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Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition

Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_68991152

Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition

About this item

Full title

Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition

Publisher

London: Nature Publishing Group UK

Journal title

Nature, 2007-02, Vol.445 (7128), p.635-638

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

Contents

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...

Alternative Titles

Full title

Tibetan plateau aridification linked to global cooling at the Eocene–Oligocene transition

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_68991152

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_68991152

Other Identifiers

ISSN

0028-0836

E-ISSN

1476-4687,1476-4679

DOI

10.1038/nature05516

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