Podrobnosti záznamu

Název
    Key Lower Palaeozoic faunas from near the Trans-European Suture Zone
Údaj o odpovědnosti
    L. Robin. M. Cocks
Další názvy
    Palaeozoic Amalgamation of Central Europe (Variant.)
Autor
    Cocks, L. Robin M.
Jazyk
    anglicky
Zdrojový dokument - seriál
    Geological society special publication
Svazek/č.
    Vol. 201
Strany
    p. 37-46
Rok
    2002
Poznámky
    2 obr., 1 fot., 2 s. bibl.
    il.
    Zkr. název ser.: Geol. Soc. spec. Publ. (London).
Předmětová skupina
    Brachiopoda
    brunovistulikum
    kambrium
    ordovik
    paleobiogeografie
    paleogeografie
    rotace desek
    tektonika bloková
    terán
    trace fossils
    Trilobita
    zóna suturová
Geografické jméno
    ČR-Morava
    Polsko
    SRN
Klíčové slovo
    Faunas
    Key
    Lower
    Near
    Palaeozoic
    Suture
    Trans-European
    Zone
Abstrakt (anglicky)
   Following recognition of the Vendian to mid-Ordovician rotation of Baltica, with more than 55° of that rotation occurring in the Upper Cambrian and Lower Ordovician, the Tornquist Margin of Baltica must have faced northwards towards Laurentia and the Panthalassic Ocean, rather than, as now, southwestwards towards Gondwana (including Avalonia). Unequivocally Baltic endemic trilobite, brachiopod and other faunas are known from both the Cambrian and the Ordovician of the Holy Cross Mountains, Poland, and from both parts of them, i.e. the Malopolska Block and the Lysogóry Block. Whether or not these two blocks were united into a single terrane or were separate as two terranes is equivocal from the faunal evidence, and there is no faunal evidence of substantial strike-slip faulting of the blocks in relation to the main Baltic craton: they are perceived as having made up part of the margin of Baltica itself.
   However, both Holy Cross Mountain blocks were different and palaeogeographically separate from the Bruno-Silesian Block, whose continental origins are yet to be finally determined. The Ordovician clastic sediments at both Riigen, north Germany, and Pomerania, NW Poland, have yielded no macrofossils other than graptolites, but microfossils (acritarchs and chitinozoa) are interpreted as having been deposited at relatively high palaeolatitudes, i.e. at a higher palaeolatitude than Baltica, and may have been deposited in an ocean basin within the Tornquist Ocean between Baltica and Avalonia
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    25. 3. 2008
Datum importu
    8. 8. 2012