Late Moscovian terrestrial biotas and palaeoenvironments of Variscan Euramerica

Cleal, C. J.; Opluštil, S.; Thomas, B. A.; Tenchov, Y.; Abbink, O. A.; Bek, Jiří; Dimitrova, T.; Drábková, J.; Hartkopf-Fröder, Ch.; van Hoof, T.; Kedzior, A.; Jarzembowski, E.; Jasper, K.; Libertín, M.; McLean, D.; Oliwkiewicz-Miklasinska, M.; Pšenička, J.; Ptak, B.; Schneider, J. W.; Schultka, S.; Šimůnek, Z.; Uhl, D.; Waksmundzka, M. I.; van Waveren, I.; Zodrow, E. L.

Počet záznamů: 1

Late Moscovian terrestrial biotas and palaeoenvironments of Variscan Euramerica

1.

SYSNO ASEP	0356689
Druh ASEP	J - Článek v odborném periodiku
Zařazení RIV	J - Článek v odborném periodiku
Poddruh J	Článek ve WOS
Název	Late Moscovian terrestrial biotas and palaeoenvironments of Variscan Euramerica
Tvůrce(i)	Cleal, C. J. (GB) Opluštil, S. (CZ) Thomas, B. A. (GB) Tenchov, Y. (BG) Abbink, O. A. (NL) Bek, Jiří (GLU-S)_{RID, SAI, ORCID} Dimitrova, T. (BG) Drábková, J. (CZ) Hartkopf-Fröder, Ch. (DE) van Hoof, T. (NL) Kedzior, A. (PL) Jarzembowski, E. (GB) Jasper, K. (DE) Libertín, M. (CZ) McLean, D. (GB) Oliwkiewicz-Miklasinska, M. (PL) Pšenička, J. (CZ) Ptak, B. (PL) Schneider, J. W. (DE) Schultka, S. (DE) Šimůnek, Z. (CZ) Uhl, D. (DE) Waksmundzka, M. I. (PL) van Waveren, I. (NL) Zodrow, E. L. (CA)
Zdroj.dok.	Netherlands Journal of Geosciences-Geologie en Mijnbouw - ISSN 0016-7746 Roč. 88, č. 4 (2009), s. 181-278
Poč.str.	98 s.
Jazyk dok.	eng - angličtina
Země vyd.	NL - Nizozemsko
Klíč. slova	Pennsylvanian Subsystem ; climates ; vegetation ; faunas ; sedimentology
Vědní obor RIV	DB - Geologie a mineralogie
CEZ	AV0Z30130516 - GLU-S (2005-2011)
UT WOS	000280716000001
EID SCOPUS	77954988269
Anotace	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.
Pracoviště	Geologický ústav
Kontakt	Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
Rok sběru	2011

Počet záznamů: 1