Late Moscovian terrestrial biotas and palaeoenvironments of Variscan Euramerica

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F09%3A00000521" target="_blank" >RIV/00025798:_____/09:00000521 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985831:_____/09:00356689 RIV/00228745:_____/09:00000006 RIV/00216208:11310/09:10118647

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Late Moscovian terrestrial biotas and palaeoenvironments of Variscan Euramerica

Popis výsledku v původním jazyce

A synthesis of the upper Moscovian sedimentological and palaeontological record of terrestrial habitats across the Variscan foreland suggests a contraction and westward shift of the coal swamps. These changes can be correlated with pulses of tectonic activity resulting from the northwards migration of the Variscan Front. This tectonic activity caused drainage patterns where the coal swamps were growing and replacement of swampy arborescent lycopsids by vegetation dominated by marattialean ferns. Reductions in rainfall further affected the swamp vegetation. In Asturian times, the swamps in Variscan Euramerica became replaced by predominantly conifer and cordaite vegetation that favoured much drier substrates. The last development of coal swamps in Variscan foreland was of early Cantabrian age. In the USA, lycopsid-dominated coal swamps persisted for a little longer and disappeared by middle-late Cantabrian times.

Název v anglickém jazyce

Late Moscovian terrestrial biotas and palaeoenvironments of Variscan Euramerica

Popis výsledku anglicky

A synthesis of the upper Moscovian sedimentological and palaeontological record of terrestrial habitats across the Variscan foreland suggests a contraction and westward shift of the coal swamps. These changes can be correlated with pulses of tectonic activity resulting from the northwards migration of the Variscan Front. This tectonic activity caused drainage patterns where the coal swamps were growing and replacement of swampy arborescent lycopsids by vegetation dominated by marattialean ferns. Reductions in rainfall further affected the swamp vegetation. In Asturian times, the swamps in Variscan Euramerica became replaced by predominantly conifer and cordaite vegetation that favoured much drier substrates. The last development of coal swamps in Variscan foreland was of early Cantabrian age. In the USA, lycopsid-dominated coal swamps persisted for a little longer and disappeared by middle-late Cantabrian times.

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%2F05%2F2034" target="_blank" >GA205/05/2034: Medullosní pteridospermy a kordaity z permokarbonu Českého masívu (Studium kutikul a fertilních orgánů)</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2009

Kód důvěrnosti údajů

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

Název periodika

Netherlands Journal of Geosciences - Geologie en Mijnbouw

ISSN

0016-7746

e-ISSN

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Svazek periodika

88

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

98

Strana od-do

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Kód UT WoS článku

000280716000001

EID výsledku v databázi Scopus

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