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The Pacific bryozoan, Smittoidea prolifica Osburn, 1952, is reported for the first time from the Northwest Atlantic coast. Colonies were discovered during routine benthic sampling of Casco Bay, Maine, encrusting mussel shells and barnacles. Aiming to compare specimens from native and introduced locations, uncertainties about the Pacific range of S. prolifica were resolved by re-examining specimens from Japan, southern Korea, the United States west coast, and Mexico. The occurrence of this species in Japan was confirmed but southern Korea specimens were found to be Smittoidea spinigera (Liu, 1990). Comparisons of biometrics among specimens from widely dispersed locations where S. prolifica is native and introduced showed significant trends in variation with most characters largest for California and smallest for Germany. Zooid width was largest for Maine specimens. Comparisons between oceans showed that Pacific and Atlantic specimens differed significantly in all measures except zooid length and orifice width. Low substrate specificity and broad range of temperatures and salinities in occupied habitats suggests the potential for successful introduction is high. Smittoidea prolifica was most likely introduced through commercial shipping from the North Sea where it is an established non-native species. This was the third non-indigenous species found in Casco Bay discovered within the same timeframe and which shared the same likely region of origin. This spike matched a rise in commercial shipping from the Northeast Atlantic to Portland, Maine, suggesting this seaport is shifting towards becoming a bioinvasion hotspot.
Umbilicaria ahtii sp. nov. is described based on morphological and molecular characters. The new species resembles Umbilicaria vellea but the former has larger and submuriform ascospores, a darker lower surface, longer dark brown to black rhizinomorphs, and lacks thalloconidia directly on the lower surface and basal part of the rhizinomorphs. Phylogenetic analyses (ITS, mtLSU and RPB2) confirmed the distinctness of U. ahtii and indicated its sister relationship to U. meizospora. Umbilicaria ahtii is described from Finland and is currently known from several localities in Northern Europe (Svalbard, Norway, Finland, Kola Peninsula in Russia), Asia (Kodar Range, Siberia) and North America (Alaska). Within the U. vellea group, new molecular data confirmed U. koidzumii as a widespread, separate species sister to U. cinereorufescens. Diagnostic traits and variability of species, as well as their distribution patterns and nomenclature, are discussed.
The Cuvier's beaked whale, Ziphius cavirostris, is a cosmopolitan species and the only beaked whale species commonly found in the Mediterranean Sea. Five strandings of Cuvier's beaked whale were reported along the Aegean/Mediterranean Seas coasts of Türkiye and northern coast of Cyprus in 2016–2017. Mitochondrial DNA (mtDNA) control region (430–444 bp) and cytochrome b (cytb) (382–424 bp) sequences each revealed two different haplotypes (four out of five individuals had the same haplotype for each locus) on these stranded animals. The control region haplotypes were identical to two previously identified haplotypes from the Ionian (Greece) and Adriatic (Croatia) Seas. Only one of the cytb haplotypes had previously been described from the Adriatic Sea (Italy) and the other one was detected for the first time. In a comparison of these haplotypes with Cuvier's beaked whale haplotypes previously reported from outside the Mediterranean Sea, the Mediterranean subpopulation shows genetic differentiation based upon the presence of two unique haplotypes. Additional mtDNA sequences from the Mediterranean Sea are needed for a better understanding of the genetic population structure of this species and to elaborate more concrete conservation measures.
Polychaetes from tropical ecosystems of the eastern Pacific have been poorly studied; thus, the aim of this study was to analyse their taxonomic composition in the southern Mexican Pacific shelf and to examine their biogeographic affinities. A total of 3741 specimens from 82 species, 52 genera, and 27 families were identified from 38 stations at 42–109 m depth. The Sedentaria group was more diverse (40 species, 48.8%) and abundant (1753 ind., 46.9%) compared to the Errantia (36 species, 43.9%; 346 ind., 9.2%) and the Basal Annelida groups (6 species, 7.3%; 1642 ind., 43.9%). The families Onuphidae (14 spp.), Spionidae (8 spp.), and Paraonidae (8 spp.) were the most diverse. The Amphinomidae and Spionidae accounted for 72.6% of the fauna; the remarkably high abundance of both families together is unusual in the tropical eastern Pacific. The polychaete species had high biogeographic affinities with the Mexican tropical Pacific ecoregion (45.1%), which has tropical conditions, and the Cortezian (29.3%), which has warm-temperate characteristics. Twelve amphiamerican species and ten with worldwide distribution were found. The tropical eastern Pacific is one of the world regions with the lowest number of polychaete records, thus underlining the importance of the taxonomic and biogeographic information provided here. The sampling effort should increase, since the non-parametric estimators indicated that 116–138 species were expected, instead of the 82 species actually found.
Three twig-growing lichen species belonging to the family Teloschistaceae from southern Patagonia are described as new to science: Marchantiana pyramus sp. nov., with minute apothecia, orange due to dominant content of emodin, M. ramulicola sp. nov., with minute olive apothecia with dominant parietin and Austroplaca thisbe sp. nov., with clear yellow apothecia also with dominant parietin. Marchantiana subpyracea, M. epibrya and M. queenslandica are new combinations for species which, so far, are known only from New Zealand and Australia. Blastenia circumpolaris is shown to be very common in Patagonia and Marchantiana asserigena is documented for the first time from the Southern Hemisphere, viz. the Falkland Islands. The genus Marchantiana is analyzed here using three genes and is shown to be closely related to Yoshimuria; although appearing as paraphyletic, a monophyletic origin cannot be ruled out. Morphology, ecology and distribution support a monophyletic treatment and Marchantiana is therefore treated as such.
Fungi are probably the most diverse group of eukaryotic organisms in the Antarctic continent and nearby archipelagos, and they dominate communities in either mild or harsh habitats. However, our knowledge of their global distribution ranges and the temporal origins of their Antarctic populations is rather limited or almost absent, especially for species that do not lichenize. We focused for the first time on elucidating the taxonomic identity and phylogenetic relationships of several Antarctic collections of the deadly fungal Basidiomycota genus Galerina. By using molecular sequence data from the universal fungal barcode and a dataset encompassing 178 specimens, the inferred phylogeny showed that the Antarctic specimens corresponded with the sub-cosmopolitan species Galerina marginata, Galerina badipes and Galerina fallax, and their most closely related intraspecific genetic lineages were from northern Europe and North America. We found that these species probably host Antarctic-endemic intraspecific lineages. Furthermore, our dating analyses indicated that their Antarctic populations originated in the Pleistocene, a temporal frame that agrees with that proposed for the Antarctic colonization of plants such as the grass Deschampsia antarctica, mosses and some amphitropical lichens. Altogether, these findings converge on the same temporal scenario for the assembly of the most conspicuous terrestrial Antarctic plant and fungal communities.
In the present contribution we report, for the first time, records of the nudibranch Zelentia ninel from Norway. The species is previously known only from the Barents Sea coast in northern Russia where it was described for the first time in 2017. Records of Z. ninel from six different localities in northern Norway from 2019–2023 are presented and discussed. The identity of the specimens was determined by investigation of external and internal morphology as well as molecular analysis of preserved specimens. Photographs of live specimens and radulae of preserved specimens are presented, and species delimitation is confirmed by molecular phylogenetic analysis. In order to assess the biogeographic distribution of Z. ninel based on all available information, recent unanticipated genetic data supporting a putative occurrence of Z. ninel at the Aleutian Islands, Alaska is also discussed where we provide arguments in support of occasional anthropogenic transportation outside its natural range. The present records significantly expand the known natural range of distribution for Z. ninel and demonstrate that the species is not restricted to the Russian Barents Sea coast but that the range encompasses also at least northern Norway. These data can provide important insights to the understanding of natural ranges of marine invertebrates across biogeographical regions affected by rapid ongoing climatic change.
This study provides new species records (NRs) of macroalgal assemblages present in rocky habitats from the South Shetland Islands (SSI) and north-eastern Antarctic Peninsula (EAP), Weddell Sea. Surveys were conducted during the summers of 2013/2014 to 2017/2018 at Elephant, Deception, Half Moon and Vega islands. Data from the present study and those available in the literature from the western Antarctic Peninsula (WAP) were combined to provide an updated checklist, giving insights into macroecology and potential changes in thermohaline circulation patterns. A total of 48 macroalgal taxa were identified from our sampling, with eight representing NRs to the EAP sector of the Weddell Sea and five representing NRs to the SSI. Statistical differences among the assemblages from the SSI, WAP and EAP were identified. NRs, including opportunistic species and new information about the biogeographical distributions of species reported here, give insights into ecoregional connectivity and environmental changes. This study updates macroalgal diversity records in regions that are currently experiencing the impacts of climate change. Future and ongoing monitoring for conservation purposes is required to detect non-native species, new dispersal pathways and patterns related to thermohaline anomalies in Antarctic waters.
To provide context for the later chapters and analysis, the chapter outlines the key characteristics of Europe’s environment and nature, and the effects of human actions on it. It firstly describes the biophysical geography and natural history of Europe, including the legacy of the last Ice Age, and the current characteristics of the biogeographical regions and marine regions. It then summarises the main impacts of human activities on biodiversity in Europe, starting with early agriculture and forest clearances that created seminatural ecosystems and cultural landscapes, followed by the profound impacts of the industrial and agricultural revolutions, and more recent changes in land- and sea-use and resulting pressures over the last forty years. Other key pressures are also identified, including in relation to forestry, water and air pollution, fisheries, invasive alien species and climate change. The chapter concludes with an outline of Europe’s remaining biodiversity, identifying hotspots, and the implications for nature conservation approaches and priorities.
Environmental DNA is a powerful tool for monitoring biodiversity. Although environmental DNA surveys have successfully been implemented in various environments, protocol choice has been shown to affect results and inferences. Thus far, few method comparison studies for soil have been undertaken. Here, we optimized the workflow for soil metabarcoding through a comparative study encompassing variation in sampling strategy (individual and combined samples), DNA extraction (PowerSoil®, NucleoSpin® Soil, PowerSoil® + phosphate buffer and NucleoSpin® Soil + phosphate buffer) and library preparation (one-step and two-step quantitative polymerase chain reaction methods). Using a partial 18S rRNA marker, a total of 309 eukaryotic taxa across 21 phyla were identified from Antarctic soil from one site in the Larsemann Hills. Our optimized workflow was effective with no notable reduction in data quality for a considerable increase in time and cost efficiency. The NucleoSpin® Soil + phosphate buffer was the best-performing extraction method. Compared to similar studies in other regions, we obtained low taxonomic coverage, perhaps because of the paucity of Antarctic terrestrial organisms in genetic reference databases. Our findings provide useful methodological insights for maximizing efficiency in soil metabarcoding studies in Antarctica and other low-biomass environments.
Protection of Antarctica's biodiversity and ecosystem values is enshrined in the Protocol on Environmental Protection to the Antarctic Treaty, which provides for the designation of Antarctic Specially Protected Areas (ASPAs) to areas with outstanding values. Concern has been raised that existing ASPAs fail to prioritize areas to maximize the likelihood of ensuring the long-term conservation of Antarctic ecosystems and biodiversity. The absence of systematic and representative protection is particularly acute for inland aquatic ecosystems, which support a disproportionate amount of inland biodiversity. This paper promotes the case for overt inclusion of inland waters as a critical component of a representative protected area framework for Antarctica, thereby addressing their current underrepresentation. We set out a structured approach to enable the selection of representative freshwater systems for inclusion in the ASPA framework that, with modification, could also be applied across other Antarctic habitats. We acknowledge an overall lack of information on the biogeography of inland aquatic diversity and recommend increased use of remote data collection along with classification tools to mitigate this, as well as the need for the consideration of catchment-scale processes. Changes that accompany contemporary and anticipated climate change make the need for the conservation of representative biodiversity increasingly urgent.
Planting trees for climate services – storing carbon, cooling surface climate, enhancing rainfall, providing aerosols that reflect solar radiation, creating favorable microclimate refuges, or other benefits – is not small-scale or immediate. It requires vast tracts of healthy and thriving forests and setting aside the land to grow forests for 50 to 100 years or longer. Achieving the climate benefits of forests requires a permanent forest presence over many decades. Climate will change during that time, and a forest planted today may not thrive in the climate of tomorrow. The forests of the future will grow in a climate different from today's and likely in regions of the world that differ from today's. They will be stressed by climate change, increased wildfires, disease, and insects. Asking forests to solve the climate problem requires a long-term commitment to and investment in forests and their health. Forest growth, too, is not one-directional. Wildfires, droughts, insects, and wind storms continually reset forests back to young stages of development. An old-growth forest that has accumulated enormous stores of carbon in its trees and soil becomes a young, regenerating forest.
A new isolate of Mesorhabditis monhystera (Bütschli, 1873) Dougherty, 1955 is described and illustrated with morphological and molecular data. The phylogenetic analysis based on the D2/D3 segment of 28S rDNA using the Bayesian inference method, revealed monophyly of the genus Mesorhabditis as the subordinate taxa clustered in one clade. The clade further divided into two subclades representing the Monhystera-group and Spiculigera-group with 100% posterior probability values. However, GenBank sequences of several species constituting the Monhystera-group, showed high similarity and very little genetic divergence (98–99%) of up to 4–5 bases. In order to ascertain the status of those isolates, detailed morphological comparison is provided along with a pictorial key. A sequence-based phylogeography of haplogroups of Mesorhabditis using the median-joining network method, was also inferred. The results suggested the need for morphological validation of a species before its sequences are deposited in GenBank.
Cyclopes didactylus, the smallest of all anteaters, inhabits Amazonian and Atlantic forests with an apparently disjunct distribution. Yet, phylogeography reveals historical connections through the forests of the Northeast Region of Brazil. Its populations in this region are classified by the Red List of Threatened Species as Data Deficient and with a trend towards decline. However, Northeast Brazil has a large sampling gap, and the potential distribution of this species has yet to be evaluated. We investigated the potential distribution of C. didactylus to evaluate the hypothesis of a disjunct distribution between Amazonian and Atlantic forests and estimate the amount of protected area in its predicted distribution. We generated a Maxent distribution model using occurrence records, according to the new taxonomic revision of Cyclopes, and selected current bioclimatic variables to evaluate the continuity of the predicted distribution of the species in Northeast Brazil. We also performed past projections to assess historical connections and overlapped maps of protected areas onto their current distribution. Although its distribution is probably disjunct, at least one as-yet-unknown population may be present in the forests of Northeast Brazil, an area poorly protected. The results are useful for targeting field efforts in this under-sampled region.
We give a review of all published Palaeogene snake taxa from all localities worldwide. Several conceptual and material advances in the past two decades—a focus on apomo+P31rphies, greater attention to variation, quantification of morphology, and new fossil discoveries—have vivified the fossil record. Particularly noteworthy have been new fossils from Gondwanan continents and complete, articulated skeletons. Species known only from vertebrae are unlikely to be placed precisely phylogenetically, but a high number of vertebrae is a strong indication that cranial remains are present, which in turn allow more precise phylogenetic placement. Extrapolations of snake palaeodiversity are of the same order of magnitude as rough calculations of cumulative lineage diversity in the Palaeogene, raising the prospect that palaeontological morphospecies may more closely approximate biological species than is commonly conceived. As their interrelationships become better known, Palaeogene fossils will increasingly help elucidate the early evolution of snakes.
Long-haul tourists visiting South Africa are always fascinated by the clicks of isiXhosa. Foreign to their ears, the eighteen click consonants can be grouped into three types: the ‘c’ is a dental click made by the tongue at the back of the mouth, the lateral ‘x’ is made by the tongue at the sides of the mouth, and the alveolar ‘q’ is made by the tip of the tongue on the roof of the mouth.
IsiXhosa is part of the Nguni language group, which also includes Zulu and southern and northern Ndebele. Yet few of these or the other South African vernacular languages have clicks, and those that do have them use them far less. How is it that isiXhosa came to use clicks so commonly?
One clue comes from the other languages of southern Africa that also make use of clicks – and there are lots of them.
The authors provide an initial report on possibly the southernmost expansion of humans in pre-industrial times. The archaeological site, in the Cape Horn archipelago, consists of a campfire site, fragments of a weapon, and butchered bones. Radiocarbon dating places the site c. 260–460 years BP.
The western Antarctic Peninsula is facing rapid environmental changes and many recent publications stress the need to gain new knowledge regarding ecosystems responses to these changes. In the framework of the Belgica 121 expedition, we tested the use of a nimble vessel with a moderate environmental footprint as an approach to tackle the urgent needs of the Southern Ocean research community in terms of knowledge regarding the levels of marine biodiversity in shallow areas and the potential impacts of retreating glaciers on this biodiversity in combination with increasing tourism pressure. We discuss the strengths and drawbacks of using a 75’ (23 m) sailboat in this research framework, as well as its sampling and environmental efficiency. We propose that the scientific community considers this approach to 1) fill specific knowledge gaps and 2) improve the general coherence of the research objectives of the Antarctic scientific community in terms of biodiversity conservation and the image that such conservation conveys to the general public.
This chapter considers the observation, comparison and visual representation of a range of altitudinal limits in the Himalaya: plants, animals, crops and human habitation. These limits were addressed especially through the lens plant geography. The chapter begins by examining the absolute limits of vegetation and attempts to divide up the Himalaya using a vocabulary of verticality borrowed from the horizontal (tropical, temperate and arctic). The second section extends these debates to animals. The third section examines debates over the ‘tropicality’ of the Himalaya, and inconsistences in the line of perpetual snow. The fourth section considers the altitude limits of cultivation, firewood and human habitation. The final section considers attempts to represent and understand these altitude limits visually by considering charts made by William Griffith and Richard Strachey. The chapter argues that as much as from abstract scientific interests, observations of altitude thresholds were wrapped up with the concerns of empire. Ultimately, applying existing horizontal divisions meant simultaneously overwriting pre-existing local cosmologies, and broader South Asian imaginings.
Of the monkeys in Africa, the colobines comprise 19% of the 16 genera and 30% of the 79 species. They occur all across tropical African from sea level to 3,400 m above sea level, and where temperatures range from -7°C to 41°C and mean annual rainfall ranges from 50 cm to 1,100 cm. Ninety-six percent of the 24 species of Africa’s colobines are threatened with extinction, whereas 68% of the subspecies are threatened with extinction. Six of the species are ‘Critically Endangered’, including one that is probably already extinct. The two primary proximate threats to colobines in Africa are forest loss and hunting by humans, while the ultimate threat is humans and their widespread over-exploitation of natural resources. This chapter reviews the biological traits that make Africa’s colobines especially susceptible to extinction through forest loss and hunting, the threats they face, and the impacts of those threats. Predictions are presented concerning which species of African colobine will be among the first extinctions and where Africa’s colobines are expected to persist for at least the coming 30 years. Finally, this chapter presents an overview of the main conservation actions that Africa’s colobines require and gives priorities for research that will support their conservation.