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Endosymbiosis in Ordovician-Silurian corals and Stromatoporoids: A new lingulid and its trace from eastern Canada

Published online by Cambridge University Press:  11 August 2017

Leif Tapanila  and
Lars E. Holmer
Leif Tapanila
Affiliation:
Department of Geosciences, Idaho State University, Pocatello 83209-8072,
Lars E. Holmer
Affiliation:
Department of Earth Sciences, Norbyv. 22, S-75236 Uppsala, Sweden,
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Abstract

The earliest known record of lingulid-coral associations is described from Ashgill tabulate corals preserved on Manitoulin Island, Ontario. Lingulid infestation of tabulate corals and stromatoporoids also is locally abundant in Ashgill and Llandovery limestones on Anticosti Island, Québec, and these preserve the new lingulid species Rowellella? anticostiensis inside the cavities of Trypanites borings. In all examples, lingulids appear to nestle in previously formed Trypanites, likely in a dead host coral or stromatoporoid. In some instances in the Silurian of Anticosti, regeneration of host growth while infested by lingulids is evidenced by a new type of compound trace fossil, Klemmatoica linguliforma new ichnogenus and ichnospecies. Similar endosymbiotic relationships previously observed in Silurian corals from Wales and Sweden suggest that the lingulid association with tabulate corals and stromatoporoids was widespread in early Paleozoic shallow marine settings.

Type
Research Article
Information
Journal of Paleontology , Volume 80 , Issue 4 , July 2006 , pp. 750 - 759
Copyright
Copyright © The Paleontological Society 

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References

Balinski, A. 1997. Evolution of the embryonic development in lingulid brachiopods. Acta Palaeontologica Polonica, 24:45–56.Google Scholar
Balinski, A. 2001. Embryonic shells of Devonian linguloid brachiopods. The Systematics Association Special Volume 63 (Brachiopods past and present):91–101.Google Scholar
Billings, E. 1865. Notice of some new genera and species of Palaeozoic fossils. Canadian Naturalist and Geologist, new series 2:432–452.Google Scholar
Bromley, R. G. 1970. Borings as trace fossils and Entobia cretacea Portlock, as an example, p. 49–90. In Crimes, T. P. and Harper, J. G. (eds.), Trace Fossils. The Seel House Press, Liverpool.Google Scholar
Bromley, R. G. 1972. On some ichnotaxa in hard substrates, with a redefinition of Trypanites Mägdefrau. Paläeontologische Zeitschrift, 46: 93–98.Google Scholar
Bromley, R. G. 1994. The palaeoecology of bioerosion, p. 134–154. In Donovan, S. K. (ed.), The Palaeobiology of Trace Fossils. John Wiley, New York.Google Scholar
Bromley, R. G., and Surlyk, F. 1973. Borings produced by brachiopod pedicles, fossil and recent. Lethaia, 6:349–365.CrossRefGoogle Scholar
Bruguière, J. G. 1797. Tableau Encyclopédique et Méthodique des Trois Règnes de la Nature, 2, Vers, Coquilles, Mollusques et Polypiers. Paris, p. 190–286.Google Scholar
Copper, P. 1978. Paleoenvironments and paleocommunities in the Ordovician-Silurian sequence of Manitoulin Island. Michigan Basin Geological Society Special Paper, 3:47–61.Google Scholar
Copper, P. 1995. Five new genera of Late Ordovician-Early Silurian brachiopods from Anticosti Island, eastern Canada. Journal of Paleontology, 69:846–862.CrossRefGoogle Scholar
Copper, P. 1999. Brachiopods during and after the Late Ordovician mass extinctions, on Anticosti Island, E Canada. Acta Universitatis Carolinae-Geologica, 43:207–209.Google Scholar
Copper, P. 2001. Reefs during the multiple crises towards the Ordovician-Silurian boundary: Anticosti Island, eastern Canada, and worldwide. Canadian Journal of Earth Sciences, 38:153–171.Google Scholar
Copper, P., and Grawbarger, D. J. 1978. Paleoecological succession leading to a Late Ordovician biostrome on Manitoulin Island, Ontario. Canadian Journal of Earth Sciences, 15:1987–2005.Google Scholar
Copper, P., and Long, D. G. F. 1990. Stratigraphic revision of the Jupiter Formation, Anticosti Island, Canada: A major reference section above the Ordovician-Silurian boundary. Newsletters on Stratigraphy, 23:11–36.CrossRefGoogle Scholar
Copper, P., and Long, D. G. F. 1993. Upper Ordovician-Early Silurian geology of the Manitoulin Island area, Ontario (Caradoc-Llandovery). Canadian Paleontology Conference Field Trip Guidebook, Third Canadian Paleontology Conference, 1–2 October 1993. Sudbury, 36 p.Google Scholar
Desrochers, A., Copper, P., and Long, D. G. F. 1998. Sedimentology and paleontology of the Early Ordovician through Early Silurian shallow water carbonates of the Mingan Islands National Park and Anticosti Island; Québec. Field Trip B8 Guidebook, Geological Association of Canada-Mineralogical Association of Canada Joint Annual Meeting, 20–26 May 1998. Québec, 97 p.Google Scholar
Dixon, O. A., Bolton, T. E., and Copper, P. 1986. Ellisites, an Upper Ordovician heliolitid coral intermediate between coccoserids and proporids. Palaeontology, 29:391–413.Google Scholar
Ekdale, A. A., and Bromley, R. G. 2001. A day and a night in the life of a cleft-foot clam: Protovirgularia-Lockeia-Lophoctenium . Lethaia, 34:119–124.Google Scholar
Ekdale, A. A., Bromley, R. G., and Pemberton, S. G. 1984. Ichnology: the use of trace fossils in sedimentology and stratigraphy. Society of Economic Paleontologists and Mineralogists (short course), 15:1–317.Google Scholar
Flower, R. H. 1961. Montoya and related colonial corals. Memoir of the New Mexico State Bureau of Mines and Mineral Resources, 7:1–97.Google Scholar
Girty, G. H. 1898. Description of a fauna found in the Devonian black shale of eastern Kentucky. American Journal of Science, 6:384–395.Google Scholar
Gorjansky, V. Yu., and Popov, L. E. 1985. Morfologiya, systematicheskoye polozheniye i proiskhozhdeniye bezzamkovykh breakhiopod s karbonatnoy rakovinoy. Paleontologicheskiy Zhurnal, 3:3–14.Google Scholar
Hall, J. 1859. Observations on genera of Brachiopoda. Twelfth Annual Report to the New York State Cabinet, p. 8–110.Google Scholar
Holmer, L. E. 1989. Middle Ordovician phosphatic inarticulate brachiopods from Västergötland and Dalarna, Sweden. Fossils and Strata, 26: 1–172.Google Scholar
Holmer, L. E., and Popov, L. E. 2000. Class Lingulata, p. 30–146. In Williams, A. et al. (eds.), Treatise on Invertebrate Paleontology. Pt. H. Brachiopoda. University of Kansas Press, Lawrence.Google Scholar
Jin, J., and Chatterton, B. D. 1997. Latest Ordovician-Silurian articulate brachiopods and biostratigraphy of the Avalanche Lake area, southwestern District of Mackenzie, Canada. Palaeontographica Canadiana, 13:1–167.Google Scholar
Johns, R. A. 1990. A new parasitic, inarticulate brachipod infesting lithistid sponges from the Middle Ordovician Antelope Valley Limestone in central Nevada. Abstracts with Programs (Geological Society of America), 22:219.Google Scholar
Kobluk, D. R., and Nemcsok, S. 1982. The macroboring ichnofossil Trypanites in colonies of the Middle Ordovician bryozoan Prasopora: Population behaviour and reaction to environmental influences. Canadian Journal of Earth Sciences, 19:679–688.Google Scholar
Kobluk, D. R., James, N. P., and Pemberton, S. G. 1978. Initial diversification of macroboring ichnofossils and exploitation of the macroboring niche in the Lower Paleozoic. Paleobiology, 4:163–170.CrossRefGoogle Scholar
Koneva, S. P. 1986. Novoje semeistvo kembriiskikh bezzamkovykh brakhiopod. Paleontologicheskii Zhurnal, 1:49–55.Google Scholar
Lamarck, J. B. 1816. Histoire naturelle des animaux sans vertèbres, 2, Paris, 568 p.Google Scholar
Lang, W. D., Smith, S., and Thomas, H. D. 1940. Index of Palaeozoic Coral Genera. British Museum of Natural History, London, 231 p.Google Scholar
Lindström, G. 1899. Remarks on the Heliolitidae. Kungliga Svenska Vetenskapsakademiens Handlingar, 32:1–140.Google Scholar
Long, D. G. F. 1993. Limits on Late Ordovician eustatic sea-level change from carbonate shelf sequences: An example from Anticosti Island, Québec. Special Publications of the International Association of Sedimentologists, 18:487–499.Google Scholar
Long, D. G. F. 1997. Seven million years of storm redistribution along the east coast of Laurentia: Transport mechanisms, current systems and influence of siliciclastics on reef development in the Late Ordovician and Early Silurian carbonate ramp of Anticosti Island, Québec, Canada. Proceedings of the Eighth International Coral Reef Symposium, 2: 1743–1748.Google Scholar
Long, D. G. F., and Copper, P. 1987. Stratigraphy of the Upper Ordovician upper Vaureal and Ellis Bay formations, eastern Anticosti Island, Québec. Canadian Journal of Earth Sciences, 24:1807–1820.Google Scholar
Long, D. G. F., and Copper, P. 1994. The Late Ordovician–Early Silurian carbonate tract of Anticosti Island, Gulf of St. Lawrence, eastern Canada. Field Trip Guidebook B4, Geological Association of Canada–Mineralogical Association of Canada, Joint Annual Meeting, 20–25 May 1994. Waterloo, 70 p.Google Scholar
Mägdefrau, K. 1932. Über einige Bohrgänge aus dem Unteren Muschelkalk von Jena. Paläontologische Zeitschrift, 14:150–160.Google Scholar
Marsden, J. R., and Meeuwig, J. 1990. Preferences of planktotrophic larvae of the tropical serpulid Spirobranchus giganteus (Pallas) for exudates of corals from a Barbados reef. Journal of Experimental Biology and Ecology, 137:95–104.Google Scholar
Menke, C. T. 1828. Synopsis Methodica Molluscorum Generum Omnium et Specierum Earum, Quae in Museo Menkeano Adservantur. G. Uslar, Pyrmonti, 91 p.Google Scholar
Milne-Edwards, J., and Haime, J. 1849. Mémoire sur les polypiers appartenant aux groupes naturels des Zoanthaires perforés et des Zoanthaires tabulés. Comptes Rendus de l'Académie des Sciences, Paris, 29:257–263.Google Scholar
Milne-Edwards, J., and Haime, J. 1851. Monographie des polypiers fossiles des terrains paléozoïques. Archives du Muséum national d'histoire naturelle, Paris, 5:1–502.Google Scholar
Nestor, H. 1964. Stromatoporoidei ordovika I llandoveri estonii. Akademie Nauk Estonskoi SSR, Institut Geologii, 1–111.Google Scholar
Newall, G. 1970. A symbiotic relationship between Lingula and the coral Heliolites in the Silurian, p. 335–344. In Crimes, T. P. and Harper, J. C. (eds.), Trace Fossils. Seel House Press, Liverpool.Google Scholar
Nicholson, H. A. 1874. On Columnopora, a new genus of tabulate corals. Geological Magazine, 1:253–254.Google Scholar
Nicholson, H. A., and Murie, J. 1878. On the minute structure of Stromatopora and its allies. Journal of the Linnaean Society, London, 14: 187–246.Google Scholar
Pallas, P. S. 1766. Miscellanea zoological quibus novae imprimis atque obscurae animalium species describuntur et observationibus iconibusque illustrantur. Hagae Comitum, 22 p.Google Scholar
Palmer, T. J., and Wilson, M. A. 1988. Parasitism of Ordovician bryozoans and the origin of pseudoborings. Palaeontology, 31:939–949.Google Scholar
Pemberton, S. G., Kobluk, D. R., Ross, K. Y., and Risk, M. J. 1980. The boring Trypanites at the Silurian–Devonian disconformity in southern Ontario. Journal of Paleontology, 54:1258–1266.Google Scholar
Popov, L. E., and Holmer, L. E. 1994. Cambrian–Ordovician lingulate brachiopods from Scandinavia, Kazakhstan, and South Ural Mountains. Fossils and Strata (Oslo), 35:1–156.CrossRefGoogle Scholar
Rice, M. E. 1969. Possible boring structures of sipunculans. American Zoologist, 9:803–812.Google Scholar
Richards, R. P., and Dyson-Cobb, M. 1976. A Lingula-Heliolites association from the Silurian of Gotland, Sweden. Journal of Paleontology, 50:858–864.Google Scholar
Sokolov, B. S. 1948. Kommensalizm u Favositid. Izvestija Akademii Nauk SSSR, Biology Series, 1:101–110.Google Scholar
Sowerby, J. 1813. The Mineral Conchology of Great Britain, 1. Meredith, London, 234 p.Google Scholar
Stearn, C. W., and Pickett, J. W. 1994. The stromatoporoid animal revisited: Building a skeleton. Lethaia, 27:1–10.Google Scholar
Stel, J. H. 1976. The Paleozoic hard substrate trace fossils Helicosalpinx, Chaetosalpinx and Torquaysalpinx . Neues Jahrbuch für Geologie und Paläontologie Monatshefte, 12:726–744.Google Scholar
Tapanila, L. 2002. A new endosymbiont in Late Ordovician tabulate corals from Anticosti Island, eastern Canada. Ichnos, 9:109–116.Google Scholar
Tapanila, L. 2004. The earliest Helicosalpinx from Canada and the global expansion of commensalism in Late Ordovician sarcinulid corals (Tabulata). Palaeogeography, Palaeoclimatology, Palaeoecology, 215: 99–110.CrossRefGoogle Scholar
Tapanila, L. 2005. Paleoecology and diversity of endosymbionts in Paleozoic marine invertebrates: Trace fossil evidence. Lethaia, 38:89–99.Google Scholar
Tapanila, L., and Copper, P. 2002. Endolithic trace fossils in Ordovician–Silurian corals and stromatoporoids, Anticosti Island, eastern Canada. Acta Geologica Hispanica, 37:15–20.Google Scholar
Tapanila, L., Copper, P., and Edinger, E. 2004. Environmental and substrate control on Paleozoic bioerosion in corals and stromatoporoids, Anticosti Island, eastern Canada. Palaios, 19:292–306.Google Scholar
Taylor, P. D., and Wilson, M. A. 2002. A new terminology for marine organisms inhabiting hard substrates. Palaios, 17:522–525.Google Scholar
Twenhofel, W. H. 1914. The Anticosti Island fauna. Canadian Geological Survey, Museum Bulletin, 3, Geology Series, 19:1–38.Google Scholar
Valentine, J. L., Brock, G. A., and Molloy, P. D. 2003. Linguliformean brachiopod faunal turnover across the Ireviken Event (Silurian) at Boree Creek, central-western New South Wales, Australia. Courier Forschungsinstitut Senckenberg, 242:301–327.Google Scholar
Waagen, W. 1885. Salt Range Fossils, Part 4(2) Brachiopoda. Memoirs, Palaeontologia Indica, series 13, 1 (part 5):729–770.Google Scholar
Williams, A. 2003. Microscopic imprints on the juvenile shells of Palaeozoic linguliform brachiopods. Palaeontology, 46:67–92.Google Scholar
Williams, A., and Holmer, L. E. 1992. Ornamentation and shell structure of acrotretoid brachiopods. Palaeontology, 35:657–692.Google Scholar
Wilson, M. A., and Palmer, T. J. 1988. Nomenclature of a bivalve boring from the Upper Ordovician of the midwestern United States. Journal of Paleontology, 62:306–308.Google Scholar
Wright, A. D. 1963. The fauna of the Portrane Limestone. 1. The inarticulate brachiopods. British Museum of Natural History Bulletin (Geology), 8:221–254.Google Scholar
Zhang, S., and Barnes, C. R. 2002. Late Ordovician–Eary Silurian (Ashgillian–Llandovery) sea level curve derived from conodont community analysis, Anticosti Island, Québec. Palaeogeography, Palaeoclimatology, Palaeoecology, 180:5–32.Google Scholar