Podrobnosti záznamu

Název
    Biostratigraphical correlations of Early Devonian vertebrate assemblages of the Old Red Sandstone Continent
Údaj o odpovědnosti
    Alain Blieck, Richard Cloutier, David K. Elliott, Daniel Goujet, Stanislas Loboziak, Randal C. Reed, Ol'ga Rodina, Philippe Steemans, Juozas J. Valiukevicius, Ljubov' Vjuškova, Jevgenij Jolkin, V.T. Young
Autor
    Blieck, Alain
    Cloutier, Richard
    Elliott, David K.
    Goujet, Daniel
    Jolkin, Jevgenij
    Loboziak, Stanislas
    Reed, Randal C.
    Rodina, Ol'ga
    Steemans, Philippe
    Valiukevicius, Juozas J.
    Vjuškova, Ljubov'
    Young, V. T. (Sally)
Jazyk
    anglicky
Zdrojový dokument - monografie
    Palaeozoic Vertebrate Biochronology and Global Marine/Non-Marine Correlation, Final Report of IGCP 328 (1991-1996). Courier Forschungsinstitut-Senckenberg 223
Strany
    s. 223-269
Poznámky
    15 obr., 1 pl.
    il.
    Obsahuje bibliografické odkazy
Předmětová skupina
    Acanthodii
    Agnatha
    Barrandien
    Chitinozoa
    Chondrichthyes
    Conodonta
    devon-spodní
    Heterostraci
    korelace stratigrafická
    miospory
    Osteostraci
    paleogeografie
    Placodermi
    pražská pánev
    stratotyp
    Vertebrata
    zóny biostratigrafické
Geografické jméno
    Amerika severní
    ČR-Čechy
    Evropa
    Karlštejn (Beroun)
    Suchomasty (Beroun)
    Uzbekistán
Klíčové slovo
    Assemblages
    Biostratigraphical
    Continent
    Correlations
    Devonian
    Early
    Old
    Red
    Sandstone
    Vertebrate
Abstrakt (anglicky)
   The Old Red Sandstone Continent was one of the major landmasses of the Devonian period, as a result of Early Palaeozoic orogenies. Numerous vertebrate-bearing fossiliferous localities are known from this palaeocontinent. They come from lithofacies varying from, e.g. siliciclastic to carbonate. In Lower Devonian rocks, most macrovertebrate remain have been colected in Old Red Sandstone type sediments, but recent investigation have yielded microvertebrate assemblages in various carbonate sediment. One of the main problems, dealing with these Early Devonian vertebrate assemblages is concerned with biostratigraphical correlation between the different facies, and with the standard biostratigraphical zonations (conodonts and miospores in particular). This paper contains a review of vertebrate assemblages of the Lower Devonian Global Stratotype Sections and Points.
   These GSSP contain a poor record of vertebrates, but most recent samplings are promising as concerned with microremains (thelodont and acanthodian scales). Most important Early Devonian vertebrate-bearing sequences from around the Old Red Sandstone Continent are reviewed: west-central U.S.A., Canadian Arctic, Spitsbergen, Baltic area, Podolia, western Europe, eastern Canada
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    3. 10. 2007
Datum importu
    8. 8. 2012