Detailed Information on Publication Record
2003
Paleobiological Characterization of the Karpatian Stage
RÖGL, Fred, Rostislav BRZOBOHATÝ, Ivan CICHA, Stjepan ĆORIĆ, Gudrun DAXNER-HÖCK et. al.Basic information
Original name
Paleobiological Characterization of the Karpatian Stage
Authors
RÖGL, Fred (40 Austria), Rostislav BRZOBOHATÝ (203 Czech Republic, guarantor), Ivan CICHA (203 Czech Republic), Stjepan ĆORIĆ (70 Bosnia and Herzegovina), Gudrun DAXNER-HÖCK (40 Austria), Nela DOLÁKOVÁ (203 Czech Republic), Mathias HARZHAUSER (40 Austria), Šárka HLADILOVÁ (203 Czech Republic), Andreas KROL (40 Austria), Zlatko KVAČEK (203 Czech Republic), Oleg MANDIC (191 Croatia), Alexandra OLSHTYNSKA (804 Ukraine), Andrzej PISERA (616 Poland), Bettina REICHENBACHER (276 Germany), Ortwin SCHULTZ (40 Austria), Lilian ŠVÁBENICKÁ (203 Czech Republic), Petra Maria TEMPFER (40 Austria), Norbert VÁVRA (40 Austria) and Irene ZORN (40 Austria)
Edition
Brno, Brzobohatý R., Cicha I., Kováč M., Rögl F. (eds): The Karpatian - a Lower Miocene Stage of the Central Paratethys, p. 357-360, 4 pp. 55-966B-203-02/58-22/Př, 2003
Publisher
Masarykova Univerzita v Brně
Other information
Language
English
Type of outcome
Kapitola resp. kapitoly v odborné knize
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Czech Republic
Confidentiality degree
není předmětem státního či obchodního tajemství
RIV identification code
RIV/00216224:14310/03:00008688
Organization unit
Faculty of Science
ISBN
80-210-3266-9
Keywords in English
Paleobiological characterization; calcareous nannoplankton; diatoms; forams; molluscs; ostracods; fishes; amphibians and reptiles; mammals; macroflora; palynology; Karpatian; Central Paratethys
Tags
Změněno: 30/5/2004 10:37, prof. RNDr. Rostislav Brzobohatý, CSc.
Abstract
V originále
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.
Links
GA205/01/0085, research and development project |
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