Record details

    Ordovician of the Barrandian area: Reconstruction of the sedimentary basin, its benthic communities and ichnoassemblages
Statement of responsibility
    Radek Mikuláš
Other titles
    Ordovik Barrandienu: rekonstrukce sedimentární pánve, benthických společenstev a ichnospolečenstev
    Mikuláš, Radek
Source title - serial
    Journal of the Czech Geological Society
    Vol. 43, no. 3
    p. 143-159
    11 obr., 43 bibl.
    České resumé
    Zkr. název ser.: J. Czech geol. Soc.
Subject group
    pražská pánev
    trace fossils
Geographical name
    Český kras
Abstract (in english)
   Reconstruction of the development of the Barrandian area during the Ordovician (presented in a form of a series of block-diagrams) enable us to presume: 1, there is a different pattern of development of body fossil assemblages compared to ichnoassemblages; 2, the linear sedimentary basin went through a stepwise change into an open marginal sea; 3, main mechanism of sedimentation changed in a time (e.g., increase of tempestites towards the end of the Ordovician); 4, the clastic material had been transported mostly from the North in the Late Ordovician; 5, the hitherto published conclusions on the palaeogeography of the Prague basin during the Ordovician do not show substantial inconsistencies if translated into a series of linked three-dimensional models
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
Entered date
    18. 2. 2008
Import date
    8. 8. 2012