Life strategies of benthic, endobenthic and semibenthic fossil organisms of the Drahany Culm Basin (Lower Carboniferous sediments of the Myslejovice Formation, Moravosilesian Unit of the Bohemian Massif)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F15%3A33156741" target="_blank" >RIV/61989592:15310/15:33156741 - 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

Life strategies of benthic, endobenthic and semibenthic fossil organisms of the Drahany Culm Basin (Lower Carboniferous sediments of the Myslejovice Formation, Moravosilesian Unit of the Bohemian Massif)

Popis výsledku v původním jazyce

The Myslejovice Formation is one of the lithostratigraphical units in the Lower Carboniferous sequences of Drahany Culm basin which belongs to the large area of Rhenohercynian Zone of the Variscan orogenetic flysch belt. In the Moravosilesian Unit are developed two main basins, the Nízký Jeseník Mts. basin and the Drahany Upland culm basin. The flysch deposits were formed in the synorogenetic succession in the interval of Lower Viséan - Lower Namurian from siliciclastic turbidit fills of Variscan flysch(Culmian facies) in the remnant and foreland basins (Bábek et al. 2006). From the oldest (Lower Viséan) to the youngest are sediments in the Drahany Culm basin filled by Protivanov, Rozstání and Myslejovice Formation (Late Viséan, Go? to Go? zone). Forthe paleoenvironmental analysis were used especially species of bivalves and trace fossils also due to their stratigraphic and environmental importance. Most of fossil bivalves from the Myslejovice Formation were filter feeders, suspensio

Název v anglickém jazyce

Life strategies of benthic, endobenthic and semibenthic fossil organisms of the Drahany Culm Basin (Lower Carboniferous sediments of the Myslejovice Formation, Moravosilesian Unit of the Bohemian Massif)

Popis výsledku anglicky

The Myslejovice Formation is one of the lithostratigraphical units in the Lower Carboniferous sequences of Drahany Culm basin which belongs to the large area of Rhenohercynian Zone of the Variscan orogenetic flysch belt. In the Moravosilesian Unit are developed two main basins, the Nízký Jeseník Mts. basin and the Drahany Upland culm basin. The flysch deposits were formed in the synorogenetic succession in the interval of Lower Viséan - Lower Namurian from siliciclastic turbidit fills of Variscan flysch(Culmian facies) in the remnant and foreland basins (Bábek et al. 2006). From the oldest (Lower Viséan) to the youngest are sediments in the Drahany Culm basin filled by Protivanov, Rozstání and Myslejovice Formation (Late Viséan, Go? to Go? zone). Forthe paleoenvironmental analysis were used especially species of bivalves and trace fossils also due to their stratigraphic and environmental importance. Most of fossil bivalves from the Myslejovice Formation were filter feeders, suspensio

Druh

D - Stať ve sborníku

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název statě ve sborníku

16th Czech-Slovak-Polish Palaeontological Conference and 10th Polish Micropalaeontological Workshop. Abstracts Book and Excursion Guide

ISBN

978-83-941956-0-1

ISSN

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e-ISSN

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Počet stran výsledku

3

Strana od-do

50-52

Název nakladatele

Grzybowski Foundation &amp; Micropress Europe

Místo vydání

Krakov

Místo konání akce

Olomouc

Datum konání akce

10. 9. 2015

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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