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 con...
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Imperial College London
2014
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.695505 |