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dc.contributor.authorVašíček, Zdeněk
dc.contributor.authorMichalík, Jozef
dc.date.accessioned2007-10-22T10:53:26Z
dc.date.available2007-10-22T10:53:26Z
dc.date.issued1995
dc.identifier.citationGeologica Carpathica. 1995, vol. 46, no. 5, p. 303-310.en
dc.identifier.issn1335-0552
dc.identifier.issn1336-8052
dc.identifier.urihttp://hdl.handle.net/10084/63808
dc.language.isoenen
dc.publisherSlovak Academic Pressen
dc.relation.ispartofseriesGeologica Carpathicaen
dc.relation.urihttp://www.geologicacarpathica.sk/src/abstract.php?id=1995004600050303en
dc.subjectWestern Carpathiansen
dc.subjectHauterivianen
dc.subjectaptychien
dc.titleThe last Lamellaptychi in the Hauterivian sequence of the Krizna Nappe, Central Western Carpathiansen
dc.typearticleen
dc.identifier.locationVe fondu ÚKen
dc.description.abstract-enThe topmost Hauterivian aptychi collection from the Pseudothurmannia Beds of the Mraznica Formation consists of three subspecies of Lamellaptychus angulocostatus (Peters) (L. a. angulocostatus, L. a. angulicostatus, L. a. radiatus), accompanied by rare L. filicostatus Stefanov. These forms represent the stratigraphically youngest lamellaptychi association at all. The decline of the lamellaptychi-bearing ammonites is interpreted as an effect of contemporaneous changes in both paleoceanographic (sea current system) and paleobiogeographic (”Urgonian” carbonate platform development) patterns, as well as in the composition of marine microplankton associations, traceable in the area studied.en
dc.identifier.wosA1995TL89100007


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