Počet záznamů: 1  

Evolution of Silurian and Devonian sedimentary environments in the Prague basin: evidence from isotopic compositions of carbon and oxygen and trace element contents in brachiopod shells

  1. 1.
    0145091 - GLU-S 20004030 RIV DE eng C - Konferenční příspěvek (zahraniční konf.)
    Hladíková, J. - Hladil, Jindřich - Košler, J. - Jačková, I.
    Evolution of Silurian and Devonian sedimentary environments in the Prague basin: evidence from isotopic compositions of carbon and oxygen and trace element contents in brachiopod shells.
    European Palaeontological Association Workshop 2000 - Biomarkes and Stable Isotopes in Palaeontology. Frankfurt am Main: European Palaeontological Association, 2000 - (Oschmann, W.; Steininger, F.; Fürsich, F.), s. 43- 45+ 1 nečíslovaná
    [European Palaeontological Association Workshop 2000 - Biomarkes and Stable Isotopes in Palaeontology. Frankfurt am Main (DE), 30.06.2000-02.07.2000]
    Grant CEP: GA ČR GA205/98/0454
    Grant ostatní: XX(XX) IGCP386; XX(XC) IGCP421
    Výzkumný záměr: CEZ:AV0Z3013912
    Kód oboru RIV: DB - Geologie a mineralogie

    The positive delta 18O anomaly was documented on carbonates N of Koneprusy (Barrandian area). It ranges within Pragian-Eifelian time-span. This unusually strong anomaly is coupled with a moderate depression of delta 13C values, as well as increased contents of selected non-ferrous metals and rare elements (ICP-MS trace element data for brachiopod samples). An eustatically half-separated ocean/marine basin has been interpreted, where deep parts of water column were typical with anoxia, toxic pollutants and temporarily anomalous isotopic compositions.
    Trvalý link: http://hdl.handle.net/11104/0042705
     

Počet záznamů: 1  

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