Podrobnosti záznamu

Název
    Characterization of the Parakidograptus acuminatus graptolite Biozone in the Silurian of the Barrancos region (Ossa Morena Zone, South Portugal)
Údaj o odpovědnosti
    J.M. Picarra, Petr Štorch, Juan-Carlos Gutiérrez-Marco, J. T. Oliveira = Petr Štorch = Juan-Carlos Gutiérrez-Marco = J.T. Oliveira
Autor
    Gutiérrez-Marco, Juan-Carlos
    Oliveira, J. T.
    Picarra, J. M.
    Štorch, Petr
Jazyk
    anglicky
Zdrojový dokument - seriál
    Comunicacoes do Instituto Geológico e Mineiro
Svazek/č.
    Vol. 81
Strany
    p. 3-8
Rok
    1995
Poznámky
    3 obr., 25 bibl.
    res. port.
    Zkr. název ser.: Comun. Inst. geol. min. (Lisboa).
Předmětová skupina
    Graptolithina
    ordovik
    paleobiogeografie
    sedimentologie
    silur
    stratigrafická hranice
    zóny biostratigrafické
Geografické jméno
    Portugalsko
Klíčové slovo
    Acuminatus
    Barrancos
    Biozone
    Characterization
    Graptolite
    Morena
    Ossa
    Parakidograptus
    Portugal
    Region
    Silurian
    South
    Zone
Abstrakt (anglicky)
   A graptolite assemblage indicative of the basal Silurian P. acuminatus Biozone has been identified in two localities of the Barrancos region (South Portugal), within the Ossa Morena Zone of the Hesperian Massif. It represents the first record of this biozone in Portugal and the third one in the whole Iberian Peninsula. Identified taxa include Parakidograptus acuminatus, Normalograptus trifilis, N. medius, N. angustus, Cystograptus ancestralis and Neodiplograptus cf.lanceolatus. Owing to the presence of N.trifilis, the assemblage may be referred to about the middle part of the P. acuminatus Biozone. The graptolites were recorded at the base of a black-shale sequence with remarkable lyditic intercalations in its lower part (the "Xistos com Nódulos" Formation), which overlies barren quartzites of supposed Ordovician age (Colorada Formation). The new biostratigraphic data prove Ordovician-Silurian transition in this region of the Ossa Morena Zone.
   Both the graptolite assemblages, thickness of the P. acuminatus Biozone, and the facies development of the earliest Silurian of the Barrancos region can be well compared with coeval sections throughout the whole peri-Gondwanan Europe
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    25. 6. 2008
Datum importu
    8. 8. 2012