Post-Lau Event (late Ludfordian, Silurian) recovery of conodont faunas of Bohemia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F12%3A00381838" target="_blank" >RIV/67985831:_____/12:00381838 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.3140/bull.geosci.1368" target="_blank" >http://dx.doi.org/10.3140/bull.geosci.1368</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3140/bull.geosci.1368" target="_blank" >10.3140/bull.geosci.1368</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Post-Lau Event (late Ludfordian, Silurian) recovery of conodont faunas of Bohemia

Popis výsledku v původním jazyce

The effects of the Lau Event on conodont faunas in shallow water environments of the Prague Synform were rather moderate in comparison with Gotland. The post-event restoration of conodont diversity following the characteristic post-siluricus faunas withdiminished elements and dominated by a long-ranging stock of Delotaxis was gradual and not abrupt. This points to absence of such large gaps in the sedimentation like they had occurred below and had caused the lack of a large upper part of the siluricusZone. Accordingly, the Bohemian conodont record of diversifying conodont faunas, starting with the entry of ?slender spathognathodontids, is comparably complete. Increased diversity and abundance of incoming conodont taxa has enabled a refinement of theregional zonal subdivision. This includes the succession of the plodowskii, latialatus, parasnajdri and crispa conodont biozones for the interval following the Lau Event in the late Ludfordian. The conodont data from Bohemia show that ?Oz

Název v anglickém jazyce

Post-Lau Event (late Ludfordian, Silurian) recovery of conodont faunas of Bohemia

Popis výsledku anglicky

The effects of the Lau Event on conodont faunas in shallow water environments of the Prague Synform were rather moderate in comparison with Gotland. The post-event restoration of conodont diversity following the characteristic post-siluricus faunas withdiminished elements and dominated by a long-ranging stock of Delotaxis was gradual and not abrupt. This points to absence of such large gaps in the sedimentation like they had occurred below and had caused the lack of a large upper part of the siluricusZone. Accordingly, the Bohemian conodont record of diversifying conodont faunas, starting with the entry of ?slender spathognathodontids, is comparably complete. Increased diversity and abundance of incoming conodont taxa has enabled a refinement of theregional zonal subdivision. This includes the succession of the plodowskii, latialatus, parasnajdri and crispa conodont biozones for the interval following the Lau Event in the late Ludfordian. The conodont data from Bohemia show that ?Oz

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F09%2F0703" target="_blank" >GA205/09/0703: Integrovaná stratigrafie mladšího siluru (ludlow-přídolí) v pražské synformě</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2012

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Bulletin of Geosciences

ISSN

1214-1119

e-ISSN

—

Svazek periodika

87

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

18

Strana od-do

815-832

Kód UT WoS článku

000311214100013

EID výsledku v databázi Scopus

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