The middle Eocene climate transition : insights from foraminiferal and sedimentary records
New seawater oxygen isotope reconstructions support the presence of a dynamic cryosphere since the early Middle Eocene with significant ice storage in both hemispheres. The onset of early Cenozoic glaciation is hypothesised to be intimately linked with levels of atmospheric <i>p</i>CO<...
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University of Cambridge
2009
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.598412 |