A new Early Jurassic (ca. 183 Ma) fossil Lagerstätte from Ya Ha Tinda, Alberta, Canada

作者: Rowan C. Martindale , Theodore R. Them , Benjamin C. Gill , Selva M. Marroquín , Andrew H. Knoll

DOI: 10.1130/G38808.1

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摘要: Lagerstatten —deposits of exceptionally preserved fossils—offer vital insights into evolutionary history. To date, only three Konservat-Lagerstatten are known from Early Jurassic marine rocks (Osteno, Posidonia Shale, and Strawberry Bank), all located in Europe. We report a new assemblage fossils from Alberta, Canada, the first Konservat-Lagerstatte described from North America. The Ya Ha Tinda assemblage includes articulated vertebrates (fish, ichthyosaurs), crinoids, crustaceans, brachiopods, abundant mollusks (coleoids with soft tissues, ammonites, gastropods, bivalves), wood, microfossils. Paired bioand chemostratigraphies show that Lagerstatte deposition occurred during late Pliensbachian through early Toarcian, capturing the carbon isotope excursion associated Toarcian Oceanic Anoxic Event. Therefore, Panthalassan biota is coeval with Toarcian Tethys Ocean (Posidonia Shale and Strawberry Bank). Comparisons among these deposits permit new insights diversity, ecology, biogeography Jurassic marine communities during time pronounced biological and environmental change (e.g., expanded subsurface anoxia, warming, and extinctions). They also highlight possibility Mesozoic Anoxic Events are temporal foci exceptional preservation.

参考文章(23)
Derek E. G. Briggs, Amanda J. Kear, Decay and preservation of polychaetes: taphonomic thresholds in soft-bodied organisms Paleobiology. ,vol. 19, pp. 107- 135 ,(1993) , 10.1017/S0094837300012343
Bryony A. Caswell, Angela L. Coe, The impact of anoxia on pelagic macrofauna during the Toarcian Oceanic Anoxic Event (Early Jurassic) Proceedings of the Geologists' Association. ,vol. 125, pp. 383- 391 ,(2014) , 10.1016/J.PGEOLA.2014.06.001
K. Glass, S. Ito, P. R. Wilby, T. Sota, A. Nakamura, C. R. Bowers, J. Vinther, S. Dutta, R. Summons, D. E. G. Briggs, K. Wakamatsu, J. D. Simon, Direct chemical evidence for eumelanin pigment from the Jurassic period. Proceedings of the National Academy of Sciences of the United States of America. ,vol. 109, pp. 10218- 10223 ,(2012) , 10.1073/PNAS.1118448109
Crispin T. S. Little, Michael J. Benton, Early Jurassic mass extinction: A global long-term event Geology. ,vol. 23, pp. 495- 498 ,(1995) , 10.1130/0091-7613(1995)023<0495:EJMEAG>2.3.CO;2
Bernard Lathuilière, Denis Marchal, Extinction, survival and recovery of corals from the Triassic to Middle Jurassic time Terra Nova. ,vol. 21, pp. 57- 66 ,(2009) , 10.1111/J.1365-3121.2008.00856.X
Hans-Joachim Röhl, Annette Schmid-Röhl, Wolfgang Oschmann, Andreas Frimmel, Lorenz Schwark, None, The Posidonia Shale (Lower Toarcian) of SW-Germany: an oxygen-depleted ecosystem controlled by sea level and palaeoclimate Palaeogeography, Palaeoclimatology, Palaeoecology. ,vol. 165, pp. 27- 52 ,(2001) , 10.1016/S0031-0182(00)00152-8
D. J.K. Ross, R. M. Bustin, Sediment Geochemistry of the Lower Jurassic Gordondale Member, Northeastern British Columbia Bulletin of Canadian Petroleum Geology. ,vol. 54, pp. 337- 365 ,(2006) , 10.2113/GSCPGBULL.54.4.337