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Endobiotic cornulitids in Upper Ordovician tabulate corals and stromatoporoids from Anticosti Island, Quebec

Published online by Cambridge University Press:  11 August 2017

Owen A. Dixon
Owen A. Dixon*
Affiliation:
R.R. 1, McArthur's Mills, ON K0L 2M0, Canada,
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Abstract

Conoidal shells of Cornulites celatus n. sp. occur commonly within host coralla of Propora conferta Milne-Edwards and Haime, 1851, sensu lato, from the Laframboise Member of the Ellis Bay Formation (Ashgill: Upper Ordovician) at Pointe Laframboise on western Anticosti Island. Examples have also been found at the same locality in the tabulate corals Paleofavosites sp., Acidolites arctatus Dixon, 1986, and A. compactus Dixon, 1986, and the stromatoporoid Ecclimadictyon sp., but not in other associated tabulate coral species. Growth interference between the shells and their hosts indicates a commensal relationship. C.celatus apparently had a more limited paleoenvironmental range than its principal coral host species, which occurs abundantly elsewhere on the island without its endobiotic partner. The diagnosis of Cornulites is emended to include forms having a two-layered shell wall with a distinctive outer layer consistently preserved as prismatic calcite. This new species extends the known stratigraphic range of cornulitids in commensal relationships with corals and stromatoporoids from the Silurian back to the Upper Ordovician.

Type
Research Article
Information
Journal of Paleontology , Volume 84 , Issue 3 , May 2010 , pp. 518 - 528
Copyright
Copyright © 2010, The Paleontological Society 

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References

Billings, E. 1865. Notice of some new genera and species of Palaeozoic fossils. Canadian Naturalist and Geologist, new series, 2: 425–432.Google Scholar
Bolton, T. E. 1981. Late Ordovician and Early Silurian Anthozoa of Anticosti Island, Québec, p. 107–135. In Lespérance, P. J. (ed.), Field Meeting, Anticosti-Gaspé, Québec, 1981, Vol. II: Stratigraphy and Paleontology. International Union of Geological Sciences, Subcommission on Silurian Stratigraphy, Ordovician-Silurian Boundary Working Group.Google Scholar
Bouček, B. 1964. The Tentaculites of Bohemia. Publication of Czechoslovakian Academy of Sciences, Prague, 125 p.Google Scholar
Dixon, O. A. 1974. Late Ordovician Propora (Coelenterata: Heliolitidae) from Anticosti Island, Quebec, Canada. Journal of Paleontology, 48: 568–585.Google Scholar
Dixon, O. A. 1986. The heliolitid coral Acidolites in Ordovician-Silurian rocks of Eastern Canada. Journal of Paleontology, 60: 26–52.CrossRefGoogle 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
Dzik, J. 1991. Possible solitary bryozoan ancestor from the early Palaeozoic and the affinities of the Tentaculita, p. 121–131. In Bigey, F. P. and d'Hondt, J.-L. (eds.), Bryozoaires actuels et fossiles: Bryozoa Living and Fossil. Societé des Sciences Naturelles de l'Ouest de la France, Mémoire hors, série 1.Google Scholar
Fisher, D. W. 1962. Small conoidal shells of uncertain affinities, p. W98–W143. In Moore, R. C. (ed.), Treatise on Invertebrate Paleontology, Pt. W. Miscellanea. Geological Society of America and University of Kansas Press, Lawrence.Google Scholar
Flower, R. H. 1961. Montoya and related colonial corals. New Mexico Bureau of Mines and Mineral Resources, Memoir 7, p. 1–97.Google Scholar
Foerste, A. F. 1909. Fossils from the Silurian formations of Tennessee, Indiana and Illinois. Bulletin of the Scientific Laboratories of Denison University, 14: 61–107.Google Scholar
Hall, J. 1847. Palaeontology of New York, Volume 1. In Natural History of New York, Part VI. Carroll and Cook, Albany, New York, xxiii + 338 p.Google Scholar
Hall, J. 1888. Tubicolar Annelida. Natural History of New York. Palaeontology, Volume 7. Geological Survey, Albany, New York, 278 p.Google Scholar
Herringshaw, L. G., Thomas, A. T., and Smith, M. P. 2007. Systematics, shell structure and affinities of the Palaeozoic Problematicum Cornulites . Zoological Journal of the Linnaean Society, 150: 681–699.Google Scholar
Huntley, J. W. and Kowalewski, M. 2007. Strong coupling of predation intensity and diversity in the Phanerozoic fossil record. Proceedings of the National Academy of Sciences, 104(38): 15006–15010.Google Scholar
Kriz, J., Frida, J., and Galle, A. 2001. The epiplanktic anthozoan, Kolihaia eremita Prantl, 1946 (Cnidaria), from the Silurian of the Prague Basin (Bohemia). Journal of the Czech Geological Society, 46: 239–245.Google Scholar
Lardeux, H., Jaouen, P.-A., and Plusquellec, Y. 2003. Reticornulites reticulatus n. gen. n. sp. (Cornulitidae) de l'Emsian supérieur de la rade de Brest (Massif armoricain, France). Geodiversitas 25: 649–655.Google Scholar
Lindström, G. 1899. Remarks on the Heliolitidae. Kungliga Svenska Vetenskapsakademiens Handlingar, 32: 1–140.Google Scholar
Long, D. G. F. and Copper, P. 1987. Stratigraphy of the Upper Ordovician upper Vaureal and Ellis Bay formations, eastern Anticosti Island, Quebec. Canadian Journal of Earth Sciences, 24: 1807–1820.Google Scholar
Miller, S. A. 1874. Description of new species of fossils. Cincinnati Quarterly Journal of Science, 1: 234–235.Google Scholar
Milne-Edwards, H. and Haime, J. 1851. Monographie des polypiers fossiles des terrains palaeozoiques. Archives du muséum national d'histoire naturelle de Paris, 5: 1–502.Google Scholar
Nicholson, H. A. 1872a. On the genera Comulites and Tentaculites and a new genus Conchicolites . American Journal of Science, 3: 202–206.Google Scholar
Nicholson, H. A. 1872b. Ortonia, a new genus of fossil tubicolar annelides. Geological Magazine, 9: 446–449.Google Scholar
Prantl, F. 1944. Kolihaia eremita n. gen. n. sp. a new tubicolar annelid from the Silurian of Bohemia. Vestnik Kralovska Ceska Spolecnost Nauk, 24: 1–12.Google Scholar
Richards, P. R. 1974. Ecology of the Cornulitidae. Journal of Paleontology, 48: 514–523.Google Scholar
Schlotheim, E. F. von. 1820. Die Petrefakten-Kunde auf ihrem jetzigen Standpunkte durch die Beshreibung seiner Sammlung versteinerter und fossiler Ueberreste des Thier-und Planzenreichs der Vorwelt erläutert. Gotha, 437 p.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.Google Scholar
Tapanila, L. 2005. Palaeoecology and diversity of endosymbionts in Palaeozoic marine invertebrates: trace fossil evidence. Lethaia, 38: 89–99.CrossRefGoogle Scholar
Tapanila, L. 2008. Direct evidence of ancient symbiosis using trace fossils, p. 19–35. In Kelley, P. H. and Bambach, R. K. (eds.), From Evolution to Geobiology: Research Questions Driving Paleontology at the Start of a New Century, Paleontological Society Short Course. Paleontological Society Papers, v. 14.Google Scholar
TWENHOFEL, W. H. 1928. Geology of Anticosti Island. Geological Survey of Canada Memoir, 154, 481 p.Google Scholar
Vinn, O. 2005. A new comulitid genus from the Silurian of Gotland, Sweden. GFF (Geologiska Foreningens I Stockholm Forhandungar), 127: 205–210.Google Scholar
Vinn, O. and Mötus, M-A. 2008. The earliest endosymbiotic mineralized tubeworms from the Silurian of Podolia, Ukraine. Journal of Paleontology, 82: 409–414.CrossRefGoogle Scholar
Vinn, O. and Mutvei, H. 2005. Observations on the morphology and affinities of cornulitids from the Ordovician of Anticosti Island and the Silurian of Gotland. Journal of Paleontology, 79: 726–737.Google Scholar
Vinn, O. and Wilson, M. A. In press. Endosymbiotic Cornulites in the Sheinwoodian (Early Silurian) stromatoporoids of Saaremaa, Estonia. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen.Google Scholar
Young, G. A. and Elias, R. J. 1995. Latest Ordovician to Earliest Silurian Colonial Corals of the East-Central United States. Bulletins of American Paleontology, 108(347), p. 1–148.Google Scholar
Renbin, Zhan and Vinn, O. 2007. Cornulitid epibionts on brachiopod shells from the Late Ordovician (middle Ashgill) of East China. Estonian Journal of Earth Sciences, 56: 101–108.Google Scholar