Transient temperature asymmetry between hemispheres in the Palaeogene Atlantic Ocean
Transient temperature asymmetry between hemispheres in the Palaeogene Atlantic Ocean
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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During the Late Palaeogene between ~40 and 23 million years ago (Ma), Earth transitioned from a warm non-glaciated climate state and developed large dynamic ice sheets on Antarctica. This transition is largely inferred from the deep-sea oxygen isotope record because records from independent temperature proxies are sparse. Here we present a 25-milli...
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Transient temperature asymmetry between hemispheres in the Palaeogene Atlantic Ocean
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TN_cdi_proquest_journals_2097996482
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2097996482
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ISSN
1752-0894
E-ISSN
1752-0908
DOI
10.1038/s41561-018-0182-9
