From jungle to ice: the role of changes in weathering and ocean circulation patterns in the onset of Antarctic glaciation
The transition from the Greenhouse Eocene climate (55 – 34Ma) to the Icehouse regime of the Oligocene (34 – 23Ma) was marked by a widespread cooling at the Eocene-Oligocene Transition (EOT) (~34Ma), followed by major Antarctic glaciation. The relative contribution of changes in ocean circulation and...
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Imperial College London
2014
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| Online Access: | https://dx.doi.org/10.25560/42228 http://spiral.imperial.ac.uk/handle/10044/1/42228 |