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Trace fossils and bioturbation in the lower part of the Šárka Formation at Praha - Červený vrch Hill (Ordovician, Barrandian area, Czech Republic)

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    0145708 - GLU-S 20033079 RIV CZ eng J - Journal Article
    Mikuláš, Radek
    Trace fossils and bioturbation in the lower part of the Šárka Formation at Praha - Červený vrch Hill (Ordovician, Barrandian area, Czech Republic).
    Bulletin of Geosciences. Roč. 78, č. 2 (2003), s. 141-146. ISSN 1214-1119. E-ISSN 1802-8225
    Grant - others:UNESCO(XX) IGCP 410
    Institutional research plan: CEZ:AV0Z3013912
    Keywords : Ordovician * ichnofossils * Pilichnus
    Subject RIV: DB - Geology ; Mineralogy
    http://www.geology.cz/bulletin/contents/2003/vol78no2/a08-mikulas.pdf

    Sediments of the Šárka Formation are exposed at the Červený vrch Hill in Prague. The lower part of the outcrop shows biogenic structures belonging almost exclusively to the ichnogenus Pilichnus. Most of the distinctive traces (Planolites, Palaeophycus, Nereites) come from an interval rich body fossils of graptolites and phyllocarids. The overall character of the ichnoassemblage indicates ecologic stress, probably a low oxygen level, and only short-time fluctuations in the oxygen content.
    Permanent Link: http://hdl.handle.net/11104/0043266

     
     

Number of the records: 1  

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