Polar front shift and atmospheric CO2 during the glacial maximum of the Early Paleozoic Icehouse

Our new data address the paradox of Late Ordovician glaciation under supposedly high pCO(2) (8 to 22x PAL: preindustrial atmospheric level). The paleobiogeographical distribution of chitinozoan ("mixed layer") marine zooplankton biotopes for the Hirnantian glacial maximum (440 Ma) are reco...

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Bibliographic Details
Published in:Proceedings of the National Academy of Sciences of the United States of America, Vol. 107, No. 34 (2010), p. 14983-6
Main Author: Vandenbroucke, Thijs R A
Other Involved Persons: Armstrong, Howard A ; Williams, Mark ; Paris, Florentin ; Zalasiewicz, Jan A ; Sabbe, Koen ; Nõlvak, Jaak ; Challands, Thomas J ; Verniers, Jacques ; Servais, Thomas
Format: electronic Article
Item Description:Date Completed 23.09.2010
Date Revised 13.11.2018
published: Print-Electronic
Citation Status MEDLINE
Copyright: From MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine
Physical Description:Online-Ressource
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