Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition
Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition
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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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Local climate goes global
The Eocene–Oligocene transition, about 33.5 million years ago, was a major global climate event. The end of the Eocene was unusually warm with no significant ice on Antarctica but the Oligocene saw the arrival of a permanent Antarctic ice-sheet. Two papers this week relate to the continental effects of this global chang...
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Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition
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TN_cdi_proquest_miscellaneous_68991152
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_68991152
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0028-0836
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1476-4687,1476-4679
DOI
10.1038/nature05516