Cold spells in the Nordic Seas during the early Eocene Greenhouse
Madeleine L. Vickers (),
Sabine K. Lengger,
Stefano M. Bernasconi,
Nicolas Thibault,
Bo Pagh Schultz,
Alvaro Fernandez,
Clemens V. Ullmann,
Paul McCormack,
Christian J. Bjerrum,
Jan Audun Rasmussen,
Iben Winther Hougård and
Christoph Korte
Additional contact information
Madeleine L. Vickers: IGN, University of Copenhagen
Sabine K. Lengger: Plymouth University
Stefano M. Bernasconi: ETH Zurich, Geologisches Institut
Nicolas Thibault: IGN, University of Copenhagen
Bo Pagh Schultz: Museum Salling, Fur Museum
Alvaro Fernandez: University of Bergen
Clemens V. Ullmann: University of Exeter, Penryn Campus
Paul McCormack: Plymouth University
Christian J. Bjerrum: IGN, University of Copenhagen
Jan Audun Rasmussen: Museum Mors, Fossil- and Mo-clay Museum
Iben Winther Hougård: IGN, University of Copenhagen
Christoph Korte: IGN, University of Copenhagen
Nature Communications, 2020, vol. 11, issue 1, 1-12
Abstract:
Abstract The early Eocene (c. 56 - 48 million years ago) experienced some of the highest global temperatures in Earth’s history since the Mesozoic, with no polar ice. Reports of contradictory ice-rafted erratics and cold water glendonites in the higher latitudes have been largely dismissed due to ambiguity of the significance of these purported cold-climate indicators. Here we apply clumped isotope paleothermometry to a traditionally qualitative abiotic proxy, glendonite calcite, to generate quantitative temperature estimates for northern mid-latitude bottom waters. Our data show that the glendonites of the Danish Basin formed in waters below 5 °C, at water depths of
Date: 2020
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:11:y:2020:i:1:d:10.1038_s41467-020-18558-7
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DOI: 10.1038/s41467-020-18558-7
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