Number of the records: 1  

Uppermost Ordovician (upper Katian-Hirnantian) graptolites of north-central Nevada, U.S.A

  1. 1.
    SYSNO ASEP0361335
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleUppermost Ordovician (upper Katian-Hirnantian) graptolites of north-central Nevada, U.S.A
    Author(s) Štorch, Petr (GLU-S) RID, SAI, ORCID
    Mitchell, Ch. E. (US)
    Finney, S. C. (US)
    Melchin, M. J. (CA)
    Source TitleBulletin of Geosciences. - : Česká geografická společnost - ISSN 1214-1119
    Roč. 86, č. 2 (2011), s. 301-386
    Number of pages86 s.
    Publication formWWW - WWW
    Languageeng - English
    CountryCZ - Czech Republic
    KeywordsOrdovician ; graptolites ; mass extinction ; biostratigraphy
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsIAA301110908 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000291926200009
    EID SCOPUS79959732311
    DOI10.3140/bull.geosci.1264
    AnnotationRich graptolite fauna described from Katian and Hirnantian of central Nevada suggests that graptolite diversity decreased abruptly at the beginning of Hirnantian glaciation. Faunal turnover reached a peak in the lower part of the extraordinarius Biozone. Ordovician clades were rapidly replaced by normalograptids, presumably evolved in, and invading from, less-temperate higher latitude settings where overall graptolite diversity was extremely low already in pre-glacial times and the old fauna entirely vanished with ongoing glaciation. In tropics, however, elements of the old fauna locally survived and emerged from hypothetical refugia in the upper part of the extraordinarius Zone and, second times, in the persculptus Biozone. The last phase of mass extinction of the long-dominant Ordovician clades took place during postglacial transgression, along with major radiation among normalogratids. Reasons for ultimate extinction of the former fauna may be biological rather than environmental.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2012
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.