Lower cretaceous ammonite and dinocyst biostratigraphy and paleoenvironment of the silesian basin (Outer Western Carpathians)

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dc.contributor.authorSkupien, Petr
dc.contributor.authorVašíček, Zdeněk
dc.date.accessioned2006-11-03T10:29:37Z
dc.date.available2006-11-03T10:29:37Z
dc.date.issued2002
dc.description.abstractThe basinal, or Godula Sequence of the Silesian Unit of the Outer Western Carpathians incorporated in the present nappe structure is characterized by a considerable thickness of Lower Cretaceous dark-grey, prevailingly pelitic deposits. Barremian and Lower Aptian ammonites occur in several isolated fossiliferous beds. Non-calcareous dinoflagellate associations were analysed in the same beds to provide a correlation of both ammonite and dinoflagellate ranges. Where index ammonites are missing, associations of dinocysts become a key stratigraphic element in thick lithologically monotonous deposits. The composition of dinocysts also supports environmental and paleoclimatic reconstructions in the area studied.en
dc.identifier.citationGeologica Carpathica. 2002, vol. 53, no. 3, p. 179-189.en
dc.identifier.issn1335-0552
dc.identifier.issn1336-8052
dc.identifier.locationNení ve fondu ÚKen
dc.identifier.urihttp://hdl.handle.net/10084/57733
dc.identifier.wos000177836200005
dc.language.isoenen
dc.publisherVedaen
dc.relation.ispartofseriesGeologica Carpathicaen
dc.relation.urihttp://www.geologicacarpathica.sk/src/abstract.php?id=2002005300030179en
dc.subjectSilesian Uniten
dc.subjectLower Cretaceousen
dc.subjectBarremian-Aptianen
dc.subjectdinoflagellate cystsen
dc.subjectammonitesen
dc.subjectpaleoecologyen
dc.titleLower cretaceous ammonite and dinocyst biostratigraphy and paleoenvironment of the silesian basin (Outer Western Carpathians)en
dc.typearticleen

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