Podrobnosti záznamu

Název
    Higher classification of Paleozoic gastropods inferred from their early shell ontogeny
Údaj o odpovědnosti
    Jiří Frýda
Další názvy
    Vyšší klasifikace paleozoických gastropodů odvozená z ontogeneze jejich rané schránky
Autor
    Frýda, Jiří
Jazyk
    anglicky
Zdrojový dokument - seriál
    Journal of the Czech Geological Society
Svazek/č.
    Vol. 44, no. 1-2
Strany
    p. 137-153
Rok
    1999
Poznámky
    1 obr., 6 fot., 3 s.bibl.
    České resumé
    Zkr. název ser.: J. Czech geol. Soc.
Předmětová skupina
    Barrandien
    Gastropoda
    klasifikace
    ontogeneze
    paleozoikum
    pražská pánev
    schránky
Geografické jméno
    ČR-Čechy
Klíčové slovo
    Classification
    Early
    Gastropods
    Higher
    Inferred
    Ontogeny
    Paleozoic
    Shell
Abstrakt (anglicky)
   The presence of six natural groups (Amphigastropoda, Archaeogastropoda, Mimospirina, Cyrtoneritimorpha, Euomphalomorpha, and Perunelomorpha) were revealed among Silurian and Devonian gastropods of the Prague Basin (Czech Republic) on the basis of their protoconch morphology. The nature of the early shells in the core genus Bellerophon demonstrates that the Amphigastropoda does not belong to the subclass Archaeogastropoda and that it forms a long-lived (cambrian through Triassic), independent molluscan group. The very small size of the bilaterally symsterical early shell of Bellerophon (Amphigastropoda) indicates the presence of a planktotropic larval stage. The higher taxonomic position of the Cambro-Devonian Mimospirina, uniting the paleozoic gastropods with sinistrally coiled shells bearing a large sinistrally coiled, non-archaeogastropod protoconch, is still open.
   The discovery of archaeogastropod-type protoconch in Early Devonian gastropods indicates that the Archaeogastropoda have had the same early ontogenetic pattern for at least 400 Ma (Devonian to recent) and represent a very old, independent gastropod group. The Early Ordovician-Late Permian members of the order Cyrtoneritimorpha (Neritimorpha) with their characteristic fish hook-like protoconch probably gave rise to the modern Cycloneritimorpha (Neritimorpha). The Euomphalomorpha with a cyrtoconic and planispiral openly coiled protoconch form an independent gastropod group, hnown only from the Paleozoic (Cambrian-Permian). The Early Ordovician-Early Devonian members of the order Perunelomorpha, with an open, trochospiral protoconch, evolved larvae which secreted their typical larval shell. The Perunelomorpha may represent an ancestral group of the Caenogastropoda and Heterostropha.
   The uncoiled protoconchs found in Cyrtoneritimorpha, Euomphalomorpha and Perunelomorpha represent a very old shell feature. The higher gastropods (Caenogastropoda, Heterostropha, and Neritimorpha), as well as the extinct Euomphalomorpha, may have evolved from a common ancestor with an uncoiled tubular shell, and thus, not directly from the Paleozoic Archaeogastropoda and/or Amphigastropoda
Přispěvatel
    Česká geologická služba
Kód přispěvatele
    ČGS (UNM)
Zdrojový formát
    U
Datum vložení
    19. 2. 2008
Datum importu
    8. 8. 2012