Record details

Title
    Calcareous nannoplankton from the Eggenburgian stratotype and faciostratotypes (Lower Miocene, Central Paratethys)
Statement of responsibility
    Katarína Holcová
Author
    Holcová, Katarína
Language
    anglicky
Source title - serial
    Geologica carpathica
Vol./nr.
    Roč. 53, č. 6
Pages
    s. 381-390
Year
    2002
Notes
    5 obr., 37 bibl.
    il.
    Zkr. název ser.: Geol. carpath.
Subject group
    biostratigrafie
    eggenburg
    facie
    miocén-spodní
    nannofosílie
    Paratethys
    stratotyp
    vápnitost
    Západní Karpaty
    zóny biostratigrafické
Geographical name
    Rakousko
    Slovensko
Keyword
    Calcareous
    Central
    Eggenburgian
    Faciostratotypes
    Lower
    Miocene
    Nannoplankton
    Paratethys
    Stratotype
Abstract (in english)
   Calcareous nannoplankton was studied at the Eggenburgian holostratotype and faciostratotypes of Loibersdorf, Achberg, Brunnstube, "Judenfriedhof", Burgschleinitz, Fels am Walgram, Vaďovce, Podkylava, Sverepec, Veľká Čausa and Lipovany. As sections with rich shallow-water molluscan fauna were chosen for Eggenburgian type sections, most of the samples are not favourable for the analysis of calcareous nannoplankton. Of 51 samples, 28 samples contain common to abundant calcareous nannoplankton which can be quantitatively analysed. Three bioevents were searched for in the type sections: FAD of Discoaster druggii (NN1/NN2 boundary), FAD of Helicosphaera ampliaperta (middle part of NN2 Zone, approximately Egerian/Eggenburgian boundary sensu Rögl 1998), FAD of Sphenolithus belemnos (NN2/ NN3 boundary, upper part of the Eggenburgian).
   In areas with continuous sedimentation from the Egerian to Eggenburgian (the Outer Western Carpathians: Waschberg, Pouzdřany and Ždánice Units and the remnant flysch trough of the Skole-Skiba Zone; the Inner Western Carpathians: the Fiľakovo (Pétervására) Basin, all three events are successively observed while in areas with transgressive Eggenburgian sediments (Lower Austria, the Vienna Basin, the Danube Basin, the Váh River Valley and Horná Nitra Basin), sequences started with FAD of Helicosphaera ampliaperta. Two types of autochthonous assemblages were distinguished by multivariate statistical analysis (cluster and factor analysis): (1) abundant, dominated by Coccolithus pelagicus, (2) rare, dominated by reticulofenestrids. The third type of assemblage is dominated by reworked Cretaceous species
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    18. 7. 2007
Import date
    8. 8. 2012