike many members of the genus, the thallus never dissolves into goniocysts and generally lacks greenish hues when dry. Bacidina circumpulla shares the microsquamulose habit and the mixture of brown and green apothecial pigments with B. neosquamulosa (Aptroot & van Herk Reference Aptroot and van Herk1999) which, however, possesses a thicker apothecial margin and a greenish thallus composed of deeply incised microsquamules that sometimes disintegrate to form patches with goniocysts.

Bacidina circumpulla Ekman & Spribille ined.’ reported by McCune et al. (Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018) does not belong here but rather to the taxon named Bacidia friesiana by Ekman (Reference Ekman1996).

Additional specimens examined

Canada: British Columbia: Clearwater Valley, ‘Edgewood West’, 51°52.0′N, 120°01.8′W, overgrowing polypore fungus in swamp forest, 2006, Björk 13219 (UBC).—USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Queen Inlet, shoreline, 58.8770°N, 136.5060°W, 0–5 m, rotting log, 2012, Fryday 10016, 10017 (MSC—topotypes).

Biatora marmorea T. Sprib. sp. nov.

MycoBank No.: MB 830093

Similar to Biatora sphaeroidiza but differing in the deposition of pigment as distinct granules around the tips of the paraphyses, by the presence of a prominent dark hypothallus, and by the apothecial margin which remains white, prominent and not excluded at maturity.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, west side of Glacier Bay, base of Marble Mountain directly opposite Drake Island, 58°37.894′N, 136°14.639′W, corticolous on large, old Oplopanax horridus in dense beach fringe thicket of Alnus incana, just above sea level, 3 July 2012, Spribille 38009, Pérez-Ortega & Tønsberg (MSC—holotype; NY—isotype).

(Fig. 13)

Fig. 13. Biatora marmorea (holotype). A & B, habitus; C, section through hymenium and hypothecium, arrows indicate pigment incrustations on paraphysis tips; D, section through excipulum; E, asci and ascospores in Lugol's solution. Scales: A = 1 mm; B = 100 μm; C–E = 10 μm.

Thallus crustose, rimose to weakly areolate at the thallus margin, smooth, the individual areoles flat to weakly convex, creamish white, 0.2–0.4 mm diam.; thin, 50–120 μm in section, weakly stratified, with medullary hyphae strongly birefringent under polarized light, cortex scarcely differentiated, <15 μm thick, biofilm-like; sterile thalline hyphae I+ gold; hypothallus prominent, dark bluish to blue-black. Photobiont chlorococcoid, abundant; cells 6–10 μm diam.

Ascomata apothecia, round, single or in pairs, (0.3–)0.4–0.5(–0.7) mm diam.; disc convex, variably creamish white, aeruginose, blue-black to black depending on the exposure of the apothecia and intensity of pigment, with light-exposed sides of apothecia darker, matt; proper margin prominent, biatoroid, white to whitish to pale grey, becoming ±excluded as viewed from above, matt. Excipulum 35–40 μm wide laterally and 60–65 μm wide basally, composed of radiating, thick-walled hyphae with locally broadened lumina (Fig. 13D), embedded in a heavily gelatinized layer extending up to 10 μm beyond the hyphal tips, lacking crystals as viewed in polarized light. Hymenium hyaline except for the paraphysis tips, 45–60 μm tall, I+ blue changing to rust red with increasing iodine concentration, I+ blue following pretreatment with KOH, lacking crystals in polarized light; paraphyses straight, simple to weakly branched, 2 μm wide medianly, gradually widening to 3.5 μm apically, encrusted with bluish black pigment granules (Fig. 13C), these HCl+ blue, reversibly HNO3+ mauve ↔ KOH+ greenish, sequentially HNO3+ mauve −> HCl+ unchanged −> KOH dissolving yellowish, and HNO3+ mauve −> KOH+ strong green fading to yellowish −> HCl+ unchanged (similar to Cinereorufa-green, Printzen & Tønsberg (Reference Printzen and Tønsberg2003)). Hypothecium 130–150 μm tall, with algal cells frequently wedged between hypothecium and lower inner excipulum, giving the section a lecanorine appearance, hyaline above with a very pale brownish subhymenial layer visible c. 50–60 μm thick below. Asci Bacidia-type to Biatora-type (Fig. 13E), 8-spored, 25–27 × 6–12 μm; ascospores simple, narrowly ellipsoid, (8.0–)9.8–10.7(–12.5) × (2.5–)2.9–3.2(–4.5) μm (n = 23 over two collections).

Conidiomata not seen.


Thallus C−, KOH−, Pd−, UV+ pale orange. A dominant xanthone, perhaps thiophanic acid, with a secondary unidentified xanthone, detected by TLC.


Named after the type locality and, so far, only known location, Marble Mountain (Latin ‘marmor’, marble). Also a fanciful reference to the marbled pigmentation of the apothecial discs.


Corticolous on the bases of Oplopanax horridus (Smith) Miquel and bark of Alnus incana (L.) Moench subsp. tenuifolia (Nutt.) Breitung.


We were initially unsure of the genus assignment of this species because of the presence of algal cells between the lower hypothecium and lower excipulum in many sections, suggesting an affinity to Lecania A. Massal. s. lat. Biatora marmorea has an ascomatal habit (Fig. 13B) resembling Myrionora R. C. Harris (Palice et al. Reference Palice, Printzen, Spribille, Svensson, Tønsberg, Urbanavichene, Yakovchenko and Ekman2013; now also included in Biatora, Kistenich et al. Reference Kistenich, Timdal, Bendiksby and Ekman2018) or species of the B. beckhausii group (Printzen Reference Printzen2014), and DNA sequences confirmed its placement in Biatora (Fig. 10). Biatora marmorea appears to be closest, at least morphologically and chemically, to B. sphaeroidiza Printzen & Holien (Printzen Reference Printzen1995). It shares the chemical profile of B. sphaeroidiza in TLC but does not closely resemble the species in habit. In B. sphaeroidiza, the apothecia quickly become convex and emarginate with age, but in B. marmorea they maintain a prominent whitish margin which contrasts strongly with the pigmented disc (Fig. 13B). Most striking in the field is the presence of a dark blue-black hypothallus (Fig. 13A), which B. sphaeroidiza lacks. At the microscopic level, B. marmorea contains a pigment similar in reaction type to that present in B. sphaeroidiza, but it is concentrated in granules around the tips of the paraphyses that lead the apothecia to appear greenish speckled from the outside, although blackish under the light microscope. In addition, it has a thicker hymenium (45–60 μm) than B. sphaeroidiza (30–40 μm). The species is also genetically distinct from B. sphaeroidiza in a test phylogeny of only Biatora species (C. Printzen, personal communication 2017).

Oddly, despite the heavy collecting on Alnus and Oplopanax elsewhere in GLBA, this species was found in only one place, on the shoreline at the base of Marble Mountain. Here, however, it was abundant.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, west side of Glacier Bay, base of Marble Mtn directly opposite Drake Island, 58°37.894′N, 136°14.639′W, corticolous on Oplopanax horridus, 2011, Spribille 36364 & Fryday (MSC, topotype); ibid., corticolous on Alnus incana subsp. tenuifolia, sea level, 2012, Spribille 38015, Pérez-Ortega & Tønsberg (MSC, topotype); ibid., corticolous on Oplopanax horridus, 2012, Tønsberg 41650 (MSC, topotype).

Carneothele Fryday, T. Sprib. & M. Svenss. gen. nov.

MycoBank No.: MB 830094

Similar to Thelocarpon but with red-brown ascomata, the wall pigment forming magenta crystals in 10% KOH.

Type: Carneothele sphagnicola Fryday, M. Svenss. & Holien (see below).


From the Latin carnalis (‘of the flesh’) and –thele (Gr.: nipple), a reference to the shape and colour of the ascomata.

Carneothele sphagnicola Fryday, M. Svenss. & Holien sp. nov.

MycoBank No.: MB 830095

Thallus biofilm-like, coating Sphagnum mosses; ascomata red-brown, perithecioid, the wall pigment forming magenta crystals in 10% KOH, attenuating to a narrow ostiole, with asci 220–250 × 30–35 μm, polysporous, containing ellipsoid ascospores.

Type: USA, Alaska, Petersburg Borough, Mitkof Island, ‘Towers muskeg’, 56.672750°N, 132.918500°W, 10 m, Sphagnum bog (muskeg) with Oxycoccus oxycoccos, 1 September 2014, Fryday 10667, K. Dillman & Spribille (MSC—holotype, E—isotype).

(Fig. 14)

Fig. 14. Carneothele sphagnicola (A & B from Spribille 40821; C–F from Spribille 40824). A & B, habitus; C, section through ascoma; D, ascomatal section in Lugol's solution, showing deeply amyloid hymenial region and adjacent non-amyloid zone; E, ascoma in K, demonstrating dendritic crystals; F, ascospores in Lugol's solution, showing characteristic amyloid reaction. Scales: A & B = 0.5 mm; C–E = 50 μm; F = 10 μm.

Thallus biofilm-like. Photobiont present as scattered bundles of green algal cells, 20–60 μm across, present around the base of the perithecia; individual cells orbicular, 5–9 μm diam.

Ascomata perithecioid, scattered, brick red, occasionally with light yellow pruina around the ostiole, becoming pale brown in the herbarium, flask-shaped, 0.20–0.25–0.30 mm diam., 0.4–0.5 mm tall, ½ to ⅔ immersed in substratum. Ascomatal wall hyaline (blue in 10% HCl), composed of longitudinally arranged hyphae 2–2.5 μm thick but with numerous, minute, golden brown crystals that dissolve in KOH to give a fleeting magenta solution followed by the formation of ± rectangular or dendroid magenta crystals, mostly c. 10–18 μm across but up to 30 × 10 μm, crystals not dissolving in 10% HCl or 50% HNO3, but becoming golden brown. Hamathecium composed of numerous, slender (c. 1 μm thick), lax, unbranched filaments, I−. Asci 220–250 × 30–35 μm, slightly clavate at base, gradually tapering to a narrow apex, wall I+ blue, tholus I+ blue with a narrow, I− ocular chamber; ascospores unicellular, numerous (>200) per ascus, broadly ellipsoid with pointed ends, 9–10 × 4–5 μm, amyloid (IKI+ blue).


Thallus spot tests negative, ascomatal wall with KOH+ magenta crystals (see below), HNO3− (50% solution), HCl− (15% solution). No substances detected by TLC.


A reference to the apparently obligate occurrence on the tops of Sphagnum hummocks.


Found only on the dry tops of Sphagnum hummocks, apparently most frequent on S. fuscum (Schimp.) Klinggr. At the type locality it occurs in a distinctive community with Absconditella sphagnorum Vězda & Poelt, as well as an undescribed ascomycete superficially resembling Geltingia associata (Th. Fr.) Alstrup & D. Hawksw. and Epibryon sp.


Carneothele sphagnicola is a highly distinctive species that defied placement in any known genera. It is apparently close to Thelocarpon, with which it shares the minute ascomata on organic substrata with the occasional presence of a yellow pruina, plus the multi-spored asci that gradually taper to a narrow apex. However, it differs from that genus in the more robust red-brown ascomata with the wall pigment forming magenta crystals in 10% KOH.

Carneothele sphagnicola is readily recognizable in the field on account of its ascomata that, when wet, resemble little pointed pieces of raw red meat as viewed through a hand lens (Fig. 14B), and which dot patches of moribund Sphagnum. Microscopically it is characterized by its multi-spored asci and the ascomatal wall containing small orange crystals that dissolve in KOH to form different, magenta crystals. Using standard 10% KOH these crystals are ±rectangular (c. 20–30 × 5–10 μm) but with a higher concentration of KOH, long, branching (dendroid) needle-shaped crystals are formed (Fig. 14E).

In our efforts to find an existing genus in which to place the new species, we shared material and photographs with several specialists (O. Eriksson, Sweden; P. Döbbeler, Germany; B. Coppins, UK; A. Rossman, USA). One of us (HH) recognized the species from material collected in oceanic bogs in Trøndelag, Norway. We have since found the species outside of GLBA in muskeg on Mitkof Island, which we have designated the type locality based on the greater abundance of material collected from this site. We expect it to be widespread in such habitats in SE Alaska and possibly in other temperate rainforest regions of the world. Indeed, the associated ascomycete resembling Geltingia associata and the Epibryon sp. have recently been collected from a similar habitat in Newfoundland, NE Canada, although C. sphagnicola was not seen (J. M. McCarthy, personal communication).

Attempts to establish the evolutionary relationships of Carneothele sphagnicola using DNA have so far not been successful. The one extraction that has yielded usable DNA produced ITS and 28S rDNA sequences with affinities to Dothideomycetes and Sarea, respectively (isolate T1110, Table 1), but it is not certain whether these sequences derive from the fungus that forms the fruiting bodies described here.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, NE of Gustavus, Falls Creek area, ‘Yellowlegs Savanna’ muskeg, 58.44367°N, 135.60583°W, terricolous on wet ground next to flark, 250 m, 2012, Spribille 38741 (MSC), Fryday 10046 (MSC), Svensson 2577 (MSC); ibid., 58.44742°N, 135.60593°W, 245 m, Spribille 38738 (MSC, NY); Petersburg Borough, Mitkof Island, muskeg c. 0.6 km S of Papkes Landing Road, W side of highway behind radio towers, 56.673015°N, 132.916128°W, 9 m, 2014, Spribille 40824, Fryday & Dillman (GZU, UPS, topotypes); ibid., Twin Creek muskeg, 56.723250°N, 132.905500°W, 2014, Spribille 40821, Fryday & Dillman (H).—Norway: S-Trøndelag: Åfjord, by Lake Måmyrvatnet, Nesodden, 64.09798°N, 10.54964°E, 260 m, on dead Sphagnum fuscum in ombrotrophic mire, 2016, Holien 15270 & 15318 (TRH). N-Trøndelag: Steinkjer, W of lakelet Svarttjønna, Jernblaestermyra, 64°03.01′N, 11°31.61′E, 200 m, on dead Sphagnum in ombrotrophic mire, somewhat eroded and trampled patches, 2008, Holien 11927 (TRH); ibid., 2012, Holien 13916 (TRH), 13917 (MSC); Meråker, N of Sulåmoen, E of Litlåa, 63.5649°N, 11.9442°E, 440 m, on dead Sphagnum fuscum in ombrotrophic mire, 2013, Holien 14221 (TRH).

Cirrenalia lichenicola Pérez-Ort. sp. nov.

MycoBank No.: MB 830096

Similar to Cirrenalia caffra Matsush. but differing in the thinner diameter of the filaments, conidia with fewer average number of septa, and different substratum.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park and Preserve, along the trail from Bartlett Cove to Point Gustavus, near campground, 58°26′43″N, 135°53′05″W, on sterile unidentified corticolous crust on Alnus, 7 July 2012, Pérez-Ortega 2284 (US–holotype).

(Fig. 15)

Fig. 15. Cirrenalia lichenicola (holotype). A, sporodochia; B, conidia; C, detail of a coiled conidium (B & C in water, using DIC microscopy). Scales: A = 100 μm; B = 20 μm; C = 5 μm.

Colonies growing on a sorediate crustose lichen, forming groups of sporodochia, black, up to 100 μm diam. Mycelium scanty, superficial or immersed in the host, hyaline or slightly brown. Conidiophores micronematous or semi-macronematous, short, acrogenous or more rarely arising laterally on hyphae, simple or very rarely dichotomously branched, straight or more rarely flexuous, pale to dark brown, smooth, 4–6 μm wide; conidiogenous cells monoblastic, terminal; conidia acrogenous, solitary, dry, helicoid, contorted one time, smooth-walled, dark brown when mature, light brown when young, septa 4–7, not or slightly constricted at the septa, apex obtuse, basal parts usually tapering, 8–12 μm, filaments 2.5–4.5(–6.0) μm wide (n = 24).


Named for its lichenicolous occurrence.


On an unidentified whitish sorediate crustose lichen; material too scant for chemical tests.


The genus Cirrenalia Meyers & R. T. Moore has been used for species of dematiaceous fungi characterized by helicoid conidia, usually constricted at the septa (Zhao & Liu Reference Zhao and Liu2005). Initially, the genus contained only marine species but it was expanded (Sutton Reference Sutton1973) to include terrestrial species and the number of accepted terrestrial and marine species is now similar. The genus has been recently studied using molecular markers and been shown to be highly polyphyletic (Abdel-Wahab et al. Reference Abdel-Wahab, Pang, Nagahama, Abdel-Aziz and Jones2010). Compared to species treated in the overview provided by Zhao & Liu (Reference Zhao and Liu2005), Cirrenalia lichenicola is characterized by the small size of the conidia and the narrow filaments. Cirrenalia caffra Matsush. is similar to the new species although the filament is slightly wider and the conidia are also larger. Cirrenalia lignicola differs in having more coiled conidia and the presence of up to 12 septa. Cirrenalia lichenicola is known only from the type specimen (Fig. 15).

Corticifraga nephromatis Pérez-Ort. sp. nov.

MycoBank No.: MB 830097

Lichenicolous on Nephroma bellum. Differing from morphologically similar species by the presence of non-septate ascospores that are ellipsoid with acute ends to teardrop-shaped (dacryoid).

Type: USA, Alaska, Hoonah-Angoon Census Area, East Arm of Glacier Bay, mouth of unnamed creek E of Muir Point, 58.83642°N, 136.05313°W, 8 m, 30 July 2012, Spribille 39257 (US—holotype).

(Fig. 16)

Fig. 16. Corticifraga nephromatis (holotype). A, ascomata; B, transverse section of ascoma; C, detail of hymenium and excipulum; D, paraphyses; E, young ascus; F, mature ascus; G–I, ascospores (B & C in lactophenol blue; D–I in water using DIC microscopy). Scales: A = 200 μm; B = 50 μm; C = 25 μm; D = 10 μm; E–I = 5 μm.

Apothecia delimited, scattered or more rarely confluent, originating from splits in the host cortex, irregularly roundish to angular, 0.10–0.25 mm diam.; disc usually at the same level as the thallus surface or slightly raised, cream-coloured with the exciple usually lighter than the disc. Exciple colourless, up to 25 μm wide but usually reduced. Hymenium colourless, 50–70 μm tall, I−, KI−; paraphyses straight, not branched, 2–3 μm wide, not capitate but increasing in diameter, gradually reaching up to 5 μm at the apex. Hypothecium hyaline, up to 85 μm tall. Asci bitunicate, clavate to subcylindrical, with a small ocular chamber seen in immature asci, 25–34 × 5–8 μm (n = 10), 8-spored, I−, KI−; ascospores simple, from ellipsoid with acute ends to teardrop-shaped (dacryoid), colourless, smooth-walled, (10–)11–12 × 3–4(–5) μm (n = 25).


Named for its occurrence on Nephroma.


On Nephroma bellum (Spreng.) Tuck.


Four species of Corticifraga D. Hawksw. & R. Sant. are known from SE Alaska. Corticifraga fuckelii (Rehm) D. Hawksw. & R. Sant. and C. peltigerae (Fuckel) D. Hawksw. & R. Sant. are common on species of Peltigera, and recently C. scrobiculatae Pérez-Ort. was described from Lobarina scrobiculata (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) and discovered in GLBA during the present survey. Corticifraga chugachiana Zhurb. was described from the Chugach National Forest as one of the few lichenicolous fungi to occur on Lobaria oregana (Zhurbenko Reference Zhurbenko2007). Corticifraga nephromatis (Fig. 16) is the second species of the genus growing on Nephroma Ach. Corticifraga santessonii Zhurb. may grow on Nephroma occultum, but it is readily differentiated from C. nephromatis by its dark-coloured ascomata and 3-septate ascospores. Furthermore, the new taxon is distinguished from other species in the genus by the presence of ellipsoid to dacryoid, simple ascospores and broader paraphyses. The recently described genus Taitaia Suija et al. shows clear affinities with Corticifraga, from which it is separated based on molecular data and the typically aggregated apothecia (Suija et al. Reference Suija, Kaasalainen, Kirika and Rikkinen2018). Taitaia aurea Suija et al. possesses apothecia of a similar colour to those of C. nephromatis. It differs, however, in the presence of 1-septate ascospores and the aggregated apothecia, as well as the occurrence on Crocodia cf. clathrata (DeNot.) Trev.

Additional specimen examined

USA: Alaska: Hoonah-Angoon Census Area, East Arm of Glacier Bay, mouth of unnamed creek E of Muir Point, 58.83642°N, 136.05313°W, 8 m, 2012, Spribille 39259 (MSC—topotype).

Fuscidea muskeg Tønsberg & M. Zahradn. sp. nov.

MycoBank No.: MB 830098

Similar to Fuscidea praeruptorum (Du Rietz & H. Magn.) V. Wirth & Vězda in being sorediate and producing alectorialic acid, but distinct from that species by the medianly constricted, shorter (7–10 μm) ascospores (vs bean-shaped and slightly longer (9.5–12 μm) in F. praeruptorum) and the corticolous habit (vs saxicolous).

Type: USA, Alaska, Hoonah-Angoon Census Area, along and N of road from Gustavus to Bartlett Cove, near entrance sign for Glacier Bay National Park and Preserve, 58°27.19′N, 135°46.64′W, corticolous on branches of Pinus contorta Dougl. ex Loudon subsp. contorta in muskeg, 1 July 2012, Tønsberg 41576 (MSC–holotype; NY–isotypes).

(Fig. 17)

Fig. 17. Fuscidea muskeg (holotype). A, habitus; B, young apothecia with SEM, showing surface of surrounding thallus; C, surface of thallus wart from (B) with SEM; D, surface of excipulum from (B) with SEM, showing short hyphal ‘spines’; E, section of apothecium; F, ascus and ascospores (DIC). Scales: A = 2 mm; B = 200 μm; C & E = 50 μm; D = 20 μm; F = 10 μm.

Thallus crustose, areolate, usually forming rounded patches to a few cm diam., rarely larger, to 0.5 mm thick. Hypothallus often distinct as ramifying hyphae bordering the thallus and also evident as pale brown pigmentation of the substratum between thallus areoles. Esorediate areoles discrete, pale greenish to greenish with a yellowish tinge (becoming brown or pinkish in the herbarium), convex, 0.12–0.20 mm diam., soon bursting apically to form soralia. Soralia concolorous with esorediate parts, discrete at first, later some becoming confluent, rarely forming a leprose crust throughout. Soredia mostly aggregated in irregularly rounded consoredia, 14–55 μm wide. Photobiont trebouxioid, cells (8–)11–15(–18) μm diam.

Apothecia often absent, occasionally abundant, pale to dark brown, discrete, regularly to irregularly rounded, to 1.0 mm diam., attached to the thallus only at the centre of the base; disc pale to dark brown, more or less flat; proper margin concolorous with disc or, sometimes, paler brown than disc or pale greenish brown, raised above the disc, flexuose, ±involute, 0.06–0.08 mm wide, bearing spiny protrusions visible in SEM (Fig. 17D). Excipulum rim 60–65 μm wide, brown along the edges, colourless inside; cells rounded and thin-walled; walls brown in pigmented parts; lumina wide, 7–10 × 6–7 μm. Hymenium colourless or, rarely, brownish, 48–65 μm tall; paraphyses sparingly anastomosed and, especially in upper part, branched, 1.5–2 μm wide; apical cells enlarged, to (2–)3(–4) μm, with a pigmented cap. Hypothecium colourless, 25–52 μm tall. Asci clavate, 27–45 × 10–12 μm; ascospores 7–10 × (3–)4–5 μm (n = 22), simple or rarely 1-septate, medianly constricted (Fig. 17F).

Pycnidia brown, convex, 0.06–0.12 mm wide; conidia dacryoid, 3 × 1.5–2 μm.


Thallus PD+ yellow, C+ red; alectorialic acid with satellite(s) by TLC.


From muskeg, the Algonquin name for a blanket bog (USDA Forest Service 1990).


In Alaska, Fuscidea muskeg occurs in muskeg (a blanket bog), a habitat closely associated with cool summers and abundant rain. In these habitats in GLBA it grows mainly on branches of Pinus contorta but also on Picea sitchensis (Bong.) Carrière, Alnus and Vaccinium ovalifolium Sm.


In the past (Fryday Reference Fryday2008a), F. muskeg has been mistaken for a corticolous form of F. praeruptorum, which is chemically identical. However, recent examination of richly fertile, corticolous material has revealed medianly constricted and rather short ascospores, 7–10 μm. In F. praeruptorum the ascospores are bean-shaped and slightly longer (9.5–12 μm), the areoles are smaller and more scattered than in F. muskeg, and the brownish or blackish hypothallus is more conspicuous. The overall colour of fresh material of F. muskeg is light green or green with a yellowish tinge on a pale brownish background, whereas F. praeruptorum has a distinct brown or black overall colour. In old herbarium material, both species are brown to pinkish. Within Fuscidea, the combination of medianly constricted ascospores and production of alectorialic acid distinguishes F. muskeg as a distinct species. Fuscidea arboricola Coppins & Tønsberg and F. lightfootii (Sm.) Coppins & P. James are also sorediate and have medianly constricted ascospores (see Gilbert et al. Reference Gilbert, Purvis, Skjolddal, Tønsberg, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009), but those species are chemically different from F. muskeg in producing fumarprotocetraric acid and divaricatic acid, respectively. Fuscidea lightfootii was reported as new to North America by Aptroot (Reference Aptroot1996) but this was shown by Fryday (2008a) to be an error; it is not currently known to occur in North America.

Fuscidea muskeg is a widely distributed species in North America. Its phylogenetic position will be discussed by M. Zahradniková et al. (unpublished data).

Additional specimens examined

USA: Alaska: Glacier Bay National Park and Preserve, along and N of road from Gustavus to Bartlett Cove, near park entrance, 58°27.087′N, 135°47.284′W, 32 m, corticolous on Pinus contorta in glacial outwash plain, 2011, Spribille 36302, 36306 & Fryday (MSC, topotypes); ibid., 58°27.153′N, 135°46.604′W, corticolous on branches of Pinus contorta in muskeg, 2012, Tønsberg 41567 (MSC, topotype); ibid., 58°27.185′N, 135°46.643′W, corticolous on branches of Pinus contorta in muskeg [with Equisetum], Tønsberg 41577 (MSC, topotype); ibid., 58.45115°N, 135.79013°W, corticolous on Pinus contorta branches, 2012, Spribille 38698 (MSC, topotype), Svensson 2561 (MSC); Bartlett Lake trailhead, 58°27.292′N, 135°52.240′W, 48 m, corticolous on Vaccinium ovalifolium, 2011, Spribille 36035 (MSC); E of Bartlett Cove along road, Crane Flats, just S of road along edge of meadows, 58.450110°N, 135.841521°W, 33 m, corticolous on Alnus, 2011, Spribille 36803 (MSC); ridge above Fern Harbor, at and E of the pond, 58°18.803′N, 136°27.635′W, 235 m, corticolous on branches/twigs of Pinus contorta in muskeg, 2012, Tønsberg 41771, 41773 (MSC); east shore of mouth of Glacier Bay, small point 5.5 km N of Point Gustavus and 2.8 km S of Bartlett Cove NPS compound, along seashore, 58.43005°N, 135.90211°W, 4 m, corticolous on Picea sitchensis, 2012, Spribille 39118 (MSC); ibid., 3.8 km N of Point Gustavus and 4.4 km S of Bartlett Cove NPS compound, along seashore, 58.41458°N, 135.89868°W, 4 m, corticolous on Picea sitchensis, 2012, Spribille 39154 (MSC).

Fuscopannaria dillmaniae T. Sprib. sp. nov.

MycoBank No.: MB 830099

Differing from all other Fuscopannaria species and Moelleropsis nebulosa in the thallus consisting entirely of corticate, isidioid granules 20–50 µm in diam., these usually branching, olivaceous brown; differing from Leciophysma furfurascens in the presence of a robust, black hypothallus.

Type: USA, Alaska, Hoonah-Angoon Census Area, just outside of boundaries of Glacier Bay National Park, NW of Gustavus, Tower Road, 58.46253°N, 135.77430°W, corticolous on Alnus viridis subsp. crispa (Aiton) Turrill, 33 m, 4 July 2012, Spribille 38036, Tønsberg & Pérez-Ortega (UPS—holotype; BG—isotype).

(Fig. 18)

Fig. 18. Fuscopannaria dillmaniae and species that it may be confused with. A & B, F. dillmaniae, habitus of holotype, from which a DNA sequence was reported as Santessoniella grisea by Schneider et al. (Reference Schneider, Resl and Spribille2016); C, a specimen (Tønsberg 24918, BG) reported as Santessoniella grisea from Washington State, USA by Tønsberg & Henssen (Reference Tønsberg and Henssen1999), and later as a DNA voucher by Ekman et al. (Reference Ekman, Wedin, Lindblom and Jørgensen2014), which appears to belong in the genus Rockefellera; D, a specimen (Tønsberg 32520) identified as S. grisea from Alaska (P.M. Jørgensen, unpublished data); E, isotype specimen of Placynthium griseum (W); F, holotype specimen of Pannaria furfurascens (H). Scales: A = 2 mm; B & C = 0.5 mm; D & F = 1 mm; E, mobile phone photograph, no scale bar available.

Thallus a sprawling crust, irregularly oval, 2–4.5 cm long and 1.5–2.5 cm wide, composed of minute isidioid growths on a black hypothallus, these cracking into areole-like patches when dry, the areoles 0.8–1 mm diam.; thalline isidioid outgrowths olivaceous brown, irregularly branched, not opuntioid, individual fingers 20–50 μm diam., consisting of tightly packed Nostoc-like cyanobacterial cells with fungal hyphae sheathed in a gelatinous cortex-like layer, a cellular cortex lacking.

Ascomata apothecia, round, single, 0.4–0.9 mm diam.; disc flat to strongly convex, reddish brown to dark red-brown, matt; proper margin soon receding, pale brown, matt. Excipulum to 62 μm wide laterally and 50–55 μm wide basally, composed of radiating, moniliform hyphae, up to 6 μm diam., lacking apparent pigments or crystals, but with thin pigment line occasionally separating excipular region from hymenium, I−. Hymenium 100–130 μm tall, hyaline, asci and surroundings I+ blue before KOH treatment, uppermost part of hymenium (‘epihymenium’) with mauve-brown pigments between the tips of the paraphyses, crystals lacking; paraphyses moniliform, weakly branched to branched and anastomosing, tips 2–3 μm wide, with KOH+ dirty green wall pigment. Hypothecium 150–200 μm thick, hazy hyaline, KOH+ slightly creamish, of tightly woven hyphae, lumina not >2 μm. Asci widely flask-shaped, c. 75 × 17 μm, 5–6 ascospores observed but probably 8 per ascus, lightly amyloid externally, with a strongly I+ apical tholus pierced by a distinct apical tube; ascospores simple, broadly ellipsoid, (11.5–)16.0–16.3(–22) × (7.5–)8.0–9.5(–11) μm, sometimes with apical end thickenings, lacking ornamented perispore (n = 18 from three specimens).

Pycnidia not observed.


All thallus spot tests negative; no substances detected by TLC.


Named to honour the outstanding contributions of Karen Dillman in documenting the lichen biota of south-east Alaska.


On the bark of Alnus and Populus in lowland temperate rainforests, so far known only from south-east Alaska. Fuscopannaria dillmaniae has been found at three sites in GLBA and on the nearby mainland near Juneau. It is probably more widespread in south-east Alaska than the few records currently suggest.


Minutely fruticose pannarioid cyanolichens have caused considerable confusion amongst taxonomists. Closely related species were described in the genera Pannaria Delise ex Bory, Lemmopsis (Vain.) Zahlbr. and Placynthium (Ach.) Gray, but Henssen (Reference Henssen1997) united them into a new genus, Santessoniella, based mainly on thallus architecture. Molecular studies have since revealed the profuse, branched, finger-like thallus projections, characteristic of the morphologically defined Santessoniella, to be a product of convergent evolution of morphology that appears to have arisen at least three times in the Pannariaceae (Ekman et al. Reference Ekman, Wedin, Lindblom and Jørgensen2014; four if one counts the genus Atrophysma, described in this paper).

Fuscopannaria dillmaniae (Fig. 18A & B) is most similar to Leciophysma furfurascens (Nyl.) Gyeln. (Fig. 18F) in overall habit but differs in possessing a well-developed black hypothallus. Based on Henssen's work and subsequent keys to pannarioid lichens (Jørgensen Reference Jørgensen2000, Reference Jørgensen2005), the new species could also be assumed to belong to Santessoniella grisea (Hue) Henssen and this led one of us (TS, in Schneider et al. Reference Schneider, Resl, Westberg and Spribille2015) to incorrectly report an LSU rDNA sequence from the type of F. dillmaniae as S. grisea. Santessoniella grisea was reported from Washington State (Tønsberg & Henssen Reference Tønsberg and Henssen1999) and later Alaska and Mexico (Jørgensen Reference Jørgensen2000); the Washington State material is also the basis for an ITS rDNA NCBI nucleotide database voucher (Ekman et al. Reference Ekman, Wedin, Lindblom and Jørgensen2014). Neither the Washington State specimen (Fig. 18C) nor another specimen subsequently collected from Alaska and named as S. grisea by P. M. Jørgensen (unpublished data) (Fig. 18D), closely resemble the isotype of Placynthium griseum Hue ≡ Santessoniella grisea (Hue) Henssen (W!, Fig. 18E). The DNA sequences of the Washington State specimen place it in the wider Protopannaria clade (Fig. 9), in an unsupported subclade with the eastern North American species Rockefellera crossophylla (Lendemer et al. Reference Lendemer, Stone and Tripp2017).

Another species with which Fuscopannaria dillmaniae could understandably be confused, based on the key and thallus dimensions in Jørgensen (Reference Jørgensen2000), is F. coralloidea P. M. Jørg. Jørgensen reported for this species ‘thallus to 150 μm thick’ but did not provide measurements for individual coralloid lobes. Based on our study of the holotype (USA, California, Sharnoff & Sharnoff 1323.23, CANL–119402!), the thallus of F. coralloidea is 2–3 mm thick, and compared to F. dillmaniae has a much coarser thallus architecture, with fruticose branches an order of magnitude thicker (210–270 μm, flaring to 410 μm wide, vs 20–50 μm in F. dillmaniae). It grows on soil in California and Oregon.

Perhaps the Fuscopannaria species most similar to F. dillmaniae is Moelleropsis nebulosa (Hoffm.) Gyeln. Moelleropsis is clearly nested within Fuscopannaria (Fig. 9), a result that has been obtained before (see also Ekman et al. Reference Ekman, Wedin, Lindblom and Jørgensen2014) but is the older generic name. A proposal to conserve Fuscopannaria over Moelleropsis is pending (Jørgensen et al. Reference Jørgensen, Ekman and Wedin2013). Fuscopannaria dillmaniae possesses more structured, coralloid isidioid growths, compared to the loose granules that characterize M. nebulosa, and differs from the latter in its prominent black hypothallus.

Additional specimens examined

USA: Alaska: Glacier Bay National Park and Preserve, East Arm of Glacier Bay, mouth of unnamed creek E of Muir Point, 58.83642°N, 136.05313°W, corticolous on Populus balsamifera, with Rostania occultata, 8 m, 2012, Spribille 39251 (MSC); ibid., 58.83477°N, 136.05717°W, on Alnus, 2012, Svensson 2780 (UPS); W side of Glacier Bay, Shag Cove, 58°37.924′N, 136°19.715′W, corticolous on Alnus, sea level, 2011, Spribille 36401 (MSC); Juneau City and Borough, Montana Creek, 58°25.567′N, 134°37.979′W, on Alnus, 77 m, ix 2010, Spribille s. n., Hampton-Miller & Taurer (ALTA, BG, NY, UBC, UPS).

Halecania athallina Fryday sp. nov.

MycoBank No.: MB 830100

Similar to Halecania rhypodiza (Nyl.) Coppins but with smaller ascospores and lacking any visible epilithic thallus.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, 58.46349°N, 135.55807°W, 922 m, alpine heath with rock outcrops, alkaline argillite, 22 July 2012, Fryday 10114, Spribille & Svensson (MSC—holotype).

(Fig. 19)

Fig. 19. Halecania athallina (holotype). A & B, habitus; C, section of apothecium; D, detail showing paraphyses; E–H, ascospores. Scales: A = 1 mm; B = 0.2 mm; C = 50 μm; D–H = 10 μm (scale bar provided only in H).

Thallus completely immersed in substratum. Photobiont chlorococcoid, cells 6‒10 μm diam.

Apothecia scattered, dark reddish brown, lecideine, (0.2‒)0.3‒0.4(‒6) mm diam.; disc flat to slightly convex when mature, with a persistent, slightly raised proper margin, 0.05 mm wide. Excipulum internally hyaline composed of narrow, branched and anastomosing hyphae c. 1.0 μm wide, outer 10 μm brown, with cortical cells 3‒4 μm wide with dark brown cap (similar to paraphyses). Hymenium 35‒40 μm tall; epihymenium brown, 5‒10 μm wide; paraphyses simple, 1‒1.5 μm wide, abruptly thickening at apex to 3‒4 μm with a brown cap. Hypothecium c. 30 μm tall, hyaline, composed of randomly orientated hyphae 2‒3 μm wide. Asci Catillaria-type, slightly clavate to clavate, 30‒35 × 12‒18 μm; ascospores hyaline, 1-septate, (9.5–)11.8 ± 1.9(–14.5) × (3.5–)4.7 ± 0.4(–5.5) μm, l/w ratio (2.2–)2.5 ± 0.4(–3.0), n = 10, with thin perispore.

Conidiomata not observed.


Apothecial section and adjacent thalline material KOH−, C−, PD−; unidentified substance at R f classes A4, B4, C4 by TLC.


A reference to the lack of thallus.


On mildly basic argillitic rock in the alpine zone.


This is an inconspicuous but easily identified species on what appear to be almost uncolonized surfaces of argillitic rock (Fig. 19A). Attempts to amplify DNA were not successful.

The genus Halecania was erected by Mayrhofer (Reference Mayrhofer1987) for a group of six species previously included in Lecania, from which they differed in having Catillaria-type asci, distinctly capitate paraphyses and halonate ascospores. Additional species have subsequently been added (e.g. Coppins Reference Coppins1989a; Fryday & Coppins Reference Fryday and Coppins1996; van den Boom & Elix Reference van den Boom and Elix2005; van den Boom Reference van den Boom2009) so that the genus now includes over 20 species (Index Fungorum 2019). Many species are saxicolous but the genus also includes corticolous, muscicolous and lichenicolous species.

The new species differs from all previously described species by the almost complete absence of an epilithic thallus. It most closely resembles Halecania rhypodiza but that species differs in having a distinct, dark brown, granular thallus and larger ascospores (12–15 × 4.5–6 μm; Fletcher & Coppins Reference Fletcher, Coppins, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009).

Additional specimen examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, 58.46349°N, 135.55807°W, 922 m, alpine heath with rock outcrops, alkaline argillite, 2012, Fryday 10130, Spribille & Svensson (MSC, sub Lecidella patavina).

Hydropunctaria alaskana Thüs & Pérez-Ort. sp. nov.

MycoBank No.: MB 830101

Similar to Hydropunctaria oceanica Orange but differing in the shorter ascospores, distinctly fimbriate prothallus in some specimens, and nuclear ITS and mitochondrial SSU sequence data.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Taylor Bay, 58.2549°N, 136.5675°W, 0–5 m, on metamorphic rocks (hornblende augen gneiss) beside creek with Buellia coniops and Verrucaria aethiobola, 9 August 2012, Fryday 10458 & Spribille (MSC—holotype).

(Fig. 20)

Fig. 20. Hydropunctaria alaskana. A–C, habitus (A from holotype, B & C from isotype specimens); D, section of perithecium from holotype. Scales: A–C = 1 mm; D = 50 μm.

Thallus episubstratal, thin to moderately thick, sterile areas c. 40–115 μm thick (n = 7), cracks numerous, creating small areoles, continuous areas without cracks absent or restricted to the thallus margin, fertile areoles up to 400–600 μm diam., c. 2–3 times larger than sterile ones (25 largest measured on four thalli); surface of infertile areoles in the type material smooth, except on the thallus margin where jugae are protruding over the surrounding thallus and become visible as black dots; development of jugae is more variable in specimens from coastal rocks. Thallus surface brown to black-brown but occasionally rusty reddish tinged due to mineral particles deposited on the thallus, without any green component, not subgelatinous (remaining opaque when wet). Pseudocortex absent to max. 5–8 μm high, with faint brown pigmentation or hyaline, KOH−. Prothallus cream-coloured to clear white, distinctly fimbriate when well developed, but more often thin or absent. Photobiont cells mostly irregularly arranged, rarely in short vertical chains, (6.6–)7–8(–10.4) × (3.9–)6.1–6.7(–7) μm (n = 30), in section mostly ± cuboid (rarely orbicular), interspersed with some more elongated cells with length/width ratio of c. 2.1:1. Medulla brown-black in upper parts (‘black basal layer’), in parts fading to colourless at the base, fading more frequently observed under the perithecia, KOH−. Black protrusions (jugae) of up to 35 μm diam. frequent, in central parts of the thallus mostly emerging from black basal layer, some also disconnected from basal layer and initiating from a zone at approximately half the height of the thallus but usually not penetrating the pseudocortex, except on the flanks and in the direct vicinity (same areole) of the perithecia and on the edge of the thallus.

Perithecia forming flat projections, ±raised above the surrounding thallus (ratio perithecia/thallus height c. 1.5:1–4:1), crowded to widely-spaced and isolated (variation within a single thallus). Involucrellum conical, enveloping the exciple and merging laterally with black basal layer. Exciple 150–185(–230) μm wide (n = 5), with brown-black pigmentation from top to bottom. Periphyses 22–35 × 1–2 μm (n = 4). Interascal filaments quickly gelatinized in ontogeny. Asci 8-spored, 30–51 × 14–15.7 μm (n = 10). Ascospores (10.8–)12.2–15.0(–17.9) × (4.7–)5.3–7.1(–9.2) μm (n = 152), l/w ratio (1.6–)1.8–2.4(–3.4), without halonate perispore.


Pseudocortex pigment KOH−, brown pigment in basal layer KOH−. Hymenial gel I+ red, K/I+ blue. No metabolites detected by TLC.


Named for its discovery in Alaska.


The type collection is from a small stream close to the coastline, not inundated at the time of collection, where the species is locally frequent. The associated species (e.g. Buellia coniops) indicate at least the temporary influence of saline spray from the nearby seashore. Two other populations are known from the upper littoral zone on coastal rocks (e.g. with Mastodia tessellata) along the NW North American coast, on Mitkof Island (Alaska) and Vancouver Island (British Columbia).


This new species is morphologically most similar to Hydropunctaria oceanica, H. aractina (Wahlenb.) Orange, H. maura (Wahlenb.) C. Keller et al. and H. orae Orange. It differs in having, on average, shorter ascospores (12.5–15.0–18.0 μm in H. oceanica, 14.5–16.6–19.0 μm in H. maura, 13.0–16.1–19.5 μm in H. orae) and the presence of a fimbriate white prothallus in some specimens. The thallus is much thinner compared to the sun-exposed thalli of H. maura (40–115 μm vs 60–300 μm). From H. orae and H. aractina it also differs by the lack of green pigmentation in the cortex and brown-black colour in thallus surface view. There is an overlap with some forms of these species and identification of taxa from this genus in coastal areas (where occurrences of freshwater and salt-tolerant species can intermingle) can remain ambiguous if not supported by sequencing of the ITS region (Orange Reference Orange2012). Two ITS sequences of the new species place H. alaskana apart from its morphologically most similar lookalike, H. oceanica, and in proximity to the freshwater taxon H. scabra (Vězda) C. Keller et al. (Fig. 21). It differs from H. scabra, most markedly, in its regularly cracked-areolate thallus with a generally smooth surface of the infertile areoles in the centre of the thallus, a non-subgelatinous structure with the photobiont cells in an irregular arrangement, on average slightly smaller ascospores and the absence of green colour components in the pseudocortex. Occasionally occurring cracks in H. scabra (particularly in older herbarium specimens) are thinner and usually clustered in the vicinity of fruiting bodies, but not throughout the entire thallus as in H. alaskana (and H. oceanica). In addition, the fimbriate prothallus as observed in parts of one of the sequenced topotypes of H. alaskana (Fig. 20B) has never been seen in H. scabra or any other freshwater Hydropunctaria. These differences are based on comparison with sequenced specimens of H. scabra from Europe and two North American vouchers from Alaska and Montana (McCune 32162, 32163 [OSC]) for which ITS sequencing failed. Among the coastal species, a white prothallus is often seen in H. oceanica but it is never fimbriate in that species and only H. maura is known to occasionally develop a scarcely fimbriate prothallus.

Fig. 21. Majority-rule consensus tree of the genus Hydropunctaria (Eurotiomycetes) based on ITS and mtSSU loci, showing placement of the new species H. alaskana (bold) relative to previously known species. Values indicate percent bootstrap support. Further voucher information and GenBank Accession numbers are outlined in Table 1 and Supplementary Material Table S3 (available online).

Additional specimens examined

Canada: British Columbia: Vancouver Island, W of Sooke, Flea Beach, 48°22′54.84″N, 123°55′55.92″W, on N-facing rocks at top of seashore, in slight shade, 2015, A. Orange 22768 (NMW, specimen not seen).—USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Taylor Bay, 58.2549°N, 136.5675°W, 0–5 m, Fryday 10455, 10456 (MSC—topotypes); Petersburg, South Mitkof Island, Sumner Strait, seashore of sedimentary rocks, 56°33′10″N, 132°38′41″W, 0–5 m, 2012, Pérez-Ortega 2042, K. Dillman & Spribille (MA-Lich); ibid., Pérez-Ortega 2045, K. Dillman & Spribille (MA-Lich).

Lambiella aliphatica T. Sprib. & Resl sp. nov.

MycoBank No.: MB 830102

Similar to Lambiella globulosa but with fatty acids instead of stictic acid.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, 58.46233°N, 135.55349°W, 907 m, saxicolous on argillite in alpine talus, 14 July 2012, Spribille 38388 (MSC—holotype).

(Fig. 22)

Fig. 22. Lambiella aliphatica (holotype). A & B, habitus; C–E, SEM images of the surface of the apothecium, showing the umbo (C) and perforations in the surface of the umbo (D & E); F, section through apothecium; G, asci, in Lugol's solution; H, thallus cross-section. Scales: A = 1 mm; B = 0.2 mm; C = 100 μm; D = 20 μm; E, G & H = 10 μm; F = 50 μm.

Thallus crustose, forming patches to 3.5 cm across; areolate, the individual areoles 0.2–0.5 mm diam., bicoloured, with a dark grey edge and light grey centre; in section not stratified, differentiated cortex absent, but upper 10 μm of thallus pigmented grey; sterile hyphae non-amyloid. Photobiont chlorococcoid, roundish, cells 5–10 μm diam.

Ascomata apothecia, rounded to angular or even forming ‘U’ or ‘C’ shapes, (0.25–)0.3–0.5(–0.7) mm diam., single or forming groups of 2–3, or in tubercles to 0.8 mm diam., with a distinct umbo; disc deeply concave, black, matt to slightly lustrous, with a prominent black margin, the umbo with a sieve-like pattern visible in SEM (Fig. 22D & E). Excipulum 55–95 μm wide laterally, brown internally, outer 20–40 μm jet black (‘carbonized’), composed of hyphae to 4 μm diam., swelling to 6 μm in KOH, non-amyloid, excipulum but not epihymenium almost covered by bacterial colonies (stained in LCB). Hymenium 65–90 μm tall, pale yellow-brown to hyaline, strongly amyloid (I+ wine red, I+ blue after KOH), full of lipid bodies in lower half, in upper part pigmented brown-olivaceous; paraphyses branched and anastomosing, with kinks, separating in KOH, 1.8–2 μm wide medianly, to 4 μm wide apically, with internal terminal brown pigmentation. Hypothecium 70–90 μm tall, pale brown-yellow to brown, composed of heavily pigmented, thick-walled hyphae to 3 μm diam. Asci c. 42 × 15–18 μm, 8-spored; ascospores simple, ovoid or broadly ellipsoid, (6.5–)8.2–9.3(–12) × (4.5–)5.5–6.3(–7) μm (n = 28 over three specimens).

Conidiomata not observed.


All thallus spot tests negative; two unidentified fatty acids with R f classes A2 and A3, B4, C3 and C4 by TLC.


A reference to the presence of aliphatic (fatty) acids that characterize this species.


On argillite rock on alpine ridgeline and in talus.


Lambiella aliphatica (Fig. 22) is the first member of the genus to be described that contains primarily fatty acids in the thallus. The genus Lambiella Hertel was recently treated in some detail, as a split from Rimularia Nyl., in a phylogenetic study by Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015). DNA sequences from L. aliphatica (first published by Resl et al. Reference Resl, Fernández-Mendoza, Mayrhofer and Spribille2018) clearly place it in the L. impavida group as sister to a clade that includes L. globulosa (Coppins) M. Westb. & Resl and L. gyrizans (Nyl.) M. Westb. & Resl (Fig. 8). It is similar to L. globulosa, a species described from Scotland (Coppins & Kantvilas Reference Coppins and Kantvilas2001), especially on account of its near-globose ascospores, but it differs from that species and L. gyrizans in secondary metabolite chemistry as both possess thalli that are K+ yellow to orange and contain the stictic acid complex (Hertel & Rambold Reference Hertel and Rambold1990; Coppins & Kantvilas Reference Coppins and Kantvilas2001). It is so far known only from the type locality but is an inconspicuous species and is likely to occur elsewhere in the mountains around the Gulf of Alaska, though it may be restricted to the few regions with argillite or slightly basic rocks.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, 58.46233°N, 135.55349°W, 907 m, saxicolous on argillite in alpine talus, 2012, Spribille 38392 (sub Amygdalaria subdissentiens), 38395-B (MSC—topotypes).

Lecania hydrophobica T. Sprib. & Fryday sp. nov.

MycoBank No.: MB 830103

Similar to Lecania baeomma but richly fertile and lacking soredia/soralia.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Cross Sound, Taylor Bay at ‘campsite cove’, 58.25467°N, 136.56860°W, saxicolous on vertical shale outcrop W of camp, 9 m, 8 August 2012, Spribille 39680 & Fryday (MSC—holotype; NY—isotype).

(Fig. 23)

Fig. 23. Lecania hydrophobica (holotype). A & B, habitus; C & D, SEM images of thallus showing (C) film-like covering of medullary hyphae and (D) hyphal coating of thin (<100 nm in diam.) spaghetti-like (wax?) fibrils; E, section through apothecium; F–I, ascospores. Scales: A = 1 mm; B = 0.2 mm; C, F–I = 10 μm; D = 5 μm; E = 20 μm.

Thallus crustose, composed of small convex areoles, ±bullate, becoming almost granular, creamish white to ochre-yellowish, hydrophobic; individual areoles 0.15–0.45 mm diam., thallus scarcely stratified, internally with wefts of hyphae, these covered by a thin, biofilm-like cortex (Fig. 23C); sterile hyphae appearing ornamented or papillate at × 1000 magnification, this probably owing to thick layers of spaghetti-like filaments <100 nm in diam. throughout the internal thallus (Fig. 23D), that resemble certain plant waxes, for example in Barthlott et al. (Reference Barthlott, Neinhuis, Cutler, Ditsch, Meusel, Theisen and Wilhelmi1998: Fig. 19A). Photobiont chlorococcoid, cells 6–17 μm diam.

Ascomata apothecia, round, well-spaced, single, flat to convex, becoming tuberculate, (0.5–)0.75–0.87(–1.6) mm diam.; disc reddish brown to greyish brown to piebald, matt, apparently epruinose or with a light appearance of pruina, sometimes heavily pruinose; proper margin very prominent in youngest ascomata, the disc emerging through a ‘doughnut hole’, ‘pruinose’ on account of heavy layering of wax-like filaments, margin becoming thin, brown, giving a ‘lecanorine’ impression, eventually becoming excluded with age. Excipulum 60–100 μm wide laterally, composed of radiating thick-walled hyphae to 7 μm diam., not amyloid, full of crystals as viewed under polarized light; hymenium 60–120 μm tall, hyaline to hazy yellowish, IKI+ blue both before and after treatment with KOH; paraphyses strongly conglutinated, even after treatment with KOH, not widened apically; epihymenium full of POL+ crystals, these golden brown in transmitted light. Hypothecium hyaline or pale yellowish brown, 50–150 μm tall, full of grana, apparently full of old asci (Fig. 23E) as if apothecium builds upwards upon older hymenia; not amyloid, containing interspersed POL+ crystals, some of the hyphae thin, <2 μm diam., containing a very narrow cytoplasm. Asci Bacidia-type, 8-spored, difficult to visualize due to hamathecial conglutination, many containing yellowish grana, c. 50 × 10 μm; ascospores 1-septate, broadly ellipsoid, (10.5–)12.4–13.8(–18) × (3.5–)4.3–4.8(–5.5) μm (n = 35, three specimens used).


Thallus all spot tests negative, except faintly UV+ yellowish; atranorin and gangaleoidin detected by TLC.


Named for its highly hydrophobic properties, perhaps on account of its unusual wax-like filament structures.


Saxicolous on rain-sheltered underhangs of shale rocks near sea level.


This species was first reported for North America from British Columbia by Brodo (Reference Brodo1976) as Catillaria biformigera (Leight.) P. James ( = Tylothallia biformigera (Leight.) P. James & H. Kilias) and distributed by him as Lichenes Canadenses Exsiccati 93. In his notes on that exsiccatae, Brodo (Reference Brodo1976) discussed his collection in relation to Catillaria baeomma (Nyl.) Zahlbr. (=Lecania baeomma (Nyl.) P. James & J. R. Laundon) and concluded that, because the original material of that species examined by him lacked soralia, James (Reference James1965) was correct in including the species in the synonymy of C. biformigera. However, the current concept of L. baeomma is of a species with diffuse blue-grey soralia (Reese Næsborg Reference Næsborg R2008; Fletcher et al. Reference Fletcher, James, Purvis, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009a) and the situation is further complicated by the fact that James (Reference James1970) originally named this taxon Lecania rupicola (Nyl.) P. James and only later, without explanation, synonymized that name with the earlier L. baeomma (Hawksworth et al. Reference Hawksworth1980).

Our phylogeny confirmed the close relationship of our collection with L. baeomma (Fig. 10). To ascertain whether our species was synonymous with L. baeomma s. str., which according to Brodo (Reference Brodo1976) was also esorediate, we obtained from H-Nyl and BM the type material and other original collections of Lecanora baeomma Nyl. and its synonyms (viz. Lecanora caesia W. Johnson, L. caesiolepra Nyl., L. glaucocarnea Nyl. and Lecidea rupicola Nyl.), all of which, apart from L. caesia, were collected by Larbalestier from Connemara in the west of Ireland. Although all these collections were small, it was immediately apparent that L. caesia, L. caesiolepra and L. rupicola were synonymous with the current concept of L. baeomma as a species with diffuse, blue-grey soredia and were not conspecific with our species. Furthermore, close examination of the type collection of L. baeomma showed that it was also sorediate, but the soralia were small (c. 0.3 mm diam.) and white-coloured and easily overlooked. Clearly our species was also not conspecific with the type of L. baeomma. The apothecia of all four of these taxa had a thick, non-corticate thalline margin that persisted into mature apothecia, unlike that of our new species in which only young apothecia have a thalline margin and mature apothecia are apparently lecideine. This left L. glaucocarnea as the only possible species that might represent a previously published name for our species but, although the type collection lacked soredia, it was otherwise quite different, having a thick, areolate thallus and apothecia that lacked any sign of a thalline margin, even when young. To confirm these conclusions, we compared apothecial sections of our new species with those of representative specimens of L. baeomma, L. glaucocarnea and L. rupicola. Although all were clearly similar and all had inspersed crystals, they differed in the position, size and solubility of these crystals; specifically, whereas all sections had crystals in the subhymenium and exciple, the hymenium of our new species contained large crystals that did not dissolve in K. The hymenium of the other three taxa, by contrast, either lacked crystals or contained small crystals that dissolved in K.

Although not required to justify describing our collection as a new species, we were curious whether L. baeomma and L. rupicola were indeed synonyms. Two collections helped us decide this. The first was a collection from H labelled ‘Larbalestier's Lichen Herbarium (Exsiccatum britannicum) # 26 Lecanora baeomma’ that had diffuse blue soralia, indicating that Larbalestier thought L. rupicola and L. baeomma were conspecific. The second collection was a specimen in BM (BM000975337) that had both diffuse, blue-grey and small, white soralia on the same specimen, clearly indicating that only one species was involved. The only remaining issue was the identity of L. glaucocarnea, which appeared quite different from L. baeomma and possibly represents a distinct species, but the resolution of this was beyond the scope of the current study.

Reese Næsborg (Reference Næsborg R2008) indicated that ‘the proper taxonomic placement of Lecania baeomma remains uncertain’. Our phylogenetic reconstruction with only one locus (mtSSU) suggests, as did the original work of Reese Næsborg, a close relationship to Ramalina Ach. (Fig. 10); it is certainly not a Lecania in the sense of the type of that genus (L. fuscella (Schaer.) A. Massal.). Exploring the proper placement with more loci is not possible at this time.

Lecania hydrophobica was collected once in GLBA near the outer coast where it was abundant on sheltered rock underhangs. It is otherwise known from collections outside and to the south of GLBA by Mary Stensvold (née Muller) on southern Baranof Island and by Irwin Brodo from British Columbia.

Additional specimens examined

Canada: British Columbia: Haida Gwaii (= ‘Queen Charlotte Islands’), Graham Island 1967, Brodo 10165, Lichens Canadenses Exsiccati 93 (MSC, as Catillaria biformigera (Leight.) P. James).—USA: Alaska: Sitka Borough, Baranof Island, west coast, point of land W of Yamani Islets, N side at the mouth of Neker Bay, 56.67°N, 135.20°W, E-facing cliff of Sitka graywacke and adjacent area, 1992, M. C. Muller 5716 (TNFS-3117); ibid., narrow marine passageway connecting Redfish Bay and Big Branch Bay, 56.33°N, 134.86°W, rocky exposure just above high tide line, 1992, M. C. Muller 5721 (TNFS-3119).

Lecanora viridipruinosa M. Svenss. & T. Sprib. sp. nov.

MycoBank No.: MB 830104

Distinguished by the thallus of scattered, ±adnate areoles, the lecideine, greenish pruinose (C−, KC−) apothecia and by the thallus containing atranorin and zeorin.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, 58.46349°N, 135.55807°W, 920 m, alpine heath with rock outcrops, on exposed argillite rock, 22 July 2012, Svensson 2626, Fryday & Spribille (MSC—holotype)

(Fig. 24)

Fig. 24. A, Lecanora viridipruinosa, habitus of Spribille 38419; B, an undescribed Lecanora from the L. formosa group found at the type locality of L. viridipruinosa (Spribille 38425). Both specimens are represented in the phylogenetic tree in Fig. 10. Scales: A = 2 mm; B = 1 mm.

Thallus of dispersed, discrete, ±adnate areoles, 0.5–1.5 mm diam., dull white; hypothallus not apparent, but edges of areoles sometimes encrusted in a black mat of cyanobacteria. Photobiont chlorococcoid, cells 8–15 μm diam.

Apothecia semi-immersed to sessile, scattered on areoles, (0.35–)0.5–0.8(–1.5) mm diam., lecideine, ±round to somewhat irregular, at first with a flat, black disc and a thin, rarely flexuose margin concolorous with the disc, but soon becoming convex; disc usually with a faint, greenish pruina (C−, KOH+ dissolves, KC−, N−). Excipulum 80−120 μm wide, greenish black, without photobiont cells. Hymenium 45–70 μm high; epihymenium green-aeruginose, 5–15 μm high; paraphyses numerous, branched and anastomosing, 1.0–1.5 μm thick, not or slightly thickened (to 2(–4) μm) at the apex, with a green pigment cap. Hypothecium pale though sometimes discoloured orange-brown by mineral particles, occasionally with a small number of photobiont cells basally. Ascus Lecanora-type, 8-spored, broadly clavate, 30–50 × (9–)12–15 μm; ascospores simple, hyaline, thick-walled (to 1 μm), broadly ellipsoid, (7–)10(–14) × (4–)5(–7) μm (n = 22).

Conidiomata not observed.


Thallus C−, KOH+ yellow, PD−, UV−; apothecial section C−, KOH−, HNO3+ red; atranorin and zeorin by TLC.


A reference to the greenish pruina on the apothecial discs.


On argillite rocks in the alpine zone, so far known only from the type locality.


Lecanora viridipruinosa belongs to a group of black-fruited, saxicolous species that are probably closely related to each other and the genus Palicella Rodr. Flakus & Printzen (Fig. 10), but not to Lecanora Ach. s. str. They are still generally retained in Lecanora pending a systematic revision of lecanoroid genera. Several of these, such as L. viridipruinosa, contain atranorin and zeorin: Lecanora formosa (Bagl. & Carestia) Knoph & Leuckert has a more well-developed thallus of convex ± bullate areoles, greyish-pruinose apothecia and contains ± psoromic acid in addition to atranorin and zeorin (Edwards et al. Reference Edwards, Aptroot, Hawksworth, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009). Lecanora sulphurea (Hoffm.) Ach. has a more well-developed, yellowish thallus, larger (to 2.5 mm) apothecia with grey pruina and contains gangaleodin, α-collatolic acid and usnic acid in addition to atranorin and zeorin (Edwards et al. Reference Edwards, Aptroot, Hawksworth, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009). Lecanora griseofulva Elix & Øvstedal has epruinose apothecia and contains griseofulvin as a major substance in addition to atranorin and zeorin (Elix & Øvstedal Reference Elix and Øvstedal2004). Species with other chemistries might also belong here. Lecanora atromarginata (H. Magn.) Hertel & Rambold has a more well-developed, yellowish thallus with a prominent, pale prothallus, larger (to 2.5 mm), epruinose apothecia and contains usnic and stictic acids (Edwards et al. Reference Edwards, Aptroot, Hawksworth, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009). Lecanora atrosulphurea (Wahlenb.) Ach. has larger apothecia (to 2.5 mm) with both aeruginose and brown pigments and contains usnic acid, ±norstictic acid, and ±xanthones (Edwards et al. Reference Edwards, Aptroot, Hawksworth, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009). Lecanora caesiosulphurea Vain. has a sulphur yellow thallus, an HNO3 violet epihymenium, and bluish or lead-coloured pruina that react KC+ red (Thomson Reference Thomson1997). Lecanora marginata (Schaer.) Hertel & Rambold has a better developed, yellowish thallus (except whitish in subsp. elata (Schaer.) Clauzade & Cl. Roux), epruinose apothecia and contains atranorin and ±usnic acid (Edwards et al. Reference Edwards, Aptroot, Hawksworth, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009). Lecanora scrobiculata (Th. Fr.) Elix & Øvstedal has epruinose apothecia and contains psoromic acid in addition to atranorin (Elix & Øvstedal Reference Elix and Øvstedal2004). Lecanora viridiatra (Stehn.) Zahlbr. has a yellowish green thallus and contains usnic acid (Aptroot et al. Reference Aptroot, Gilbert, Hawksworth, Coppins, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009 as Lecidea luteoatra Nyl.). Lecidella viridans (Flot.) Körb. could be confused with L. viridipruinosa owing to the black, greenish pruinose apothecia and similar-sized ascospores, but it contains arthothelin, thiophanic acid and 4,5-dichloro-norlichexanthone (C+ orange, UV+ orange; Fletcher et al. Reference Fletcher, Purvis, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009b).

Material from GLBA includes two thallus forms, one with thick, roundish areoles (Fig. 24A) represented by Spribille 38419 and Fryday 10130, and another with a thin, non-areolate thallus (Fig. 24B) exemplified by Spribille 38425. These initially appeared to be extreme ends of thallus variation within a single population, and grew intermixed on the same mountain top, but DNA data, from one specimen each, suggest they are different species, both from the Lecanora formosa group. The only overlapping locus obtained, mtSSU, differs at 10 shared positions for the amplicons obtained for L. viridipruinosa (Fryday 10130, voucher T1806) and the additional species (Spribille 38425, voucher T1181), as well as L. viridipruinosa lacking a 10 bp insertion present in the latter. The second species contains atranorin but lacks zeorin, and may be undescribed. It is probably conspecific with a collection from the Yukon (Spribille 28362, GZU; T1019 in Fig. 10).

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, sharp point on eastern side of ridge, 58.46304°N, 135.55062°W, 936 m, saxicolous on argillite, 2012, Spribille 38419 (MSC); ibid., 58.46349°N, 135.55807°W, 920 m, alpine heath with rock outcrops, on exposed rock, 2012, Svensson 2603, Fryday & Spribille (MSC); ibid., Svensson 2604, Fryday & Spribille (MSC); ibid., Svensson 2638, Fryday, & Spribille (MSC); ibid., Spribille 38828 (MSC, sub Lecidea lapicida); ibid., Fryday 10130 (MSC, sub Halecania athallina).

Other specimens examined (Lecanora aff. viridipruinosa)

Canada: Yukon Territory: Mt Martin, Spribille 28362 (UPS).—USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, sharp point on eastern side of ridge, 58.46304°N, 135.55062°W, 936 m, saxicolous on argillite, 2012, Spribille 38425 (MSC).

Lecidea griseomarginata Fryday sp. nov.

MycoBank No.: MB 830109

Similar to Lecidea lapicida but separated from that species and all other species of the genus by the broad, grey proper margin.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Ptarmigan Creek, along shore N of creek, 58.8890°N, 136.8970°W, 0‒10 m, shoreline granitic rock, 15 July 2012, Fryday 9938, Spribille & Svensson (MSC—holotype).

(Fig. 25)

Fig. 25. Lecidea griseomarginata (Fryday 9937). A, habitus; B, apothecial section; C, section through hymenium, with asci and ascospores. Scales: A = 0.5 mm; B = 100 μm; C = 10 μm.

Thallus effuse, mostly immersed in the substratum, visible only as a black hypothallus between the rock granules and rarely as small patches of a thin grey, cracked-areolate thallus; medulla I+ blue. Photobiont chlorococcoid, cells 9‒15 μm diam.

Apothecia scattered, 0.6‒1.0 mm diam., lecideine, ±orbicular with a flat, black disc and a wide grey margin 0.5 mm across that is barely raised above the level of the disc. Excipulum internally hyaline with mottled brown patches composed of radiating hyphae with cells 4‒5 μm wide, outer 35‒50 μm similar but with additional blue-black (HNO3+ red) pigment; extending below the hypothecium where it is composed of narrower, randomly orientated hyphae, this structure sometimes extending into the lateral section. Hymenium 75‒80 μm high; epihymenium bright aeruginose, 10‒12 μm thick; paraphyses simple, 1.5‒2.0 μm thick, widening slightly at the apex up to 3 μm, with a blue-black (HNO3+ red) cap, septate; lax in KOH. Hypothecium brown, up to 175 μm thick at centre of apothecium narrowing to nothing at the excipulum. Ascus Lecidea-type, slightly clavate, 40‒50 × 12‒15 μm; ascospores simple hyaline, broadly ellipsoid, (10.5–)12.6 ± 1.3(–14.5) × (5.5–)6.5 ± 0.7(–8.0) μm, l/w ratio (1.6–)1.9 ± 0.2(–2.3), n = 18.

Conidiomata not observed.


The name refers to the wide, grey proper margin.


On recently deglaciated granitic rock at sea level.


Apothecial section C−, KOH+ yellow solution; stictic acid by TLC.


Known only from the type locality, where it occurs near the shore but near the end of a sheltered fjord and probably little affected by maritime influences. Lecidea griseomarginata belongs to the Lecidea lapicida group, which includes species of Lecidea s. str. with relatively broad ascospores (>5 μm) and a thallus with an amyloid medulla but lacking an epinecral layer (i.e. not atrobrunnea-type). Hertel (Reference Hertel1995) recognized three species in the group: L. ecrustacea (Anzi ex Arnold) Arnold, which lacks an epilithic thallus, and L. lapicida (Ach.) Ach. and L. swartzoidea Nyl. with an epilithic thallus. He separated the last two species by hypothecium colour; hyaline to pale brown in L. lapicida but dark brown in L. swartzoidea. He further recognized two varieties of L. lapicida: var. lapicida (stictic acid or no substances) and var. pantherina (DC.) Ach. (norstictic acid). However, two morphologically distinct entities exist with an epilithic thallus containing norstictic acid: a norstictic acid-containing variety of L. lapicida, and a distinct species with a thick, white thallus and ±immersed apothecia that is usually referred to as L. lactea Flörke ex Schaer. (e.g. Aptroot et al. Reference Aptroot, Gilbert, Hawksworth, Coppins, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009), sequences of which are published here (Table 1; from a KLGO specimen). The taxonomy of the group is highly confused and much in need of a thorough modern revision, along with the rest of Lecidea s. str.

Lecidea griseomarginata differs from all the above-mentioned taxa, and other species of Lecidea s. str., most noticeably in its thick, grey proper margin (Fig. 25A). The lack of an epilithic thallus further distinguishes it from all the above species except L. ecrustacea, from which it differs in its distinctive exciple structure and by lacking norstictic acid. The new species is just one of the distinct morphotypes in the L. lapicida group that we are aware of in the North American Arctic.

We obtained fungal DNA sequences of Lecidea griseomarginata from three loci, namely 28S, mtSSU and Mcm7. However, so few other Lecidea species have published sequences from these loci that building a tree from the available data would be uninformative. We publish the sequences here for future reference (Table 1).

Additional specimen examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Ptarmigan Creek, along shore N of creek, 58.8890°N, 136.8970°W, 0‒10 m, shoreline granitic rock, 2012, Fryday 9937, Spribille & Svensson (MSC—topotype; sub Rhizocarpon lecanorinum).

Lecidea streveleri T. Sprib. sp. nov.

MycoBank No.: MB 830110

Thallus whitish with dark chocolate brown, flattened apothecia with ascospores 8–12(–18) × 3–4(–5) μm. Differing from Lecidea albofuscescens Nyl. and L. lesdainii Zahlbr. in the narrower ascospores, lack of ascospore ornamentation, flattened apothecia and thin, filmy thallus.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, steep slopes above unnamed lake in basin on west side of Dundas Bay, 58.34713°N, 136.39937°W, 180 m, corticolous on Alnus along mountain stream, 25 July 2012, Spribille 39030 (US—holotype; MSC—isotype).

(Figs 26 & 27)

Fig. 26. Lecidea streveleri (and putatively related species). A & B, Lecidea streveleri (holotype); C, habitus, Lecidea albofuscescens, (holotype, H-Nyl-20725); D, habitus, Lecidea lesdainii (holotype of Helocarpon corticola, LI-271019); E–G, SEM images of ascospores of (E) L. streveleri (from holotype), (F) L. lesdainii (from holotype of Helocarpon corticola) and (G) L. albofuscescens (from Spribille 36527). Scales: A = 1 mm; B = 200 μm; C & D = 2 mm; E & G = 2 μm; F = 5 μm.

Fig. 27. Lecidea streveleri (anatomical details of apothecium). A, section of apothecium (Spribille 39197); B, z-stack of apothecial section in lactophenol cotton blue, showing putative bacteria in epihymenium; white line indicates break between vertical and perpendicular surfaces (Spribille 39707); C & D, hypothecium in brightfield (C) and polarized (D) light showing upwards contortion and integration of outermost layers of Alnus periderm into the apothecium (arrowed) (Spribille 39707); E–G, asci, in Lugol's solution (E & F, holotype; G, Brodo 11042 [GZU]); H, ascospores (Spribille 39197). Scales: A = 100 μm; B, E–H = 10 μm; C & D = 50 μm.

Thallus smooth, rimose, not clearly areolate but algal cells aggregated in clumps beneath the thallus surface, giving a mottled appearance when moist; thin, up to 100 μm in section, greyish white to greenish white; forming patches 0.5–4 cm diam.; stratification weak, but cortical polysaccharide layer 10–15 μm thick. Photobiont chlorococcoid, cells 7–9 μm diam.

Ascomata apothecia, round, (0.25–)0.5–0.67(–0.9) mm, single or in small groups, weakly convex or appearing nearly flattened, sometimes ±tuberculate, medium brown, matt to weakly shiny, strictly epruinose; proper margin prominent, not excluded when old, shiny, black to brown or rarely pigment-deficient, swelling and translucent when wet. Exciple 40–60 μm wide laterally, 30–60 μm wide basally, streaked reddish to medium brown internally, lacking visible crystals in polarized light, I−, composed of radiating hyphae with apparently papillate walls, hyphae embedded in a bacteria-containing gelatinous layer that can extend for 6–10 μm beyond the ends of the hyphal tips. Hymenium pale brown, brownish streaked to almost hyaline, 48–60 μm tall, I+ deep blue, sometimes with apparent lipid accumulations in lower hymenium; epihymenium not or weakly developed, structures similar to bacilli visible in LCB staining, but gelatinous, epipsammoid layer and crystals lacking (POL−) (Fig. 27B), pigment accumulations brownish, KOH−; paraphyses simple or weakly branched, 4–5 μm diam. apically, with wall to 1.5 μm, mostly not capitate although a few capitate hyphae seen (belonging to L. streveleri?). Hypothecium dark reddish brown, 110–200(–250) μm tall, I−, lacking visible crystals in polarized light, composed of strikingly thick-walled hyphae 7–9 μm diam., with lumen c. 1 μm diam., anchored directly in the substrate phloem (Figs 27C & D). Asci clavate (Figs 27E–G), Bacidia-type, 34–35 × 6–8 μm, with 8 ascospores; ascospores narrowly ellipsoid, (7.0–)9.5–10.5(–13) × (2.7–)3.0–3.5(–4.0) μm (n = 52), not ornamented (Figs 26E & 27H).


Thallus all spot tests negative; no substances detected by TLC.


Named in honour of Dr Gregory P. Streveler, an extraordinary naturalist and polymath, and author of numerous scientific papers, who has dedicated much of his life to understanding the natural history of Glacier Bay.


On bark of Alnus and Populus balsamifera. In addition to its occurrence in Glacier Bay, an exsiccatae from Haida Gwaii, British Columbia, also from Alnus, has been widely distributed under the name Lecidea albofuscescens (Brodo Reference Brodo1971).


Lecidea streveleri is similar to L. albofuscescens Nyl., a widespread species of boreal-montane forests of the Northern Hemisphere, and L. lesdainii Zahlbr., a species described from Macaronesia and disjunct along the North American Pacific Coast (Breuss Reference Breuss1990, Reference Breuss2001). It differs from both species, however, in its consistently narrower ascospores (3.3 ± 0.36 μm (n = 52) in L. streveleri vs 5.0 ± 0.64 μm (n = 71) in L. albofuscescens, P = <0.001; ascospores are even wider in L. lesdainii, see Breuss (Reference Breuss1990)). Lecidea streveleri can further be distinguished from both of these species by the lack of ascospore ornamentation (Fig. 26E); in L. albofuscescens and L. lesdainii the ascospores are almost always clearly warted (compare Figs 27F & G), a feature that can usually also be observed as an irregular ascospore surface in microscopic water mounts. In addition, L. streveleri forms smooth, rimose, whitish thalli, whereas L. albofuscescens and L. lesdainii both form minutely granular to granular-areolate thalli.

Lecidea streveleri is superficially similar to other crustose lichens that possess apothecia with dark, brownish hypothecia and one-celled ascospores. One group of species that it could, in theory, be confused with is the so-called ‘Lecidea plebeja group’ (Palice et al. Reference Palice, Malíček, Peksa and Vondrák2018), likely including the eastern North American Biatora peliaspis Tuck. However, members of this group possess apothecial discs with epithecial crystals that are soluble in KOH, giving the apothecial disc a grainy appearance, unlike in L. streveleri and other members of the L. albofuscescens group which lack such crystals and possess glossy apothecia. Probably also related to both L. albofuscescens and the ‘L. plebeja group’ are members of the ‘Lecidea malmeana group’, also discussed by Palice et al. (Reference Palice, Malíček, Peksa and Vondrák2018), which differ in possessing polysporous asci (in low multiples of eight, ‘plusiosporic’ sensu Palice et al. (Reference Palice, Malíček, Peksa and Vondrák2018)), and thus are less likely to be confused with L. streveleri.

Attempts to amplify DNA from L. streveleri for this study were unfortunately not successful. However, we were able to obtain DNA sequences from L. albofuscescens, including three specimens from GLBA, albeit from only two loci. Analyzed within the broader context of the order Lecanorales, these sequences resolve within the family Malmideaceae, in the vicinity of genera such as Cheiromycina B. Sutton, Malmidea Kalb et al., Puttea S. Stenroos & Huhtinen, and Savoronala Ertz et al. (Fig. 10), as well as a specimen of Lecidea malmeana from GLBA. However, the genus Kalbionora, which has been postulated to belong to Malmideaceae (Sodamuk et al. Reference Sodamuk, Boonpragob, Mongkolsuk, Tehler, Leavitt and Lumbsch2017), did not cluster with this family in our phylogenetic analyses. Many more lichen-forming genera and species need to be sampled to paint a more complete picture of phylogenetic relationships in Malmideaceae. Several generic names are thus in contention and, given the poor support for the ingroup phylogeny and the poor taxon sampling for our phylogenetic tree, we refrain from describing a new genus for the L. albofuscescens group at this time.

Exsiccatae (L. streveleri)

Canada: British Columbia: Queen Charlotte Islands [= Haida Gwaii], Moresby Island, Takakia Lake, 1967, Brodo 11042, Lichenes Canadenses Exsiccati 38 (GZU, as L. albofuscescens).

Additional specimens examined (L. streveleri)

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Geikie Inlet, Shag Cove, 58°37.924′N, 136°19.715′W, corticolous on Alnus just above sea level, 2011, Spribille 36400 (MSC); ibid., Bartlett Cove, 58.44557°N, 135.89712°W, just above sea level, corticolous on Populus balsamifera, 2012, Spribille 38244 (MSC); ibid., East Arm of Glacier Bay, mouth of unnamed creek E of Muir Point, 58.83642°N, 136.05313°W, c. 8 m, corticolous on Alnus, 2012, Spribille 39197 (MSC); ibid., Cross Sound, Taylor Bay at ‘campsite cove’, 58.25467°N, 136.56860°W, 4 m, corticolous on Alnus, 2012, Spribille 39707 (MSC).

Comparison material examined (L. albofuscescens; see also GLBA vouchers cited in ‘Catalogue of All Named Taxa Found’ (below))

Austria: Styria: Mühlbacher 230 (GZU); ibid., 24 x 1962, Schauer s. n. (GZU).—Canada: British Columbia: Queen Charlotte Islands, Brodo 9723 (Lich. Canadenses Exs. 127, GZU).—Finland: Evois, ad corticem Abies, 1866, Norrlin s. n. (H-NYL 20725—holotype).—Russia: Khabarovskiy Krai: 33.7 km (air line) due W of Lazarev, up small side road in Sredniy Khrebet Mountains, between Studeniy and Zvuchnaya streams, 52°13.451′N, 141°00.428′E, corticolous on Abies nephrolepis, 56 m, 2009, Spribille 30886 (GZU); ibid., Sredniy Khrebet Mountains, Polоsataya Mountain, 45.5 km (air line) NW of Lazarev, between Pravaya Tumi River and Krutoberezniy stream, 52°22.779′N, 140°53.503′E, corticolous on Abies nephrolepis trunk, 212 m, 2009, Spribille 31024 (GZU); ibid., De Kastri-Komsomolsk route, 30 km (air line) WSW of De Kastri, near watershed divide between Chistiy and Khanda River watersheds, 51°23.260′N, 140°21.758′E, corticolous on Picea jezoensis, 135 m, 2009, Spribille 31147 (GZU).

Comparison material examined (L. lesdainii)

Spain: Tenerife: Macizo de Teno, laurisilva oberhalb von Los Silos an der Forststraße von Erjos del Tanque nach El Palmar (Monte del Agua), 900–1000 m, auf Stämmen von Laurus, 1984, O. Breuss 3680 (LI—holotype of Helocarpon corticola Breuss).

Miriquidica gyrizans Fryday sp. nov.

MycoBank No.: MB 830111

Distinguished from all other species of the genus by the gyrose apothecia. Further characterized by the subsquamulose thallus and the dark hypothecium that reacts KOH+ magenta.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Dundas Bay, unnamed mountain W of bay, 58.3421°N, 136.4015°W, 460 m, upper surface of large, flat granitic boulder on alpine ridge, 25 July 2012, Fryday 10175, Spribille & Svensson (MSC—holotype).

(Fig. 28)

Thallus effuse, composed of dispersed or ±contiguous areoles, 0.2‒1.0 mm across, pale brown but with an irregular layer of dead fungal cells giving them a grey appearance, areoles always associated with cyanobacteria (Gloeocapsa; cells 7.5‒12.5 μm diam., red (KOH+ purple), single or in groups of 2–4) either arising from a cyanobacterial mat, or on the surface or within the thallus; smaller areoles ±circular with hyaline to red-brown ±unpigmented area, larger areoles becoming divided into subareoles and developing a semi-effigurate margin; upper cortex absent, but upper 10 μm with a pale brown pigment; basal layer of thallus dark brown (KOH+ magenta); hypothallus lacking but space between areoles often filled with red-brown covering of Gloeocapsa; medulla I−. Photobiont chlorococcoid, cells 5‒9 μm diam.

Fig. 28. Miriquidica gyrizans (holotype). A & B, habitus; C, section through apothecium; D, ascospores in KOH; E, paraphyses in KOH. Scales: A = 1 mm; B = 0.5 mm; C = 50 μm; D & E = 10 μm.

Apothecia frequent, scattered, lecideine, black, 0.4‒0.6 mm diam.; proper margin thick, raised, 0.05 mm wide; disc black with a central umbo when young becoming ±completely gyrose when mature. Excipulum dark brown, composed of radiating hyphae 5 μm wide with cortical cells 7‒8 μm wide; KOH ±magenta (Atra-red). Hymenium 65‒75 μm tall; epihymenium dilute brown, 10‒15 μm tall; paraphyses simple with occasional branching, 1.5‒2.0 μm wide, widening slightly (3‒4 μm) at the apex, upper 5‒10 μm with a brown pigment. Hypothecium dark brown to red (KOH+ magenta; Atra-red), composed of irregularly orientated hyphae 5 μm wide. Asci indistinct Lecanora-type, slightly clavate, 50‒60 × 12‒15 μm; ascospores simple, hyaline, becoming pigmented when overmature, broadly ellipsoid with rounded apices, thick walled, (8.5–)10.6 ± 1.6(–14.5) × (4.5–)5.4 ± 0.4(–6.5) μm, l/w ratio (1.57–)2.1 ± 0.9(–2.4), n = 14.

Conidiomata not observed


Thallus KOH−, C−, PD−; miriquidic acid by TLC.


Named for the gyrose apothecia.


Most frequent on the upper (flat) surfaces of large granitic boulders in snowy subalpine or alpine areas near the timberline but also from the side of a boulder at a lower altitude.


Miriquidica gyrizans is unique within the genus for its gyroid (umbonate) ascomata. The subsquamulose thallus is also unusual, being previously known in the genus only from two species from New Zealand (Fryday Reference Fryday2008b). Coincidentally, these two species are also associated with cyanobacteria. Miriquidica gyrizans is currently known from three areas, the Dundas Bay area of GLBA, White Pass in Klondike Gold Rush National Historical Park and two collections from Kenai Fjords National Park. An ITS rDNA sequence of a specimen from the type locality (Spribille 38993; voucher T1196) places it in Miriquidica (Fig. 10), but not enough taxa of that group have been sampled to determine which species it is most closely related to. The Miriquidica griseoatra group was treated by Hafellner et al. (Reference Hafellner, Obermayer and Tretiach2014) but the genus as a whole has not been recently revised.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Dundas Bay, 58.350567°N, 136.399067°W, 150 m, side of granitic rock by tarn in muskeg, 2012, Fryday 10153, Spribille & Svensson (MSC); ibid., unnamed mountain W of bay, 58.3422°N, 136.4002°W, 435 m, rock outcrops on alpine ridge, 2012, Fryday 10164, Spribille & Svensson (MSC); ibid., 58.3421°N, 136.4015°W, 460 m, upper surface of large, flat granitic boulder on alpine ridge, 2012, Fryday 10173, Spribille & Svensson (MSC, topotype); ibid., eastern approach to mountain top between Dundas Bay and Fern Bay, along ridgetop, 58.34212°N, 136.40008°W, 465 m, saxicolous on large boulder in snowbed, 2012, Spribille 38993 (MSC); ibid., 58°20.527′N, 136°24.006′W, 2012, Svensson 2696 (MSC); Klondike Gold Rush National Historical Park, White Pass, 58.3421°N, 136.4015°W, 460 m, top of boulder next to snowbed, 2008, Spribille 26813, Pérez-Ortega & Tønsberg (KLGO, sub Lecanora leptacina); ibid., White Pass, Pérez-Ortega s. n. (KLGO 53923); Kenai Peninsula Borough, Kenai Fjords National Park, near Harding Icefield Trail, ridge above Exit Glacier, 60.1828°N, 149.6713°W, on stones, flat area with late snow, 770 m, 2015, McCune 36369 (hb. McCune); ibid., McArthur Ridge near National Park Service weather station, granitic ridgetop with alpine tundra and Tsuga mertensiana krummholz, 59.4726°N, 150.337°W, 386 m, 2016, McCune 36989, 36990b (hb. McCune).

Niesslia peltigerae Pérez-Ort. sp. nov.

MycoBank No.: MB 830112

Similar to Niesslia cladoniicola but ascospores slightly smaller (7–8 × 2.5–3) and different host (Peltigera kristinssonii) and lifestyle (parasitic vs saprotrophic).

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, muskeg and forest below Excursion Ridge, 58.45527°N, 135.57344°W, 460 m, parasitic on Peltigera kristinssonii growing epiphytically on Tsuga mertensiana, snowbed habitat, 1 August 2012, Spribille 39341 (MSC—holotype).

(Fig. 29)

Fig. 29. Niesslia peltigerae (holotype). A, ascomata, dry state collapsed; B, detail of ostiolum; C, periphyses; D, detail of perithecial wall; E, young asci; F, mature ascus; G, detail of a perithecial seta; H & I, ascospores (all except A in water, using DIC). Scales: A = 200 μm; B = 25 μm; C–F = 10 μm; G = 20 μm; H & I = 2 μm.

Ascomata perithecioid, sessile on the upper surface of the host thallus, 170–240 μm diam., richly setose, densely aggregated, black, subspherical, collapsed (concave) when dry, with a central ostiole. Exciple dark brown internal layer composed of elongated and flattened cells. Setae acute, with a wide base, simple, usually with one septum, dark brown, 45–95 μm long, basally to 12 μm wide (c. 5 μm at the median part). Periphyses formed around the ostiole, hyaline, to 12 μm in length. Paraphyses not observed in mature ascomata. Asci clavate, with a short ‘foot’ at the base and a truncate apex, unitunicate, 8-spored, I−, KI− (but epiplasm orange), 23–30 × 5–6 um; ascospores biseriate in asci, hyaline, elongated ellipsoid to fusiform, without perispore, with obtuse ends, 1-septate, 6–8 × 2.5–3(–4) μm (n = 20), usually with one or two guttules per cell.


Named for its occurrence on a species of Peltigera.


Parasitic, bleaching host thallus, on Peltigera kristinssonii Vitik. in Tsuga mertensiana (Bong.) Carrière parkland near the timberline.


The genus Niesslia Auersw. contains a number of lichenicolous species (Etayo et al. Reference Etayo, Flakus and Kukwa2013), many of them growing on members of the Peltigerales (Etayo & Sancho Reference Etayo and Sancho2008; Etayo Reference Etayo2017). Niesslia peltigericola (D. Hawksw.) Etayo, described originally growing on Peltigera leucophlebia (Nyl.) Gyeln. (Hawksworth Reference Hawksworth, James and Coppins1980), is known to occur on several Peltigera species (Puolasmaa et al. Reference Puolasmaa, Toivanen, Marsh, Huhtinen and Stenroos2012). This species differs from N. peltigerae by its smaller ascomata (up to 90 μm diam.), longer asci (40–58 μm), larger ascospores (10–15 × 4–4.5 μm) (Hawksworth Reference Hawksworth1980; Puolasmaa et al. Reference Puolasmaa, Toivanen, Marsh, Huhtinen and Stenroos2012) and different lifestyle (saprotrophic or parasymbiont). Morphologically, the most similar species to N. peltigerae within the genus is N. cladoniicola D. Hawksw. & W. Gams. This species has slightly larger and narrower ascospores ((6.5‒)8.3‒10.3(‒13.1) × (1.6‒)2.2‒2.6(‒3.0) μm, but see Hawksworth (Reference Hawksworth1975)) and smaller ascomata ((50‒)100‒130(‒150) μm; Zhurbenko & Pino-Bodas Reference Zhurbenko and Pino-Bodas2017) than N. peltigerae and does not cause visible damage to its host (Cladonia species). Niesslia tatjanae (S. Y. Kondr.) Etayo, growing on Pseudocyphellaria species and reported from Tasmania and Tierra del Fuego (Kondratyuk Reference Kondratyuk1996; Etayo & Sancho Reference Etayo and Sancho2008), also shows some similarities with N. peltigerae but its perithecia have shorter setae (to 40 μm long) and ascospores that are slightly larger (8‒10.5 × 2‒2.5 μm).

Ochrolechia cooperi T. Sprib. sp. nov.

MycoBank No.: MB 830113

An Ochrolechia species with a smooth, creamy white thallus with numerous coralloid isidiate thallus outgrowths; apothecia apparently rare, seen in only one specimen, but differing from apothecia in Ochrolechia yasudae Vain. by lacking obvious pruina on the disc.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, NE of Gustavus, Falls Creek, ‘Yellowlegs Savanna’ muskeg, 58.44742°N, 135.60593°W, 245 m, on a conifer log still retaining its bark, in a muskeg ‘tree island’, 21 July 2012, Spribille 38730 (MSC—holotype; NY—isotype).

(Fig. 30)

Fig. 30. Ochrolechia cooperi (holotype). A, habitus (composite image); B, detail of coralloid isidia; C, section of apothecium. Scales: A = 1 mm; B = 200 μm; C = 100 μm.

Thallus crustose, rimose, to 5–7 cm diam., to 1.2 mm thick, creamish white to cream, bearing scattered coralloid isidia, sometimes large parts of the thallus lacking isidia; isidia (Fig. 30B) 0.1–0.3(–0.5) mm diam., pinkish creamish brown to latte brown, darker than surrounding thallus starting out as globose outgrowths, branching upwards; prothallus not observed. Photobiont chlorococcoid, cells 10–15 μm diam., with a hyaline wall c. 1 μm wide.

Ascomata apothecia (Fig. 30C), round, 0.8–2.4 mm diam., observed in only one specimen, becoming hollowed out (abortive?); thalline margin, robust, whitish; proper margin c. 50 μm thick; amphithecium in section 190 μm wide, basally 310 μm, with algal cells occurring in small, discontinuous patches. Hymenium in best-developed specimens to 200 μm tall, hyaline, IKI+ hazy aqua blue, covered in crystals above, these KOH+ light yellow, dissipating; paraphyses thin, to 1.8 μm wide medianly, loosening in KOH. Hypothecium to 90 μm thick, hazy creamish. Asci c. 155 × 58 μm, with wall swelling to 20 μm thick in KOH; ascospores not seen.

Conidiomata not seen.


Thallus C+ red, KOH−, PD−; amphithecium cortex and epihymenium strongly C+ red; amphithecium medulla and hymenium slowly C+ red; gyrophoric acid, ±lecanoric acid by TLC.


Named to mark a century since the pioneering field trips to Glacier Bay of William Skinner Cooper (1884–1978), a prominent American ecologist whose studies on plant succession in Glacier Bay and subsequent political lobbying efforts were influential in the establishment of Glacier Bay as a National Monument in 1925.


On wood or bark of conifers, at low elevations from seashores to c. 250 m. Currently known only from southern Alaska.


The North American epiphytic species of Ochrolechia were monographed by Brodo (Reference Brodo1991). Ochrolechia cooperi is readily distinguished from other species of Ochrolechia by its elaborate, coarse coralloid isidia that arise irregularly over the thallus. Brodo (Reference Brodo1991) cites only one other North American species of Ochrolechia that develops coarse isidia, O. yasudae. Ochrolechia cooperi differs from O. yasudae (and the similar European species O. subviridis (Høeg) Erichs.) in the overall gross morphology, in which isidia are localized in coarse, shrub-like patches on an otherwise smooth thallus (compared with continuous cover of fine isidia in O. yasudae and O. subviridis), in the lack of an arachnoid hypothallus and in the epruinose apothecial discs (pruinose in the other species). Although the colour and habitus vaguely recall O. frigida (Sw.) Lynge, that species produces, at most, spines (in the var. pterulina Nyl.) but is not known to develop complex dendroid/coralloid isidia.

In recent years taxonomists have been conservative in describing new species of Ochrolechia, and in the absence of detailed molecular studies a large range of forms have been attributed to variability in two species, O. androgyna (Hoffm.) Arnold (Tønsberg Reference Tønsberg1992; Kukwa Reference Kukwa2011) and O. frigida (Kukwa Reference Kukwa2011). A DNA sequence set for O. cooperi was published by Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015, as ‘Ochrolechia sp. Spribille 38907’) in the context of a wider, eight-locus sampling of the subclass Ostropomycetidae. We combined all available, reliable, published, multilocus sequence data for Ochrolechia with a subset of the Resl et al. taxon sample to determine the broader affinities of O. cooperi (Fig. 6). Ochrolechia, in this sample, forms four main clades: 1) with O. africana Vain., 2) with alectoronic acid-containing species (see note under the section ‘Ochrolechia xanthostoma (Sommerf.) K. Schmitz & Lumbsch and similar taxa’ (below)), 3) with O. trochophora (Vain.) Oshio, and 4) with O. frigida, O. androgyna and other species. We recover O. cooperi in the third clade, suggesting that a close relationship to O. frigida can be ruled out.

Ochrolechia cooperi is so far known from GLBA, from the Chugach National Forest in south-central Alaska (two collections), from one site in Kenai Fjords National Park and from Mitkof Island (see specimen list below). Within GLBA it has been found only in areas not glaciated during the Little Ice Age, in the Falls Creek lowlands and Taylor Bay areas.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, just outside Glacier Bay National Park, near upper Falls Creek hydro plant, just E of Falls Creek, Tsuga bark, 2012, Spribille 38907 (GZU; DNA voucher P150); Glacier Bay National Park, Cross Sound, Taylor Bay at ‘campsite cove’, 58.25467°N, 136.56860°W, 9 m, lignicolous on side of suspended log on high beach, 2012, Spribille 39501, Fryday 10381 (MSC); ibid., 58.24684°N, 136.56791°W, 10 m, corticolous on Tsuga heterophylla on coastal headland, 2012, Spribille 39658 & Fryday (MSC); ibid., 58.25665°N, 136.57160°W, 20 m, muskeg, corticolous (Pinus contorta), 2012, Fryday 10424 (MSC); Valdez-Cordova Census Area, Chugach National Forest, Plot CH06-Plut 71, packet no. 16, Turnagain, Tsuga mertensiana branch, 20 ix 2011, K. Dillman s. n. (ALA); ibid., Plot CHUGACH 74, packet no. 16, Tsuga mertensiana bole, 20 viii 2012, K. Dillman s. n. (ALA); Kenai Peninsula Borough, Kenai Fjords National Park, peninsula into Three Hole Bay off Aialik Bay, 59.76306°N, 149.60042°W, 70–80 m, corticolous on trunk of Tsuga mertensiana at edge of muskeg, 2015, Tønsberg 45512 (ALA, BG); ibid., near pond at N end of Three Hole Bay off Aialik Bay, 59.78701°N, 149.60402°W, 0–10 m, corticolous on trunk of Tsuga mertensiana, 2015, Tønsberg 45528a (ALA, BG); ibid., corticolous at base of trunk of Picea sitchensis, 2015, Tønsberg 45534 (ALA, BG); N shore of Mitkof Island, Frederick Sound, 4 km SE of Petersburg, NW of Frederick Point, 56°47.939′N, 132°53.056′W, lignicolous on seashore driftwood, 2012, Spribille 37696, Dillman, Pérez-Ortega & Wagner (hb. Spribille).

Placynthium glaciale Fryday & T. Sprib. sp. nov.

MycoBank No.: MB 830114

Superficially similar to Placynthium nigrum but with a lighter-coloured, olivaceous thallus and cuboid, submuriform ascospores.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, upper end of Muir Inlet, 59.08015°N, 136.33685°W, 50 m, saxicolous on partially buried cobbles in young post-glacial soils (exposed c. 30 yr BP), dense argillite-like boulder, 28 August 2014, Spribille 40765 & Fryday (MSC—holotype and one isotype; NY—two isotypes).

(Fig. 31)

Fig. 31. Placynthium glaciale (holotype). A, thalli colonizing recently deglaciated rocks (c. 30 cm diam.) at type locality; B & D, habitus; C, detail of apothecium and branches with SEM; E, section of apothecium; F, asci and paraphyses, in Lugol's solution; G–J, ascospores, in K. Scales: B = 1 mm; C & D = 200 μm; E = 100 μm; F–J = 10 μm (scale bar the same for G–J).

Thallus crustose, rimose, olivaceous brown, to 3.5 cm diam. and 0.2 mm thick, covered in crowded, opuntioid, dactyloid lobes; individual lobes (30–)70–150 μm diam., in section weakly stratified, with continuous cellular (paraplectenchymatous) cortex, individual cells roundish, 4–6 μm diam.; hypothallus apparently absent or present, bluish, KOH+ mauve, not extending beyond edge of main thallus. Photobiont an unknown cyanobacterium, individual cells roundish, 6–7 μm diam., sometimes forming chains, easily dislodged from thallus and floating free in microscopic section.

Ascomata apothecia, round, scattered, (0.3–)0.48–0.58(–0.8) mm diam., the disc flat to concave or weakly convex, dark brown to jet black, matt; proper margin prominent and remaining so with age, black, lustrous, sometimes slightly incurved and covering the disc. Excipulum c. 50 μm wide laterally, 50–90 μm wide basally, purplish internally, blue-black towards the outer edge, the pigments KOH−, non-amyloid; composed of radiating hyphae c. 5 μm thick in the middle part of the excipulum, with terminal cells to 10 μm wide, with wide lumina and a wall 1–1.5 μm thick. Hymenium 65–90 μm tall, streaked blue-black, I+ blue before treatment with KOH, pigments more intense towards the top; paraphyses septate, mostly straight, weakly branched and anastomosing or with short ‘thumb’ branches, 1.8–2.0 μm wide medianly, swelling to 3 μm in KOH. Hypothecium to 230 μm thick, of which the top 50–60 μm differentiated into a hyaline to pale brown subhymenium and the lower part is pale brown, composed of tangled hyphae to 2.5 μm wide, I+ blue after KOH. Asci (Fig. 31F) 53–60 × 11–16 μm, with 5–7 ascospores developing to maturity, asci dehiscing when ascospores become submuriform, no asci with a full complement of 8 ascospores observed; ascospores (Fig. 31G–J) round to square or cuboid, frequently isodiametrical, submuriform, beginning simple and divided first medianly, then transversely, (6–)8.4–10.8(–13) × (5.5–)6.4–7.1(–9) μm, l/w ratio 1.4 ± 0.3 (n = 45, five samples used).

Conidiomata not observed.


All spot tests negative.


Named for its close association with glacial forelands.


On siliceous rock (mostly soil-embedded small boulders, 20–40 cm diam.) in recently deglaciated forelands.


The genus Placynthium is still poorly known in North America, having last been revised over 50 years ago (Henssen Reference Henssen1963). However, no species of Placynthium has been reported to have muriform ascospores. We obtained DNA from two specimens (Table 1) and a phylogenetic analysis (Fig. 9) shows P. glaciale to be included in a broader clade that contains the P. asperellum (Ach.) Trevis. group, P. subradiatum (Nyl.) Arnold and two accessions that are treated here as Placynthium sp. S38458 (isolates T1310 and T1304, see ‘Known Unknowns’ section).

So far P. glaciale is known only from the forelands of Muir Glacier in the upper East Arm of Glacier Bay, which would have been first exposed by the retreating Muir Glacier c. 30 yr BP, and a marble rock face on the shore of the terminal lake of Patterson Glacier (Alaska, Petersburg Borough; see below) exposed at a similar time.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, East Arm of Glacier Bay, upper end of Muir Inlet, north shore, lower mid slope, 59°05.034′N, 136°20.179′W, saxicolous on 30 yr-old surfaces, 115 m, 2011, Spribille 36576 (sterile), 36580, 36581 (MSC); ibid., 59°04.953′N, 136°20.229′W, 30 m, siliceous rock and pebbles, 2011, Fryday 9786, 9791 (MSC); Petersburg Borough, Patterson Glacier, 56.939363°N, 132.654869°W, 105 m, marble rock face on the shore of the terminal lake, 2015, Fryday 11175 (MSC).

Porpidia seakensis Fryday sp. nov.

MycoBank No.: MB 830115

Separated from other species of the genus by the combination of a thin to endolithic thallus, strongly constricted apothecia with a brown pruinose disc, large ascospores and a macrocarpa-type exciple.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Bartlett Cove, road between Park HQ and dock, 58.4569°N, 135.8628°W, 40‒50 m, granitic rock in woodland, 14 August 2012, Fryday 10485 (MSC—holotype).

(Fig. 32)

Fig. 32. Porpidia seakensis. A–C, habitus (A & B, Fryday 9626; C, holotype); D & F, section through apothecium under brightfield (D) and polarized (F) light; E, asci, ascospores and paraphyses, in KOH (D–F from holotype). Scales: A = 0.5 mm; B = 0.2 mm; C = c. 0.2 mm; D & F = 50 μm; E = 10 μm.

Thallus completely endolithic on granite but present as a thin effuse white stain when on schist and becoming slightly areolate in depressions; medulla I−. Photobiont chlorococcoid, cells globose, 8‒15 μm diam.

Apothecia scattered, lecideine, 0.4‒0.8(‒1.0) mm across, distinctly constricted below; disc red-brown, lightly pruinose; proper margin slightly raised, 0.05‒0.08 mm wide, inrolled and paler at the inner edge. Excipulum internally pale- to red-brown with darker brown cortex, 20 μm wide, composed of radiating hyphae 6‒10 μm wide; extending below the hypothecium where it can be 60‒100 μm thick. Hymenium 125 μm tall; subhymenium 25‒40 μm thick; epihymenium dilute brown, 20‒25 μm thick with small granules that do not dissolve in KOH; paraphyses narrow, 1 μm wide, branched and anastomosing, only slightly wider at the apex (up to 2 μm) which is not pigmented. Hypothecium dark brown, 100 μm thick. Ascus Porpidia-type, cylindrical to slightly clavate, 80‒95 × (12‒)15‒20 μm; ascospores hyaline, simple, ellipsoid with attenuated apices, (17.0–)21.5 ± 2.3(–24.0) × (7.5–) 9.2 ± 0.4(–10.5) μm, l/w ratio (2.0–)2.4 ± 0.4(–3.1) n = 17, with a thin perispore 2 μm thick.

Conidiomata not observed.


Thallus KOH+ yellow, C−, PD+ orange; stictic acid by TLC.


A play on the common abbreviation for south-east Alaska (‘SE AK’).


On siliceous rocks and boulders in open, well-lit wooded areas.


Porpidia seakensis (Fig. 32) is a distinctive species that has so far not been found outside the Bartlett Cove area of GLBA, although it is common there. The only other species of the Porpidia macrocarpa group (macrocarpa-type exciple, stictic acid complex; Gowan Reference Gowan1989) with large ascospores (>20 μm) is P. superba (Körb.) Hertel & Knoph, which has thick, bullate areoles and an orange-brown exciple (Superba-brown).

Two DNA sequences from Porpidia seakensis (28S rDNA and Mcm7) were obtained for this study but were not incorporated into any tree because of insufficient overlap with previously sampled loci in the genus; ITS, which has been used for example by Orange (Reference Orange2014) in studying relationships in Porpidia, was not successfully amplified from our isolate. The sequences are published here (Table 1) for future reference.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Bartlett Cove, ‘river trail’, 58.4569°N, 135.8628°W, 40‒50 m, schistose rock in woodland, 2011, Fryday 9626 & Spribille (MSC); ibid., 58.4569°N, 135.8628°W, 2012, Fryday 10486 (MSC); ibid., Bartlett Cove, entrance to Park HQ, 58°27.265′N, 135°52.380′W, 25 m, small siliceous boulder, 2011, Fryday 9648 (MSC); ibid., Bartlett Cove, 25 m E of Service Rd, N side, 58.4541°N, 135.8793°W, 20–25 m, granitic boulder, 2012, Fryday 10490, 10491, 10493 (MSC); ibid., Bartlett Cove, housing complex, 58.4556°N, 135.8756°W, 15 m, flat stones, 2012, Fryday 10499 (MSC).

Rhizocarpon haidense Brodo & Fryday sp. nov.

MycoBank No.: MB 830116

Similar to Rhizocarpon infernulum (Nyl.) Lynge and R. cinereovirens (Müll. Arg.) Vain. but distinguished from R. infernulum by its unpigmented or pale brown exciple, and from R. cinereovirens by its smaller ascospores, predominantly brown epihymenium (Cinereorufa-green absent or present in low quantities), by its thallus containing stictic acid (norstictic acid absent or in trace amounts only) and lack of a well-developed prothallus.

Type: Canada, British Columbia, Haida Gwaii (‘Queen Charlotte Islands’), Moresby Island, Jedway, along Skincuttle Inlet, E of settlement, 52°19′N, 131°12′W, rocky shore and Picea-Tsuga forest, on rock at base of cliff at edge of beach, 25 July 1967, I. M. Brodo 12480, Shchepanek & Schofield (CANL—holotype).

(Fig. 33)

Fig. 33. Rhizocarpon haidense (holotype). A & B, habitus; C & D, section through apothecium under polarized (C) and brightfield (D) light; E, ascospores in ascus, with paraphyses, using DIC microscopy. Scales: A = 5 mm; B = 1 mm; C & D = 50 μm; E = 10 μm.

Thallus effuse, creamy to pale brown, thin, cracked areolate, areoles angular, slightly convex, 0.3–0.4 mm across; cortex absent; medulla with numerous minute crystals that dissolve in KOH to give a yellow solution, I−. Photobiont chlorococcoid, cells globose, 7–12 μm diam.

Apothecia lecideine 0.4–0.7 mm diam., flat to slightly convex; disc dark brown to black; proper margin persistent, 0.05 mm wide, slightly raised, paler than the disc. Exciple composed of hyaline, radiating cells c. 8–10 × 5–8 μm that are largely obscured by numerous minute crystals that dissolve in KOH to give a yellow solution; cortical cells pale brown, 5–6 μm diam. Hymenium hyaline, 90–100 μm tall; paraphyses sparingly branched and anastomosing, 2–2.5 μm thick, not or only slightly wider at the apex; epihymenium upper 10 μm diffuse brown but usually HNO3+ red indicating presence of small quantities of Cinereorufa-green. Hypothecium dark brown, upper part of vertically orientated hyphae intergrading into the hymenium, lower part of more randomly orientated hyphae. Asci Rhizocarpon-type, 50–60 × 15–18 μm, slightly clavate; ascospores hyaline, 1-septate, (14–)16.7 ± 2.4(–22) × (6.5–)7.8 ± 1.0(–9.5) μm, l/w ratio (1.7–)2.2 ± 0.4(–2.9), n = 20, slightly constricted at the septum, apices equally rounded.

Conidiomata not observed.


Thallus KOH+ yellow, PD+ orange, C−; stictic and constictic acids by TLC, occasionally with a trace of norstictic acid and other unknown substances.


For Haida Gwaii, the type locality and where the species was first detected.


On siliceous rock near the coast, often in the aerohaline zone.


Rhizocarpon haidense is similar to R. cinereovirens, with which it shares a pale brown to hyaline proper exciple (giving the apothecia a pale margin), a character that readily separates these two species from R. infernulum. However, it differs from R. cinereovirens in that the thallus produces stictic acid as the major substance rather than norstictic acid, although this is sometimes present in trace amounts. The epihymenium of R. haidense also lacks appreciable amounts of Cinereorufa-green, the pigment present in R. cinereovirens (although again this is usually present in trace amounts causing the epihymenium to react HNO3+ red). As noted previously (Fryday Reference Fryday2002), the production of Cinereorufa-green in the epihymenium of R. infernulum appears to be related to the degree of exposure to ultraviolet light, with the substance being present in larger amounts in specimens from exposed situations. However, the difference between R. haidense (brown epihymenium) and R. cinereovirens (blue-green hymenium) appears to be consistent. The last two species also differ in R. haidense having somewhat smaller ascospores ((17–)19.5(–22) × (7–)8.8(–10) μm in R. cinereovirens) and being known only from maritime rocks in NW North America, where R. cinereovirens has yet to be reported. Rhizocarpon haidense also usually has a much less well-developed thallus and smaller apothecia, although this is probably an environmental modification to its habitat on marine rocks and specimens from less extreme environments are difficult to separate from R. cinereovirens macroscopically.

DNA sequences were obtained from three gene loci and are used in Figs 5 and 10. However, an analysis of the placement of these sequences relative to other species in the genus Rhizocarpon was not attempted for this study to avoid pre-empting the work under preparation by collaborators.

Additional specimens examined (all Canadian collections in CANL)

Canada: British Columbia: Haida Gwaii (Queen Charlotte Islands), Graham Island, 11.2 miles N of Skidegate Mission, 53°26′N, 132°54′W, 1967, Brodo 10046 & Shchepanek; ibid., Tana Bay, 53°11′N, 132°33′W, on rock just above shore, 1967, Brodo 10157, Shchepanek & Schofield; ibid., Seal Inlet in Rennell's Sound, 53°31′N, 132°44′W, on shaded rock above littoral zone, 1967, Brodo 10274, Shchepanek & Schofield; ibid., 53°29′N, 132°47′W, in lower aerohaline, 1967, Brodo 10334, Shchepanek & Schofield; ibid., north side of Russell Sound, 53°23′N, 132°31′W, 1967, Brodo 10340, Shchepanek & Schofield; ibid., head of Tian Bay, 53°47′N, 133°04′W, in aerohaline, 1967, Brodo 10522, Shchepanek & Schofield; ibid., Langara Island, off NW corner of Graham Island, Henslung Harbour (Dadens), 54°12′N, 133°00′W, in aerohaline, 1967, Brodo 10586, Shchepanek & Schofield; ibid., Haida Point, 53°15′N, 132°01′W, 1988, Brodo 11730A & Shchepanek; ibid., near head of Dinan Bay, 53°39′N, 132°41′W, on rock at edge of beach, 1971, Brodo 18362, Wong & Turner; ibid., Cone Head, SW corner of Rennell Sound, 53°23′N, 132°39′W, Coccotrema zone, 1988, Brodo 26907; ibid., Gregory Beach, 53°24′N, 132°31′W, on headland rocks in Coccotrema zone, 2000, Brodo 302650, F. G. Brodo & Bettner; Burnaby Island, Section Cove, 52°24′N, 131°21′W, 1971, Brodo 17557A, Wong & Schofield; ibid., Pelican Point, 52°24′N, 131°16′W, 2000, Brodo 17557A & Sloan; Skidegate Inlet, Maude Island, 53°12′N, 132°05′W, 1967, Brodo 11284 & Shchepanek; ibid., outside Long Inlet, 53°21′N, 132°21′W, 1967, Brodo 11392 & Shchepanek; Moresby Island, between De la Beche and Haswell Bays, 52°32′N, 131°36′W, 1967, Brodo 11955, 11961 & Shchepanek; ibid., Kootenay Inlet, 52°51′N, 132°13′W, 1967, Brodo 12138, 12168 & Shchepanek; ibid., Louscoone Inlet, 52°13′N, 131°15′W, on rocks at edge of beach, 1967, Brodo 12309, 12319 & Shchepanek; ibid., Tasu, Growing Island, 52°46′N, 132°02′W, in aerohaline, 1967, Brodo 12851, Shchepanek & Schofield; ibid., south entrance to Louise Narrows, 53°57′N, 132°54′W, 1967, Brodo 17922,Wong & Schofield; Limestone Island, Boat Cove, 52°54′N, 131°36′W, on shoreline rocks above Coccotrema zone, 2000, Brodo 30117 & F. B. Brodo; Kunghit Island, Luxana Bay area, 52°04′N, 131°00′W, on shoreline rocks 4.5 m above barnacle zone, 2000, Brodo 30015 & Sloan; Vancouver Island, south end of Long Beach, 49°01′N, 125°40′W, 1969, Shchepanek 250, Soper & Brayshaw.—USA: Alaska: Juneau, Aaron Island, 7 miles W of Auke Bay, 58°27′N, 134°49′W, on shaded shoreline rock, 1988, Brodo 10586, Hart & F. Brodo (CANL); Hoonah-Angoon Census Area, Glacier Bay National Park, Taylor Bay, 58.25467°N, 136.56860°W, 0–5 m, supralittoral zone, above splash zone, metamorphic rock (Hornblende augen gneiss), 2012, Fryday 10452 & Spribille (MSC); ibid., 9 m, vertical shale face at sea level, 2012, Spribille 39505 & Fryday (MSC); Petersburg Borough, Kupreanof Island, Little Duncan Bay, 56.6193°N, 133.1645°W, sea level, siliceous rocks by shore, 2014, Fryday 10680, Spribille & Dillman (MSC).

Comparative specimens examined (R. cinereovirens)

USA: South Dakota: Custer Co., above Game Lodge in Custer State Park (11 miles E of Custer), on N-facing hill, 4300 ft, Sec 27, T3S, R6E, 1960, Wetmore 7575 (MSC). New York: Suffolk Co., Amagansett, Bunker Hill on Bunker Hill Road, oak-hickory woods, 1961, Brodo 3265 (MSC).

Sagiolechia phaeospora Fryday & T. Sprib. sp. nov.

MycoBank No.: MB 830117

A Sagiolechia species differing from all other species in the genus in its brown, submuriform ascospores and association with a non-trentepohlioid alga as a photobiont.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, Excursion Ridge, 58.46469°N, 135.55736°W, 918 m, saxicolous on argillite, 1 August 2012, Spribille 39391 (MSC—holotype).

(Fig. 34)

Fig. 34. Sagiolechia phaeospora (holotype). A, habitus; B, section through apothecium (composite image); C, ascus and immature and mature ascospores; D, overmature ascospores (C & D in Lugol's solution after KOH). Scales: A = c. 1 mm; B = 50 μm; C & D = 10 μm.

Thallus crustose, thin, whitish, cracked areolate to rimose; areoles/cracked partitions if present 0.4–0.9 mm diam., internally hardly stratified, POL+ birefringent. Photobiont a single-celled green alga; cells roundish or angular, 10–14 μm diam.

Ascomata apothecia, jet black, matt, 0.6–1.0 mm diam.; disc effigurate, with a central umbo up to 220 μm wide, composed of thick-walled hyphae 4.5–6 μm diam.; proper margin prominent, black. Excipulum 140–150 μm wide laterally, the outer 30 μm deeply pigmented (‘carbonized’), internally medium to dark brown, 60 μm wide basally, I+ blue before pretreatment with KOH. Hymenium 180–200 μm tall, hyaline, I+ blue; paraphyses predominantly simple, thin, 1–1.5 μm diam., not widened apically, upper 1/4 of hymenium brownish pigmented. Hypothecium 50–150 μm tall, hyaline. Asci 8-spored, oblong-cylindrical, c. 70–72 × 16–17 μm; ascospores submuriform, brownish, (14–)17.8–18.5(–22) × (8–)9.5–10.6(–14) μm (n = 21, two specimens used).

Conidiomata sunken, inconspicuous; conidia c. 3 × 1 μm.


All spot tests negative.


In reference to the brownish ascospores.


Saxicolous on small slabs of argillite rock in snowbed habitats in the low alpine zone (c. 920 m).


Sagiolechia A. Massal. is a loosely defined genus that includes species with hyaline, transversely septate ascospores, deeply melanized (‘carbonized’) apothecial pigments and an association with Trentepohlia Mart. photobionts, together with at least one lichenicolous species not considered to possess its own thallus. Four species are recognized: S. fusiformis (Müll. Arg.) Zahlbr., from rocks in Japan (Mueller Reference Mueller1892); S. protuberans (Ach.) A. Massal., which is widespread on calcareous rocks (Vězda Reference Vězda1967); S. atlantica Henssen on volcanic conglomerate on Madeira (Henssen Reference Henssen1995); S. parasitica Alstrup & E. S. Hansen, which is lichenicolous on Hymenelia cyanocarpa (Anzi) Lutzoni in Greenland (Alstrup & Hansen Reference Alstrup and Hansen2001). Many authors have segregated the arctic-alpine species Sagiolechia rhexoblephara (Nyl.) Zahlbr, which would count as a fifth species, into a distinct monotypic genus, Rhexophiale Th. Fr., on account of the different observed ontogeny of its ascomata (Henssen Reference Henssen1995).

Sagiolechia phaeospora (Fig. 34) is the first described member of the genus with brown ascospores (Fig. 34C & D), the first species with muriform ascospores, and the first associated with a non-trentepohlioid photobiont. In our phylogenetic analysis (Fig. 7), we analyzed only one specimen each of S. protuberans and S. phaeospora, but even this limited sampling makes two things clear: 1) S. phaeospora forms a clade with the type species of Sagiolechia, S. protuberans, and 2) both species form a small monophyletic group with Rhexophiale rhexoblephara (Nyl.) Almq., challenging Henssen's (Reference Henssen1995) hypothesis that observed ontogenetic differences reflect deep evolutionary splits. Our result supports the close relationship postulated between S. protuberans and S. rhexoblephara in the anatomical study of Vězda (Reference Vězda1967).

An additional, possibly related species has since been seen by one of us (AMF, 27 May 2014) from Ungava Bay (Québec, Nord-du Québec, Kativik, near Tasiujaq, 58.82833°N, 69.88778°W, 36 m, maritime outcrops (Labrador Trough), Site 86.12b, 29 July 2013, J. Gagnon s. n. (QFA)) and appears to be undescribed. It has brown 3-septate ascospores (c. 18 × 6 μm), the apothecia are often short-lirelliform, and as with S. phaeospora the associated photobiont is not Trentepohlia. Also probably referable to Sagiolechia, perhaps representing yet another species, is a collection from the terminal moraine of Baird Glacier (Alaska, Petersburg Borough, Fryday 11235, MSC) that has small apothecia with a carbonized exciple and hyaline 3-septate ascospores.

Sagiolechia phaeospora was collected three times during the present survey, in the same area of alpine heath on Excursion Ridge in the south-eastern corner of GLBA.

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Excursion Ridge, 58.46274°N, 135.55288°W, 919 m, saxicolous on argillite in alpine heath tundra, 2012, Spribille 38406 (MSC; DNA isolate T1184); ibid., 58.4635°N, 135.55809°W, 915 m, saxicolous, 2012, Svensson 2633 (MSC).

Sclerococcum fissurinae Pérez-Ort. sp. nov.

MycoBank No.: MB 830129

Lichenicolous on Fissurina insidiosa. Similar to Sclerococcum parasiticum but ascospores are slightly smaller (8–12 × 3–4 μm vs 9–15 × 3.5–5 μm) and it has a different host species.

Type: USA, Alaska, Hoonah-Angoon Census Area, just outside Glacier Bay National Park boundaries, 6.5 km NE of Gustavus, along Falls Creek Road, 58.43899°N, 135.64068°W, on Fissurina insidiosa corticolous on Alnus along side drainage, 37 m, 28 July 2012, Spribille 39036 (NY—holotype; GZU, H, UPS—isotypes).

(Fig. 35)

Fig. 35. Sclerococcum fissurinae (holotype). A, ascomata on Fissurina thallus; B, transverse section of ascoma; C, detail of excipulum; D, mature ascus with ascospores and paraphyses; E, young ascospore; F & G, mature ascospores (B–H in water and using DIC microscopy). Scales: A = 0.5 mm; B = 50 μm; C = 10 μm; D–G = 5 μm.

Apothecia rounded, to 0.6 mm diam.; disc flat, black; proper margin distinct, concolorous with the disc. Excipulum upper part 25–40 μm wide in section, red-brown to maroon, KOH+ dark olivaceous green, HNO3+ becoming orange, composed of elongated, more or less radiating hyphae, becoming prismatic at the base, 6–15 × 5–7 μm diam. Hymenium hyaline, 35–50 μm tall; epihymenium reddish brown to maroon, KOH+ dark olivaceous green, HNO3+ turning vivid orange; paraphyses simple, 1–2 μm wide, enlarged at the apex (up to 6 μm wide), with swollen and reddish brown apical caps. Hypothecium reddish brown to maroon, up to 30 μm high. Asci with a K/I+ blue outer layer, 8-spored, 25–33 × 8–12 μm; ascospores brown, ellipsoid, ornamentation granulate when young, usually disappearing when mature, 3-septate, more rarely 1–2-septate, straight or rarely slightly curved, not or slightly constricted at the septa, (8–)10–12(–14) × 3–4 μm (n = 35).


Named for its occurrence on Fissurina.


On Fissurina insidiosa C. Knight & Mitt. in Alnus-dominated riparian areas, known so far only from GLBA but likely to be widespread in outer coastal SE Alaska.


Diederich et al. (Reference Diederich, Lawrey and Ertz2018) synonymized the apotheciate genus Dactylospora Körb. with the sporodochia-producing genus Sclerococcum Fr., based on molecular data. Several species of the genus Sclerococcum possess 3-septate ascospores (Triebel Reference Triebel1989; Ihlen et al. Reference Ihlen, Holien and Tønsberg2004). The most similar to S. fissurinae (Fig. 35) are S. attendendum (Nyl.) Ertz & Diederich and S. parasiticum (Flörke) Ertz & Diederich. The former has larger ascospores (12–15 × 4.5–5.5 μm) and the apothecia usually have a rough or radially striate margin. Furthermore, this species is known growing only on crustose saxicolous species such as Amygdalaria Norman, Pertusaria s. str., Pilophorus Th. Fr. and Porpidia Körb. species (Triebel Reference Triebel1989). Sclerococcum parasiticum, by contrast, has slightly larger ascospores (9–15 × 3.5–5 μm) and usually grows on Lepra and Ochrolechia species (also on Mycoblastus sanguinarius (L.) Norman; see ‘Catalogue of All Named Taxa Found’ (below)).

Additional specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Icy Straits, ridge above Fern Harbor, 58.31133°N, 136.45689°W, corticolous on Tsuga heterophylla branches, 86 m, 2012, Spribille 38091 (MSC); just outside Glacier Bay National Park boundaries, 6.5 km NE of Gustavus, along Falls Creek Road, 58.43899°N, 135.64068°W, corticolous on Alnus along side drainage, 37 m, 2012, Spribille 39050 (GZU—topotype).

Spilonema maritimum T. Sprib. & Fryday sp. nov.

MycoBank No.: MB 830119

Similar to Spilonema paradoxum but differing in developing concentrically radiating, flattened thalli and in its close association with supralittoral habitats.

Type: USA, Alaska, Juneau Borough, west side of Douglas Island at Peterson Creek beach access, 58.285534°N, 134.674141°W, on exposed seashore rocks at back of beach, about two metres above high tide line, 21 September 2010, Spribille s. n. (UPS—holotype; BG, GZU, MSC, NY—isotypes).

(Figs 36 & 37)

Thallus composed of radiating filaments, forming rosettes 0.5–1.5 cm diam., olivaceous brown; individual filaments sausage-like, 19–40 μm diam. (visible below apothecial section in Fig. 37A), with isidioid spinules to 18 μm diam. (Fig. 36D–F); entire thalline area richly occupied by minute bacterial biofilms and becoming conglutinated in a ‘biofilm cake’ with age (Fig. 36C); thallus in section composed of a Stigonema-like cyanobacterium 7–13 μm diam., enmeshed with fungal hyphae, the fungal-cyanobacterial contact areas I+ blue after KOH pretreatment, the whole filament ensheathed in a gelatinous layer; cellular cortex absent; hypothallus bluish, KOH+ mauve.

Fig. 36. Spilonema maritimum. A–C, habitus of healthy (A & B) and eroded (C) thalli, indicating in (B) an apothecium (arrow) and pycnidia (asterisks) (A, isotype; B, Fryday 10389; C, Spribille 39589); D–F, details of thallus surface with SEM, including upper (D & E) and lower (F) surfaces (Fryday 10389). Scales: A & C = 1 mm; B = 0.5 mm; D = 200 μm; E = 50 μm; F = 100 μm.

Fig. 37. Anatomical details of the apothecium in Spilonema maritimum (holotype). A, section; B, detail of excipular hyphae; C–E, ascus apical structures in Lugol's solution, at full concentration (C) and while fading (D); E, the same as D but using DIC microscopy; F–H, ascus apical structure in dissipating Lugol's solution, arrows indicate amyloid apical tube. Scales: A = 100 μm; B–H = 10 μm.

Ascomata apothecia, rare, round, single, 0.15–0.55 mm diam., difficult to distinguish from pycnidia when wet; disc convex blue-black, shiny; proper margin excluded from surface view. Excipulum (Fig. 37B) of radiating hyphae to 6 μm diam., streaked with bluish black pigments; hyphae internally with large, angular lumina, non-amyloid. Hymenium 42–70 μm tall, bluish streaked with pigments concentrated at the base of the hymenium, I+ blue before KOH; top of hymenium black-bluish, HNO3+ mauve, KOH−; paraphyses septate, sparsely branched, with bulges, 1.5–2.5 μm wide medianly, swelling to 3 μm in KOH and 5 μm terminally. Hypothecium 100–140 μm tall, pale blue to hyaline, composed of thin-walled hyphae with lumina 3–8 μm diam; upper part I+ blue; subhymenium weakly differentiated. Asci 8-spored, 30–42 × 10–13 μm, covered in a massive I+ deep blue gelatinous sheath and thus very difficult to visualize because the ascus turns almost completely black in Lugol's solution (Fig. 37F–H); ascospores sparse and hard to find, simple, ellipsoid, (6.5–)7.8–8.9(–12) × (2.5–)3.6–3.9(–5) μm (n = 16, two samples used).

Pycnidia present in four of five specimens studied, shiny black, pigmented bluish to greenish black internally, pyriform, opening up to gaping, 130–190 μm diam.; conidia bacilliform, straight, 3–4.2 × 1.3–2 μm.


All spot tests negative; no substances detected by TLC.


Named for its close association with maritime rocks.


On rocks in the supralittoral zone, known in GLBA from Taylor Bay and Fern Harbor, and outside of GLBA from Kruzof and Douglas Islands, Alaska, as well as from Haida Gwaii and Vancouver Island, British Columbia.


Spilonema maritimum was initially thought to be a member of the Lichinomycetes, perhaps related to Ephebe Fr., but discovery of fertile material showed that it belongs to the Peltigerales in the Lecanoromycetes. Spribille et al. (Reference Spribille, Tønsberg, Stabentheiner and Muggia2014a) published a molecular phylogeny of Spilonema Bornet, a small genus with three named species to date, S. americanum (Henssen & Tønsberg) T. Sprib. et al., S. revertens Nyl. and S. paradoxum Bornet. Spilonema maritimum clearly does not fit into any of these species and is distinguished by its flattened, radiating outer lobes and filamentose centre, and the tendency to become conglutinated with age. Similar to Spilonema sp. 1 (Spribille et al. Reference Spribille, Tønsberg, Stabentheiner and Muggia2014a), it occupies supralittoral habitats, but it differs from that undescribed species in its radiating habit and lack of thalline mounds. The metagenomic DNA obtained from samples of S. maritimum yielded PCR products either a) containing so much superimposed signal that the traces were unusable, or b) with readable sequences that clearly come from multiple fungal genomes. One of these was an unidentified putative Orbiliaceae (LSU sequence from isolate T1338; Table 1); another came from the lichenized class Lichinomycetes (mtSSU from isolate T1808; Table 1), which caused us to again reassess our assumptions regarding the main fungal component of this lichen. One mitochondrial SSU sequence (from isolate T1338, used in Fig. 9) aligned closely with previously obtained sequences from Spilonema and because this agrees with the fungal morphology, we have deposited this as putatively belonging to S. maritimum. The multiple fungal species we detected in S. maritimum highlight the difficulties in sequencing fungal DNA with general fungal primers without knowing the cellular source of the genomic DNA. However, we note that all aspects of ascomatal anatomy are consistent with other species of Spilonema.

Spilonema maritimum is found in the upper supralittoral zone in the Icy Straits near the open ocean in GLBA. It appears to be common along the outer Pacific coast of NW North America as far as southern Vancouver Island. According to I. M. Brodo (personal communication, 2019), material of S. maritimum was the basis for the first report of S. revertens Nyl. from British Columbia (Benton et al. Reference Benton, Brodo and Richardson1977). That species is now known from other localities in British Columbia but occurs in rock crevices or over mosses in dry, inland habitats, unlike S. maritimum. The distinctive position of S. maritimum in the zonation of maritime rocks on Haida Gwaii is discussed by Brodo & Sloan (Reference Brodo and Sloan2005, as S. revertens).

Additional specimens examined (all Canadian specimens from CANL)

Canada: British Columbia: Queen Charlotte Islands [ = Haida Gwaii], Maude Island in Skidegate Inlet, 53°12′N, 132°05′W, on rocks at edge of beach in aerohaline, 1967, Brodo 11253 & Shchepanek; ibid., Torrens Island, Skidegate Inlet, 53°15′N, 131°59′W, on rocks, upper aerohaline, 1971, Brodo 17309 & Wong; ibid., Murchison Island, 52°36′N, 131°28′W, in lower aerohaline, 1967, Brodo 11862 & Shchepanek; ibid., Hibben Island, off the W coast of Moresby Island, 53°00′N, 132°22′W, rocks high above water, 1968, Brodo 14029; ibid., Lina Island, Skidegate Inlet, 53°13′N, 132°08′W, exposed shoreline rocks, aerohaline, 1967, Brodo 11337 & Shchepanek; ibid., Skidegate Inlet, Robbers Island, 53°13′N, 132°02′W, shore rocks on beach, 1967, Brodo 11148 & Shchepanek; ibid., Skidegate Inlet, Balch Island (North), 53°14′N, 132°05′W, stone at edge of beach, 1967, Brodo 11527 & Shchepanek; ibid., Graham Island, Seal Inlet in Rennell Sound, 53°29′N, 132°47′W, rock at shore, 1967, Brodo 10313 & Shchepanek; ibid., Graham Island, Skidegate Landing at Haida Point, 53°15′N, 132°01′W, shoreline rock in lower aerohaline, Brodo 11716 & Shchepanek; ibid., Graham Island, Cone Head, SW corner of Rennell Sound, 53°23′N, 132°39′W, upper hygrohaline, 1988, Brodo 26941; ibid., E coast of Moresby Island, N side of Gray Bay, 53°08′N, 131°47′W, shoreline rocks, aerohaline, 1967, Brodo 12603; ibid., Moresby Island, N shore of Copper Bay, 53°11′N, 131°46′W, on rock of upper hygrohaline, 1971, Brodo 17260; ibid., Moresby Island, 1/2 mile W of Ikeda Point, 52°19′N, 131°09′W, shoreline rocks, lower aerohaline, 1971, Brodo 17577; ibid., Moresby Island, Cumshewa Head, 53°02′N, 131°36′W, upper surface of headland rocks, 1971, Brodo 17427 & Wong; ibid., Moresby Island, Ingraham Point, entrance to Carpenter Bay, S shore, 52°14′N, 131°02′W, exposed headland rocks, 2000, Brodo 29962B; ibid., Kunghit Island, foot of Balcom Inlet, 52°06′N, 131°01′W, rock outcrop at shoreline in aerohaline, 1967, Brodo 12372 & Shchepanek; ibid., Cape St James, 51°56′N, 131°01′W, on rock at edge of ridge, 1971, Brodo 17618, Wong & Schofield; ibid., Limestone Island, Boat Cove, 52°54′N, 131°36′W, on shoreline rocks, c. 2 m, above Fucus limit, 2000, Brodo 30120A & Brodo; ibid., Langara Island, 54°12′N, 133°00′W, rocks in lower aerohaline, 1967, Brodo 10598; ibid., Huxley Island, N shore, 52°28′N, 131°21′W, rock in hygrohaline, 1971, Brodo 17538, Wong & Schofield; ibid., Wathus Island, in Masset Inlet, 53°40′N, 132°29′W, southern point of land, shoreline rock, aerohaline, 1971, Brodo 18341A, Wong & Turner; ibid., Chaatl Island, cove on W coast, 53°08′N, 132°35′W, rock wall on headland, lower aerohaline, 1988, Brodo 26973, Brodo, Sharnoff & Sharnoff; Vancouver Island, Bamfield Marine Station, rocky point immediately N of station, 48°70′N, 125°10′W, 1976, Benton & Richardson.—USA: Alaska: Juneau, Shrine of Ste.-Therese, 10 miles W of Auke Bay, 58°28′N, 134°47′W, lower aerohaline, 1988, Brodo 26145 (CANL); Sitka, Starrigavan Bay, near campground, 57°08′N, 135°22′W, protected headland rocks, aerohaline, 1988, Brodo 26075 (CANL); Sitka harbour, saxicolous, 2010, Spribille s. n. (GZU); Hoonah-Angoon Census Area, Glacier Bay National Park, Taylor Bay, 58.25428°N, 136.56633°W, 0–5 m, on hornblende augen gneiss, in splash zone, 2012, Fryday 10389 (MSC, fertile); ibid., Fryday 10408 (MSC); ibid., Spribille 39586, 39588, 39589 (MSC); Icy Straits, Fern Harbor, 58.30938°N, 136.45254°W, seashore crags, 0–4 m, 2012, Spribille 38205 (MSC; sub Physcia caesia).

Thelocarpon immersum Fryday sp. nov.

MycoBank No.: MB 830120

Separated from all other species of the genus by the combination of immersed perithecia, the presence of paraphyses, and the globose ascospores.

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, park entrance, 58.45281°N, 135.77898°W, 16 m, on soil in calcareous wet meadow in glacial outwash plain, 1 July 2012, Spribille 37899, Pérez-Ortega & Tønsberg (MSC—holotype).

(Fig. 38)

Fig. 38. Thelocarpon immersum (holotype). A & B, habitus (arrows indicate ascomata); C & D, section through ascoma under brightfield (C) and polarized (D) light; E, ascospores, in KOH. Scales: A = 1 mm; B = 100 μm; C & D = 50 μm; E = 10 μm.

Thallus absent, although the perithecia are associated with various cyanobacteria and chlorococcoid algae.

Ascomata perithecioid, yellow-green, 0.08‒0.12 mm diam., embedded in a mat of cyanobacteria and chlorococcoid algae, with only the tips protruding. Excipulum hyaline except upper 100 μm which is yellow-brown; periphyses present, simple, 30–40 μm long. Hymenium I+ orange-brown; paraphyses long (80–100 μm), narrow (1 μm wide), sparingly branched and anastomosing. Ascus initially cylindrical 75‒90 × 15‒17 μm with the upper 12‒15 μm narrowed to 5‒7 μm wide, later becoming clavate and up to 20 μm wide; wall I+ orange-brown, contents I+ yellow, tholus absent; ascospores globose, 5‒7 μm diam., I+ yellow.

Conidiomata not observed.


All spot tests negative.


The name refers to the immersed ascomata.


Known only from the holotype collection, which occurred on a biofilm over calcareous soil in a glacial outwash plain.


Thelocarpon is a genus of small, inconspicuous species that occur on various substrata, usually in damp habitats. Eight species have been reported from North America, of which only one, T. sphaerosporum H. Magn., has globose ascospores. The species are morphologically and anatomically varied and attempts have been made in the past to subdivide the genus. To date, DNA sequence data is available for only three species.

The family Thelocarpaceae was first monographed by Magnusson (Reference Magnusson and Rabenhorst1935), who recognized 11 species in Thelocarpon Nyl. and two in Thelococcum Nyl., the latter genus having immersed rather than sessile ascomata. As our new species has immersed ascomata, Magnusson would have included it in Thelococcum but the two species he included in that genus both have larger, ellipsoid ascospores. Among the species Magnusson included in Thelocarpon, only T. sphaerosporum has globose ascospores but that species, in addition to having sessile ascomata, also has an exposed hymenium.

Salisbury (Reference Salisbury1966) also monographed the genus and recognized 13 species. He included the species with immersed ascomata in Thelocarpon but removed the species with an exposed hymenium (including T. sphaerosporum) to Ahlesia Fuckel. Of the species he retained in Thelocarpon, only T. coccosporum Lett. has globose ascospores. However, that species, unlike our new species, has sessile ascomata and lacks paraphyses.

Poelt & Hafellner (Reference Poelt and Hafellner1975) reviewed the varying characters of the genus, including relative immersion of ascomata, exposure of hymenium, development of ascus apical apparatus and presence/structure of paraphyses. They concluded that subdividing the genus using any one character would bring different results and therefore accepted a wide circumscription of the genus that included the species previously included in Ahlesia and Thelococcum. Subsequently, Poelt & Vězda (Reference Poelt and Vězda1977), in their key to the species of Thelocarpon in Europe, included 18 species but the only species with globose ascospores were T. sphaerosporum and T. coccosporum. In more recent studies, Orange et al. (Reference Orange, Watson, James, Moore, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009a) included 15 species from the British Isles but only T. sphaerosporum with globose ascospores, whereas only two species, neither with globose ascospores, were included from the Greater Sonoran Desert (Knudsen & Lumbsch Reference Knudsen, Lumbsch, Nash, Gries and Bungartz2007).

Toensbergia blastidiata T. Sprib. & Tønsberg sp. nov.

MycoBank No.: MB 830122

Resembling Toensbergia leucococca in the corticolous habit, the cream-coloured areoles and the production of alectorialic acid, but distinct in being blastidiate (sorediate in T. leucococca) and in sometimes forming thick and more or less continuous thalli to a decimetre or more wide (unlike the persistently discrete squamules of T. leucococca).

Type: USA, Alaska, Glacier Bay National Park and Reserve, base of Marble Mtn at Whidbey Passage, 58°37.90′N, 136°14.68′W, 3–10 m, corticolous on Alnus viridis subsp. crispa just uphill from beach, 3 July 2012, Tønsberg 41670 & Spribille (MSC—holotype; NY—isotype).

(Fig. 39)

Thallus corticolous, crustose, episubstratal, areolate, blastidiate, cream-coloured and in herbarium specimens becoming rose (due to the presence of alectorialic acid); areoles initially solitary, rounded, convex, usually constricted below, to about 0.3 mm wide, soon starting to produce blastidia and then becoming larger, irregular, and often confluent with adjacent areoles that in some well-developed specimens, such as in parts of the type collection, result in patches to 1 dm or more wide that may crack and form angular, irregular, flat ‘secondary areoles’ to 0.8 mm high and 2 mm or more wide (Fig. 39C); surfaces of areoles blastidiate almost from the beginning, minutely coralloid when viewed under the dissecting microscope. Blastidia globose to opuntioid, to 60 μm wide, lined with a layer of rounded fungal cells, 5–7 × 5–6 μm, sometimes dotted blue, the pigment probably due to the presence of hypothallus hyphae that have been lifted upwards with the growth of the areoles. Medullary layer not observed. Hypothallus usually distinct, thin, not felty, usually bluish grey, sometimes bluish black or blackish, visible between areoles and along thallus margin. Photobiont chlorococcoid, cells ± globose, to 15 μm diam.

Fig. 39. Toensbergia blastidiata (holotype). A–C, habitus, thallus with dispersed (A & B) and confluent (C) blastidia; D–F, details of blastidia with SEM. Scales: A = 1 mm; B, C & E = 0.5 mm; D = 200 μm; F = 50 μm.

Ascomata and pycnidia not seen.


Thallus PD+ yellow, C+ red; alectorialic acid with satellite(s) detected by TLC.


For the blastidiate thallus surface.


On bark of Alnus viridis subsp. crispa, A. incana subsp. tenuifolia, A. rubra Bong., Frangula purshiana (DC.) A. Gray, Malus fusca (Raf.) C. K. Schneid. and Pinus contorta. Apparently widespread in coastal NW North America from Kodiak Island in south-central Alaska to the Olympic Mountains of Washington State.


This is a sterile sorediate crust (Fig. 39) containing dominant alectorialic acid forming creamish patches on alder trunks. Toensbergia blastidiata may be superficially similar to Fuscidea muskeg, especially when old and pink. This is a sterile crust and is easily distinguished when the latter is fertile. Multilocus rDNA sequencing reveals that T. blastidiata is closest to Pertusaria geminipara (Th. Fr.) C. Knight ex Brodo, a species that we had previously sequenced for a study on evolution within Ostropomycetidae (Resl et al. Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015) and ultimately excluded because it was too different from other Pertusaria species. A phylogenetic analysis shows that DNA sequences from the new species and P. geminipara, both of which contain alectorialic acid, form a strongly supported clade (Fig. 5) with the genera Toensbergia Bendiksby & Timdal (which likewise contains alectorialic acid) and Sporastatia A. Massal. (which contains gyrophoric acid). According to the results of Bendiksby & Timdal (Reference Bendiksby and Timdal2013), Toensbergia and Sporastatia form a group sister to the rest of the subclass Lecanoromycetidae, a result we also obtained. The DNA sampling of Sporastatiaceae has not been extensive and we await more sequenced loci before further speculating on the phylogenetic relationships within this group. In the meantime, we propose moving Pertusaria geminipara into an expanded Toensbergia (see below). It is the first fertile species to be included in Toensbergia; its ascomatal anatomy is described and illustrated by Brodo (Reference Brodo1984a).

Additional specimens examined (T. blastidiata)

Canada: British Columbia: Vancouver Island, Pacific Rim National Park Reserve, Radar Hill, near summit, 49°05.060′N, 125°50.501′W, 100 m, corticolous on Alnus rubra, 2010, Tønsberg 40799 (BG).—USA: Alaska: Hoonah-Angoon Census Area, near Gustavus, vicinity of Bear Track Lodge N of Gustavus airport, 6.5 km NE of Gustavus, along Falls Creek Road, 58.43792°N, 135.63803°W, 30 m, corticolous on Malus fusca, 2012, Spribille 39061 (MSC); ibid., Glacier Bay National Park, Glacier Bay, S Sandy Cove, 58.71026°N, 135.97581°W, sea level, corticolous on Alnus, 2014, Spribille 40737 (MSC); ibid., base of Marble Mtn at Whidbey Passage, 58°37.90′N, 136°14.68′W, 3–10 m, corticolous on Alnus viridis subsp. crispa uphill from beach, 2012, Tønsberg 41671, 41673 (MSC–topotypes); Borough of Sitka, Baranof Island, c. 10 km E (direct) of Sitka, off the main road from Sitka to Herring Cove (Sawmill Creek Rd) at Alaska Pulp Corporation pulp mill, 2 miles along road to Blue Lake, along road to Beaver Lake, 60 m, corticolous on Alnus rubra, 1991, Tønsberg 16347 (BG); Old Sitka, E of Starrigavan Bay, along the beach N of the mouth of Starrigavan River, 57°07.942′N, 135°22.221′W, 0–10 m, corticolous on twig of Alnus (shrub), 1991, Tønsberg 16455 (BG); Kodiak Island Borough, Kodiak Island E, along road to Anton Larsen Bay, bank of Red Cloud River, 57°49′N, 152°37′W, 20 m, corticolous on trunk of Alnus, 1991, Tønsberg 15245 (BG); Petersburg Borough, Mitkof Island, SE of Petersburg, inland from Sandy Beach [along road to Frederic Point], 56°48.2′N, 132°54.7′W, 10–20 m, corticolous on branches/twigs of Pinus contorta in muskeg, 2001, Tønsberg 30322b (BG); Borough of Juneau, Douglas Island E, West Juneau, 0.5 miles along Douglas Hwy NW of Juneau-Douglas Bridge, 58°18′N, 134°27′W, 10 m, on trunk of Alnus rubra, 1991, Tønsberg 16132 (BG). Washington: Clallam Co., Olympic Peninsula, Olympic National Park, just N of Ozette Lake, W bank of Ozette River, 48°09′20″N, 124°40′10″W, 10 m, corticolous on Rhamnus purshiana [ = Frangula p.], 1993, Tønsberg 19448 (BG); ibid., Ozette Lake, north end, Deer Point, 48°08.2′N, 124°38.2′W, 10 m, on Alnus rubra on lakeshore, 1999, Tønsberg 27113 (BG).

Toensbergia geminipara (Th. Fr.) T. Sprib. & Resl comb. nov.

MycoBank No.: MB 830124

Basionym: Lecanora geminipara Th. Fr., Lich. Scand. (Upsaliae) 1(1), 236 (1871). —Pertusaria geminipara (Th. Fr.) C. Knight ex Brodo, Bryologist 87, 105 (1984); type: Norway, Telemark, Tinn, Gusta-fjell, 1856, Th. M. Fries (UPS-L-150351, syntype!).

Xenonectriella nephromatis Pérez-Ort. sp. nov.

MycoBank No.: MB 830125

A Xenonectriella species characterized by the size of the asci (120–130 × 8–12 μm), ascospores (12–16 × 5–8 μm) and the host (Nephroma cf. bellum).

Type: USA, Alaska, Hoonah-Angoon Census Area, Glacier Bay National Park, near end of Geikie Inlet, NE shore, 58°36.421′N, 136°30.970′W, just above sea level, on Nephroma cf. bellum over Alnus, 7 September 2011, Spribille 36426 (US—holotype).

(Fig. 40)

Fig. 40. Xenonectriella nephromatis (holotype). A, ascomata; B, detail of ascomata; C, transverse section of a perithecium; D, detail of periphyses; E, detail of perithecial wall; F, ascus; G & H, ascospores (C–H in water, using DIC microscopy). Scales: A = 1 mm; B = 250 μm; C = 100 μm; D = 25 μm; E & F = 10 μm; G & H = 2.5 μm.

Ascomata perithecioid, dispersed, immersed in host thallus, erumpent, dark red, subspherical to obpyriform, to 600 μm diam., without hairs. Ascomata wall dark reddish orange, KOH+ quickly violet-purple, without orange oil guttules, composed of several layers of cells; outer layer dark reddish orange, to 25 μm wide, composed of several layers of enlarged prismatic cells, 10–18 × 2–4 μm; inner part hyaline, to 20 μm wide, composed of several layers of flattened cells. Periphyses abundant around the ostiole, forming a protruding cone, thin, 15–25 × 1.5–2.5 μm. Interascal elements not observed in mature specimens. Asci unitunicate, ±cylindrical with a thin wall, widened at the apex, with obtuse apex, 8-spored, 120–130 × 8–12 μm; ascospores uniseriately arranged inside the ascus, broadly ellipsoid but quite variable in shape, 1-septate, hyaline, not or slightly constricted at the septum, apices rounded or obtuse, ornamented, 12–16 × 5–8 μm (n = 24).


Named for its occurrence on Nephroma.


On Nephroma cf. bellum (thallus in poor condition).


The genus Xenonectriella was introduced by Weese (Reference Weese1919) for the species X. lutescens (Arnold) Weese, which is lichenicolous on Solorina spp. It was resurrected by Rossman et al. (Reference Rossman, Samuels, Rogerson and Lowen1999) for species of the order Hypocreales similar to Pronectria Clem. with dark-coloured perithecial walls reacting KOH+ and lactic acid+ dark purple-red, with long cylindrical asci and uniseriate, ornamented, usually light brown, ascospores. The genus Cosmospora Rabenh. is similar to Xenonectriella and it is likely that species assigned to these genera are congeneric. However, we follow Etayo & Sancho (Reference Etayo and Sancho2008) who maintain the difference between the genera based on the lifestyle of Xenonectriella, which is only lichenicolous with the development of the ascomata always inside the host thallus, whereas Cosmospora is fungicolous, saprotrophic or lichenicolous (one species) and usually possesses sessile ascomata.

Xenonectriella nephromatis (Fig. 40) is similar to X. rosea Etayo and X. ornamentata (D. Hawksw.) Rossman in the colour of the ascomata, although X. rosea may possess pinkish perithecia (Rossman et al. Reference Rossman, Samuels, Rogerson and Lowen1999; Etayo & Sancho Reference Etayo and Sancho2008). Xenonectriella rosea has slightly smaller ascospores (9.5–12.5 × 6–7.5 μm) with verrucose ornamentation and occurs on Pannaria leproloma (Nyl.) P. M. Jørg. and Psoroma spp. whereas X. ornamentata has 4-spored asci with much larger ascospores (25–31 × 7–9 μm). Xenonectriella aurantiaca Etayo from Tierra del Fuego (Etayo & Sancho Reference Etayo and Sancho2008) has similarly sized ascospores but its ascomata are clearly orange and it grows on Pseudocyphellaria vaccina (Mont.) Malme. So far, X. nephromatis is known only from the type collection growing together with Tremella nephromatis Diederich.

Other Species Treated in Detail

Absconditella rosea Kalb & Aptroot

MycoBank No.: MB 824111

Bryologist 5, 57 (2018); type: Venezuela, Merida, Rangel, Aug. 1989, K. Kalb, A. Kalb & M. López-Figueiras 25745 (VEN—holotype, n.v.; isotype from hb. Kalb, studied by Z. Palice).

Fig. 41. Absconditella rosea (Spribille 39168). A & B, habitus; C, section of apothecium and thallus with fragments of bryophyte material, in Lugol's solution; D, ascospores, asci and paraphyses, in Lugol's solution after pretreatment with K. Scales: A = 1 mm; B = 100 μm; C = 50 μm; D = 10 μm.

(Fig. 41)

Thallus filmy, greenish, covering mosses and to a lesser extent plant detritus, in section essentially a biofilm, with spreading fungal hyphae, bacterial colonies and roundish algal cells 6–12 μm diam.

Ascomata apothecia, round, (0.13–)0.22(–0.35) mm diam. (n = 12), single to clustered in small groups, strongly globose when young, opening with a small pore, eventually disc exposed but remaining highly concave when dry; disc deep pink to orange-pink, matt; proper margin pale whitish pink. Excipulum c. 50 μm wide laterally, 40 μm wide basally, composed of structured, interwoven, small fungal filaments c. 1.5 μm wide (±prosoplectenchymatous). Hymenium c. 75–85 μm tall, hyaline, weakly I+ golden; paraphyses separating easily in water, c. 0.5 μm wide, with little structural strength and easily breaking or becoming ‘wavy’ under pressure of microscope cover slip, widened to c. 1.2 μm apically. Hypothecium c. 30 μm high, hyaline. Asci 8-spored, narrowly cylindrical, non-amyloid, c. 55–85 × 6–7 μm [sic]; ascospores narrowly ellipsoid to ellipsoid, the majority 3-septate, a few 2-septate or even 1-septate, often with slightly pointed ends, occasionally ± papillate-warted (residual ascoplasma?), (12–)16.3(–21) × (4–)4.9(–6) μm (n = 30).


All spot tests negative.


On bryophytes in meadows in the uppermost beach zone.


In earlier versions of this manuscript, we treated this as a new species provisionally called Absconditella rosea, until Kalb & Aptroot (Reference Kalb and Aptroot2018) published a taxon from páramo habitats in Venezuela with exactly that name. The GLBA specimens shared with the description of the Venezuelan material the pink to orange-pink colour of the apothecia, deeply concave apothecial discs and 3-septate ascospores, and initially we thought our Alaskan material differed in ascospore length. We measured 12–21 × 4–6 μm in the GLBA specimens, with an average length of 16.25 μm, while Kalb & Aptroot (Reference Kalb and Aptroot2018) reported ascospores measuring 11–13 × 5.5–6.5 μm in A. rosea. However, Zdeněk Palice (personal communication) measured a range of ascospore sizes from an isotype specimen of A. rosea (15–21.5 × (4.5)5–5.5(–6) μm (n = 10)) that strongly overlap with the range measured in GLBA specimens. Similarly, apothecial diameters were larger than reported in the protologue, with some apothecia measuring up to 0.45 mm. As a result of these discrepancies, we provide a full description of the Alaskan specimens. Despite the long distance between the two localities, we can find no justification for distinguishing the Alaskan material as a separate species from A. rosea at this time.

Baloch et al. (Reference Baloch, Lücking, Lumbsch and Wedin2010), in their phylogenetic revision of Ostropales, showed that the type of Absconditella Vězda, A. sphagnorum Vězda & Poelt, as well as several other species, are closely related to the non-lichenized genera Bryodiscus B. Hein et al. and Sphaeropezia Sacc. One of the most commonly collected species, A. lignicola Vězda & Pišút, is however more closely related to the genus Cryptodiscus Corda. In the current literature, Absconditella rosea may key to A. lignicola on account of its 3-septate ascospores, but in habit it more closely resembles the type of the genus, A. sphagnorum. DNA sequences were already obtained from A. rosea and published by Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015) under the name ‘Absconditella sp. Spribille 39168’. Analysis of A. rosea in a set of all available published Absconditella sequences shows it belongs to a clade including A. sphagnorum with strong support (Fig. 7). Our phylogeny includes all currently available, named Absconditella species from GenBank that seemed logical to include (A. rubra van den Boom et al. is represented in GenBank only by ITS sequences, which are absent from several other species so would not be useful for inferring relationships). Our phylogeny shows more clearly than a previous study (Aptroot et al. Reference Aptroot, Parnmen, Lücking, Baloch, Jungbluth, Cáceres and Lumbsch2014) that Absconditella and Geisleria Nitschke are likely congeneric, assuming that a specimen from Sweden labelled Absconditella sp. 2 by Baloch et al. (Reference Baloch, Lücking, Lumbsch and Wedin2010) is correctly placed in Absconditella. We refrain from making any changes to the nomenclature, however, as we have not sampled Absconditella with the intention of testing the Geisleria-Absconditella hypothesis, and many species remain unsampled. We note, that Geisleria is the older name.

Specimens examined

USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, along shoreline N of Point Gustavus, 58.40633°N, 135.90598°W, 2–4 m, on bryophytes on upper beach, 2012, Spribille 39168 & Svensson (MSC), Spribille 39165 (MSC, sub Gyalideopsis muscicola), Svensson 2769 (MSC).

Lecanora alaskensis H. Magn.

MycoBank No.: MB 410846

Annals Cryptog. Exot. 5, 19 (1932); type: USA, Alaska, Wrangell, on slate beach, 1900, A. S. Foster s. n. (UPS L-74656—holotype!).

(Fig. 42)

Fig. 42. Lecanora alaskensis. A & B, habitus; C & D, section through apothecium under brightfield (C) and polarized (D) light; E, asci containing immature ascospores, in Lugol's solution; F, thallus granule, with SEM; G, surface of thallus granule with SEM, showing extrusion of wax-like fibrils. Scales: A = 1 mm; B = 200 μm; C, D & F = 100 μm; E = 10 μm; G = 1 μm. A, E, F & G from Dillman 714a (TNFS); B–D from Tønsberg 41794 (BG).

Thallus crustose, to 4.5 cm across, rugulose to minutely bullate or scurfy, usnic yellow to ochre-usnic yellow or pale latte brown (dark greenish in type); areoles distinct to indistinct, 0.15–0.5 mm diam., strongly convex; internally undifferentiated; medulla hydrophobic, perhaps on account of wax-like extrusions (Fig. 42G); hypothallus not seen. Photobiont chlorococcoid, cells globose, 8.5–11 μm diam.

Ascomata apothecia, round, globose to strongly tuberculate, (0.5–)0.9–1.6(–3.9) mm diam.; disc strongly convex, reddish brown to medium brown (to black), matt; margin lecanorine, pale ochre-grey, quickly becoming excluded. Excipulum to 70 μm wide laterally, 45–100 μm basally, of radiating, thick-walled hyphae, I−, filled or streaked with POL+ crystals. Hymenium 60–80 μm tall, hyaline to hazy golden brown, I+ blue both before and after treatment with KOH; uppermost part of hymenium inspersed with POL+ granules, red-brown to golden brown in transmitted light; paraphyses mostly simple, thin, c. 1–1.5 μm wide medianly and 2 μm wide terminally; subhymenium slightly darker, KOH+ golden, I− except top of hypothecium including ascogenous hyphae sometimes I+ bluish. Hypothecium variable, 160–500 μm tall, hazy yellow-brown to golden brown, pale brown or ochre, composed of thick-walled hyphae with narrow lumina, including many grana. Asci 8-spored, Lecanora-type, 40–60 × 9–14(–18); ascospores simple, narrowly ellipsoid, (10–)12.1–13.4(–17) × (3.7–)4.0–4.7(–6) μm (n = 45, four specimens used).

Pycnidia seen once, 110–170 μm diam., dark brown; conidia filiform, falcate, c. 15 × 0.5 μm.


Usnic acid, zeorin, thiophanic acid (major constituents), unidentified xanthone (aff. arthothelin), expallens unknown.


On siliceous rocks just above the high tide line; currently known only from SE Alaska.


Lecanora alaskensis was described by Magnusson (Reference Magnusson1932) and until now has been reported only from the type specimen, collected by A. S. Foster at Wrangell, Alaska. The same specimen was originally reported as Lecidea flexuosa Fr. ( = Trapeliopsis flexuosa (Fr.) Coppins & P. James) by Herre (Reference Herre1919). We did not immediately recognize the conspecificity of the new material reported here and the type of L. alaskensis because the type is strikingly dark green, the apothecia have a persistent, somewhat beaded amphithecium, and the discs are dark brown to black. This may be an artifact of shade or other modifying factors (bird excrement) that occasionally darken thalli in supralittoral habitats. Analysis by TLC confirmed the highly distinctive chemical profile of both the type and the recently collected material, including one specimen from GLBA. Remarkably, this secondary metabolite profile (usnic acid, zeorin and a series of xanthones) matches that of L. expallens Ach., typically an epiphytic species. Unlike L. expallens, which is fully leprose, L. alaskensis does not produce asexual thalline propagules and is richly fertile. It also overlaps with the chemistry of L. atrosulphurea, (discussed under the description of L. viridipruinosa earlier in this paper), though that species always has black apothecial discs with a greenish pigment (probably Cinereorufa-green), and the thallus sometimes contains norstictic acid (Edwards et al. Reference Edwards, Aptroot, Hawksworth, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009). We obtained a single mitochondrial SSU DNA sequence (Table 1) but this is not informative enough to place it in a specific clade within the broader genus Lecanora. Although a supralittoral species, L. alaskensis does not correspond to any taxon discussed by Brodo (Reference Brodo2010), most of which probably belong in the genus Myriolecis (Zhao et al. Reference Zhao, Leavitt, Zhao, Zhang, Arup, Grube, Pérez-Ortega, Printzen, Śliwa and Kraichak2015; more recently treated as Polyozosia, see Kondratyuk et al. (Reference Kondratyuk, Lőkös, Jang, Hur and Farkas2019)).

Specimens examined

USA: Alaska: Tongass National Forest, Kupreanof Island, north shore, 57°5′N, 133°50′W, on rocks at high tide line, 1994, K. Dillman 714 (TNFS); Frederick Sound, NE of Petersburg, 56°N, 133°W, growing on rocks at high tide line, 15 v 1994, K. Dillman s. n. (TNFS L-3370); Kupreanof Island, Lindenberg Peninsula, N of Portage Bay, mouth of Todahl Creek, 59°N, 133.17°W [sic; incorrect coordinates], 0 m, growing on rock outcrop above high tide line, K. Dillman 1182 (TNFS-3345); Hessa Island, S Prince of Wales Wilderness, N of Douglass and Seagull Islands, 54.77214°N, 131.3244°W [sic; incorrect coordinates], 100 m, on rock outcrops in muskeg, 1999, K. Dillman 1999-11 (MSC); Etolin Island, west side, S of King George Bay along beach fringe rocks near large waterfall, 56.2908°N, 132.5758°W, 2 m, schist in salt spray zone, 25 vii 2005, L. Geiser s. n. (MSC); Hoonah-Angoon Census Area, Glacier Bay National Park, Fern Harbor area, 58.3100°N, 136.4533°W, 5–15 m, saxicolous on top of boulder under overhanging rock wall (but probably subjected to direct rain), 2012, Tønsberg 41794 (MSC).

Lecanora leptacina Sommerf.

MycoBank No.: MB 388574

Supplementum Florae Lapponiae (Oslo), 96 (1826).—Lecanora varia var. leptacina (Sommerf.) Leight., Lich.-Fl. Great Brit., Edn 3, 177 (1879).—Lecanora intricata var. leptacina (Sommerf.) Stizenb., Ber. Tät. St. Gall. Naturw. Ges., 371 (1882) [1880–81]; type: Norway, Nordland, Saltdal, in Andraeis alpinum summor[um], Aug. 1824, S. C. Sommerfelt s. n. (O-L-000411—holotype!); TLC: isousnic acid, usnic acid, zeorin by TLC).

This is a characteristic species found on Andreaea spp. on acidic rock and boulders in open, more or less oceanic heaths. It was originally described by Sommerfelt (Reference Sommerfelt1826) from Saltdal, Norway. The chemistry of the species appears to be somewhat shrouded in confusion. According to Foucard (Reference Foucard2001) and Edwards et al. (Reference Edwards, Aptroot, Hawksworth, James, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009), the chemical constituents in Lecanora leptacina include psoromic acid, conpsoromic acid and atranorin. However, the type specimen contains usnic acid, isousnic acid and zeorin. Specimens from coastal Norway are concordant with the type specimen in lacking psoromic acid, but may contain small amounts of atranorin. Whether or not material treated as L. leptacina in Scandinavia and the British Isles represents more than one species or only chemotypes is uncertain.

Lecanora leptacina accounts for the ‘known unknown’ species Lecanora sp. S26813 from KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010). The chemistry reported there includes miriquidic acid, but this was almost certainly an artifact of the inclusion of a small fragment of Miriquidica gyrizans (with which it is admixed on the specimen) in the TLC assay. In North America, L. leptacina is otherwise known from previous reports from Alaska (the first being Murray & Murray Reference Murray, Murray and Tieszen1978), as well as from Mt Katahdin, Maine (Fryday Reference Fryday2006).

Lecanora leptacina was regarded as a variety of Lecanora varia and Lecanora intricata by 19th century authors (see synonymy). Our phylogenetic analysis has a limited taxon sample but recovers L. leptacina on an isolated branch between the Lecanora polytropa group and the clade that includes Myriolecis, Protoparmeliopsis and Rhizoplaca (Fig. 10).

Specimens examined

Norway: Nord-Trøndelag: Meråker, N-facing slope of Steinfjellet, 63.3263°N, 12.0095°E, muscicolous on Andreaea mosses on boulder in low alpine heath, 640 m, 2013, Holien 14257 (TRH L-16109); Namdalseid, between Kjerringklumpen and Tverrelva, 64.1331°N, 10.9186°E, muscicolous on Andreaea growing on boulder in low alpine heath, 505 m, 2009, Holien 12403 (TRH L-12988); Steinkjer, SE of Mokk, Litlklumpen, 63.955°N, 12.1331°E, muscicolous on mossy boulder in low alpine heath, 590 m, 2009, Holien 12382 (TRH L-13004).—USA: Alaska: Hoonah-Angoon Census Area, Glacier Bay National Park, Dundas Bay, rock outcrops on alpine ridge, 58.3422°N, 136.4002°W, 435 m, 2012, Fryday 10166 (MSC).

Lepra subvelata (G. K. Merr.) T. Sprib. and similar taxa

The basis for North American Lepra taxonomy continues to be the Pertusaria monograph of Dibben (Reference Dibben1980). Dibben contributed observations of ascomatal characteristics but in assessing the chemistry of species now treated as Lepra he did not take fatty acids into account; thus, species with rich fatty acid profiles are listed by Dibben as ‘chemical constituents unknown’ or ‘unverified’. Two such species are Lepra ophthalmiza and L. panyrga. In the study of lichens of KLGO, Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) reported two distinct chemical strains of L. ophthalmiza (as Pertusaria), which also appeared to be morphologically distinct. One of these, which they reported as Pertusaria sp. TT32951, possessed a characteristic pair of fatty acids identified as nephrosterinic and isonephrosterinic acids, as well as traces of atranorin and chloratranorin (based on analysis of Spribille 15403, GZU). The other, reported as P. ophthalmiza (Nyl.) Nyl., yielded major myelochroic and isomyelochroic acids and accessory atranorin, an unusual substance in Pertusariales (based on analysis of Spribille 24747, KLGO and a series of types, see below). We have now had the chance to study, with the help of J. Elix (Canberra), the chemistry of all relevant types and numerous specimens from western North America. The lichen previously called Pertusaria sp. TT32951 corresponds to the type of Pertusaria subvelata, described by Merrill (Reference Merrill1908) from near Skagway, Alaska. Dibben (Reference Dibben1980) synonymized P. subvelata with Pertusaria panyrga. However, the two, differ in their fatty acid profiles. Hanko (Reference Hanko1983) characterized the chemistry of a number of specimens of L. panyrga from northern Europe and described them as containing the fatty acids 1H (major) and bH in trace amounts. The first substance has not been clarified to our knowledge in any lichen but the second substance has been resolved as (–)-pertusarinic acid (Huneck et al. Reference Huneck, Tønsberg and Bohlmann1986; Shimada et al. Reference Shimada, Hashimoto and Saigo1993). Notwithstanding further work needed on the chemistry of L. panyrga, all three species, L. ophthalmiza, L. panyrga and Pertusaria subvelata (combined into Lepra below), can be easily separated by TLC (Fig. 43).

Fig. 43. Thin-layer chromatography spot patterns in solvent systems A, B and C for fatty acids in Lepra ophthalmiza (from holotype, H), L. subvelata (from isotype, CANL) and L. panyrga (from Greenland: Poelt & Ullrich s. n., August 1983, GZU).

Wei et al. (Reference Wei, Schmitt, Hodkinson, Flakus, Kukwa, Divakar, Kirika, Otte, Meiser and Lumbsch2017) provided a revised phylogeny of Lepra species, including DNA sequences from a GLBA specimen of Pertusaria subvelata that we had previously published (Resl et al. Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015) as Lepra subvelata in their Fig. 1. Contrary to what might be expected given the synonymization by Dibben (Reference Dibben1980), the topology they recovered does not support the monophyly of L. subvelata and L. panyrga. For its part, P. subvelata was strongly supported as sister to much of the rest of the genus Lepra that excludes the L. ophthalmiza group. At the same time, if the vouchers sequenced by Wei et al. (Reference Wei, Schmitt, Hodkinson, Flakus, Kukwa, Divakar, Kirika, Otte, Meiser and Lumbsch2017) were correctly identified, L. panyrga may be part of the L. ophthalmiza complex, which might include additional species not analyzed here. In any case, Wei et al. (Reference Wei, Schmitt, Hodkinson, Flakus, Kukwa, Divakar, Kirika, Otte, Meiser and Lumbsch2017) did not make the formal combination of Pertusaria subvelata into Lepra, which is provided below. Lepra subvelata and L. ophthalmiza occur in the same regions and habitats in western North America but can be distinguished by the prominent, flat-topped fertile warts of L. subvelata, typically with sharply demarcated ‘tower’ walls and often an exposed, bluish grey disc, compared to the whitish grey, flattened, pruinose granule-dominated mounds of L. ophthalmiza, as outlined in the key below.

Lepra ophthalmiza (Nyl.) Hafellner

MycoBank No.: MB 818770

Stapfia 104(1), 173 (2016). —Pertusaria multipuncta var. ophthalmiza Nyl., Lich. Scand. (Helsinki), 180 (1861).—Pertusaria ophthalmiza (Nyl.) Nyl., Flora 48, 354 (1865); type: Finland, Lapponia kemensis, 1856, Edwin Nylander (H-NYL 33726—holotype!; myelochroic acid (major), isomyelochroic acid (major), atranorin (trace) determined by HPLC).

Pertusaria multipuncta f. sphaerulifera Erichs., Feddes Repert. 35, 386 (1934); type: Canada, British Columbia, Aleza Lake, ad corticem abietis, 24 vii 1931, V. Kujala (H—holotype! and isotype!; myelochroic acid [major], isomyelochroic acid [major], atranorin [trace] detected in both specimens by HPLC).

Pertusaria lecanina subsp. nigra Fink in Hedr., Mycologia 26, 160 (1934).— P. lecanina var. nigra (Fink) Zahlbr., Cat. Lich. Univers. 10, 454 (1940); type: USA, Montana, [Lake Co.,] Rost Lake, dead yew tree at 3000 ft, 15 July 1901, W. P. Harris (MICH—lectotype!, designated by Dibben (Reference Dibben1980); myelochroic acid [major], isomyelochroic acid [major], atranorin [trace] determined by HPLC).

Lepra panyrga (Ach.) Hafellner

MycoBank No.: MB 818771

Stapfia 104(1), 173 (2016). —Urceolaria panyrga Ach., Methodus Lichenum, Sectio prior (Stockholmiæ): 146, tab. IV, fig. 2 (1803). —Pertusaria panyrga (Ach.) A. Massal., Framm. Lichenogr., 53 (1855); type: Lapland, habitat in radicibus et caulibus herbarum prope terram, quos incrustat in Alp., Wahlenberg (H-ACH, n.v.).

Lepra subvelata (G. K. Merr.) T. Sprib. comb. nov.

MycoBank No.: MB 830126

Basionym: Pertusaria subvelata G. K. Merr., Bryologist 11, 111 (1908); type: USA, Alaska, on birch bark at Skagway, 4 September 1902, [G. K. Merrill s. n.] (FH—holotype, n.v.; CANL—isotype!; nephrosterinic and isonephrosterinic acid by TLC).

Key to distinguish Lepra ophthalmiza, L. panyrga and L. subvelata

  1. 1 Apothecia embedded in soralium-like warts, typically not with corticate, ringed edges; apothecial disc seldom clearly visible, pinkish; myelochroic and isomyelochroic acids as major substances.L. ophthalmiza

    Apothecia usually highly raised above thallus, often with ring-like, corticate folds surrounding the wart; apothecial disc often visible, greenish pruinose; myelochroic and isomyelochroic acids absent 2

  2. 2(1) With nephrosterinic and isonephrosterinic acids; epiphytic.L. subvelata

    With fatty acids 1H (major) and (–)-pertusarinic acid (trace; bH sensu Hanko (Reference Hanko1983)); terricolous over bryophytes in tundra L. panyrga

Ochrolechia xanthostoma (Sommerf.) K. Schmitz & Lumbsch and similar taxa

Brodo (Reference Brodo1988) studied a group of Pertusaria species characterized by apothecia with one to several perithecioid ostioles in a wart, thin-walled ascospores and the presence of alectoronic acid, sometimes among other substances, as a secondary metabolite. He transferred them to Ochrolechia and recognized two species, O. rhodoleuca (Th. Fr.) Brodo from northern Norway and O. subplicans from the northern Pacific; the latter with two subspecies, subsp. subplicans (Nyl.) Brodo and subsp. hultenii (Erichsen) Brodo. He mentioned the existence of an additional taxon, Pertusaria xanthostoma (Sommerf.) Fr., which he acknowledged was similar to O. subplicans subsp. hultenii but possessed different substratum preferences (corticolous and terricolous) and four, rather than eight, ascospores per ascus. Schmitz et al. (Reference Schmitz, Lumbsch and Feige1994) subsequently transferred P. xanthostoma into Ochrolechia.

Two lichens from this group are present in GLBA. The first occurs on rock both along seashores and in the alpine zone, and is a good match for O. subplicans subsp. hultenii (see ‘Catalogue of All Named Taxa Found’). The second occurs on bark and wood and appears to correspond to the species reported by Brodo & McCune (Reference Brodo and McCune2017) as O. xanthostoma. However, we came to suspect it may not belong to O. xanthostoma s. str., as it typically produces only one ostiole per wart, as opposed to 2–4 (and up to 8). Resolving whether or not the GLBA corticolous material is conspecific with O. xanthostoma requires an assessment of the variability within that species.

Ochrolechia xanthostoma was originally described from juniper bark in the area around Bodø, Nordland, Norway by Sommerfelt (Reference Sommerfelt1823, as Porina xanthostoma; lectotypes in O, see Kukwa Reference Kukwa2011). It has been reported from Norway, Iceland and Scotland, as well as North America, Russia, Greenland and Australia (Kukwa Reference Kukwa2011). In Europe, the application of the name has been extended to cover material from rock at Ben Lawers, Scotland described by Nylander (Reference Nylander1865) as Lecanora poriniformis Nyl. (UPS-L-717928, isolectotype!). Like the northern Pacific O. subplicans subsp. hultenii, L. poriniformis was described as having 6–8 ascospores per ascus (though no 8-spored asci were found by Kukwa Reference Kukwa2011). Lecanora poriniformis was only moved to Pertusaria as late as Clauzade & Roux (Reference Clauzade and Roux1985) and later treated as a synonym of O. xanthostoma by Kukwa (Reference Kukwa2011). Ochrolechia xanthostoma was first reported from North America by Räsänen (Reference Räsänen1933) from New Brunswick, but the specimen upon which that was based was shortly thereafter named as the new species P. rubefacta Erichsen (Erichsen Reference Erichsen1934; Dibben Reference Dibben1980), which does not appear to be closely related. Pertusaria xanthostoma was subsequently reported by Dibben (Reference Dibben1980) from areas surrounding the hypermaritime Gulf of Alaska and the Aleutian Islands, from British Columbia by Noble et al. (Reference Noble, Ahti, Otto and Brodo1987; no voucher cited), and from British Columbia and Oregon by Brodo & McCune (Reference Brodo and McCune2017).

We sequenced DNA from multiple specimens from Alaska and the one specimen labelled O. xanthostoma from Europe that was fresh enough to obtain DNA from, which however came from rock. We found the GLBA material to be genetically distinct from the European specimen labelled as O. xanthostoma, and both together formed a sister group to O. subplicans subsp. hultenii within a strongly supported, monophyletic Ochrolechia (Fig. 6). It is tempting to conclude that these data support the interpretation that GLBA corticolous material is distinct from O. xanthostoma. However, while it is true that material from the type locality of O. xanthostoma has multiple ostioles per verruca, some corticolous European specimens studied at UPS have 1–2 ostioles per verruca and look similar to those from GLBA. This means that, strictly speaking, we still cannot rule out 1) that the saxicolous European specimen sampled may be a second European species distinct from O. xanthostoma, and 2) that the range of variability of the European corticolous material encompasses that of the GLBA corticolous material, and that they are conspecific. We consider the latter scenario unlikely, but no fresh European corticolous material is available to us to directly test this hypothesis; the most recent specimen collected from bark that we could find in Norwegian herbaria was from 1981. For this reason, we refrain from describing the GLBA corticolous material as a new species, and treat it as Ochrolechia sp. S38011 (see ‘Known Unknowns’).

Yet another taxon exists that has not previously been discussed in the context of this group, namely Perforaria minuta Degel., and while it is likely not relevant to delimiting O. xanthostoma, this may be as good of a place as any to take it into account and correct some misinformation about its characters. Degelius (Reference Degelius1937) described P. minuta from a small specimen collected on Kodiak Island by Eric Hultén. The species was characterized by poriform ascomata and punctiform soralia on a creamish thallus over Picea bark. Brodo (Reference Brodo1973) placed P. minuta as a synonym under Coccotrema pocillarium (Cumm.) Brodo, but John Elix studied the chemistry of the soralia and several ascomata from the specimen by HPLC (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) and found it to contain alectoronic acid. In keeping with an annotation by Rolf Santesson on the type specimen, Spribille et al. validated the combination Coccotrema minutum (Degel.) R. Sant. ex T. Sprib. et al. and published a photograph of the type. However, the first author (TS) missed some important details. Brodo (Reference Brodo1973) stated, based on personal communication from Santesson, that the type possessed cephalodia and the chemistry of Coccotrema pocillarium (Cumm.) Brodo (that is, stictic and constictic acids and an unknown). Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) neglected to notice that the type specimen showed no indication that its chemistry had been tested, other than perhaps via spot test (discoloration in the corner of one thallus fragment). More critically, they failed to notice that the type specimen lacks cephalodia (and they were also not noted in Degelius’ detailed protologue, which mentioned only a green alga (‘protococcaceae’)). The lack of cephalodia, in addition to the secondary metabolite profile of the type specimen (alectoronic acid), makes it clear that P. minuta does not belong in Coccotrema but instead is related to the alectoronic acid-containing species of poriform Ochrolechia discussed here. To rectify the taxonomic position of P. minuta, we propose to accommodate it in Ochrolechia.

Ochrolechia minuta (Degel.) T. Sprib. comb. nov.

MycoBank No.: MB 830127

Perforaria minuta Degel., Acta Horti Gothoburg. 12, 122 (1937).—Coccotrema minutum (Degel.) R. Sant. ex T. Sprib. et al., Bryologist 113(3), 449 (2010); type: USA, Alaska, Kodiak Island Borough, ‘ad Kodiak in insula Kodiak in cortice Piceae’, 1932, E. Hultén 5030b (UPS—holotype, studied again July 2019).

Steineropsis alaskana T. Sprib. & Muggia

MycoBank No.: MB 516028

Bryologist 113(3), 454 (2010); type: USA, Skagway Borough, White Pass, 59°37.147′N, 135°09.657′W, 1051 m, on rock in snowbed with late-lying snow, 2008, Spribille 26809 & Pérez-Ortega (US—holotype; NY—isotype).

(Fig. 44)

Fig. 44. Steineropsis alaskana (Mendenhall Glacier, 21 September 2010, Spribille s. n., ALTA). A & B, habit of thallus with apothecia. Scales: A = 2 mm; B = 1 mm.

Apothecia (Fig. 44) biatorine, 0.8–1.5 mm diam., sessile, slightly convex; disc red-brown with a paler proper margin; thalline isidia forming an irregular pseudothalline margin. Exciple of radiating hyphae 3–4 μm thick; cells c. 10 μm long; cortical cells isodiametric c. 4–5 μm across, dilute brown. Hymenium c. 150 μm tall, KI−; paraphyses c. 1.5–2.0 μm thick, simple or sparingly branched and anastomosing, not or only slightly widening at the apex (to 3 μm); epihymenium dilute brown c. 10 μm tall. Hypothecium hyaline, composed of randomly organized hyphae, dilute brown near base with a dark brown lower edge. Asci cylindrical, 60–80 × 12–15 μm, KI+ pale yellow, Pannaria-type sensu Spribille & Muggia (Reference Spribille and Muggia2013); ascospores broadly ellipsoid, 18–20 × 9–11 μm, wall <1 μm thick, not ornamented.

The genus Steineropsis T. Sprib. & Muggia was described to accommodate a sterile placodioid cyanolichen from south-eastern Alaska, named S. alaskana T. Sprib. & Muggia (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010). Spribille & Muggia (Reference Spribille and Muggia2013) subsequently presented molecular data to support the position of Steineropsis as sister to Protopannaria (Gyeln.) P. M. Jørg. & S. Ekman in the Pannariaceae (Collematineae) and also mentioned recently discovered fertile material. The ascomata of the species have, however, not been formally described until now.

Fertile specimens examined (additional sterile collections listed in ‘Catalogue of All Named Taxa Found’)

USA: Alaska: near Juneau, Mendenhall Glacier Visitor's Centre, 58°24.985′N, 134°32.692′W, 77 m, abundant, saxicolous on seepy rock, 2010, Spribille s. n. (ALTA, GZU); Glacier Bay National Park, Excursion Ridge, ridgetop, 58.46503°N, 135.55757°W, 903 m, 2012, Spribille 39437 (MSC); Petersburg Borough, Patterson Glacier, 56.9356°N, 132.6530°W, 130 m, rock outcrop in mature Alnus forest, 2015, Fryday 11146, 11153, 11155 & K. Dillman (MSC).

Steineropsis laceratula (Hue) T. Sprib. & S. Ekman comb. nov.

MycoBank No.: MB 830128

Pannaria laceratula Hue, Bull. Soc. Bot. Fr. 48, LIX (1902) [1901]. —Fuscopannaria laceratula (Hue) P. M. Jørg., J. Hattori Bot. Lab. 76, 205 1994); type: Japan, Hakkoda, sur Betula, 1200 m, 10 August 1904, Faurie 5946 (W—isotype!).

Sequences generated from an epiphytic specimen of Fuscopannaria laceratula (USA, Alaska, Tongass National Forest, c. 5 km N of Petersburg, Sukoi Islets, on Picea sitchensis, Nash 43995, BG) alerted Ekman et al. (Reference Ekman, Wedin, Lindblom and Jørgensen2014) to the evolutionary proximity of this species to Steineropsis (see also Lendemer et al. Reference Lendemer, Stone and Tripp2017). Our three-locus dataset from a rock-dwelling specimen from the outer coast of GLBA confirms this placement (Fig. 9).

The similarity of S. laceratula to S. alaskana is striking enough that some members of the field expedition assumed, on first impression, that S. laceratula was an epiphytic occurrence of the locally more common S. alaskana. The two share a characteristic range of cervine brown cortical pigments (illustrated for S. alaskana in Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) and in Fig. 44), and also lack an amyloid apical ring structure in the ascus. Steineropsis laceratula was reported to possess such a structure by Jørgensen (Reference Jørgensen2000), but this was lacking in material we studied (e.g. Brodo 14150, UPS L-563845). Instead, the ascus compares favourably with that in S. alaskana and Protopannaria (see Spribille & Muggia Reference Spribille and Muggia2013: Fig. 3P).

The inclusion of Fuscopannaria laceratula in Steineropsis expands that genus to now include both an apparently obligately saxicolous species (S. alaskana) and a species usually found on tree bark but secondarily also on rock (S. laceratula), and extends the distribution of the genus to East Asia.

Known Unknowns

We treat as ‘known unknowns’ lichens for which we have no names, but which we are convinced are not otherwise accommodated in species included in the study. Some of these may constitute species new to science, and indeed several are well known to us but material or data have not been sufficient for proceeding with a description. In other cases, identification is not currently possible as a worldwide taxonomic treatment for the group in question is lacking, and thus a validly published name possibly already exists.

  • Amygdalaria sp. F10121 — Saxicolous on pebbles on beach ridges and in sparse alpine tundra, 0–922 m. EX: 319, S37941; 407, F10121; WA: 319, S37941; 105, F9999, F10000; 391, S38637 (sub Lecanora polytropa). This species appears to be close to Amygdalaria consentiens, differing mainly in the pseudocyphellate pseudothalline margins of the ascomata. We have obtained a single ITS rDNA sequence (Table 1) but are prevented from comparing it in the absence of a more comprehensive sampling of A. consentiens, for which we currently have no ITS sequences. Also seen from the Olympic Peninsula of Washington (Clallam Co., 47.8564°N, 123.0359°W, R. Droker 16 June 2015-1, MSC).

  • #Arthonia sp. S38095 — Lichenicolous on Lecanactis, over bark of Picea sitchensis, 124 m. DUN: 334, S38095. Ascospores are 1-septate, c. 10 × 3 μm with the upper cell slightly larger than the lower.

  • Arthonia sp. S38167 — Corticolous on Picea sitchensis twig, 27 m. DUN: 339, S38167. This species is similar to A. arthonioides in possessing 2–3-septate ascospores, 12–15 × 5–6 μm, but differs in having an I+ blue hymenium, and in the different habitat.

  • Arthonia sp. S38303 — Lignicolous on sheltered, soft lignum of giant stump, 568 m. EX: 357, S38303. Botryose apothecia with dark hypothecium and KOH− hymenium, I+ blue after KOH; ascospores not seen. Despite not observing ascospores, no other species in the current survey matches this specimen.

  • Arthopyrenia sp. S38039 — Corticolous on Alnus, 33 m. GUS: 879, S36809; [V329, S38039, S38055]. This species does not match any species of Arthopyrenia known to us. The ascospores are 3-septate and brown, c. 16 × 6 μm.

  • Arthopyrenia sp. S39514 — Corticolous on Alnus and Salix, 10 m. DUN: 463, S39514; WA: 384, S38506. Following Harris (Reference Harris1975), this species would key to Arthopyrenia analepta, but ascospores are narrower and longer (17–18 × 4–5 μm), breaking at the septum. The perithecia tend to be smaller than in GLBA collections of A. analepta (not much more than 130 μm diam.) and the perithecium wall is brown, KOH+ paler or brownish, lacking green-black pigments. It is similar to the description of Sporoschizon petrakianum Riedl, from Austria (Riedl Reference Riedl1960), which has been treated as a synonym of Naetrocymbe punctiformis (Hafellner & Türk Reference Hafellner and Türk2016). In GLBA this appears to be a distinct species.

  • Bacidia sp. S36806 — Corticolous on Alnus and Salix, 20 m. GUS: 879, S36806 (UPS); [574, T41821]; 547, T41847. This is a member of Bacidia s. str. with weak brown pigmentation and minute crystals in the excipulum. Internally it resembles B. absistens but the exterior looks different, with small, piebald apothecia that are comparatively more convex.

  • Bacidina sp. A — Lichenicolous over senescent Peltigera collina, 60 m. GUS: 857, S36164. This corresponds to Bacidina sp. A of Spribille et al. (Reference Spribille, Björk, Ekman, Elix, Goward, Printzen, Tønsberg and Wheeler2009).

  • Bellemerea sp. F9943 — Saxicolous on granitic rock, 0–30 m. EA: just S of terminus of Riggs Glacier, F10651; WA: 319, SS37933; 326, S37993 (sub Rhizocarpon lecanorinum); 386, S38536; 102, F9928, F9943 (sub Rhizocarpon lecanorinum); 103, F9950, S37933, S37940, S37994; 205, M2492. TLC: norstictic and gyrophoric acids. Similar to B. cinereorufescens but separated from that species and all other species of the genus by the raised apothecia with a thick thalline margin and an umbonate disc, and the tall hymenium (100–125 μm high). We initially intended to describe this as a new species from GLBA but molecular work in Bellemerea, including on GLBA specimens, has shown it to be nested within a more widespread species occurring throughout the western cordillera as far south as Montana (T. Wheeler, personal communication). Specimens with umbonate apothecia have also been seen by us elsewhere (e.g. in Montana; TS).

  • Bilimbia sp. S38926 — Corticolous on Cupressus nootkatensis and Populus balsamifera, 0–68 m. DUN: 413, S38926; GB: 874, S36699. Similar to B. microcarpa but differing from typical specimens in the thin and immersed thallus, the darker hypothecium, and ascospores with a tendency to have constricted septa.

  • Chaenotheca sp. S38742 — Corticolous in sheltered underhangs of large, leaning Cupressus nootkatensis, 237–250 m. EX: 401, S38739, S38742, S38743; 446, S39339, S39340. This species possesses a powdery greenish thallus that fades to white in herbarium specimens; the ascomata are borne on stalks which are pale basally, with distinct white pruina on the upper stalk and capitulum. No substances were detected by TLC. An mtSSU sequence was obtained (T1137, Table 1) but is insufficient to place the species at the present time due to the low level of sampling of this locus in the genus.

  • Chaenothecopsis sp. 7 — Lignicolous on snag, 569 m. EX: 358, S38326, S38331, S38332. This appears to correspond to Chaenothecopsis sp. 7 (‘viridis’) of Goward (Reference Goward1999). See also the discussion of this species by Titov (Reference Titov2006; English and German translation of keys by Stordeur et al. Reference Stordeur, Braun and Tkach2010).

  • Chaenothecopsis sp. S37846 — Lignicolous on snag, 222 m. EX: 313, S37846. Capitulum KOH−, appearing lightly pruinose, stalk dark, c. 1 mm, with a paraplectenchymatous-type cellular structure; asci c. 40–45 × 4 μm, with apical canal at maturity; ascospores 6.5–8.5 × 3–3.5 μm, pigmented lightly brown, smooth, with ± pointed ends. This species is similar in the dimensions of the asci and ascospores to Chaenothecopsis sp. 7 (above) but differs in the lack of aeruginose pigments and the presence of distinctive pruina around the excipulum. It also differs from the Chinese Chaenothecopsis tibellii Titov in the lack of ascospore ornamentation (see Titov Reference Titov2006; English and German translation of keys by Stordeur et al. Reference Stordeur, Braun and Tkach2010).

  • Cliostomum sp. S36738 — Corticolous on Picea sitchensis in or immediately behind beach fringe, 2 m. GUS: 876, S36738 (sub C. leprosum); 341, S38234; 436, S39161. TLC: sphaerophorin. A sterile species consisting of an inconspicuous white thallus with irregular sorediate patches. The species is characterized by the presence of sphaerophorin, an uncommon substance. The genus is speculative.

  • Cliostomum sp. T41758 — Lignicolous on snag, 37–569 m. DUN: 563, T41758; EX: 108, F10045; [858, S36191]; 358, S38305; [V431, S39054]. An unknown sorediate-leprose species consistently bearing large, black, pyriform pycnidia c. 0.25 mm diam.; wall pale brown (KOH yellowish brown); conidia short oblong, 3.5–4.0 × 1.5–2.0 μm. TLC revealed only an unidentified pigment. The genus is speculative and this could alternatively be a species of Anisomeridium.

  • [Fuscopannaria sp. T41714b — Corticolous on trunk of Populus balsamifera, 16 m. GUS: 557, T41714b. This species has elongated lobes and marginal/terminal, bead-like soredia. It could not be identified to genus by P. M. Jørgensen (personal communication, 2013). We place it provisionally in Fuscopannaria.]

  • Gyalideopsis sp. S39617 — Muscicolous on log in upper beach meadow, 0–2 m. GUS: 437, S39167. This species differs from the locally common G. epicorticis in the long elongated, not hooked, conidial mass, strongly resembling G. cyanophila (Sérusiaux Reference Sérusiaux1998). The material is sparse and not fertile.

  • Gypsoplaca sp. S38752 — Saxicolous on argillite, 830 m. EX: 404, S38752. This specimen was included by Garima Singh in an evolutionary study of Protoparmelia, but published results of DNA sequences (Singh et al. Reference Singh, Dal Grande, Divakar, Otte, Leavitt, Szczepanska, Crespo, Rico, Aptroot and Cáceres2015) as well as a subsequent phylogenetic analysis (Shi et al. Reference Shi, Wang, Zhou, Liu, Zhang, Yang, Timdal and Wang2018) indicate it is an undescribed member of the genus Gypsoplaca.

  • Halecania sp. S38343 — Saxicolous on argillitic rock, 895 m. EX: 370, S38343. Similar to H. athallina (newly described in this paper) but with apothecia on small discrete areoles.

  • Hypogymnia sp. S36014 — Corticolous and lignicolous on Tsuga bark, 48–713 m. GUS: 855, 36014; EX: ‘Mooselator’ [west slope of Excursion Ridge], S38905. This species has the chemistry of H. wilfiana Goward et al. (atr, physodic and 2′-O-methylphysodic acids) but lacks apinnatic acid. In addition, it differs in its trailing habit, with slightly upturned lobe tips that tend to end in flared ‘thumbs’ (as opposed to the ‘paws’ formed by H. wilfiana).

  • Hypogymnia sp. S36481 — Corticolous on Alnus bark, 30 m. GB: 868, S36481. This species superficially resembles H. vittata in possessing trailing, narrow lobes with lobe tips that end in flared hood-soralia. However, it differs in that the lower surface is completely eroded, recalling the East Asian species H. fragillima, and in chemistry (atr, physodic and 2′-O-methylphysodic acids), lacking vittatolic acid, which is otherwise present in all specimens of H. vittata tested in GLBA (n = 10).

  • Hypogymnia sp. S38816 — Corticolous on krummholz Picea, 922 m. EX: 407, S38802, S38816. This is a ‘Cavernularia’-type Hypogymnia in which the entire upper surface is covered with erumpent isidia; soredia, pycnidia and apothecia are absent. The form was not recognized in the field, where it was mistaken for Imshaugia aleurites. This species contains atranorin, physodic acid and unidentified substances. An ITS sequence from S38816 (isolate DNA T1315, Table 1) has base call ambiguities at 14 positions relative to a reference sequence of Hypogymnia lophyrea (HQ725073), which could indicate the presence of multiple haploid strains in the PCR template.

  • Lecanora sp. F10122 — Saxicolous on alpine argillite, 922–942 m. EX: 375, S38425; 407, F10122, S38827; 408, S38863. TLC: atr. This is a member of the L. formosa group, probably related to our new species L. viridipruinosa (described above). It differs from the latter in possessing a scurfy, rimose thallus and lacking zeorin. The apothecia apparently vary from pruinose (S38425) to somewhat shiny (F10122). DNA sequences (isolate T1181, Fig. 10) support its distinctness.

  • Lecanora sp. F10126 — Saxicolous, 618–922 m. DUN: 428, S39021 (aeruginose form; sub Euopsis granatina); EX: 407, F10126; 408, S38865 (sub Sagedia simoënsis). This appears to be a member of the L. polytropa group with strongly aeruginose apothecia. TLC: usnic acid, zeorin.

  • Lecanora sp. S36321 — Corticolous on dead Alnus twigs below eagle perches, c. 0–5 m. GB: 864, S36353, S36355 (sub Physcia adscendens); Willoughby Island, S36321 (leg. A. Fryday). TLC: usnic and cf. variolaric acids. Ascospores 10 × 5.5 μm; apothecial section with POL+ crystals, KOH−, C−, PD−. We know of no species with this chemistry.

  • Lecanora sp. S38412 — Saxicolous on argillite on alpine ridgetop, 919 m. EX: 374, S38412. TLC: atr, roccellic/angardianic acids. This species is morphologically similar to L. gangaleoides but lacks the characteristic substance gangaleoidin. We have sequenced the ITS and mitochondrial SSU rDNA of this specimen (isolate T1333, Fig. 10, Table 1) but cannot place it with certainty without a more comprehensive molecular taxon sampling of Lecanora s. lat.

  • Lecanora sp. S38599 — Corticolous on Salix, 2 m. WA: 391, S38599, S38605. TLC: atr, zeorin. Known from two collections, this is a member of the L. subfusca group, similar to L. glabrata, with atranorin and a faint trace of zeorin and no detectable fatty acids. The asci are strikingly thick-walled but no ascospores could be found in our material. The epihymenium lacks a continuous crystal layer; instead it is inspersed with scattered, fine crystals.

  • Lecanora sp. T41777 — Lignicolous on driftwood, 2 m. DUN: 571, T41777. Similar to L. symmicta but with strongly clustered apothecia and possessing only an unknown pigment in TLC.

  • Lempholemma sp. S39326 — Terricolous on silt over bedrock in creek, 155 m. EX: 444, S39326. Similar to L. radiatum but with wider, canaliculate lobes.

  • Lepraria sp. S39564 — Terricolous on roots under tip-up, 9 m. DUN: 463, S39564. TLC: atr, angardianic/roccellic acid, stictic acid + satellite, two pigments. This does not fit any species known to us, but the material is insufficient to describe it here as new.

  • Megalaria sp. F10005 — Saxicolous on an upper beach pebble, 0–5 m. WA: 105, F10005. This species differs from known species of Megalaria in being saxicolous, as well as in having smaller ascospores (15‒17 × 5‒6 μm) and a hyaline hypothecium. The placement in Megalaria is provisional, and is based on the 1-septate ascospores and Lecidella-type ascus structure. The type specimen of Megalaria, M. grossa, possesses a Lecidella-type ascus and not Lecanora-type as usually reported (e.g. Hafellner Reference Hafellner1984).

  • Micarea sp. F10313 — Corticolous, 687 m. EX: 448, F10313. Unpigmented apothecia; ascospores 3-septate, 25–28 × 4–5 μm; internally unpigmented, C−, KOH−. This species may be a gyrophoric acid-deficient form of M. peliocarpa; the ascospore size is comparable to M. alabastrites, but the epihymenium in that species is C+ red.

  • Micarea sp. F10320 — Saxicolous on rocks near ground level in snowbed (upper bay) or subalpine ridges, 43–700 m. EX: 449, F10320 (sub Rhizocarpon anaperum); WA: 319, S37940. This species has a pale grey, almost white thallus, a red-brown, KOH− hypothecium and an unidentified lichen substance detected by TLC. It is similar to Micarea subconfusa (which has a smaller and lead grey thallus) and M. assimilata (which is muscicolous and has a KOH+ red hypothecium). No other species with secondary chemistry is known in the M. assimilata group.

  • Micarea sp. S38509 — Corticolous on Shepherdia canadensis, 10 m. WA: 384, S38508 (sub ‘Unknown genus S38989’), S38509 (sub Biatora meiocarpa). TLC: methoxymicareic acid (G. Thor, 7/2019). Similar to Micarea nowakii Czarnota & Coppins in the size of the apothecia and ascospores and the presence of KOH+ mauve pigments, but differing in thallus chemistry (methoxymicareic instead of micareic acid).

  • Mycocalicium sp. S39331 — On Tsuga resin, 155 m. EX: 444, S39331. Stalk KOH+ bleeding reddish brown; ascospores 8–9 × 4.5–5 μm, with distinctly blunt ends.

  • Myochroidea sp. S39317 — Corticolous on Salix, 2 m. EA: near 438, S39317. Similar in morphology to Myochroidea minutula, with ascospores 10 × 5 μm, but disc distinctly concave.

  • Ochrolechia sp. S38011 — Corticolous on Alnus, Cupressus nootkatensis, Picea sitchensis, Populus balsamifera and Salix, on Tsuga twigs and also lignicolous on beach logs, 0–58 m. DUN: 462, S39728; 463, S39528; 467, S39671; EA: 122, F10228; near 438, S39303, S39304; EX: 858, S36180; GB: 864, S36340, S36368; 868, S36475, S36534; 327, S38011; S Sandy Cove, S40751; GUS: 857, S36123; 876, S36744; 878, S36783; 879, S36802; 434, S39103; 230, M2753; 556, T41657; 576, T41835; WA: 391, S38593, S38603; 549, T41640. This species is discussed at length in the ‘Other Species Treated in Detail’ section and appears to be related to Ochrolechia xanthostoma, a species reported from Norway, Scotland and New Zealand. It is not possible to determine whether the GLBA material is a new species, however, until the status of O. xanthostoma s. str. is resolved and more is known about the range of variability of the sorediate taxon O. minuta, which was described from Kodiak Island, Alaska.

  • Ochrolechia sp. S38864 — Saxicolous on the highest ridgetop rocks, possibly snow-free most of winter, 942 m. EX: 408, S38864. TLC: gyrophoric acid. A species with a thick thallus formed of peculiar bullate areoles that, over time, turn tan in herbarium specimens. The cortex is C+ red, the medulla C−. The cortex is also heavily inspersed with small crystals that dissolve in KOH to give a yellow solution. DNA was obtained (isolate T1341, Fig. 6) and suggests that this species is distinct from O. tartarea (L.) A. Massal., a species that can share a similar thallus morphology.

  • Ochrolechia sp. S38970 — Muscicolous on exposed rock, 406 m. DUN: 423, S38968, S38970. TLC: gyrophoric and lecanoric acids, 1–2 fatty acids. A sterile species characterized by areoles which break open and reveal soredia within, in some cases forming small irregular ‘hoods’. A collection from Excursion Ridge (EX: 455, 39421) is not an exact morphological match but may also belong here, and the chemistry is similar (gyrophoric and lecanoric acids, one fatty acid).

  • Palicella sp. T41595 — Corticolous on Salix, 2 m. WA: 391, S38598; 542, T41595, T41597. TLC: usnic acid, zeorin, 1–3 unidentified pigments. The GLBA material resembles Palicella filamentosa in habit but that species contains atranorin, usnic acid and paraensic acid D (Palice et al. Reference Palice, Printzen, Spribille and Elix2011). The material differs from L. symmicta in its small, highly convex, brown apothecia.

  • Parmeliella sp. S24412 — Terricolous on fine organic accumulations, 903–918 m. EX: 454, S39414; 455, S39453. This matches Parmeliella sp. S24412 from KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010), DNA sequences of which were already published by Muggia et al. (Reference Muggia, Nelson, Yakovchenko, Tønsberg and Spribille2011; 28S and mitochondrial SSU from two specimens). It is ecologically and morphologically distinct from Parmeliella triptophylla, but unfortunately our material is not sufficient to describe it as a new species. This would also require the review of numerous types, an effort that is beyond the scope of this study.

  • Pertusaria sp. S26420 — Saxicolous on underhang, 10 m. WA: 384, S38523. This appears to be an exact match to Pertusaria sp. S26420 from KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010). The thallus reacts KOH+ red needles in section (norstictic acid) and contains pinkish pigments in the soralia. The genus is speculative.

  • Pertusaria sp. S38786 — Saxicolous (closely adhering to rock) on argillite in the alpine zone, 903–922 m. EX: 406, S38786; 407, S38835. TLC: norstictic acid. This species is similar to P. alaskensis, described from Unalaska (Erichsen Reference Erichsen1938), but differs in having ascospores 6 per ascus (observed on intact asci), 80–98 × 26–28 μm, and an epithecium KOH+ magenta.

  • Pertusaria sp. S39274 — Corticolous on Alnus, 2 m. EA: 441, S39274. Similar to P. sommerfeltii but possesses warts with a highly constricted base and a whitish rim around the ostiole; the hymenium is creamish, KOH+ intensifying, and the ostiole is brown and KOH−.

  • Pertusaria sp. T41520 — Corticolous on Tsuga trunks, 40 m. GUS: 341, S38257; 531, T41520. TLC: fpc. This species is unusual in being dominated by large, pink pycnidia (conidia rod shaped, c. 5 × 1 μm), giving it the habit of an Ochrolechia, but containing fumarprotocetraric acid.

  • Placopsis sp. F9765 — Saxicolous on rocks in recently deglaciated forefields, 50 m. EA: 869, F9765 (sub P. fusciduloides). This is an undescribed member of the P. lambii group (dubbed Placopsisscripta’ by Schneider et al. (Reference Schneider, Resl and Spribille2016): Fig. 2, a nomen nudum) characterized by darkly pigmented soredia in soralia arranged perpendicular to the lobe axis. It will be described in detail elsewhere.

  • Placopsis sp. S39599 — Saxicolous on rocky headlands and boulders, 0–11 m. DUN: 463, S39599; EA: 872, S36598; EX: 217, M2609; 218, M2663; GUS: 876, S36752. This species has often been referred to P. lambii in the western North American literature but differs from that species in, amongst other things, possessing cephalodia. It also differs from P. fusciduloides in its mostly epruinose lobe tips. It will be described elsewhere.

  • Placynthium sp. S38458 — Saxicolous on limestone, 15–22 m. GB: 864, F9720, F9725, F9730; WA: 318, S37914; 381, S38458. Specimen S38458 was sequenced and clusters with a specimen from Coronation Island on the Tongass NF (isolates T1310 and T1304, respectively; Fig. 9), and broadly with other specimens identified in the past as P. nigrum from western North America. However, none of the material so far sequenced from western North America, except one specimen from Montana, genetically matches European P. nigrum. Specimens have 3-septate ascospores. It is possible that material with 1-septate and 3-septate ascospores is genetically distinct and the assumption that they are not by Henssen (Reference Henssen1963) has led to a species circumscription that is now heterogeneous. We cannot rule out at this point that this species occurs in Europe and already has a name.

  • Placynthium sp. S38419 — Saxicolous in the alpine zone, 936 m. EX: 375, S38419 (sub Lecanora viridipruinosa). This Placynthium species differs from all others collected in its combination of 1-septate ascospores and thick paraphyses. A DNA sequence (isolate T1305, Fig. 9) was recovered in the P. asperellum group.

  • Platismatia sp. S38191 — Corticolous on Picea sitchensis and Tsuga heterophylla branches, 0–27 m. DUN: 339, S38191; GB: 868, S36519. TLC: atr, caperatic acid. This morph, collected at Fern Harbor and Seebree Island, has much smaller pycnidia than P. glauca and does not develop a dark lower surface; it could easily be confused with a pale Tuckermannopsis chlorophylla. Extractions have yielded DNA but no PCR products have been obtained.

  • Polycauliona sp. S39572 — Saxicolous on rocky headlands, 10 m. DUN: 463, S39572, S39573. Analysis of ITS rDNA sequences (including isolate T1301 (Table 1) and a sequence from a specimen from Mitkof Island, below) based on the taxon sample of Arup et al. (Reference Arup, Søchting and Frödén2013) suggest that this species is sister to Polycauliona candelaria. In GLBA and elsewhere in SE Alaska, this species appears to be restricted to the upper supralittoral zone, which combined with its thick, strap-shaped lobes distinguish it from the other frequent species of Polycauliona in the area, P. pollinarioides (see ‘Catalogue of All Named Taxa Found’). The latter species can occur on both coastal rocks and trees. We hesitate to proceed with describing a new species after sequencing a specimen from Vancouver Island, British Columbia (data not shown) that morphologically fits the GLBA material but yielded an ITS rDNA sequence corresponding to P. pollinarioides. Other specimen examined: Mitkof Island, Fryday 10661 (MSC; DNA voucher KS140, Table 1).

  • #Polycoccum sp. P2287 — Lichenicolous on Acarospora sp. near glacier terminus, 15 m. WA: A571, P2287. Two other Polycoccum species are known growing on Acarospora species, namely P. microsticticum and P. acarosporicola (Atienza et al. Reference Atienza, Calatayud and Hawksworth2003; Halıcı et al. Reference Halıcı, Akgül, Oztürk and Kılıç2013). Both species also grow on members of the subgenus Phaeothallia but they have larger ascospores than the specimen studied from Glacier Bay. Polycoccum microstictum ascospores are 14–18 × 7–8 μm and those of P. acarosporicola are even larger (28.5–31.5 × 8–9.5 μm). Ascospores observed in specimen P2287 are 13–14 × 5–6 μm. This size is similar to ascospores found in P. rubellianae (11–14 × 6–7 μm), a species known only from Caloplaca rubelliana. Material found so far is too scanty for a formal description.

  • Porpidia sp. F10440 — Saxicolous on side of large glacial erratic in muskeg, 22 m. DUN: 468, F10440. This collection was initially identified as P. carlottiana because of the pruinose apothecia and exciple with a dark cortex and ± hyaline medulla. However, the apothecia are sessile with a well-developed proper margin, which is anomalous for that species, and furthermore an ITS sequence (U. Ruprecht, unpublished data) placed it in the P. cinereoatra group. The exciple pigmentation separates it from all known species of this group, in which the exciple is ± uniformly dark.

  • +Ptychographa sp. T41644 — Lignicolous on loose piece of deciduous shrub near the ground, 5–10 m. WA: 552, T41644. Distinguished from the only described species in the genus, P. xylographoides, by the lack of a lichenized thallus and the tendency for wood to be eroded everywhere except under the ascomata.

  • Puttea sp. S38314 — Lignicolous in deep recess of living, large Tsuga tree, 569 m. EX: 358, S38314. Ascospores short-fusiform, asymmetrical, 6–10 × 1.8–2 μm; epihymenium POL+, with blue-green, KOH+ green pigments; exciple robust; pycnidia abundant. This does not match any species known to us and its placement in Puttea is tentative.

  • Pycnora sp. S40795 — Corticolous on Salix branch, 2 m. EA: terminus of Riggs Glacier, S40795 (sub Lecanora symmicta). Similar in habit to Lecidea roseotincta but with a distinctly brown thallus. The ascus in this specimen is similar to that seen in Pycnora s. str. (‘tholus with lateral amyloid zone’ (Bendiksby & Timdal Reference Bendiksby and Timdal2013); similar to that in Candelaria, illustrated by Hafellner (Reference Hafellner1984), not surprising given that Pycnora is now placed in Candelariales).

  • Ramboldia sp. S38597 — In apothecia of Lecanora symmicta, corticolous on Salix, 2 m. WA: 391, S38597. Ascospores are 15–16 × 5 μm, often with a slight curve, and the hymenial pigment is green (KOH+ green intensifying). Ramboldia insidiosa (Fr.) Hafellner was described from the Alps as a hymenial parasite of Lecanora varia that eventually becomes autonomous (Poelt Reference Poelt1974). The present collection appears to have taken over a thallus of Lecanora symmicta and differs from R. insidiosa in its different host, its relatively convex apothecia and longer ascospores ((8–)6–12 μm in R. insidiosa).

  • Rhizocarpon sp. S39392 — Saxicolous on alpine ridge, 918 m. EX: 454, S39392. This collection is close to Rhizocarpon badioatrum but differs in the thallus containing diffractaic acid (no substances in R. badioatrum) and having usually paler brown, thinner, and more convex areolae with a less angular margin. See Rhizocarpon badioatrum in the ‘Catalogue of All Named Taxa Found’ for further details.

  • Rhizocarpon sp. F10115 — Saxicolous on alkaline argillite rock outcrop in alpine heath, 922 m. EX: 407, F10115. A member of the R. geographicum group, this species is unique within the group in having a thallus containing rhizocarpic and norstictic acids and pigmented, muriform ascospores. However, what is truly remarkable about this single collection is the presence of two different types of ascospores, either subglobose (c. 15 μm diam.) or broadly ellipsoid (c. 45 × 15 μm), in different apothecia and, in one case, the same apothecium, where they occur in discrete hymenia separated by an excipulum.

  • Rinodina sp. S38838 — Saxicolous on soft argillite in the alpine zone, 922 m. EX: 407, S38838. Similar to Rinodina badiexcipula Sheard but the ascospores are more than 25 μm long, the thalline rim is greyish (not reddish brown) and the thallus is largely lacking or immersed (well developed in R. badiexcipula).

  • Stereocaulon sp. S24431 — Saxicolous on rocky shores, 0–10 m. EA: just S of terminus of Riggs Glacier, S40806; GB: 868, F9757. TLC: atr, lobaric acid. These specimens should be compared to Stereocaulon sp. S24431 from KLGO which Spribille et al. (Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) discuss in relation to described Stereocaulon species. The thalli are characterized by slender pseudopodetia with a scabrose stereome surface and phyllocladia almost completely converted into sorediate masses. In the GLBA specimens two types of cephalodia are represented: pale brown with a reddish brown cyanobacterium (S40806) and grey-brown and cerebriform, with a blue-green cyanobacterium (F9757).

  • Stereocaulon sp. S39567 — Saxicolous on rocky headland, 5–8 m above the high tide line. DUN: 463, 39567. TLC: atr, lobaric acid. This species comes closest to Stereocaulon depreaultii in the key of Lamb (Reference Lamb1978) but differs from all species described by Lamb (Reference Lamb1977) in having a completely corticate stereome and bud-like phyllocladia constricted at the bases. Only limited material from a single locality is available. More surveys are needed in Cross Sound and nearby areas to try to locate more populations of this enigmatic species. A DNA sequence is published here (Table 1) for use in future studies.

  • Tingiopsidium sp. F9804 — Saxicolous on sedimentary rock just back from shore, 2 m. EA: 872, F9804, F9805; WA: 101, F9917. An ITS rDNA sequence from F9805 (isolate T1189, Table 1) suggests it is close to the more southern species T. sonomense (unpublished data), but it differs from that species in its peg-like as opposed to strap-shaped isidia and much narrower lobes.

  • Trapeliopsis sp. S40723 — Lignicolous and muscicolous on rotting log suspended in old-growth Tsuga heterophylla rainforest, 20 m. GUS: Bartlett Lake trail, S40723. This peculiar species is esorediate and fertile, and is characterized by the development of abundant proliferating ascomatal buds: the apothecia are essentially tuberculate in one plane. DNA was obtained (isolate KS87) and places the species on an isolated branch in Trapeliopsis relative to well-known species (Fig. 8).

  • Unknown genus F10343 — Saxicolous in alpine heath, on alkaline argillite, 918 m. EX: 454, F10343 (sub Rhizocarpon chioneum). The apothecia resemble those of the genus Catillaria microscopically (lax paraphyses with a brown, sharply delimited cap) but have simple ascospores. The material is sparse. An mtSSU sequence (T1192, Table 1) was not sufficiently informative to place the species.

  • Unknown genus S37916 — Terricolous in freshly deglaciated soil, 22 m. WA: 318, S37916. This peritheciate species is characterized by large, dark brown, muriform ascospores, to 140 × 45 μm, which can even be seen under a dissecting microscope. Paraphyses remain intact and are anastomosing.

  • #Unknown genus S38748 — Lichenicolous on Xylographa on snag, 717 m. EX: 403, S38748. Does not correspond to any known species or genus (M. Zhurbenko, personal communication 2018) but the ascus and ascomatal characters suggest a relationship to Arthoniaceae; it differs from most Arthonia species in its simple ascospores. Also known from Scotland on X. trunciseda (B. Coppins, personal communication 2020).

  • Unknown genus S38989 — Corticolous on Shepherdia canadensis and Tsuga mertensiana, 10–465 m. DUN: 426, S38989; WA: 319, S37921; 384, S38508, S38509 (sub Biatora meiocarpa). TLC: unknown phenolic substance. A crust perhaps part of an expanded Biatora sensu Kistenich et al. (Reference Kistenich, Timdal, Bendiksby and Ekman2018) with small apothecia with a thin exciple, and ascospores 11–13 × 5–7 μm; ascus ± Bacidia-type.

  • Unknown genus S39453 — EX: 455, S39453 (sub Parmeliella sp. S24412). A minute species with a well-developed thallus and black perithecia. The ascospores are 1 per ascus and 79–82 × 25–34 μm; paraphyses disintegrate but periphyses persist. Asci I+ blue.

  • Unknown genus T41551 — Corticolous on Sambucus bark, 2 m. GUS: 532, T41551a (in part), T41551b. An inconspicuous but highly distinctive species that forms a continuous crust of cyanobacterium-filled goniocysts when wet, with apothecia embedded between the goniocysts. Ascospores long-fusiform, non-septate. GUS: 857, S36109 may also belong here.

  • Varicellaria sp. S38337 — Loosely saxicolous over ridgetop rocks, 895 m. EX: 370, S38337. TLC: gyrophoric acid, unidentified pigment. This sterile species resembles Ochrolechia sp. S38864 but its thallus areoles do not become tan in the herbarium packet over time and it is more loosely attached to the rock substratum. An ITS rDNA sequence (isolate T1342, Fig. 6) suggests an affinity to Varicellaria, but further research is required.

  • Varicellaria sp. S39454 — Terricolous/muscicolous on organic accumulations, 880 m. EX: 455, S39454; 459, F10357. TLC: lecanoric acid. A distinctive sterile species characterized by a chunky coralloid thallus with lobe tips ending in what appear to be incipient but abortive apothecia that are strongly KOH+ yellow in the medulla. The genus placement is speculative in the absence of ascomata or molecular data.

Catalogue of All Named Taxa Found

  • #Abrothallus parmeliarum (Sommerf.) Arnold — Lichenicolous on corticolous and saxicolous Parmelia and Platismatia spp. and once on Parmeliopsis hyperopta, 0–922 m. DUN: 339, S38179 (sub Lichenopuccinia poeltii), S38197 (sub L. poeltii); 463, S39555, S39590; S583, P2256; S586, P2093; EX: 407, S38823 (sub Stigmidium conspurcans); S612, P2227; GB: 868, S36543 (anamorph), S36538; GUS: A569, P2222, P2369, P2387.

  • #Abrothallus prodiens (Harm.) Diederich & Hafellner — Lichenicolous on thalli of Hypogymnia apinnata and H. enteromorpha growing on Picea sitchensis, 20 m. GUS: 881, S36837; 397, S38711; A569, P2255.

  • #Abrothallus welwitschii Tul. — Lichenicolous on Sticta limbata, 0–10 m. GB: 868, S36512, S36482. This species has been found previously in south-east Alaska from Prince of Wales Island (Diederich Reference Diederich2003), Mitkof Island (unpublished record) and the Chilkoot Trail (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010).

  • **Absconditella rosea Kalb & Aptroot — See ‘Other Species Treated in Detail’.

  • *Absconditella sphagnorum Vězda & Poelt — Muscicolous on Sphagnum on hummock in cold muskeg. DUN: 415, S38937. First published record for western North America.

  • Acarospora badiofusca (Nyl.) Th. Fr. — Saxicolous; alpine heath with rock outcrops; on alkaline argillite, 830 m. EX: 407, F10131 (sub Protoparmeliopsis muralis); 409, S38882 (det. M. Westberg, as ‘cf.’). Previously known in Alaska from the Pitmegea River (Thomson Reference Thomson1979).

  • Acarospora cervina A. Massal. — Saxicolous in alpine heath, 830 m. EX: 404, F10073 (det. K. Knudsen).

  • Acarospora fuscata (Schrad.) Th. Fr. — Saxicolous on alpine ridge, 919 m. EX: 374, S38409 (group; det. M. Westberg). A widespread group containing taxonomically difficult cryptic species.

  • Acarospora glaucocarpa (Ach.) Körb. var. glaucocarpa — Saxicolous on pebbles in limestone-influenced areas, rubbly slopes and high beaches, 0–14 m. WA: 390, S38581; north beach on isthmus separating north end of Scidmore Bay from main West Arm, S37998.

  • Acarospora glaucocarpa var. sarcogynoides H. Magn. — Saxicolous on soft argillite, alpine slope, 922 m. EX: 407, S38836 (det. M. Westberg).

  • Acarospora sinopica (Wahlenb.) Körb. — Saxicolous, mainly on metal-rich (highly oxidized) rocks, found in crags and on small boulders behind beaches, 10–15 m. EA: 872, S36619 (det. M. Westberg, as ‘cf.’); GUS: 435, S39136 (sub Tremolecia atrata); WA: 105, F10007.

  • *Adelolecia kolaënsis (Nyl.) Hertel & Rambold — Saxicolous on metamorphic (hornblende augen gneiss) to sedimentary rocks from the supralittoral zone to the alpine zone, 0–918 m. DUN: 463, F10390, F10391, F10409, F10410; EX: 454, F10334.

  • Adelolecia pilati (Hepp) Hertel & Hafellner — Saxicolous in alpine talus, 907 m. EX: 373, S38395.

  • Agonimia gelatinosa (Ach.) Brand & Diederich — Growing over bryophytes on limestone and granite outcrops, 10–100 m. WA: 101, F9903 (sub Leptogium imbricatum).

  • Agonimia tristicula (Nyl.) Zahlbr. — Muscicolous over rock, 0–10 m. GB: 868, F9755, S36541; N Sandy Cove, F9814 (sub Verrucaria sp.).

  • + Agyrium rufum (Pers.) Fr. — Lignicolous on stump in mixed conifer forest, 40 m. EX: 125, F10271.]

  • Alectoria ochroleuca (Hoffm.) A. Massal. — Terricolous in alpine heath with rock outcrops, 883–922 m. EX: 405, F10079; 407, S38850.

  • Alectoria sarmentosa (Ach.) Ach. — Corticolous on conifer branches and tree trunks, on Picea, Pinus and Tsuga, mostly in montane habitats away from marine influence, and into the krummholz zone, 12–922 m. DUN: 337, S38120; 338, S38131; 339, S38185; 463, S39523; EX: [858, S36181, S36186]; 353, S38289; 407, S38810; ‘Mooselator’, S38906; 448, S39355; GB: 868, S36493; GUS: 316, S37878; 397, S38690; 862, S36298. TLC (S36493): usnic, alectoronic, barbatic acids.

  • Allocalicium adaequatum (Nyl.) M. Prieto & Wedin — Corticolous on Alnus in beach fringe, 2 m. GUS: 341, S38224.

  • Alyxoria culmigena (Libert) Ertz (syn. Opegrapha herbarum Mont.) — Lignicolous on hard driftwood just above high tide line, 2 m. DUN: 462, F10380, S39500, S39506; 572, T41789, T41790, T41792.

  • Amygdalaria consentiens (Nyl.) Hertel et al. — a) acid-deficient chemotype: saxicolous, found twice, on pebble on elevated beach and on top of boulder in muskeg, 0–68 m. EX: 413, S38929; WA: 384, S38525; 391, S38632. TLC: nil; b) stictic chemotype: saxicolous on rocks in the alpine zone, 903–936 m. EX: 375, S38423, S38420; 455, S39424; TLC: stictic, constictic acids; c) chemotype not identified: saxicolous on granitic rocks on beach ridges, 0–30 m. EA: 869, F9761; WA: 103, F9949; 105, F9997; 545, T41620.

  • Amygdalaria continua Brodo & Hertel — Saxicolous on granitic rock outcrops in forest and on alpine ridges, including in areas of water seepage, 80–435 m. DUN: 120, F10172; 414, F10141.

  • Amygdalaria pelobotryon (Wahlenb.) Norman — Saxicolous on pebbles and small rocks from uplifted beach ridges (c. 20 yr old) to alpine tundra, 43–937 m. EA: 869, S36557 (as ‘aff.’); EX: 405, F10102; 409, S38899 (as ‘aff.’); 373, S38384; 454, S39407, F10331. TLC: gyrophoric acid.

  • Amygdalaria subdissentiens (Nyl.) M. Inoue & Brodo — Saxicolous on vertical rock face, 406 m. DUN: 423, S38977 (as ‘aff.’); EX: 373, S38392. TLC: stictic, gyrophoric acids. The specimen from Dundas (S38977) has a more dispersed thallus than the typical Excursion Ridge specimen, with an indeterminate margin and much less frequent apothecia and cephalodia. Furthermore, the cephalodia appear to contain the cyanobacterium Gloeocapsa (normally Stigonema in this lichen).

  • *Anisomeridium polypori (Ellis & Everh.) M. E. Barr — Corticolous on Populus balsamifera, 3 m. GB: 874, S36697.

  • Arctomia delicatula Th. Fr. — Unspecific in substratum association: most often corticolous on Alnus and Populus balsamifera, but also once on Picea sitchensis twigs, once lichenicolous over Physcia, once muscicolous in glacial outwash plain, and once terricolous in the alpine zone, 0–880 m. Often mixed in amongst other lichens in small quantities and not detected in the field. EA: 440, S39192, S39194, S39245, S39236; 233, M2776; EX: 459, F10360 (sub Candelariella sp.); GB: 865, S36401 (sub Cheiromycina petri); GUS: 857, S36139 (sub Leptogium saturninum); WA: 105, F10001 (sub Porpidia cf. thomsonii); 322, S37968; 323, S37969; 384, S38512; 395, S38667 (sub Caloplaca atrosanguinea), S38682 (sub Fuscopannaria convexa); 542, T41592; 545, T41621b; 549, T41634. We extracted DNA from one sample (isolate P166, from S37968, published by Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015)) to explore whether the GLBA species might be divergent from the putatively tundra-restricted arctic-alpine form known in Europe, but ITS rDNA data did not suggest any divergence.

  • Arthonia arthonioides (Ach.) A. L. Sm. — Corticolous on Cupressus nootkatensis, Picea sitchensis and Tsuga heterophylla in coastal Tsuga-Picea forest, 0–50 m. DUN: 131, F10446; 332, S38065; 334, S38097, S38099; EX: 213, M2568; [858, S36189]; 446, S39336; 448, S39347; GUS: 100, F9893; 136, F10466; 855, F9606; Bartlett Cove housing complex, F9849, F9861; 876, S36734.

  • #Arthonia biatoricola Ihlen & Owe-Larss. — Lichenicolous on Micarea, overgrowing Picea sitchensis twigs, also over Populus balsamifera, 0–10 m. GB: 868, S36531; GUS: 341, S38246.

  • *Arthonia aff. didyma Körb. — Lignicolous on snag and corticolous on Picea sitchensis, 0–33 m. GUS: [V329, S38053]; 436, S39156; 204, S38438. Our material is similar to A. didyma, differing in subtle traits of size and habit (M. Grube, personal communication). However, in the absence of detailed study it is not clear this warrants recognition as another taxon.

  • *#Arthonia digitatae Hafellner — Lichenicolous on Cladonia cf. umbricola, 0–60 m. DUN: 219, M2674b; WA: A578, P2364.

  • Arthonia ilicina Taylor — Corticolous on Alnus and Malus, 9–86 m. DUN: 562, T41746; 333, S38075, S38077, S38086; 462, S39720 (as ‘aff.’); EX: [125, F10277]; 433, S39074.

  • **#Arthonia lepidophila (Anzi) Clauzade et al. — Lichenicolous on Cladonia cf. squamosa, 203 m. EX: 565, P2338. Characterized by the combination of 2-septate ascospores and the KOH+ olive hymenial reaction.

  • **Arthonia ligniaria Hellb. — Lignicolous on snag, 51 m. GUS: 882, S36839. Ascospores 1-septate, c. 18 × 7.5 μm and hymenium I−. Arthonia ligniaria was described from Sweden and has been reported from the UK (Coppins Reference Coppins1989b) and elsewhere in Europe.

  • Arthonia ligniariella Coppins — Lignicolous in deep recess (hollow) of large, live Tsuga, 569 m. EX: 358, S38315.

  • Arthonia muscigena auct., s. lat. — Over metamorphic rock in the supralittoral zone, in splash zone; also corticolous on Populus balsamifera and on Tsuga twig, and foliicolous on Picea sitchensis, 0–48 m. DUN: 134, F10464 (sub Hydropunctaria maura); 573, T41812; GUS: 855, S36024; 341, S38241.

  • *#Arthonia peltigerea Th. Fr. — Lichenicolous on Solorina crocea, terricolous, 903 m. EX: 455, S39440.

  • Arthonia phaeobaea (Norman) Norman — Saxicolous on gneiss in the supralittoral zone, 0–5 m. DUN: 462, F10379 (sub Myriolecis aff. contractula); 220, M2672; GB: 865, F9741, F9744; 873, F9821; 874, F9835; 875, F9841, F9842; GUS: 340, S38223.

  • Arthonia aff. radiata (Pers.) Ach. — Corticolous on Alnus bark, 10 m. DUN: 463, S39509; 467, S39647.

  • #Arthonia stereocaulina (Ohlert) R. Sant. — Lichenicolous on Stereocaulon spp., on sea stacks and in post-glacial Dryas mats, 0–115 m. DUN: 586, P2161; EA: 870, F9781.

  • **#Arthonia thelotrematis Coppins — Lichenicolous on Thelotrema lepadinum, corticolous on Alnus, 86 m. DUN: 333, S38093. This species was described by Coppins (1989a) from the UK and the Azores, and subsequently reported from mainland Europe (Etayo & Diederich Reference Etayo and Diederich1998) and New Zealand.

  • *Arthonia vinosa Leight. — Corticolous in mixed woodland, 3 m. GB: 874, F9829; GUS: road to dock, F9852.

  • #Arthophacopsis parmeliarum Hafellner — Lichenicolous on Parmelia sulcata, both in rock- and bark-dwelling specimens, 0–10 m. DUN: 463, S39556; WA: 395, S38676; 542, T41588.

  • +Arthopyrenia analepta (Ach.) A. Massal. — Corticolous on Alnus and Salix, 0–152 m. DUN: 430, S39034; EA: 440, S39217; GB: 864, S36342, S36375; GUS: [V329, S38039 (sub Arthopyrenia sp. S38039)]; WA: 319, S37919; 327, S38013; 391, S38595.

  • *+Arthopyrenia plumbaria (Stizenb.) R. C. Harris — Corticolous on Alnus, 9–27 m. DUN: 339, S38147; 462, S39727, S39711.

  • *Arthothelium macounii (G. Merr.) W. J. Noble — Corticolous on Cupressus nootkatensis branch, 68 m. DUN: 413, S38928.

  • *Arthothelium norvegicum Coppins & Tønsberg — Corticolous on Picea sitchensis branch, 2 m. GB: 868, S36505 (ver. M. Grube). Previously reported from California to British Columbia by Tønsberg & Williams (Reference Tønsberg and Williams2006).

  • Arthrorhaphis alpina (Schaer.) R. Sant. — On soil accumulations in crack on side of granitic boulder in muskeg, 90 m. DUN: 115, F10144.

  • **#Arthrorhaphis muddii Obermayer — Lichenicolous on Dibaeis baeomyces, seepy soil, 597 m. DUN: 427, S38997. This species was described from the UK and Austria by Obermayer (Reference Obermayer1994), who described it in detail, and outside of those countries it has been found only in Norway (Ihlen Reference Ihlen1998).

  • *Aspicilia cf. fumosa Owe-Larsson & A. Nordin — Saxicolous, 125 m. WA: 388, S38559. Thallus light grey, KOH−; ascospores 20–24 × 13–15 μm; epihymenium olive-brown to olive; hymenium 160–180 μm; excipulum 20–50 μm; paraphyses moniliform; conidia not found. TLC: nil.

  • *Aspicilia aff. indissimilis (H. Magn.) Räsänen — Saxicolous on argillite in the alpine zone, 125–922 m. EX: 407, F10117; 458, S39487; WA: 388, S38560 (det. T. Wheeler and B. Owe-Larsson). Ascospores (6–)8 per ascus, 19–25 × 10–15 μm (8–10 μm wide in S39487); epihymenium olive to brown; hymenium 100–180 μm; excipulum 30–50 μm, paraphyses (sub-)moniliform; thallus KOH−; conidia 12–16(–18) μm. TLC: nil. The taxonomy of this group requires more research.

  • *Aspicilia aff. olivaceobrunnea Owe-Larss. & A. Nordin — Saxicolous in alpine heath with rock outcrops; on alkaline argillite, 883 m. EX: 405, F10095 (sub Lecidea aff. griseomarginata; det. B. Owe-Larsson).

  • Aspicilia subradians (Nyl.) Hue — Saxicolous on argillite in the alpine zone, 883–919 m. EX: 374, S38413 (as ‘aff.’, paraphyses non- to submoniliform, perhaps A. cinerea group); 405, F10095 (sub Lecidea aff. griseomarginata); 407, F10117 (det. B. Owe-Larsson). TLC: norstictic acid.

  • **Atla recondita Savić & Tibell — Saxicolous on semi-inundated slightly basic rock, with Staurothele cf. verruculosa, 225 m. EX: 128, F10302. The affinity of F10302 to A. recondita was confirmed by ITS rDNA (Table 1). This appears to be the first report of the species since it was described from Sweden by Tibell & Tibell (Reference Tibell and Tibell2015).

  • Atrophysma cyanomelanos T. Sprib. — See ‘Descriptions of New Genera and Species’.

  • #Bachmanniomyces punctum (A. Massal.) Diederich & Pino-Bodas (syn. Phaeopyxis punctum (A. Massal.) Rambold et al.) — Lichenicolous on Cladonia pyxidata, 0–3 m. WA: A573, P2368.

  • #Bachmanniomyces uncialicola (Zopf) D. Hawksw. — Lichenicolous on Cladonia amaurocraea, terricolous, 922 m. EX: 407, S38822.

  • Bacidia bagliettoana (A. Massal. & De Not.) Jatta — Muscicolous/terricolous on plant detritus, organic accumulations in rock crevices and on soil in post-glacial Dryas mats, 0–115 m. EA: 869, S36554; 870, F9774, F9779, F9789; GB: 867, S36436; WA: 101, F9901 (sub Thalloidima sedifolium); 381, S38444; 390, S38587.

  • Bacidia rosellizans S. Ekman — Corticolous on Alnus, 46 m. GUS: 879, S36808.

  • **Bacidina brandii (Coppins & van den Boom) M. Hauck & V. Wirth — On organic accumulations on gravelly high beaches and in Plantago maritima zone, 0–4 m. EA: 438, S39186, F10222; GB: 873, S36658. Described from Europe by Coppins & van den Boom (Reference Coppins and van den Boom2002) and has since been widely reported there but, apparently, until now, not from elsewhere. Colour photographs have been published by Czarnota (Reference Czarnota2016).

  • Bacidina circumpulla S. Ekman — See ‘Descriptions of New Genera and Species’.

  • *Bacidina egenula (Nyl.) Vězda — Saxicolous on gneiss rocks beside creek, 0–5 m. DUN: 133, F10457 (sub Verrucaria sp.).

  • **Bacidina saxenii (Erichsen) M. Hauck & V. Wirth — Saxicolous on vertical shale rock face at sea level and side of large roadside boulder, 5–20 m. DUN: 462, S39507; GUS: 140, F10488. Bacidina saxenii has until now been reported only from Europe. Its known distribution and ecology are discussed by Ekman et al. (Reference Ekman, Jonsson and Hermansson2012), who also provide photographs of the morphology.

  • **Bacidina sulphurella (Samp.) M. Hauck & V. Wirth — Corticolous on Ribes lacustre, 2 m. GUS: 341, S38254. Until now reported only from Europe, this species is similar to B. arnoldiana in ascomatal characters, but differs in the shape of its conidia (hooked at one end like a walking stick; B. arnoldiana has curved but never hooked conidia) and its occurrence as an epiphyte (B. arnoldiana is predominantly saxicolous; Coppins & Aptroot Reference Coppins, Aptroot, Smith, Aptroot, Coppins, Fletcher, Gilbert, James and Wolseley2009).

  • Bactrospora cascadensis Ponzetti & McCune — Corticolous in rain-sheltered underhangs of Tsuga heterophylla trunks. In GLBA found only in montane forests, 222–687 m. EX: 112, F10064; 313, S37839 (aff.; discussed below); 366, S38335; 448, F10316, S39348; 358, S38308; no waypoint, M2587. S37839 is intermediate between B. cascadensis and B. brodoi. It resembles B. brodoi (and differs from the rest of B. cascadensis material cited here) in possessing an entirely endophloedal thallus, with no sign of the typical effuse, scurfy, pinkish thallus of B. cascadensis. However, it differs from B. brodoi (and agrees with B. cascadensis) in possessing Patellarioides-type ascospores (2.2–)2.8(–3.5) μm wide (narrower than in the otherwise similar B. brodoi; Ponzetti & McCune Reference Ponzetti and McCune2006), asci (11–)12.7(–15) μm wide, an I+ pale blue hymenium and subhymenium, and a strongly I+ blue excipulum.

  • Baeomyces rufus (Huds.) Rebent. — Saxicolous, muscicolous and terricolous on boulders and soil in shaded to open areas from forest to Dryas-covered glacial forelands, 0–115 m. EA: 869, S36561 (sub Epilichen scabrosus); 870, F9780; GB: 865, S36414; 868, F9753; WA: 383, S38485. One GLBA specimen has been used as a source of DNA in phylogenetic studies (Resl et al. Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015, isolate P82).

  • Bellemerea cinereorufescens (Ach.) Clauzade & Cl. Roux — Saxicolous in alpine heath with rock outcrops; on alkaline argillite, 830 m. EX: 404, F10068 (sub Lecidella carpathica), F10069.

  • Bellemerea subsorediza (Lynge) R. Sant. — Saxicolous on 20 yr-old gravels and granitic rocks, 0–43 m. EA: 869, S36559; WA: 383, S38493; 102, F9935; 388, S38561 (sub Candelariella vitellina). TLC: norstictic acid.

  • *Belonia incarnata Th. Fr. & Graewe — Terricolous in alpine sod, 918 m. EX: 454, S39411.

  • Belonia russula Körb. ex Nyl. — Saxicolous in alpine heath with rock outcrops; on alkaline argillite, 918 m. EX: 454, F10342.

  • Biatora aegrefaciens Printzen — Corticolous on Picea sitchensis twigs on exposed coastal headland, 27 m. DUN: 339, S38172.

  • Biatora alaskana Printzen & Tønsberg — Corticolous on Alnus, Picea sitchensis and Tsuga heterophylla, 0–213 m. EX: 312, S37816; [V431, S39057]; GUS: [V329, S38026]; 436, S39137; 876, S36728; Tower Rd, S38270; 210, M2555. We also include a form here we considered describing as a new species because it consistently has single-celled, fusiform ascospores up to 35 × 6 μm. This form was already treated in KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010) as Biatora sp. 24799. We, however, remain unconvinced and molecular data have not been obtained to test the hypothesis one way or another. Representative specimens are: DUN: 463, S39551; GUS: 856, F9616; 857, F9635. TLC: nil.

  • Biatora albohyalina (Nyl.) Bagl. & Carestia — Corticolous on Ribes bracteosum, 710 m. EX: 450, S39363 (det. C. Printzen). Ascospores 8–10.5 μm long, shorter than typical for the species.

  • Biatora alnetorum S. Ekman & Tønsberg — Corticolous on Alnus, 8 m. EA: 440, S39231. TLC: atr. Sterile, soredia as in Ekman & Tønsberg (Reference Ekman and Tønsberg2019).

  • *Biatora aureolepra T. Sprib. & Tønsberg — Corticolous on Picea sitchensis branch, 33 m. GUS: 204, S38436.

  • Biatora beckhausii (Körb.) Tuck. — Corticolous on Salix, 24 m. WA: 206, M2505.

  • Biatora aff. chrysantha (Zahlbr.) Printzen — Corticolous on Alnus and Cupressus nootkatensis, 8–42 m. DUN: 469, S39696 (det. C. Printzen); EA: 440, S39212; WA: 549, T41627b. Specimens are sterile and treated as ‘aff. chrysantha’ here because it is not possible to distinguish B. chrysantha and B. chrysanthoides in the sterile state (Printzen & Tønsberg Reference Printzen and Tønsberg2003).

  • Biatora cuprea (Sommerf.) Fr. — On moss and detritus over rock, 922–936 m. EX: 375, S38418; 407, S38860.

  • Biatora efflorescens (Hedl.) Räsänen — Corticolous on Alnus, 9 m. DUN: 462, S39718; EA: 440, S39219, S39223; GB: 868, S36535; 556, T41683. TLC: argopsin, norargopsin (trace).

  • Biatora flavopunctata (Tønsberg) Hinteregger & Printzen — Corticolous on Shepherdia canadensis and Vaccinium, 10–713 m. EX: 376, S38430 (sub Biatora meiocarpa var. tacomensis); WA: 384, S38511; 544, T41603.

  • Biatora hypophaea Printzen & Tønsberg — Corticolous on Alnus, Malus fusca, Oplopanax horridus, Picea sitchensis, Ribes lacustre, Salix, Sambucus racemosa and Viburnum edule, 0–195 m. An extremely common low elevation crustose epiphyte in GLBA. DUN: 333, S38076, S38083; 336, S38115; 462, S39700, S39703 (sub Arthopyrenia sp.); EA: 123, F10245; 440, S39203 (conf. C. Printzen), S39226, S39237, S39255; 441, F10193; 442, 39291 (sub Micarea cinerea); 872, S36610; 234, M2804; no waypoint, M2808, M2816; EX: [125, F10255, F10260]; 432, S39067; GB: 864, S36339; 865, S36407; GUS: 100, F9895; 138, F10468, F10472, F10474; [V329, S38027]; 330, S38063 (sub Fellhaneropsis vezdae); 341, S38248 (sub Biatora sphaeroidiza), S38251, S38263 (conf. C. Printzen); 857, F9641, S36094, S36135; 857, S36138 (sub Micarea cinerea); 879, S36815, S36804; 436, S39162; housing complex, F9865; 224, M2706; 228, M2742; 230, M2764; 232, M2772.

  • Biatora kodiakensis Printzen & Tønsberg — Corticolous on Alnus, Oplopanax horridus and Viburnum edule, 0–10 m. GB: 864, S36362, S36343; 866, S36420 (sub Bacidina sp.); 556, T41649, T41681, T41682; GUS: 341, S38249 (det. C. Printzen), S38260; 531, T41533; 576, T41849; 228, M2743; WA: 549, T41627a, T41638, T41639. TLC: gyrophoric acid [no lecanoric].

  • Biatora ligni-mollis T. Sprib. & Printzen — Lignicolous on conifer, 25 m. GUS: Tower Road, M2485.

  • Biatora marmorea T. Sprib. — See ‘Descriptions of New Genera and Species’.

  • Biatora meiocarpa (Nyl.) Arnold — Corticolous on Alnus, Oplopanax horridus, Salix and Shepherdia canadensis, 8–92 m. EA: Muir Inlet, S36595; 440, S39216, S39232 (sub Lichenochora lepidiotae); GUS: 341, S38263 (sub B. hypophaea; det. C. Printzen); 436, S39145; WA: 384, S38509; 387, S38537, S38538 (det. C. Printzen).

  • Biatora meiocarpa var. tacomensis Printzen & Tønsberg — Corticolous on Alnus bark and Vaccinium stalks, 0–713 m. EX: 376, S38430; GUS: 138, F10476. TLC: xanthones.

  • Biatora oligocarpa Printzen & Tønsberg — Corticolous on Populus balsamifera, 0–33 m. GUS: [V329, S38050]; [557, T41714a]; WA: Blue Mouse Cove plot BM2a (det. TS).

  • Biatora rufidula (Graewe) S. Ekman & Printzen — Corticolous on trunk of fallen Picea sitchensis, 3 m. GB: 874, S36704.

  • Biatora sphaeroidiza (Vain.) Printzen & Holien — Corticolous on Oplopanax horridus, Picea sitchensis, Salix, Sambucus racemosa and Viburnum edule, 0–27 m. DUN: 339, S38153; GB: 864, S36374; GUS: 341, S38248 (det. C. Printzen, as ‘aff.’), S38249 (det. C. Printzen, sub B. kodiakensis), S38251 (sub Biatora hypophaea), S38261; 434, S39099 (sub Biatora subduplex), S39102 (det. C. Printzen, as ‘aff.’); 436, S39162 (sub Biatora hypophaea), S39145 (sub Biatora meiocarpa). TLC: a xanthone. In several specimens the apothecia are paler and the ascospores larger than is usually the case in B. sphaeroidiza s. str. (C. Printzen, personal communication 2019).

  • Biatora subduplex (Nyl.) Räsänen ex Printzen, s. lat. — Corticolous on Alnus and terricolous/muscicolous in alpine tundra, also once saxicolous in the alpine zone, 0–922 m. Material here includes an unusually wide range of ascospore sizes and might constitute more than one species. DUN: 336, S38113 (s. lat.); 466, S39638; EA: 440, S39252 (det. C. Printzen, as ‘cf.’), S39254; 441, F10202, F10220; EX: [858, S36173]; 404, F10070; 407, F10110; 218, M2667; 455, S39449, S39452; GB: 865, S36406; 866, S36427 (s. lat.); 868, S36525; 433, S39083; GUS: 138, F10469; 855, S36028, S36034; 857, F9638, S36152; 862, S36310; 878, S36762; 879, S36816; 317, S37896; [V329, S38020]; 341, S38248 (sub Biatora sphaeroidiza), S38251 (with large ascospores, sub Biatora hypophaea); 434, S39099; Tower Road, S37503; WA: 206, M2507; 319, S37920, S37922 (s. lat.), S37927 (det. C. Printzen); 320, S37957; 383, S38487; 387, S38538 (sub Lecidea albohyalina), S39541 (s. lat.); 542, T41594; 544, T41607 (sub Lecidella elaeochroma).

  • Biatora toensbergii Holien & Printzen — Corticolous on Alnus, 4–8 m. DUN: 462, S39721, S39703 (sub Arthopyrenia sp.; det. C. Printzen); GB: 556, T41680; GUS: 531, T41532. TLC: argopsin.

  • Biatora vacciniicola (Tønsberg) Printzen — Corticolous on Alnus, Salix and Vaccinium stalks, 0–713 m. DUN: 429, S39031; EA: Muir Inlet S shore, S36594, S36597; 440, S39219; EX: 376, S38430 (sub Biatora meiocarpa var. tacomensis), S38431; 441, F10206; GB: 866, S36422; WA: 384, S38505; 387, S38539; 544, T41604 (fertile). TLC: gyrophoric acid.

  • Biatora vernalis (L.) Fr. — On organic accumulation over vertical rock face, 2–830 m. EX: 404, S38750; 213, M2574; WA: 391, S38617 (det. C. Printzen).

  • #Biatoropsis usnearum Räsänen s. lat. — Lichenicolous on Usnea longissima, which was corticolous on windblown Picea, headland, 9 m. DUN: 463, S39557.

  • Bilimbia microcarpa (Th. Fr.) Th. Fr. — On organic accumulations on base of Pinus contorta in open flats, 16 m. GUS: 317, S37897.

  • Blennothallia fecunda (Degel.) Otálora et al. — Saxicolous on granitic rocks on seashore, 0–10 m. WA: 102, F9941.

  • *Brianaria bauschiana (Körb.) S. Ekman & M. Svenss. — Saxicolous on boulders in deep shade of old-growth forest and Alnus thickets, 0–58 m. GB: 865, S36413 (det. B. Coppins); GUS: 139, F10483, F10484, F10487; 856, F9627; 878, S36778 (det. B. Coppins).

  • Brianaria sylvicola (Flot. ex Körb.) S. Ekman & M. Svenss. — Saxicolous on boulder in open woodland, 15 m. GUS: housing complex, F9858.

  • Brigantiaea fuscolutea (Dicks.) R. Sant. — Terricolous between and at the edges of boulders in alpine sod and tundra, 830–922 m. EX: 374, S38415; 404, S38756; 407, F10112; 456, S39462; 457, S39480; 218, M2618a.

  • *Brigantiaea praetermissa Hafellner & St. Clair — Corticolous on Cupressus nootkatensis, 13 m. DUN: 466, S39634 (fertile). TLC: atr, zeorin. A predominantly inland species of British Columbia, south to Montana.

  • Bryobilimbia hypnorum (Lib.) Fryday et al. — Terricolous on organic accumulations over bases of trees and over rocks, as well as directly on bryophytes, from beaches to alpine ridges, 0–903 m. DUN: 120, F10168 (as ‘cf.’); EX: 455, S39439; 218, M2631a, M2635; GUS: 317, S37898; WA: 103, F9958; 104, F9968; 105, F9995 (sub Caloplaca sinapisperma), F9996; 318, S37909; 381, S38469; 205, M2492.

  • Bryocaulon divergens (Ach.) Kärnefelt — Terricolous in alpine heaths and tundra, 894–922 m. EX: 372, S38373; 407, S38848; 455, S39450; 406, S38794.

  • Bryocaulon pseudosatoanum (Asahina) Kärnefelt — Lignicolous on Pinus contorta in muskeg, 255 m. EX: Yellowlegs Savanna, S37852. Medulla C+ red.

  • **Bryodina rhypariza (Nyl.) Hafellner & Türk — Muscicolous over top of rock, alpine zone, 937 m. EX: 409, S38876 (det. W. Obermayer). New to continental North America, previous North American records have been from the Canadian Arctic Archipelago (Fryday Reference Fryday2000; Zhurbenko et al. Reference Zhurbenko, Matveeva, Vonlanthen, Walker and Raynolds2010).

  • Bryonora curvescens (Mudd) Poelt — Muscicolous over rock, 903 m. EX: 406, S38778.

  • Bryoria americana (Motyka) Holien — Corticolous on Picea sitchensis, Pinus contorta and Tsuga heterophylla, 0–687 m. EX: 358, S38312 (det. T. Goward); 448, S39356, S39357; GB: 874, S36674, S36675; GUS: 107, F10024, F10026; 397, S38700 (det. T. Goward).

  • Bryoria bicolor (Ehrh.) Brodo & D. Hawksw. — Corticolous on Picea sitchensis branches, mainly in beach fringe or headland habitats, 10–60 m. DUN: 339, S38163; GB: 868, S36502; GUS: [V329, S38048]; 857, S36106. TLC: pc (3×) or fpc (1×).

  • Bryoria carlottae Brodo & D. Hawksw. — Lignicolous on Pinus contorta trees or snags in muskeg, 0–236 m. DUN: 338, S38129 (ver. T. Goward), S38135, S38139; 463, S39525 (det. T. Goward, as ‘cf.’); EX: 399, S38728; GUS: 397, S38699. TLC: pc.

  • Bryoria friabilis Brodo & D. Hawksw. — Corticolous on Picea sitchensis; our records are all from beach fringe habitats, 0–60 m. GB: 868, S36492; 874, S36676 (ver. T. Goward), S36678; GUS: 435, S39119, S39129; 857, S36116. TLC: gyrophoric acid.

  • [Bryoria fuscescens (Gyeln.) Brodo & D. Hawksw. — Corticolous on Tsuga snag, 59 m. EX: 860, S36247.]

  • Bryoria glabra (Motyka) Brodo & D. Hawksw. — Corticolous on Picea sitchensis, 3 m. GB: 874, S36673. TLC: pc.

  • Bryoria inactiva Goward et al. — Corticolous, probably on Picea sitchensis branch, found on branch fallen from canopy, 4 m. GUS: between lodge and beach, Park HQ GLBA, S38269 (det. T. Goward).

  • Bryoria lanestris (Ach.) Brodo & D. Hawksw. — Corticolous on Pinus contorta and Tsuga mertensiana branches in muskeg, 12–333 m. EX: 353, S38288; GUS: 316, S37873; 397, S38701. TLC: pc (2×) and fpc (1×).

  • Bryoria nitidula (Th. Fr.) Brodo & D. Hawksw. — Terricolous in alpine heath, 872–907 m. EX: between 405 and 406, S38773; 373, S38379; 456, S39468. TLC: pc.

  • Bryoria pikei Brodo & D. Hawksw. — Corticolous on Picea sitchensis branches; our records are all from beach or headland habitats, 0–12 m. DUN: 463, S39527; 467, S39650; GB: 874, S36679; GUS: 204, S38437; 397, S38696, S38706; 435, S39117; 463, S39531. TLC: alectorialic, barbatolic acids.

  • Bryoria pseudofuscescens (Gyeln.) Brodo & D. Hawksw. — Corticolous on Picea sitchensis branches, 3 m. GB: 874, S36672, S36677. TLC: norstictic acid.

  • Buellia coniops (Wahlenb.) Th. Fr. — Saxicolous, mainly on gneiss boulders and closely associated with seashores, 0–5 m. DUN: 463, F10379 (sub Myriolecis aff. contractula), F10403; S39580; GB: 863, F9704; 865, F9737, F9739, F9743; 873, F9824, S36655, S36656; GUS: 875, F9843, F9844, F9845; WA: 322, S37963; 549, T41629b.

  • Buellia erubescens Arnold — Corticolous on Alnus in beach fringe, sea level. GB: 864, S36326.

  • Buellia griseovirens (Turner & Borrer ex Sm.) Almb. — Corticolous on Alnus, Picea sitchensis and Shepherdia canadensis, also lignicolous on beach logs, 0–46 m. DUN: 113, F10133 (sub Xylographa hians); GUS: 876, S36741; 316, S37884; 434, S39107; 879, S36805; 531, T41537; 576, T41848, T41850. TLC: atr, norstictic acid.

  • *Buellia cf. sequax (Nyl.) Zahlbr. — Saxicolous on alpine ridgetop, 919 m. EX: 374, S38412 (sub Lecanora sp.). A southern species, identification tentative.

  • *Buellia triseptata A. Nordin — Corticolous on fine twigs of Picea sitchensis and Tsuga heterophylla, 0–27 m. DUN: 339, S38184; 463, S39541; GUS: 435, S39123.

  • Calicium abietinum Pers. — Lignicolous on conifer in muskeg, 250 m. EX: 109, F10053; GUS: 435, S39131.

  • Calicium glaucellum Ach. — Lignicolous on snags and exposed dead wood of otherwise still living Pinus contorta trees, 12–217 m. EX: 313, S37844; 398, S38726; 227, M2737; GUS: 397, S38707, S38713, S38714.

  • Calicium lenticulare Ach. — Lignicolous on Tsuga trunks and on snags, 124–717 m. DUN: nr 334, S38103; 563, T41759; EX: 403, S38744; [V431, S39060].

  • Calicium parvum Tibell — Corticolous on Tsuga bark, 687 m. EX: 448, S39359. First reported for Alaska from Lake Clark by McCune et al. (Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018).

  • Calicium viride Pers. — Corticolous on Picea sitchensis and Tsuga underhangs, 12–124 m. DUN: 334, S38102; EX: 313, S37841; 433, S39094; 448, S39359; GUS: 397, S38715.

  • Caloplaca allochroa Y. Joshi et al. (syn. Gyalolechia allochroa (Y. Joshi et al.) Søchting et al.) — Saxicolous on vertical sheltered rock with overhanging vegetation, 809 m. EX: 452, S39368. A DNA sequence from this specimen was published by Vondrák et al. (Reference Vondrák, Frolov, Davydov, Urbanavichene, Chesnokov, Zhdanov, Muchnik, Konoreva, Himelbrant and Tchabanenko2016b, as Gyalolechia allochroa) as new to Alaska and North America.

  • Caloplaca ammiospila (Wahlenb.) H. Olivier (syn. Blastenia ammiospila (Wahlenb.) Arup et al.) — Terricolous or muscicolous from raised beaches to the alpine zone, 0–922 m. EX: 407, F10105; WA: 391, S38640.

  • Caloplaca atrosanguinea (G. Merr.) I. M. Lamb — Corticolous on Alnus, Populus balsamifera and Salix, 0–215 m. EA: 127, F10280; 440, S39195; 441, F10192; 872, S36604; E Muir Pt, M2807, M2820, M2812; GB: 864, S36337; 862, S36313; 556, T41675; GUS: 862, F9675; [574, T41816]; 576, T41845; 210, M2552; WA: 391, S38590; 395, S38667, S38677 (sub Scoliciosporum chlorococcum); 542, T41587.

  • Caloplaca borealis (Vain.) Poelt — Corticolous on Populus balsamifera and Salix, beach fringe habitats, 0–10 m. GB: 864, S36334; WA: 391, S38608, S38609; 395, S38672.

  • Caloplaca caesiorufella (Nyl.) Zahlbr. — Corticolous on Salix in beach fringe, 0–10 m. DUN: 463, S39519; EA: 122, F10229; 123, F10244; nr 438, S39314, S39315; GB: 864, S36360; GUS: 316, S37864; 435, S39130. Hansen et al. (Reference Hansen, Poelt and Søchting1987) questioned the distinctiveness of C. caesiorufella, and subsequent North American checklists have treated it as a synonym of C. phaeocarpella, but we prefer to recognize it until its status can be systematically resolved. An ITS sequence is published here (Table 1).

  • Caloplaca exsecuta (Nyl.) Dalla Torre & Sarnth. — Saxicolous in snowbed habitats, on erratic in muskeg, and on soft argillite in alpine tundra, 22–922 m. DUN: 468, S39677; EX: 407, F10116 (det. Vondrák); 453, F10325, F10326 (sub Lecidea lapicida), 458, S39489; 460, F10361 (det. Vondrák; sub Rhizocarpon polycarpum); 218, M2661. A sequence from S24441, from KLGO, has been deposited in GenBank, under Accession MG954227 (Vondrák et al. Reference Vondrák, Frolov, Davydov, Yakovchenko, Malíček, Svoboda and Kubásek2019a).

  • Caloplaca flavocitrina (Nyl.) H. Olivier (syn. Flavoplaca flavocitrina (Nyl.) Arup et al.) — Saxicolous, just above sea level. DUN: 460, F10372. Cliffs with something resembling this species were also seen from the boat in the north arm of Dundas Bay, but were not accessible.

  • Caloplaca fuscorufa H. Magn. — Saxicolous in the alpine zone, 907–918 m. EX: 373, S38386; 406, S38780; 454, S39387. First reported as new for North America from Lake Clark by McCune et al. (Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018). Sequences from S39387 are available in GenBank: ITS sequences MF114598; Beta-tubulin MF115104; mitochondrial LSU MF114860 (Vondrák et al. Reference Vondrák, Frolov, Košnar, Arup, Veselská, Halıcı, Malíček and Søchting2019b).

  • Caloplaca holocarpa (Hoffm.) A. E. Wade (syn. Athallia holocarpa (Hoffm.) Arup et al.) — Saxicolous on soft argillite in the alpine zone, at least once associated with a bird perch, 890–922 m. EX: 407, F10131 (sub Protoparmeliopsis muralis), S38839; 453, F10322 (sub Tephromela atra), F10323; 455, S39432. Two DNA sequences (isolate T1228 from S39432 = KR902672 and T1233 from S38839 = KR902671) were published by Vondrák et al. (Reference Vondrák, Halıcı, Güllü and Demirel2016a, as Athallia holocarpa).

  • *Caloplaca kamtczatica Savicz — Corticolous on Alnus, Picea sitchensis and Tsuga heterophylla, beaches or headlands, 9–27m. DUN: 339, S38162, S38195; 463, S39513. We obtained DNA from one specimen (Table 1).

  • Caloplaca litoricola Brodo — Saxicolous on rocky headland, 9 m. DUN: 463, F10392 (sub Herteliana alaskensis), S39571, S39574.

  • Caloplaca nivalis (Körb.) Th. Fr. — Muscicolous over granitic rock in the alpine zone, 460 m. DUN: 121, F10179.

  • Caloplaca persimilis Wetmore (syn. Gyalolechia persimilis (Wetmore) Søchting et al.) — Corticolous on Cupressus nootkatensis, 68 m. DUN: 413, S38925; 567, T41766. A previously published ITS rDNA sequence from GLBA (KT804988 from S38925) places this specimen within the Caloplaca persimilis group (Vondrák et al. Reference Vondrák, Frolov, Davydov, Urbanavichene, Chesnokov, Zhdanov, Muchnik, Konoreva, Himelbrant and Tchabanenko2016b) where it clusters with a taxon described as C. ussuriensis from the Russian Far East. However, it is unclear if this will resolve as a species distinct from C. persimilis.

  • Caloplaca sinapisperma (Lam. & DC.) Maheu & A. Gillet (syn. Bryoplaca sinapisperma (Lam. & DC.) Søchting et al.) — Muscicolous or on organic accumulations over limestone, beaches and outcrops, 0–52 m. GB: 867, S36441, S36443 (without anthraquinones!); 382, S38480; WA: 105, F9995. We obtained DNA from two specimens (Table 1).

  • Caloplaca sorocarpa (Vain.) Zahlbr. — Corticolous on Alnus and Salix, 10 m. GB: 866, S36420, S36425 (sub Nephroma resupinatum); WA: 384, S38507; 544, T41605; 206, M2503.

  • Caloplaca stillicidiorum (Vahl) Lynge — Growing on Dryas detritus and bryophytes, 0–22 m. WA: 105, F9995 (sub Caloplaca sinapisperma); 318, S37902.

  • Caloplaca tetraspora (Nyl.) H. Olivier (syn. Bryoplaca tetraspora (Nyl.) Søchting et al.) — Terricolous on organic accumulations over rock outcrops, 10–100 m. WA: 101, F9903 (sub Scytinium imbricatum).

  • Caloplaca tiroliensis Zahlbr. (syn. Parvoplaca tiroliensis (Zahlbr.) Arup et al.) — Terricolous/muscicolous in alpine heath, 922 m. EX: 407, F10125. Verified by an ITS rDNA sequence, obtained too late to be included in the present GenBank submission.

  • Caloplaca tornoënsis H. Magn. — Saxicolous on small rock in snowbed, 830 m. EX: 404, S38753. DNA sequences from KLGO (S29473 = MG954221 and S26816 = MG954220) are published in Vondrák et al. (Reference Vondrák, Frolov, Davydov, Yakovchenko, Malíček, Svoboda and Kubásek2019a).

  • Calvitimela aglaea (Sommerf.) Hafellner — Saxicolous on argillitic rocks in the alpine zone, 883–922 m. EX: 370, S38341 (sub Melanelia hepatizon); 373, S38382; 405, F10101; 407, S38829, S38830; 455, S39433; 218, M2655b. TLC: atranorin.

  • Calvitimela perlata (Haugan & Timdal) R. Sant. — Saxicolous on exposed alpine summit, 618 m. DUN: 428, S39024. This species was reported as new to North America based on material from GLBA and KLGO (Bendiksby et al. Reference Bendiksby, Haugan, Spribille and Timdal2015); previously known from Norway.

  • Candelariella arctica (Körb.) R. Sant. — Saxicolous on rocky seashore, 27 m. DUN: 339, 38204 (det. M. Westberg). An uncommon species reported in AK from the Bering Sea and several locations in inland western AK (Thomson Reference Thomson1997). A 19th century report from Baranof Island under the name Placodium crenulatum (Cummings Reference Cummings, Cardot, Cummings, Evans, Peck, Thériot and Trelease1904) could refer to this species but should be checked.

  • Candelariella efflorescens R. C. Harris & W. R. Buck — Corticolous and muscicolous over Alnus and Populus balsamifera, 0–22 m. EA: 440, S39233, S39260; GB: 864, S36336; S36339 (sub Micarea peliocarpa); Marble Mtn, S38012; GUS: Tower Rd, S40731.

  • Candelariella vitellina (Hoffm.) Müll. Arg. — Saxicolous on bird perches, 125–942 m. EX: 408, S38865; 459, F10360 (as ‘aff.’); WA: 388, S38561. F10360 is parasitic on Placynthium. The occurrences on small cyanolichens deserve further study; C. vitellina was also recorded as parasitic on Tingiopsidium in KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010).

  • #Capronia peltigerae (Fuckel) D. Hawksw. — Lichenicolous on Peltigera, terricolous on beach ridge, 4 m. EA: 438, S39185.

  • *#Carbonea aggregantula (Müll. Arg.) Diederich & Triebel — Lichenicolous on Lecanora polytropa group near glacier terminus, 15 m. WA: A571, P2287, P2314.

  • Carbonea vorticosa (Flörke) Hertel — Saxicolous on rocks in the alpine zone, 465–937 m. DUN: 426, S38991; EX: 407, S38826; 409, S38893; 454, S39405.

  • Carneothele sphagnicola Fryday, M. Svenss. & Holien — See ‘Descriptions of New Genera and Species’.

  • Catapyrenium cinereum (Pers.) Körb. — Terricolous on organic accumulations and open ground from supralittoral sea stacks to the alpine zone, 0–922 m. DUN: 463, F10387, F10400; EX: 407, S38852.

  • Catapyrenium daedaleum (Kremp.) Stein — Terricolous and muscicolous, 11–43 m. EA: 872, S36637; WA: 319, S37925; 381, S38470.

  • Catillaria chalybeia (Borrer) A. Massal. — Saxicolous in the supralittoral zone, in splash zone, on gneiss, 0–5 m. DUN: 134, F10461, F10462.

  • #Catillaria stereocaulorum (Th. Fr.) H. Olivier — Lichenicolous on Stereocaulon on c. 20 yr-old gravels, 0–43 m. EA: 869, S36552; Muir Inlet, S40768.

  • Catinaria atropurpurea (Schaer.) Vězda & Poelt — Corticolous on Picea sitchensis and Populus balsamifera, 0–10 m. GB: 864, S36366; GUS: 576, T41839; 230, M2764.

  • Catolechia wahlenbergii (Ach.) Körb. — On organic accumulations in the side of a granitic boulder by tarn inflow in a muskeg, 150 m. DUN: 118, F10152.

  • #Cecidonia xenophana (Körb.) Triebel & Rambold — Lichenicolous on Porpidia macrocarpa aggr. on rock, or on unspecified saxicolous lichen over granite, 100–903 m. DUN: 117, F10149; EX: 406, S38782 (sub Lecidea swartzioidea). DNA was obtained from S38782 (Table 1).

  • #Cercidospora cephalodiorum Triebel & Grube — Lichenicolous on Pilophorus dovrensis in alpine heath with rock outcrops, on alkaline argillite, 918 m. EX: 454, F10340 (sub Pilophorus dovrensis).

  • #Cercidospora epipolytropa (Mudd) Arnold — Lichenicolous on Lecanora spp., 0–871 m. EX: 458, S39483 (sub Lecanora frustulosa); WA: 381, S38465 (sub Lecanora polytropa); 391, S38619, S38637 (sub Lecanora polytropa); A571, P2287; A576, P2186.

  • Cetraria aculeata (Schreb.) Fr. — Terricolous in the alpine zone and in water pools in muskeg near sea level, and once recorded lignicolous and fertile, 27–922 m. DUN: 428, 39000; 465, F10426, 39628; EX: 348, S38283 (fertile, lignicolous); 370, 38360; 405, F10080, F10093; 407, F10129; 408, S38870; 455, S39448; 459, F10358. The fertile specimen S38283, from wood in a muskeg, corresponds to the morphology of Cetraria crespoae (Barreno & Vázquez) Kärnefelt, the epiphytic form of C. aculeata originally described from Spain (Barreno & Vasquez Reference Barreno and Vázquez1981).

  • Cetraria ericetorum Opiz subsp. reticulatum (Räsänen) Kärnefelt — Terricolous in Cassiope-Fauria heath and alpine tundra, 484–922 m. DUN: 425, S38987; EX: 405, F10081; 407, S38843.

  • Cetraria islandica (L.) Ach. subsp. crispiformis (Räsänen) Kärnefelt — Terricolous in the alpine zone, 903 m. EX: 406, S38790.

  • Cetraria islandica subsp. orientalis (Asahina) Kärnefelt — Terricolous in the alpine zone, 894–918 m. EX: 372, S38374; 454, F10339 (sub Toensbergia geminipara).

  • Cetraria laevigata Rass. — Terricolous in the alpine zone, 872–895 m. EX: 370, S38352; 456, S39465.

  • Cetraria nigricans Nyl. — On small accumulations of soil over rock, 907 m. EX: 373, S38404.

  • Cetrelia cetrarioides (Duby) W. L. Culb. & C. F. Culb. — Corticolous on Alnus, 2 m. EA: 441, S39266; GB: S Sandy Cove, S40752. TLC: atr, perlatolic acid.

  • Chaenotheca brunneola (Ach.) Müll. Arg. — Lignicolous on snags or corticolous on Picea or Tsuga, 21–717 m. EX: 109, F10047; 357, S38304; 403, S38745; 433, S39093; GUS: [V329, S38059]; 204, S38442, S38443.

  • Chaenotheca chrysocephala (Turner ex Ach.) Th. Fr. — Corticolous on Pinus contorta in a muskeg, also lignicolous, 0–5 m. DUN: 421, S38961 (sub Chaenotheca ferruginea); GUS: 107, F10027; 230, M2762; 397, S38716 (sub Chaenotheca ferruginea).

  • *Chaenotheca ferruginea (Turner ex Sm.) Mig. — Corticolous on rain-shaded parts of large Picea or Tsuga trunks, or lignicolous, 248–396 m. DUN: 421, S38961; EX: 213, M2569; 354, S38294, S38296 (sub Chaenothecopsis aeruginosa); GUS: 397, S38716.

  • Chaenotheca furfuracea (L.) Tibell — Lignicolous on a Picea snag, also terricolous on rock and detritus of tip-up, 58–569 m. EX: 358, S38328; GUS: 878, S36773.

  • Chaenotheca gracillima (Vain.) Tibell — Lignicolous on snags, or fungicolous on Trichaptum abietinum, in mixed woodland by creek, 44–569 m. EX: [125, F10267 (on Trichaptum)]; [859, F9658 (on lignum)]; 358, S38325; 398, S38722, S38723, S38725. The specimen from Trichaptum was compared to Chaenotheca balsamconensis, J. L. Allen & McMullin a species described from North Carolina that occurs exclusively on Trichaptum (Allen & McMullin Reference Allen and McMullin2015), but differed in possessing a brown, KOH− stalk.

  • Chaenotheca trichialis (Ach.) Hellb. — On polypore on Tsuga snag and corticolous on Tsuga, 59–569 m. EX: [860, S36257]; 358, S38327 (sub Chaenotheca chrysocephala).

  • Chaenotheca xyloxena Nádv. — Lignicolous on snag, 58 m. GUS: 878, S36788.

  • *+Chaenothecopsis aeruginosa Goward & E. B. Peterson — Corticolous on Tsuga, 222–396 m. DUN: 469, S39697; EX: 313, S37840, S37845; 354, S38296.

  • #Chaenothecopsis arthoniae Tibell — Lichenicolous on Arthonia arthonioides, corticolous on Malus fusca and Tsuga heterophylla, 9–222 m. DUN: between 462 and 469, S39684; EX: 313, S37842; [226, M2731]; 358, S38330; 448, S39347 (sub Arthonia arthonioides); GUS: 855, S36051. First reported for Alaska by Dillman et al. (Reference Dillman, Ahti, Björk, Clerc, Ekman, Goward, Hafellner, Pérez-Ortega, Printzen and Savic2012) from KLGO.

  • #Chaenothecopsis consociata (Nádv.) A. F. W. Schmidt — On Chaenotheca trichialis over Tsuga bark, 569 m. EX: 358, S38327 (sub Chaenotheca chrysocephala).

  • *#Chaenothecopsis lecanactidis Tibell — On Lecanactis on sheltered trunk of Tsuga, 569 m. EX: 358, S38329. Recently reported as new to North America from Washington (Hardman et al. Reference Hardman, Stone and Selva2017).

  • +Chaenothecopsis nana Tibell — Corticolous on Picea and Tsuga bark, 21–396 m. EX: 354, S38295; 433, S39092.

  • +Chaenothecopsis pusiola (Ach.) Vain. — Lignicolous on snag, 58 m. GUS: 878, S36788 (sub Chaenotheca xyloxena).

  • +Chaenothecopsis savonica (Räsänen) Tibell — Lignicolous on small snag, 222 m. EX: 313, S37843 (as ‘aff.’).

  • +Chaenothecopsis tasmanica Tibell — Corticolous on Picea trunk, 124 m. DUN: 334, S38102 (sub Calicium viride); EX: 313, S37842.

  • *+Chaenothecopsis viridireagens (Nádv.) A. F. W. Schmidt — Lignicolous on small snag, 222 m. EX: 313, S37843 (sub Chaenothecopsis aff. savonica); 354, S38295 (sub Chaenothecopsis nana s. lat.).

  • Cheiromycina petri D. Hawksw. & Poelt — Corticolous on Alnus, 2 m. GB: 865, S36401. Recently reported as new for Alaska by McCune et al. (Reference McCune, Arup, Breuss, Di Meglio, Di Meglio, Esslinger, Magain, Miadlikowska, Miller and Muggia2018).

  • #Cirrenalia lichenicola Pérez-Ort. — See ‘Descriptions of New Genera and Species’.

  • Cladonia amaurocraea (Flörke) Schaer. — Terricolous in the alpine zone, 872–922 m. EX: 370, S38355; 407, S38851; 456, S39467. TLC: usnic and barbatic acids.

  • Cladonia arbuscula (Wallr.) Flot. subsp. beringiana Ahti — Terricolous on damp sandy soil, wet muskeg and in alpine tundra, 20–922 m. DUN: 338, S38145; 464, S39621, S39622; EX: between 405 and 406, S38775 (det. T. Ahti); 407, S38840; 453, S39371, S39374 (det. T. Ahti, as ‘cf. arbuscula’); 456, S39470; GUS: Tower Rd, S37518 (as ‘cf.’), S37531. TLC: usnic acid, fpc.

  • Cladonia asahinae J. W. Thomson — Terricolous on organic accumulations over rock in low elevation snowbed, 92 m. WA: 387, S38551. TLC: fatty acid, fpc.

  • Cladonia bellidiflora (Ach.) Schaer. — Terricolous in heath and muskeg, also seen corticolous (on Pinus contorta) and on stumps, 20–937 m. DUN: 338, S38141; 464, F10423; EX: [858, S36214]; [859, S36235]; 375, S38427; nr 409, S38902; 453, S39376. TLC: squamatic acid.

  • Cladonia borealis S. Stenroos — Terricolous in grassy sandy soil in the Gustavus outwash plain, also in recently deglaciated terrain, 0–33 m. EA: Muir Inlet, S40780; GUS: State Dock, S36851; Tower Rd, S37515. TLC: usnic acid, barbatic + sat, fatty acid.

  • Cladonia cariosa (Ach.) Spreng. — Terricolous at base of Pinus contorta in open flats and over marble outcrop, 0–43 m. EA: Muir Inlet, S40775, S40781; GB: 867, S36453; GUS: 317, S37893 (s. lat.); WA: 319, S37944. TLC: fpc but little material used for assay (atr cannot be ruled out).

  • Cladonia carneola (Fr.) Fr. — a) chemotype 1: terricolous and once lignicolous on burl of old Pinus contorta, 0–43 m. GUS: 876, S36757; Tower Rd, S37514; WA: 319, S37950. TLC: usnic and isousnic acids, zeorin; b) chemotype 2: terricolous in upper beach meadow to muscicolous over boulders and corticolous on Tsuga mertensiana in subalpine snowbeds, 0–788 m. DUN: 425, S38984; EX: 460, S39496; GUS: 437, S39171. TLC: isousnic/usnic and barbatic acids, zeorin; c) chemotype not determined: terricolous and corticolous, 0–10 m. DUN: 464, F10413; GUS: 316, S37888; WA: 102, F9934.

  • [Cladonia cenotea (Ach.) Schaer. — Terricolous in grassy meadow, 3 m. GUS: State Dock, S36853 (det. T. Ahti, sub C. verruculosa).]

  • Cladonia chlorophaea (Flörke ex Sommerf.) Spreng. — Terricolous and on organic accumulations over rocks and trees in muskeg and forest, 10–245 m. EA: Muir Inlet, S40782; DUN: 338, S38143; EX: 400, S38737; 457, S39478; WA: 319, S37926; 383, S38497. TLC: fpc.

  • Cladonia coccifera (L.) Willd. — Terricolous on organic accumulations along shorelines and in snowbeds, 0–115 m. EA: between 870 and 871, S36591; WA: 102, F9933; 387, S38549. TLC: isousnic/usnic acid, zeorin.

  • *Cladonia concinna Ahti & Goward — Terricolous on sandy soil of Gustavus outwash plain, also over a boulder in snowbed, 33–92 m. GUS: Tower Rd, S37533 (conf. T. Ahti); WA: 387, S38549 (sub Cladonia coccifera). Described from the west coast of Vancouver Island (Ahti Reference Ahti2007).

  • Cladonia coniocraea (Flörke) Spreng. — Terricolous in upper beach meadows, corticolous on Alnus, lignicolous on Pinus contorta, also over moss and on fine Tsuga heterophylla twigs, 0–213 m. DUN: 462, S39708; EX: 312, S37830; [858, S36225]; GB: 864, S36396 (sub Cladonia fimbriata); 874, S36718 (sub Cladonia umbricola); GUS: 397, S38705; 437, S39170; 878, S36787. TLC: fpc.

  • [Cladonia conista (Nyl.) Robbins — Terricolous on sandy soil, 3 m. GUS: State Dock, S36848. TLC: fpc, bourgeanic acid.]

  • Cladonia cornuta (L.) Hoffm. — Terricolous on sandy soils, 10–33 m. EA: terminus of Riggs Glacier, S40808; GUS: Tower Rd, S37540; WA: 384, S38528.

  • Cladonia crispata (Ach.) Flot. var. cetrariiformis (Delise) Vain. — Terricolous in muskeg (even in standing water) and alpine tundra, 20–922 m. DUN: between 412 and 415, S38919; 338, S38142; 464, S39617, S39626; 465, S39630; EX: 110, F10059; 312, S37828; 371, S38366; 400, S38736; 407, S38845; 456, S39463; 457, S39479; GUS: Tower Rd, S37525-B. TLC: squamatic acid, ±barbatic acid.

  • Cladonia crispata var. crispata — Terricolous on tip-up in muskeg, 213 m. EX: 312, S37831 (ver. T. Ahti). TLC: squamatic acid.

  • Cladonia ecmocyna Leight. — Terricolous on ‘semi-open herbaceous ridge’, 610 m. GB: slopes and ridges of mainland immediately NW of Sebree Cove and W of Caroline Point, 1968, Worley 10533 (UBC, det. T. Goward). This species was not encountered during the present survey.

  • Cladonia farinacea (Vain.) Evans — Terricolous on mossy soil in forest on coastal headland, 17 m. DUN: 467, S39674 (det. T. Ahti). TLC: fpc. A distinctive and rare species in Alaska, until now known only from Kotzebue (Krog Reference Krog1968) and Gates of the Arctic (Dillman et al. Reference Dillman, Ahti, Björk, Clerc, Ekman, Goward, Hafellner, Pérez-Ortega, Printzen and Savic2012).

  • Cladonia fimbriata (L.) Fr. — Terricolous on organic accumulations over rock, 10–903 m. EA: Muir Inlet, S40784; EX: 455, S39441; GB: 864, S36396, S36397 (sub Cladonia pyxidata); 865, S36411; GUS: 437, S39169 (sub Cladonia pyxidata); WA: 383, S38501. TLC: fpc.

  • Cladonia furcata (Huds.) Schrad. — Terricolous on sandy road banks, all collections from the Gustavus outwash plain, 30–40 m. GUS: 880, S36820, S36821; Tower Rd, S37522, S37539. TLC: fpc.

  • Cladonia gracilis (L.) Willd. subsp. elongata (Wulfen) Vain. — Terricolous in wet muskeg and alpine snowbeds, 20–903 m. DUN: 464, S39618; 465, S39633; EX: 406, S38798 (ver. T. Ahti), S38799; nr 455, S39458; 456, S39460 (dwarf morph); GUS: Tower Rd, S37524, S37525. TLC: fpc.

  • Cladonia gracilis subsp. turbinata (Ach.) Ahti — Terricolous on sandy soil, 33 m. GUS: Tower Rd, S37526.

  • Cladonia gracilis subsp. vulnerata Ahti — Terricolous in muskeg, 226 m. DUN: 338, S38146 (det. T. Ahti).

  • Cladonia kanewskii Oxner — Terricolous, 50 m. DUN: between 412 and 415, S38922. TLC: usnic acid, fatty acids.

  • Cladonia maxima (Asahina) Ahti — Terricolous in muskegs and wet headland forest, 10–222 m. DUN: 467, F10439, S39675; EX: 312, S37827.

  • Cladonia mitis Sandst. — Terricolous on sandy soil and alpine tundra, 0–903 m. EX: 312, S37822; 372, S38375; 406, S38792; 408, S38867; GUS: State Dock, F9870. TLC: usnic acid, unknown R f A1/B5/C1-2.

  • [Cladonia norvegica Tønsberg & Holien — Corticolous on Picea sitchensis log in Picea forest, 19 m. GUS: 557, T41717. TLC: barbatic and 4-O-demethylbarbatic acids.]

  • Cladonia ochrochlora Flörke — Terricolous on sandy road cut and on organic or woody accumulations over rock, 0–39 m. EA: Muir Inlet, S40769; GB: S Sandy Cove, S40759; GUS: 100, F9891; 880, S36822 (det. T. Ahti); WA: 384, S38527 (det. T. Ahti). This species, which is ubiquitous further inland in NW North America, appears to be uncommon in GLBA.

  • Cladonia phyllophora Hoffm. — Terricolous on sandy lowland soil and in alpine tundra, 33–942 m. EX: 408, S38871; GUS: Tower Rd, S37521, S37534. TLC: fpc.

  • Cladonia pocillum (Ach.) Grognot — Terricolous over limestone, 33–52 m. WA: 382, S38479; E slopes of Marble Mtn opposite Drake Island, 9 August 1968, I. A. Worley 11234 (UBC, det. C. R. Björk). Not seen during the present survey.

  • Cladonia portentosa (Dufour) Coem. subsp. pacifica Ahti — Terricolous in muskeg, 27–149 m. DUN: 415, S38935; 416, S38945. TLC: usnic and perlatolic acids.

  • Cladonia pseudalcicornis Asahina — Terricolous over boulder in snowbed Salix/Shepherdia scrub, 92 m. WA: 387, S38548, S38552. TLC: fpc.

  • Cladonia pseudoevansii Asahina — Terricolous in wet muskeg, 25 m. DUN: 465, F10425, S39629, S39631 (both det. T. Ahti). Collection S39629 represents an usnic acid-free strain that co-occurred with specimens with the typical usnic acid-containing chemosyndrome.

  • Cladonia pyxidata (L.) Hoffm. — Terricolous on organic accumulations on logs, tip-ups, over boulders, on road cuts, in snowbeds and directly on soil, 0–907 m. DUN: 462, S39747; EA: 869, S36568; 312, S37829; EX: 358, S38316; 373, S38401; 404, S38757; 456, S39461; GB: 864, S36391; 873, S36662, S36664, S36668; GUS: 880, S36824; 437, S39169; WA: 319, S37946; 322, S37962; 383, S38486; 387, S38547; 864, S36397. TLC: fpc.

  • Cladonia rangiferina (L.) F. H. Wigg. — Terricolous in muskeg, heath and on sandy soil, 0–937 m. DUN: 337, S38127; 338, S38144; between 412 and 415, S38920 (PD+ orange); 416, S38946; 464, S39620; EX: 312, S37825, S37826; 453, S39377, S39378; 409, S38896; GUS: Tower Rd, S37536; State Dock, F9871. TLC: atr, fpc.

  • Cladonia rei Schaer. — Terricolous on beach ridges and old gravels, 0–43 m. EA: 438, S39183, S39183-B; 869, S36547; 869, S36565; Muir Inlet, S40779, S40786; terminus of Riggs Glacier, S40797; GB: 864, S36395; 873, S36670; GUS: 876, S36755; WA: 325, S37983; 383, S38498. TLC: homosekikaic acid, fpc.

  • Cladonia scabriuscula (Delise) Nyl. — Terricolous on sandy soil or on organic accumulations on logs and stumps, 0–713 m. DUN: 462, S39698, S39748 (conf. T. Ahti); EX: [859, S36233]; above ‘Mooselator’, S38903 (conf. T. Ahti); GUS: State Dock, S36857. TLC: fpc.

  • Cladonia squamosa Hoffm. — On organic accumulations over rock, stumps, soil, Picea and Tsuga trunks and logs, and in alpine heath, 0–872 m. DUN: 413, S38932; 416, S38944; 423, S38979; EX: [858, S36213]; [859, S36233 (sub Cladonia scabriuscula)]; 448, S39352; 456, S39464; 460, S39495 (det. T. Ahti: ‘arctic morph’ with fpc!); GB: 874, S36716; GUS: 855, S36012. TLC: squamatic or squamatic and barbatic acids (tr) (2×) or squamatic acid and fpc (1×).

  • Cladonia stellaris (Opiz) Pouzar & Vězda — Terricolous in heath 883–922 m. EX: 371, S38364 (s. lat.); 405, F10082; 406, S38793; 407, F10104, S38842; 453, S39373, S39379. TLC: usnic, perlatolic acids.

  • Cladonia straminea (Sommerf.) Flörke — Lignicolous on wooden stick in muskeg, 294 m. EX: 352, S38286 (as C. metacorallifera). TLC: usnic, didymic, squamatic acids.

  • Cladonia stricta (Nyl.) Nyl. — Terricolous on sandy soil, 33 m. EX: 406, S38798 (det. T. Ahti; sub C. gracilis subsp. elongata); GUS: Tower Rd, S37529, S37542 (det. T. Ahti). TLC: fpc.

  • Cladonia stygia (Fr.) Ruoss — Terricolous in the alpine zone, 922 m. EX: 407, S38846 (ver. T. Ahti). TLC: atr, fpc.

  • Cladonia subfurcata (Nyl.) Arnold — Terricolous in wet muskeg and on damp sand, 20–236 m. DUN: 464, S39627; EX: 399, S38219; GUS: Tower Rd, S37517. TLC: squamatic acid.

  • Cladonia subulata (L.) F. H. Wigg. — Terricolous on sandy soil, 20–33 m. GUS: Tower Rd, S37535 (ver. T. Ahti); WA: 383, S38482 (det. T. Ahti). TLC: fpc.

  • Cladonia sulphurina (Michx.) Fr. — Terricolous over rock, 10 m. WA: 383, S38503.

  • Cladonia symphycarpa (Flörke) Fr. — Terricolous on organic/mineral accumulations over rock and on sandy road cut, 22–903 m. EX: 406, S38797; GUS: 880, S36823; WA: 318, S37912; 319, S37943; 382, S38481. TLC: atr, norstictic acid.

  • Cladonia trassii Ahti — Terricolous on sandy soil, 33 m. GUS: Tower Rd, S37519. TLC: atr, fpc.

  • Cladonia turgida Hoffm. — Terricolous in compact muskeg-meadow, 100 m. DUN: 418, S38951 (ver. T. Ahti), S38952. TLC: atr. A rare species in Alaska and western North America. We found a single but conspicuous patch in the Dundas Basin.

  • Cladonia umbricola Tønsberg & Ahti — The common red-fruited Cladonia species on tree trunks and stumps at low elevations. Chemotype 1 (squamatic acid): at base of tree, 59 m. EX: [860, 36237 (together with chemotype 2)]. Chemotype 2 (squamatic acid plus usnic acid visible in all samples but often in too low concentrations to detect by TLC): lignicolous on rotten stumps and logs and corticolous or muscicolous over Picea and Tsuga tree trunks, 0–162 m. EX: [858, S36206]; [860, S36237, S36238 (det. T. Ahti)]; GB: 874, S36714, S36718 (as ‘cf.’); N Sandy Cove, S36650; 874, S36719; GUS: 856, S36076; 316, S37862; 855, S36020; 876, S36742; Tower Rd, S37504. Chemotype 4 (usnic, thamnolic acids): lignicolous on stump, 44 m. EX: [859, S36234]. Chemotype not determined: moss/bark over base of Picea sitchensis, and side of mossy log. GUS: 107, F10036. Chemotypes numbered after Goward (Reference Goward1999).

  • Cladonia uncialis (L.) F. H. Wigg. (incl. subsp. biuncialis (Hoffm.) M. Choisy) — Terricolous on sandy soils, in muskeg and in alpine heath, 27–889 m. DUN: 338, S38140; between 412 and 415, S38921; 465, S39632; 131, F10441; EX: 312, S37823; 453, S39375; GUS: Tower Rd, S37527, S37538. TLC: usnic, squamatic acids.

  • Cladonia verruculosa (Vain.) Ahti — Terricolous on young soils in glacial forelands and mineral accumulations over rock, 10–115 m. EA: between 870 and 871, S36592 (ver. T. Ahti); [GUS: State Dock, S36853 (ver. T. Ahti)]; WA: 383, S38499 (ver. T. Ahti); 387, S38550 (ver. T. Ahti). TLC: fpc.

  • Cladonia wainioi Savicz — Terricolous in wet muskeg, 20–213 m. DUN: 464, F10416, S39624, S39625; EX: 312, 37824. TLC: atr, merochlorophaeic acid.

  • Clauzadea monticola (Schaer.) Hafellner & Bellem. — Saxicolous on limestone, including pebbles, underhangs and larger rocks, 0–886 m. EX: 217, M2594; GB: 863, F9693, F9696, F9703; 864, F9728, S36388; WA: 101, F9912, F9925; 105, F9984; 383, S38489; 391, S38622, S38624; 392, S38645; 209, M2527; waypoint not recorded, M2534.

  • Cliostomum griffithii (Sm.) Coppins — Corticolous and lignicolous on Cupressus nootkatensis and Picea sitchensis, always near the seashore, 12–68 m. DUN: 413, S38927 (aff.); 572, T41793 (poor material); EX: 433, S39069; GB: 868, S36530; GUS: 397, S38694. TLC: atr, roccellic acid, except S38927 roccellic only, poor material but morphologically similar to C. griffithii.

  • Cliostomum leprosum (Räsänen) Holien & Tønsberg — Corticolous on Tsuga heterophylla and T. mertensiana, especially on veteran trees, 20–396 m. DUN: 332, S38068; 334, S38094; 467, S39657; 131, F10444; 563, T41757; 565, T41761; EX: [860, F9665, S36246]; 313, S37835, S37837; 354, S38291, S38292; 433, S39084; waypoint not recorded, M2588; GUS: 876, S36738. TLC: atr only.

  • **#Clypeococcum placopsiiphilum Øvstedal & D. Hawksw. — Lichenicolous on Placopsis sp. on sea stacks, 2 m. DUN: 586, P2164. Previously known from Antarctica (Øvstedal & Hawksworth Reference Øvstedal and Hawksworth1986), Russia (Zhurbenko Reference Zhurbenko2009) and Iceland (Berger Reference Berger2000; Brackel Reference Brackel2010).

  • [Coccotrema hahriae T. Sprib. & Tønsberg — Corticolous on Picea sitchensis branches, 33 m. GUS: 329, S38058; 557, T41702. TLC: stictic, norstictic (tr) acids. This is the first record of the species outside of KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010).]

  • Coccotrema pocillarium (Cumm.) Brodo — Corticolous on Alnus, Cupressus nootkatensis, Picea sitchensis and Tsuga heterophylla, usually close to seashores but once (Excursion Ridge) in a high montane forest; 0–432 m. DUN: 114, F10137; 129, F10363; 333, S38088; 339, S38155, S38176; 412, S38916; 462, S39502; 466, S39636; 467, F10431, F10437, S39664, S39667; 560, T41737; 561, T41741; 573, T41802; EX: 108, F10039; 355, S38298; GB: 868, S36456, S36472, S36509, S36521; GUS: 341, S38230; 436, S39142, S39157. TLC: stictic acid, ±sats.

  • Coenogonium pineti (Ach.) Lücking & Lumbsch — Corticolous on Picea sitchensis and Populus balsamifera, 1–20 m. GUS: 434, S39097; 341, S38242. DNA sequences from S39097 were published by Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015).

  • Collema furfuraceum (Arnold) Du Rietz — Corticolous on Populus balsamifera trunk, 25 m. GUS: Tower Rd, S40727.

  • Collema glebulentum (Nyl. ex Cromb.) Degel. — Terricolous on soil over rock at edge of creek and saxicolous over basic rocks, 219–918 m. EX: 128, F10288; 310, S37807; 406, S38781; 407, S38833; 454, S39389; GB: 864, S36383.

  • Collemopsidium sublittorale (Leight.) Grube & B. D. Ryan — Saxicolous on limestone rocks on shore, 0–5 m. GB: 863, F9706.

  • Cornicularia normoerica (Gunn.) Du Rietz was originally reported by Macoun (Reference Macoun1902) as having been collected by Trevor Kincaid on 13 July 1897 at Muir Glacier. There is no indication that the material was seen in later studies (e.g. Krog Reference Krog1968; Kärnefelt Reference Kärnefelt1986). Attempts to locate the material in North American herbaria have been unsuccessful, and it is possible that the identification was revised and the material is now filed under another name. Collections by Trevor Kincaid from other parts of Alaska (St George Island, St Paul Island) from late July and August 1897 are filed at the University of Michigan herbarium, but there is no record of this specimen in the Consortium of North American Lichen Herbaria ( This is the only reported location from Alaska, although its occurrence in GLBA would not be implausible: the species is known from adjacent regions of northern British Columbia. We suspect that the Cornicularia normoerica specimen reported by Macoun (Reference Macoun1902) could be the same reported as Pseudephebe pubescens by Degelius (Reference Degelius1937), though there is nothing on the packet at UPS to indicate an earlier identification as C. normoerica. There is also a possibility that the original report by Macoun (Reference Macoun1902) was itself a clerical error; Macoun's reports on his own collections are known to be full of errors and impossible records (Godfrey Reference Godfrey1977).

  • *#Cornutispora lichenicola D. Hawksw. & B. Sutton — Lichenicolous in apothecia of Micarea and on Lepra subvelata and Pertusaria subambigens, 15–20 m. GUS: 434, S39101; A569, P2300, P2384.

  • #Corticifraga fuckelii (Rehm) D. Hawksw. & R. Sant. — Lichenicolous on Peltigera, terricolous or muscicolous over marble, 0–125 m. GB: 867, S36438; WA: 388, S38554; 389, S38579.

  • #Corticifraga nephromatis Pérez-Ort. — See ‘Descriptions of New Genera and Species’.

  • #Corticifraga scrobiculatae Pérez-Ort. — Lichenicolous on Lobarina scrobiculata, on Alnus, 8 m. EA: 440, S39258.

  • *Cryptothele neglecta Henssen — Saxicolous on small siliceous cobble deposited over limestone, 15 m. WA: 381, S38467. A distinctive species with >50 ascospores per ascus, 3.5–4.2 × 2.5 μm, previously known only from Sweden (Jørgensen Reference Jørgensen, Ahti, Jørgensen, Kristinsson, Moberg, Søchting and Thor2007). The specimen matches material from the type locality (Sweden, [Närke], Askersund, Lind, 1870, Blomberg s. n., UPS!).

  • Cystocoleus ebeneus (Dillwyn) Thwaites — Saxicolous on the side of granitic boulder, 20–25 m. GUS: 142, F10497.

  • Dendriscosticta wrightii (Tuck.) Moncada & Lücking — A symbiodeme-forming fungus that occurs in the form of two lichen symbioses in GLBA: a) chloromorph: corticolous on Alnus, 0–46 m. EA: nr 438, S39297; GB: N Sandy Cove, F9816, S36654; GUS: 876, S36723; 879, S36811; 881, S36830, S36833; [V329, S38016]; [557, T41706, T41710]; 559, T41727; b) cyanomorph (‘Dendriscocaulon’): corticolous on Alnus, 5–10 m. EA: 123, F10239; GB: S Sandy Cove, S40748; GUS: 111, F10061.

  • Dibaeis baeomyces (L. f.) Rambold & Hertel — Terricolous, forming sterile white crusts, found only in the Dundas Basin, 149–465 m. DUN: nr 416, S38948; 426, S38996. Rarely fruiting in SE Alaska (recently found with apothecia near Mendenhall Glacier). DNA from a GLBA specimen was published by Spribille et al. (Reference Spribille, Resl, Ahti, Pérez-Ortega, Mayrhofer and Lumbsch2014b, as isolate P80).

  • *#Didymellopsis pulposi (Zopf) Grube & Hafellner — Lichenicolous on Leptogium, on organic accumulations over rock, 22 m. WA: 318, S37917. One previous record from North America, from the Northwest Territories (Zhurbenko Reference Zhurbenko2013).

  • Enchylium tenax (Sw.) Gray — Muscicolous over siliceous rock, 0–10 m. GB: 868, S36542.

  • #Endococcus propinquus (Körb.) D. Hawksw. — Lichenicolous on saxicolous crustose lichen, alpine zone, 832 m. EX: 216, M2583.

  • #Endococcus rugulosus Nyl. — Lichenicolous on Aspicilia, saxicolous in snowbed, 871 m. EX: 458, S39491.

  • Ephebe lanata (L.) Vain. — Saxicolous on rocks at edge of lake, and on mountain top, 127–618 m. DUN: 419, S38955; 428, S39020.

  • #Epicladonia sandstedei (Zopf) D. Hawksw. — Lichenicolous on Cladonia pyxidata, 2 m. WA: A573, P2156, P2368.

  • *#Epicladonia stenospora (Harm.) D. Hawksw. — Lichenicolous on Cladonia, terricolous, 894 m. EX: 372, S38372.

  • Epigloea medioincrassata (Grummann) Döbbeler — On algal biofilm on dead mosses. EX: 565, P2236.

  • **#Epigloea urosperma Döbbeler — Lichenicolous on Placynthiella uliginosa, muscicolous over log in upper beach meadow, 2 m. GUS: 437, S39166. This species appears to be restricted to Placynthiella species. In addition to being widely reported in Europe, it was also recently reported from Bolivia and the Seychelles (Diederich et al. Reference Diederich, Lücking, Aptroot, Sipman, Braun, Ahti and Ertz2017).

  • #Epilichen scabrosus (Ach.) Clem. — Lichenicolous on Baeomyces rufus, terricolous, 0–115 m. EA: 869, S36561; 870, F9780 (sub Baeomyces rufus).

  • Erinacellus dendroides (Henssen) T. Sprib. et al. — Corticolous on Pinus contorta (most records) and on Picea sitchensis (1×), 18–32 m. GUS: 857, S36105; 862, S36292, S36300, S36301; 316, S37872. GLBA material was the basis of a molecular study establishing this as a new genus; it was previously placed in Spilonema (Spribille et al. Reference Spribille, Tønsberg, Stabentheiner and Muggia2014a, isolates L1728, L1729).

  • Euopsis granatina (Sommerf.) Nyl. — Saxicolous on pebbles and outcrops, 0–871 m. DUN: 428, S39021; EX: 455, S39435 (sub Atrophysma cyanomelanos); 458, S39484 (sub Lecidea phaeops); 218, M2655a; WA: 105, F9991.

  • Euopsis pulvinata (Schaer.) Vain. — Saxicolous, alpine zone, 871–907 m. EX: 373, S38381; 455, S39430; 458, S39494.

  • Farnoldia jurana (Schaer.) Hertel — Saxicolous on pebbles and underhangs, 10–43 m. WA: 319, S37938; 383, S38504 (sub Lecidella aff. carpathica).

  • Felipes leucopellaeus (Ach.) Frisch & G. Thor (Arthonia leucopellaea (Ach.) Almq.) — Corticolous on Tsuga heterophylla bark, 222 m. EX: 313, S37838; 314, S37848.

  • *Fellhanera bouteillei (Desm.) Vězda — Corticolous on Picea sitchensis and Salix on upper beach, 2 m. GUS: 857, S36155; 435, S39120 (sub Polycauliona pollinarioides), S39124 (sub Scoliciosporum chlorococcum).

  • *Fellhaneropsis vezdae (Coppins & P. James) Sérus. & Coppins — Corticolous on Alnus, Picea sitchensis, Ribes lacustre and Tsuga heterophylla twigs, and fungicolous on Fomitopsis cf. pinicola, 1–164 m. GUS: 856, S36073; 878, S36768, S36771; 330, S38063; 341, S38254 (sub Bacidina sulphurella); 229, M2746.

  • Fissurina insidiosa C. Knight & Mitten — Corticolous on Alnus (mainly), also twice on Tsuga heterophylla, 9–86 m. DUN: 333, S38074, S38091 (sub Sclerococcum fissurinae); 431, S39035; 462, S39742; 562, T41743, T41752; EX: [125, F10257, F10258]; [859, F9657, S36228]; [860, F9664, S36239]; [V431, S39035, S39050 (sub Sclerococcum fissurinae)]. Described from New Zealand but apparently frequent in the south-eastern United States and also reported from Haida Gwaii, British Columbia (Brodo Reference Brodo1995, as Graphis). It is not known if the SE Alaskan material corresponds to the type. A set of DNA sequences has been published from GLBA (Resl et al. Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015).

  • Flavocetraria cucullata (Bellardi) Kärnefelt & A. Thell — Terricolous, 922–936 m. EX: 375, S38426; 407, S38849.

  • Flavocetraria nivalis (L.) Kärnefelt & A. Thell — Terricolous in alpine heath, 907–922 m. EX: 373, S38399; 407, S38858.

  • Frutidella caesioatra (Schaer.) Kalb — Muscicolous or loosely saxicolous on tops and sides of boulders, 150–484 m. DUN: 118, F10151; 119, F10157; 423, S38975 (sub Rhizocarpon badioatrum); 425, S38983.

  • Frutidella furfuracea (Anzi) M. Westb. & M. Svenss.(syn. Lecidea pullata (Norman) Th. Fr.) — Corticolous on Picea sitchensis krummholz and Pinus contorta in muskeg, 32–883 m. EX: 405, S38766; GUS: 862, S36294. TLC: sphaerophorin.

  • Fuscidea intercincta (Nyl.) Poelt — Saxicolous on granite and argillite in subalpine and alpine habitats, 460–918 m. DUN: 121, F10176; 428, S39022 (sub Pyrenopsis sp.); EX: 454, F10333, F10346 (sub Pyrenopsis phaeococca), F10344, S39405 (sub Carbonea vorticosa); 218, M2643.

  • Fuscidea muskeg Tønsberg & M. Zahradn. — See ‘Descriptions of New Genera and Species’.

  • Fuscidea thomsonii Brodo & V. Wirth — Saxicolous on gneiss in the supralittoral zone, 0–5 m. DUN: 462, F10369; 463, F10395, F10404.

  • Fuscopannaria ahlneri (P. M. Jørg.) P. M. Jørg. — Corticolous on Alnus and branches of Picea sitchensis, 20 m. GUS: [557, T41700]; 559, T41735 (conf. P. M. Jørgensen 2013).

  • [Fuscopannaria confusa (P. M. Jørg.) P. M. Jørg. — Corticolous on Picea sitchensis branches, 20 m. GUS: 557, T41711b (det. P. M. Jørgensen 2013).]

  • Fuscopannaria convexa P. M. Jørg. — Corticolous on Alnus, Populus balsamifera and Salix, mostly close to seashore, 0–32 m. EA: 440, S39249; 441, F10194, F10196; GB: 867, S36428; GUS: 862, S36309; [V329, S38033 (sub Szczawinskia tsugae)]; no waypoint, M2482; WA: 395, S38682, S38684 (sub Fuscopannaria leucostictoides).

  • Fuscopannaria dillmaniae T. Sprib. — See ‘Descriptions of New Genera and Species’.

  • Fuscopannaria incisa (Müll. Arg.) P. M. Jørg. — Corticolous on Alnus, 30 m. EA: 441, F10207, GUS: [V329, S38028].

  • Fuscopannaria leucostictoides (Ohlsson) P. M. Jørg. — Corticolous on Alnus, Populus balsamifera and Salix, in beach fringe habitats, 0–10 m. EA: 441, S39280; GB: 868, S36470; 874, S36695 (as ‘cf.’); WA: 391, S38589; 395, S38684 (as ‘cf.’).

  • Fuscopannaria pacifica P. M. Jørg. — Corticolous on Alnus, Picea sitchensis, Populus balsamifera and Tsuga heterophylla, 0–162 m. EA: 441, F10218; EX: [V431, S39044 (brown morph)]; GUS: 100, F9900; 138, F10479, F10481; 857, F9633; [V329, S38028 (s. lat.)], S38047, S38054; 855, S36011, S36030; 878, S36769; Tower Rd, S37505, S38277 (brown morph).

  • Fuscopannaria praetermissa (Nyl.) P. M. Jørg. — Terricolous on organic accumulations or muscicolous, also on sandy soil, along beaches and in alpine zone, 0–942 m. EX: 407, F10128 (pruinose morph); 408, S38868; 455, S39434, S39435 (sub Atrophysma cyanomelanos), S39443; GB: 868, S36539; [GUS: State Dock, F9875, S36858].

  • Fuscopannaria ramulina P. M. Jørg. & Tønsberg — Corticolous on Alnus, Populus balsamifera and Salix, 8–60 m. EA: 123, F10243; 872, S36605, S36611; 440, S39191 (sub Hypotrachyna sinuosa), S39246, S39253; 441, F10195, F10196 (sub Fuscopannaria convexa); GB: 868, S36459; GUS: 138, F10482; 857, S36093 (sub Parmeliella triptophylla), S36143; [557, T41701, T41715a]; [574, T41817]; 576, T41843; WA: 391, S38594, S38618; 542, T41589.

  • *Fuscopannaria sorediata P. M. Jørg. — Corticolous on Alnus, once on fine Tsuga twigs, 5–58 m. GB: N Sandy Cove, S36641; GUS: 878, S36760; 879, S36810 (aff.); 881, S36832. GLBA specimens appear to match Fuscopannaria sp. S24650, a species recorded in KLGO (Spribille et al. Reference Spribille, Pérez-Ortega, Tønsberg and Schirokauer2010). P. M. Jørgensen (personal communication to TS, 28 February 2012) concluded that Fuscopannaria sp. S24650 is identical to F. sorediata, a species he originally described from Tennessee (Jørgensen Reference Jørgensen2000). The relationship of these lichens to Fuscopannaria alaskana, from which no DNA sequences have been published, as well as to south-east Alaskan specimens of F. ahlneri, warrants systematic study.

  • #Geltingia associata (Th. Fr.) Alstrup & D. Hawksw. — Lichenicolous on Ochrolechia subplicans, 0–2 m. DUN: 586, P2193.

  • Gowardia nigricans (Ach.) Halonen et al. — Terricolous in alpine heath with rock outcrops, 883 m. EX: 405, F10094.

  • Graphis scripta (L.) Ach. — Corticolous on Alnus, 0–86 m. DUN: 333, S38080, 38084; 462, S39739; 562, T41748; EA: 440, S39221; EX: [860, S36241]; 433, S39075; GB: 868, S36467; N Sandy Cove, S36638; GUS: 857, F9640, S36083, S36145; [V329, S38023, S38035]; 330, S38060; 462, S39739; 531, T41526; 576, T41826; 224, M2832b. One specimen was used for DNA extraction (isolate T1176, Table 1).

  • Gyalecta jenensis (Batsch) Zahlbr. — Saxicolous on limestone and argillite rocks on seashore and creek banks, 0–155 m. EX: 444, S39330; GB: 863, F9698; 864, S36390. This species was found at two localities in GLBA. The material from limestone possesses deeply urceolate apothecia with widely opened discs; that from argillite, which occurred along a stream draining a large peatland, possesses apothecia with a narrow ostiole.

  • Gyalectaria diluta (Björk et al.) I. Schmitt et al. — Corticolous on Alnus, Picea sitchensis, Tsuga heterophylla and Vaccinium ovalifolium, lignicolous, and fungicolous on a polypore, 0–220 m. DUN: 462, S39725; EX: [860, S36255]; [225, M2717]; 236, M2831; GUS: 855, S36026, S36038; 874, F9832; 878, S36775; 882, S36843; 857, S36101, S36121; 341, S38237; no waypoint, M2477. A set of DNA sequences from a GLBA specimen has been published by Resl et al. (Reference Resl, Schneider, Westberg, Printzen, Palice, Thor, Fryday, Mayrhofer and Spribille2015; isolate P145).

  • *Gyalidea fritzei (Stein) Vězda — Saxicolous in sheltered finger-sized depression in argillitic rock in alpine zone, 918 m. EX: 454, S39394.

  • Gyalidea aff. lecideopsis (A. Massal.) Lettau var. eucarpa (Servít) Vězda — Saxicolous on rock in stream, 225 m. EX: 236, S39048; 128, F10303-F10312; [225, M2715]; 236, M2830. Naming this material has been difficult owing to the lack of a global taxonomic study of Gyalidea. Clarifying the status of these collections would require checking about seven type specimens, a task beyond the scope of the present study. Sequences were obtained from S39048 (Table 1). Gyalidea lecideopsis var. lecideopsis has been reported from Haida Gwaii (Brodo Reference Brodo1995) and G. lecideopsis var. convarians (Nyl.) Vězda from the Bering Straits (Vězda Reference Vězda1966).

  • **Gyalidea subscutellaris (Vězda) Vězda — Terricolous on c. 20 yr-old glacial foreland soils, Dryas-dominated habitats, 0–115 m. EA: 869, S36566; 870, F9773. Described from Bartramia moss cushions in the High Tatra (Slovakia; Vězda Reference Vězda1960), and since reported from Poland, the UK and Sweden (summarized by Svensson et al. Reference Svensson, Ekman, Klepsland, Nordin, Thor, von Hirschheydt, Jonsson, Knutsson, Lif and Spribille2017).

  • Gyalideopsis epicorticis (A. Funk) Tønsberg & Vězda — Corticolous on Alnus bark and fine Tsuga heterophylla twigs, also once each on Malus fusca and Salix, mainly at low elevations (3–162 m) but also found once on Picea sitchensis in krummholz (922 m). EX: [125, F10278]; 407, S38817; GB: 874, S36709 (sub Gyalideopsis piceicola); GUS: [V329, S38024]; 855, S36004; 857, S36118 (sub Gyalideopsis piceicola), S36155 (sub Fellhanera bouteillei); [858, S36201]; 878, S36764, S36782; Tower Rd, S38275, S38282; [557, T41693]; 576, T41836; 230, M2749; 237, M2833.

  • Gyalideopsis helvetica van den Boom & Vězda — Corticolous on Alnus, 0–2 m. GB: 864, S36323. The collection is sterile but supports goniocystangia typical of G. helvetica.

  • *Gyalideopsis muscicola P. James & Vězda — Muscicolous on Rhytidiadelphus triquetrus and on mosses over bark on tree trunks, on high beaches and over logs, 0–9 m. DUN: 462, F10383, S39504 (fertile); GB: 874, S36717 (fertile); 556, T41647; GUS: 437, S39165; [State Dock, S36859].

  • Gyalideopsis piceicola (Nyl.) Vězda & Poelt — Corticolous on smooth Alnus bark, Picea twigs, fine Tsuga twigs and once fungicolous on polypore, 0–162 m. EX: [858, S36170 (fertile)]; [859, S36232]; GB: 857, S36155 (sub Fellhanera bouteillei); 874, S36709; GUS: 138, F10475; 855, S36054; 857, S36118, F9644; 878, S36770 (sub Parmeliella parvula); 531, T41524; 532, T41550; [557, T41692]; 224, M2704a.

  • Halecania athallina Fryday — See ‘Descriptions of New Genera and Species’.

  • *Halecania viridescens Coppins & P. James — Corticolous on Alnus twig below eagle perch, on Shepherdia canadensis stalk and on Sambucus racemosa, 0–2 m. DUN: 339, S38154, S38159; GB: 864, S36356; 867, S36434; GUS: 231, M2766. TLC: argopsin, unknowns. First reported from North America by Tønsberg (Reference Tønsberg1994), from Washington.

  • Helocarpon crassipes Th. Fr. — Saxicolous in tundra with bryophytes and Dryas, 115 m. EA: 870, F9782.

  • Herteliana alaskensis (Nyl.) S. Ekman — Saxicolous in supralittoral splash zone, on gneiss, 0–5 m. DUN: 463, F10392, F10410 (sub Adelolecia kolaënsis).

  • #Heterocephalacria bachmannii (Diederich & M. S. Christ.) Millanes & Wedin (syn. Syzygospora bachmannii Diederich & M. S. Christ) — Lichenicolous on Cladonia sp., terricolous, 895 m. EX: 370, S38354; 371, S38367.

  • #Heterocephalacria physciacearum (Diederich) Millanes & Wedin (syn. Syzygospora physciacearum Diederich) — Lichenicolous on Physcia alnophila, corticolous on Populus balsamifera, upper beach, 7 m. WA: 395, S38671 (sub Phoma physciicola).

  • Heterodermia galactophylla (Tuck.) W. L. Culb. — Corticolous on Alnus and Populus balsamifera, 0–33 m. GB: N Sandy Cove, S36642; 867, S36431; GUS: 316, S37882; 330, S38062; Tower Rd, S40728; [557, T41708].

  • Hydropunctaria alaskana Thüs & Pérez-Ort. — See ‘Descriptions of New Genera and Species’.

  • Hydropunctaria maura (Wahlenb.) Keller et al. — Saxicolous in the supralittoral splash zone on gneiss, sea level. DUN: 134, F10464; 463, F10410 (sub Adelolecia kolaënsis), F10411; GUS: 873, F9818; 875, F9836 (sub Verrucaria epimaura); shore E of Park HQ, F9647. This ubiquitous species is certainly found on seashores in all sectors.

  • Hypogymnia apinnata Goward & McCune — Corticolous on Picea sitchensis branches (9×) and Alnus (2×), 0–162 m. DUN: 339, S38160; 463, S39549; EA: nr 438, S39294; 872, S36612; GB: 868, S36483, S36496; Beardsley Island, Stephens 240 (UC, det. B. McCune 1992); GUS: 397, S38695; 435, S39128; 855, F9604, S36007; 857, S36100, S36126; [861, F9673]; WA: Blue Mouse Cove Plot BM1a, BM2a (GLBA herbarium). TLC: atr, apinnatic acid.

  • Hypogymnia duplicata (Ach.) Rass. — Corticolous on Pinus contorta (4×) and Tsuga heterophylla (2×) but common and thus often disregarded, 0–569 m. DUN: 337, S38119; 464, S39612; EX: [859, F9660]; 358, S38313; GUS: 107, F10019; 855, S36006; 878, S36786; 210, M2544.

  • Hypogymnia enteromorpha (Ach.) Nyl. — Corticolous on Pinus contorta (4×), Picea sitchensis (1×) and Tsuga heterophylla (1×), but common and thus often disregarded, 0–222 m. DUN: nr 334, S38110; 338, S38130; 464, S39610; EX: [859, F9659]; [V431, S39056]; GB: N Sandy Cove, S36643; GUS: 862, S36280; 210, M2551, M2557.

  • Hypogymnia hultenii (Degel.) Krog — Corticolous on Picea sitchensis, Pinus contorta, Tsuga heterophylla and less commonly on Alnus, from beach fringe to upper montane area, 0–687 m. DUN: 339, S38174; 463, S39547; 573, T41806; EA: 872, S36613 (sub Pertusaria glaucomela); EX: 433, S39087; 448, F10315; GB: 864, S36327; S Sandy Cove, S40742; GUS: 100, F9894; 107, F10023; 434, S39110; 855, S36018; 857, S36137; 576, T41829; WA: 391, S38602; Blue Mouse Cove plot BM1A, BM2A (GLBA herbarium). A typical rainforest epiphyte that has advanced with glacial retreat as far north as Wolf Point in the East Arm.

  • Hypogymnia inactiva (Krog) Ohlsson — Corticolous on Pinus contorta in muskeg and low elevation sand flats, 32–240 m. EX: Yellowlegs Muskeg, S37853, S37855; GUS: 862, S36303.

  • Hypogymnia lophyrea (Ach.) Krog — Corticolous on Picea sitchensis and Pinus contorta from beach fringe to krummholz, 0–922 m. DUN: 129, F10365; 338, S38136; 463, S39530; GB: 868, S36526; GUS: 857, S36129; 230, M2748.

  • Hypogymnia occidentalis L. Pike — Corticolous on Picea sitchensis, 21 m. EX: 433, S39086. TLC: atr, physodic acid, unidentified substances.

  • Hypogymnia oceanica Goward — Corticolous on Picea sitchensis and Pinus contorta twigs, 0–33 m. GUS: 316, S37880; [V329, S38049]; 857, S36112.

  • Hypogymnia physodes (L.) Nyl. — Corticolous on Alnus (2×), Picea sitchensis (2×) and Pinus contorta (2×) but often not collected, 0–32 m. EA: 440, S39211, S39235; GB: N Sandy Cove, S36644; GUS: Mans 204, S38432; 397, S38704; 862, S36286; WA: Blue Mouse Cove plot BM1a (GLBA herbarium).

  • Hypogymnia tubulosa (Schaer.) Hav. — Corticolous on Picea sitchensis, 0–922 m. EX: 407, S38806; GB: 868, S36514; GUS: 436, S39159; WA: Blue Mouse Cove plot BM2a (GLBA herbarium). Two forms occur in GLBA. One has long, narrow lobes and pointed lobe tips, and accounts for most specimens; the other (represented only by S38806) has shorter lobes that end in blunt, rounded tips, similar to H. tubulosa in Europe.

  • Hypogymnia vittata (Ach.) Parrique — Corticolous on Alnus (3×), Malus fusca (1×), Picea sitchensis (2×) and Pinus contorta (2×), 8–250 m; also terricolous in alpine heath, 872–937 m. DUN: 464, S39608; EA: 370, S38358; 405, S38765; 407, S38804; 409, S38897; 440, S39210; 441, F10208; 456, S39472; 459, F10359 (sub Parmelia omphalodes); EX: 109, F10051; [125, F10279]; 407, F