Sea-level history of Devonian bioevents in the classical Barrandian area, Czech Republic: Are biotic overturns driven by sea level?


Global extinctions and biotic overturns (bioevents) occur in striking abundance in the Devonian as compared to other periods of the Phanerozoic. At least ten remarkable bioevents (basal Pragian, Daleje, Choteč, Kačák... [ view full abstract ]


  1. Ondrej Bábek (Department of Geology, Palacký University of Olomouc)
  2. Martin Famera (Department of Geology, Palacký University of Olomouc)
  3. Jindrich Hladil (Geological Institute, Czech Academy of Sciences, Prague)
  4. Hedvika Poukarová (Department of Geological Sciences, Masaryk University of Brno)
  5. Daniel Simícek (Department of Geology, Palacký University of Olomouc)

Topic Areas

Topics: Biotic sedimentary processes , Topics: Carbonate platforms and reef , Topics: Sequence stratigraphy


MS13 » Sequences and cycles III (17:00 - Wednesday, 25th May, FES 2)

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