The Annulata events in the Moravian Karst (Famennian, Czech Republic) - remarks on stratigraphy

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F14%3A00073907" target="_blank" >RIV/00216224:14310/14:00073907 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

The Annulata events in the Moravian Karst (Famennian, Czech Republic) - remarks on stratigraphy

Popis výsledku v původním jazyce

The mid-Fammenian Annulata events are supposed to be connected with an episodic sea level rise, which interrupt the global trends of climatic cooling during the Famennian (Sandberg et al. 2002). The fauna of the Annulata events from the Moravian Karst was discovered for the first time during the late 19th century and later described by Rzehak (1910) from the vicinity of Ochoz u Brna. The event beds were later recorded by Dvořák et al. (1988) from the western Mokrá quarry near Brno. The current investigation is focused on four sections near Ochoz, Hostěnice and Mokrá villages in the southern part of the Moravian Karst. These successions of the Křtiny Limestones of the Líšeň Formation are considerably condensed. According to the presence of Palmatolepisglabra lepta, Palmatolepis minuta minuta and Palmatolepis rugosa trachytera, the event bed near Ochoz might be correlated with the Lower Annulata event.

Název v anglickém jazyce

The Annulata events in the Moravian Karst (Famennian, Czech Republic) - remarks on stratigraphy

Popis výsledku anglicky

The mid-Fammenian Annulata events are supposed to be connected with an episodic sea level rise, which interrupt the global trends of climatic cooling during the Famennian (Sandberg et al. 2002). The fauna of the Annulata events from the Moravian Karst was discovered for the first time during the late 19th century and later described by Rzehak (1910) from the vicinity of Ochoz u Brna. The event beds were later recorded by Dvořák et al. (1988) from the western Mokrá quarry near Brno. The current investigation is focused on four sections near Ochoz, Hostěnice and Mokrá villages in the southern part of the Moravian Karst. These successions of the Křtiny Limestones of the Líšeň Formation are considerably condensed. According to the presence of Palmatolepisglabra lepta, Palmatolepis minuta minuta and Palmatolepis rugosa trachytera, the event bed near Ochoz might be correlated with the Lower Annulata event.

Druh

O - Ostatní výsledky

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GA14-18183S" target="_blank" >GA14-18183S: Sekvenční stratigrafie devonských bioeventů - výkyvy mořské hladiny na přechodu od klimatického režimu greenhouse k icehouse</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2014

Kód důvěrnosti údajů

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