Podrobnosti záznamu

Název
    Dinoflagellate study of the Lower Cretaceous deposits in the Pieniny Klippen Belt (Rochovica section, Slovak Western Carpathians)
Údaj o odpovědnosti
    Petr Skupien
Autor
    Skupien, Petr
Jazyk
    anglicky
Zdrojový dokument - seriál
    Bulletin of geosciences
Svazek/č.
    Vol. 78, no. 1
Strany
    p. 67-82
Rok
    2003
Poznámky
    4 obr., 2 tab., 6 pl., 26 bibl.
    il.
    Zkr. název ser.: Bull. Geosci.
Předmětová skupina
    Algophytae
    Dinoflagellata
    křída-spodní
    paleoekologie
    paleoklimatologie
    palynomorfa
    Západní Karpaty
    zóny biostratigrafické
Geografické jméno
    Rochovica (Slovensko)
    Slovensko
Klíčové slovo
    Belt
    Carpathians
    Cretaceous
    Deposits
    Dinoflagellate
    Klippen
    Lower
    Pieniny
    Rochovica
    Section
    Slovak
    Study
    Western
Abstrakt (anglicky)
   One of the most complete and best documented sections, namely the Rochovica section, was selected for the first detailed palynological study of Lower Cretaceous sediments of the Pieniny Klippen Belt. The greatest attention was given, from not only the biostratigraphical but also the palaeoecological point of view, to the assemblages of non-calcareous dinoflagellates. Based on dinoflagellates, the age of the studied sediments corresponds to the Upper Barremian-Albian. Quantitative composition of the palynomorph assemblage reflects open-sea conditions with higher supply of terrigenous material during the Barremian and the Early Aptian as well as a marked supply of nutrients during the Early Aptian. Generally, rise in the sea level in the Barremian-Albian period is obvious (oceanic types of dinocysts are present).Abstract.
   One of the most complete and best documented sections, namely the Rochovica section, was selected for the first detailed palynological study of Lower Cretaceous sediments of the Pieniny Klippen Belt. The greatest attention was given, from not only the biostratigraphical but also the palaeoecological point of view, to the assemblages of non-calcareous dinoflagellates. Based on dinoflagellates, the age of the studied sediments corresponds to the Upper Barremian-Albian. Quantitative composition of the palynomorph assemblage reflects open-sea conditions with higher supply of terrigenous material during the Barremian and the Early Aptian as well as a marked supply of nutrients during the Early Aptian. Generally, rise in the sea level in the Barremian-Albian period is obvious (oceanic types of dinocysts are present)
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    27. 9. 2007
Datum importu
    8. 8. 2012