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Cryptic encrusting fauna inside invertebrate fossils from the Ordovician of Estonia

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
This is the first report of encrusted cryptic surfaces in the Ordovician of Estonia. Only bryozoans and cornulitids occurred in nautiloids and trilobites. Bryozoans were the dominant encrusters, in terms of both the number of specimens and the encrustation area. Stalked echinoderms are common on the hardgrounds in the Middle and Upper Ordovician of Baltica, but the restricted space in nautiloid living chambers and trilobites probably prevented colonization by stalked echinoderms. Cryptic surfaces in nautiloids and trilobites usually are somewhat more encrusted than the open surfaces of hardgrounds in the Ordovician of Estonia. Encrusters presumably favoured cryptic surfaces, as these were less accessible for predators and grazers. Low encrustation densities, compared to North American hard substrates, seem to be characteristic for the Ordovician Baltic Basin.
Słowa kluczowe
Rocznik
Strony
285--290
Opis fizyczny
Bibliogr. 29 poz., rys., tab.
Twórcy
autor
  • Department of Geology, University of Tartu, Ravila 14A, 50411 Tartu, Estonia
autor
  • Institut für Geologie, Universität Hamburg, Bundesstraße 55, 20146 Hamburg, Germany
autor
  • Department of Geology, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia
autor
  • Natural History Museum, University of Tartu, Vanemuise 46, 50410 Tartu, Estonia
Bibliografia
  • 1. Bassler, R. S., 1911. The early Palaeozoic Bryozoa of the Baltic provinces. United States National Museum Bulletin, 77: 1-382.
  • 2. Brett, C. E. & Liddell, W. D., 1978. Preservation and paleoecology of a Middle Ordovician hardground community. Paleobiology, 4: 329-348.
  • 3. Buttler, C. J. & Wilson, M. A., 2018. Paleoecology of an Upper Ordovician submarine cave-dwelling bryozoan fauna and its exposed equivalents in northern Kentucky, USA. Journal of Paleontology, 92: 568-576.
  • 4. Cuffey, R. J., 1974. Delineation of bryozoan constructional roles in reefs from comparison of fossil bioherms and living reefs. Proceedings of the Second International Coral Reef Symposium, Brisbane, Australia, 1: 357-364.
  • 5. Dronov, A. V. & Rozhnov, S., 2008. Climatic changes in the Baltoscandian Basin during the Ordovician: sedimentological and palaeontological aspects. Acta Palaeontologica Sinica, 46: 108-113.
  • 6. Jaanusson, V. 1973. Aspects of carbonate sedimentation in the Ordovician of Baltoscandia. Lethaia, 6: 11-34.
  • 7. Kobluk, D. R., 1980. Upper Ordovician (Richmondian) cavity dwelling (coelobiontic) organisms from southern Ontario. Canadian Journal of Earth Sciences, 17: 1616-1627.
  • 8. Kobluk, D. R., 1981. Middle Ordovician (Chazy Group) cavity dwelling boring sponges. Canadian Journal of Earth Sciences, 18: 1101-1108.
  • 9. Kobluk, D. R., 1988. Cryptic faunas in reefs: ecology and geologic importance. Palaios, 3: 379-390.
  • 10. Lescinsky, H. L., Edinger, E. & Risk, M. J., 2002. Mollusc shell encrustation and bioerosion rates in a modern epeiric sea: taphonomy experiments in the Java Sea, Indonesia. Palaios, 17: 171-191.
  • 11. Lidgard, S., McKinney, F. K. & Taylor, P. D., 1993. Competition, clade replacement, and a history of cyclostome and cheilostome bryozoan diversity. Paleobiology, 19: 352-371.
  • 12. Nestor, H. & Einasto, R., 1997. Ordovician and Silurian carbonate sedimentation basin. In: Raukas, A. & Teedumäe, A. (eds), Geology and Mineral Resources of Estonia. Estonian Academy Publishers, Tallinn, pp. 192-204.
  • 13. Pushkin, V. I., 1990. Bryozoa of the family Ceramoporidae of Ordovician from the eastern European platform. In: Velichkevich, F. Y. (ed.), New Representatives of the Fossil Fauna and Flora of Belorussia and Other Regions of the USSR. Collected Scientific Papers. Nauka i Tekhnika, Minsk, pp. 5-34. [In Russian.]
  • 14. Raukas A. & Teedumäe A., 1997. Geology and Mineral Resources of Estonia. Estonian Academy Publishers, Tallinn, 436 pp.
  • 15. Rozhnov, S., 2017. The beginning of the Ordovician evolutionary radiation in the Baltic Region: Substrate revolution, explosive increase in diversity of stalked echinoderms, and the cyanobacterial origin of hardgrounds. In: Zhang, Y., Zhan, R., Fan, Y & Muir, L. A. (eds), Extended Summaries for the International Geoscience Programme (IGCP) Project 653 - Annual Meeting 2017 October 8-12, 2017, Yichang, China. Zhejiang University Press, pp. 133-139.
  • 16. Segars, M. T. & Liddell, W. D., 1988. Microhabitat analysis of Silurian stromatoporoids as substrata for epibionts. Palaios, 3: 391-403.
  • 17. Spjeldnaes, N., 1975. Silurian bryozoans which grew in the shade. Document Laboratoire Géologie Faculté Science Lyon, 3: 415-424.
  • 18. Taylor, P. D. & Wilson M. A., 2003. Palaeoecology and evolution of marine hard substrate communities. Earth-Science Reviews, 62: 1-103.
  • 19. Torsvik, T. H. & Cocks, L. R. M., 2013. New global palaeogeographical reconstructions for the Early Palaeozoic and their generation. Geological Society Memoirs, London, 38: 5-24.
  • 20. Vinn, O., 2005. The distribution of worm borings in brachiopod shells from the Caradoc Oil Shale of Estonia. Carnets de Géologie, G2005_A03: 1-11.
  • 21. Vinn, O., 2015. Sparsely encrusted hardground in the calcareous sandstone from the Darriwilian of Pakri Cape, NW Estonia (Baltica). Estonian Journal of Earth Sciences, 64: 249-253.
  • 22. Vinn, O. & Toom, U., 2015. Some encrusted hardgrounds from the Ordovician of Estonia (Baltica). Carnets de Géologie, 15: 63-70.
  • 23. Vinn, O., Wilson, M. A., Zatoń, M. & Toom, U., 2014. The trace fossil Arachnostega in the Ordovician of Estonia (Baltica). Palaeontologia Electronica, 17.3.41A: 1-9.
  • 24. Wilson, M. A., 1986. Coelobites and spacial refuges in a Lower Cretaceous cobble-dwelling hardground fauna. Palaeontology, 29: 691-703.
  • 25. Wilson, M. A., 1998. Succession in a Jurassic marine cavity community and the evolution of cryptic marine faunas. Geology, 26: 379-381.
  • 26. Wilson, M. A., Bosch, S. & Taylor, P. D., 2015. Middle Jurassic (Callovian) cyclostome bryozoans from the Tethyan tropics (Matmor Formation, southern Israel). Bulletin of Geosciences, 90: 51-63.
  • 27. Wyse Jackson, P. N. & Key, M. M., Jr., 2007. Borings in trepostome bryozoans from the Ordovician of Estonia: two ichnogenera produced by a single maker, a case of host morphology control. Lethaia, 40: 237-252.
  • 28. Zatoń, M., Borszcz, T., Berkowski, B., Rakociński, M., Zapalski, M. K. & Zhuravlev, A. V, 2015. Paleoecology and sedimentary environment of the Late Devonian coral biostrome from the Central Devonian Field, Russia. Palaeogeography, Palaeoclimatology, Palaeoecology, 424: 61-75.
  • 29. Zatoń, M., Zapalski, M. K., Berkowski, B. & Wrzołek, T., 2018. Cryptic encrusting communities in a Middle Devonian mesophotic paleoenvironment of the Holy Cross Mountains, Poland. Palaeogeography, Palaeoclimatology, Palaeoecology, 501: 82-91.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-ec802f05-8ebf-4027-85bf-9293d6bcc18d
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