Paleobiological Characterization of the Karpatian Stage

Investor logo

Warning

This publication doesn't include Faculty of Economics and Administration. It includes Faculty of Science. Official publication website can be found on muni.cz.
Authors

RÖGL Fred BRZOBOHATÝ Rostislav CICHA Ivan ĆORIĆ Stjepan DAXNER-HÖCK Gudrun DOLÁKOVÁ Nela HARZHAUSER Mathias HLADILOVÁ Šárka KROL Andreas KVAČEK Zlatko MANDIC Oleg OLSHTYNSKA Alexandra PISERA Andrzej REICHENBACHER Bettina SCHULTZ Ortwin ŠVÁBENICKÁ Lilian TEMPFER Petra Maria VÁVRA Norbert ZORN Irene

Year of publication 2003
Type Chapter of a book
MU Faculty or unit

Faculty of Science

Citation
Description The marine biota is characterized during the Lower and Middle Karpatian by relatively cool water massses, widespread dysoxic bottom conditions, and extended deposition of calcareous shales ("Schlier") in the basins. In the Upper Karpatian a general shallowing and warm water influx is observed, as exemplified by the rich moluscan fauna. A strong Mediterranean marine influence existed. Palynomorphs, plant remains, and vertebrate fauna indicate a warm temperate to subtropical humid climate and high precipitation.
Related projects:

You are running an old browser version. We recommend updating your browser to its latest version.