Palaeomagnetic, astrochronological, and environmental magnetic perspective on Oligocene-Miocene climate, using drift sediments from the northwest Atlantic Ocean
The Antarctic ice sheet oscillated between nearly deglaciated and near-modern proportions, sometimes within ~110 kyr, during transient glacial phases of the Oligocene-Miocene icehouse world (5.33-33.9 Ma). Ice sheet hysteresis is closely coupled with carbon-cycle feedback mechanisms that are strongl...
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University of Southampton
2017
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.729767 |