| dc.contributor.author | Michalík, Jozef | |
| dc.contributor.author | Reháková, Daniela | |
| dc.contributor.author | Lintnerová, Otília | |
| dc.contributor.author | Boorová, Daniela | |
| dc.contributor.author | Halásová, Eva | |
| dc.contributor.author | Kotulová, Júlia | |
| dc.contributor.author | Soták, Ján | |
| dc.contributor.author | Peterčáková, Mária | |
| dc.contributor.author | Hladíková, Jana | |
| dc.contributor.author | Skupien, Petr | |
| dc.date.accessioned | 2007-08-13T13:21:53Z | |
| dc.date.available | 2007-08-13T13:21:53Z | |
| dc.date.issued | 1999 | |
| dc.identifier.citation | Geologica Carpathica. 1999, vol. 50, no. 2, p. 169-191. | en |
| dc.identifier.issn | 1335-0552 | |
| dc.identifier.issn | 1336-8052 | |
| dc.identifier.uri | http://hdl.handle.net/10084/61785 | |
| dc.language.iso | en | en |
| dc.publisher | Slovak Academic Press | en |
| dc.relation.ispartofseries | Geologica Carpathica | en |
| dc.relation.uri | http://www.geologicacarpathica.sk/src/abstract.php?id=1999005000020169 | en |
| dc.subject | Lower Cretaceous | en |
| dc.subject | Western Carpathians | en |
| dc.subject | Slovakia | en |
| dc.subject | lithology | en |
| dc.subject | stratigraphy | en |
| dc.subject | bioevents | en |
| dc.subject | anoxic sediments | en |
| dc.subject | C-isotopes | en |
| dc.title | Sedimentary, biological and isotopic record of early Aptian paleoclimatic event in the Pieniny Klippen Belt, Slovak Western Carpathians | en |
| dc.type | article | en |
| dc.identifier.location | Ve fondu ÚK | en |
| dc.description.abstract-en | Orbital perturbations of Barremian/Aptian climate traceable by sedimentological, biological and chemical proxies have been studied in Mt. Rochovica (Western Carpathians, Pieniny Klippen Belt) sedimentary sequence. This pelagic carbonate sequence represents a record of sedimentation on a distal edge of the Paleoeuropean shelf. Pelagic carbonate deposition was influenced by clastic input from the elevated Czorsztyn Ridge (microbreccia of Tithonian/Berriasian limestones) and by fluxoturbidites derived from unknown carbonate buildups. Interruption of carbonate deposition by the terrigeneous Konhora Formation has been interpreted as a consequence of a humid event in the initial stage of the mid-Cretaceous Greenhouse climate. Three anoxia models (depositional, productivity and stagnant one) have been distinguished in the depositionary regime. | en |
| dc.identifier.wos | 000080994400006 | |