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  5. An integrated multi-proxy study of cyclic pelagic deposits from the north-western Tethys: The Campanian of the Postalm section (Gosau Group, Austria)
 
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An integrated multi-proxy study of cyclic pelagic deposits from the north-western Tethys: The Campanian of the Postalm section (Gosau Group, Austria)

Author(s)
Wolfgring, Erik 
University of Vienna, Department of Geology, Althanstraße 14, 1090, Vienna, Austria 
Wagreich, Michael 
University of Vienna, Department of Geology, Althanstraße 14, 1090, Vienna, Austria 
Hohenegger, Johann 
University of Vienna, Department of Palaeontology, Althanstraße 14, 1090, Vienna, Austria 
Böhm, Katharina 
Vrije Universiteit Amsterdam, Department of Earth Sciences, the Netherlands 
Dinarès Turell, Jaume 
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia 
Gier, Susanne 
University of Vienna, Department of Geology, Althanstraße 14, 1090, Vienna, Austria 
Sames, Benjamin 
University of Vienna, Department of Geology, Althanstraße 14, 1090, Vienna, Austria 
Spötl, Christoph 
University of Innsbruck, Institute of Geology, Innrain 52, 6020, Innsbruck, Austria 
Jin, S. 
Chengdu University of Technology, College of Energy Resources, Chengdu, 610059, China 
Language
English
Obiettivo Specifico
1A. Geomagnetismo e Paleomagnetismo
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Title of the book
Cretaceous Research 
Issue/vol(year)
/120 (2021)
Publisher
Elsevier
Pages (printed)
104704
Issued date
2021
DOI
10.1016/j.cretres.2020.104704
URI
https://www.earth-prints.org/handle/2122/14212
Abstract
The Upper Cretaceous Postalm section in the Northern Calcareous Alps (Austria) exposes pelagic depositsof the northwestern Tethys whose cyclostratigraphy and palaeoenvironments were examined in thisstudy.The section displays rhythmic deposits of Santonian to late Campanian age (Gosau Group). The San-tonian/Campanian transition is characterised by condensed greyish carbonates, while the younger de-posits are composed of reddish foraminiferal packstones displaying distinct limestone-marl alternations.A biostratigraphic framework based on planktonic foraminifera and calcareous nannofossils is supportedby carbon and strontium isotope stratigraphy as well as magnetostratigraphy. The carbon isotope dataallow to correlate the Postalm section to other Tethyan reference sites and to identifyd13C events, such asthe Late Campanian Event. Spectral analyses of three independently assessed proxies (d13C, Fe contentand the thickness of limestone/marl couplets) in the upper, continuously exposed section part identified17 to 18 405 ka cycles spanning the mid to upper Campanian (Contusotruncana plummeraetoGansserinagansseriZones or CC21/UC15c to CC23a/UC16 nannofossil zones).
Type
article
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