0145452 - GLU-S 20023078 RIV SK eng J - Článek v odborném periodiku
Mikuláš, Radek - Lehotský, T. - Bábek, O.
Lower Carboniferous ichnofabric of the Culm facies: A case study of the Moravice formation (Moravia and Silesia, Czech Republic).
Geologica Carpathica. Roč. 53, č. 3 (2002), s. 141-148. ISSN 1335-0552. E-ISSN 1336-8052
Grant CEP: GA ČR GA205/00/0118
Výzkumný záměr: CEZ:AV0Z3013912
Klíčová slova: Carboniferous * turbidites * paleoenvironment
Kód oboru RIV: DB - Geologie a mineralogie
Impakt faktor: 0.147, rok: 2002
Web výsledku:
http://www.geologicacarpathica.sk/src/main.php http://arl-repository.lib.cas.cz/uloziste_av/GLU-S/cav_un_epca-0145452_01.pdf

Overall bioturbation of sediments of the Culm facies is much lower compared to the Mesozoic and Cenozoic flysch facies. Totally reworked intervals (up to 1 cm thick) occur locally at the tops of turbiditic beds. Compared to the Mesozoic and Cenozoic flysch (i.e. Rhenodanubian or Carpathian flysches), the Culm facies appears to have formed in less oxygenated settings possibly with shorter and unequally distributed colonization windows. This explains the prevalence of traces with complex feeding strategies comprising chemosymbiosis and gardening (Chondrites, Dictyodora). Their effect on the integrity of sediment (i.E. the amount of transported material) was weak.
Trvalý link: http://hdl.handle.net/11104/0043052