20.–25. Sept. 2026
Münster
Europe/Berlin Zeitzone

Palynological and palaeoecological changes within the Lubná group of coals, Bolsovian of the Kladno-Rakovník Basin, Czech Republic

22.09.2026, 09:30
15m
Auditorium F5 (Fürstenberghaus)

Auditorium F5

Fürstenberghaus

Talk Plant biodiversity dynamics through space and time Plant biodiversity dynamics through space and time

Sprecher

Jiří Bek (Institute of Geology of the Academy of Sciences of the Czech Republic, Prague, Czech Republic)

Beschreibung

Dispersed spore and pollen assemblages come from 134 boreholes drilled in the Kladno-Rakovník Basin, Czech Republic. The stratigraphic position of the Lubná group of coals, a member of the Radnice Formation, is Bolsovian (Moscovian). The assemblages consist of 167 species belonging to 53 genera. All three Lubná coal seams (Lower, Middle and Upper) represent different types of environment as documented by the palynological record. The oldest environment of the Lower Lubná group of coals is characterized by a raised ombrotrophic bog with dominance of Densosporites, spores produced by sub-arborescent lycopsids of the genus Omphalophloios. The Middle Lubná group of coals with prevalence of Lycospora, produced by the arborescent lycopsid Lepidodendron, is characteristic of a rheotrophic low-lying bog. The environment that formed the younger Upper Lubná group of coals was different, with a dominance of spores (smallest monoletes) from arborescent marattialeans. Palynology provides thus evidence of three distinct ecological environments that formed the three Lubná coal seams within ca 4 Myr (309 to 305 Myr).

Autor

Jiří Bek (Institute of Geology of the Academy of Sciences of the Czech Republic, Prague, Czech Republic)

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