Onset of long-term cooling of Greenland near the Eocene-Oligocene boundary as revealed by branched tetraether lipids

The Eocene-Oligocene (E-O) boundary interval is considered to be one of the major transitions in Earth's climate, witnessing the first major expansion of the East Antarctic Ice Sheet. However, the extent of the associated climatic cooling, especially for high northern latitude continental landm...

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Bibliographic Details
Published in:Geology
Main Authors: Schouten, S., Eldrett, J., Greenwood, D.R., Harding, I., Baas, M., Sinninghe Damste, J.S.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2008
Subjects:
Online Access:https://eprints.soton.ac.uk/50254/