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Middle Jurassic-Early Cretaceous high-latitude sea-surface temperatures from the Southern Ocean

Abstract:

Although a division of the Phanerozoic climatic modes of the Earth into "greenhouse" and "icehouse" phases is widely accepted, whether or not polar ice developed during the relatively warm Jurassic and Cretaceous Periods is still under debate. In particular, there is a range of isotopic and biotic evidence that favours the concept of discrete "cold snaps", marked particularly by migration of certain biota towards lower latitudes. Extension of the use of the palaeotemperature proxy TEX86<...>

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Publication status:
Published
Peer review status:
Reviewed (other)
Version:
Publisher's version

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Publisher copy:
10.5194/cpd-7-1339-2011

Authors


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Institution:
University of Oxford
Department:
Mathematical,Physical & Life Sciences Division - Earth Sciences
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Institution:
Royal Netherlands Institute for Sea Research (NIOZ)
Department:
Department of Marine Biogeochemistry and Toxicology
More by this author
Institution:
Royal Netherlands Institute for Sea Research (NIOZ)
Department:
Department of Marine Biogeochemistry and Toxicology
More by this author
Institution:
Royal Netherlands Institute for Sea Research (NIOZ)
Department:
Department of Marine Biogeochemistry and Toxicology
Publisher:
Copernicus Publications Publisher's website
Journal:
Climate of the Past Discussions Journal website
Volume:
7
Issue:
2
Pages:
1339-1361
Publication date:
2011-04-05
DOI:
EISSN:
1814-9359
URN:
uuid:c1e6b60a-3ab9-4985-819a-75370203342c
Local pid:
ora:5372

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