Palaeoceanographic variability in the South East Atlantic Ocean during periods of low orbital eccentricity
The Marine Isotope Stage (MIS) 11 interglacial has been considered to be analogous to the Holocene because of a similarity in the conditions of orbital forcing (low eccentricity and precession), but the role of climatic feedback processes linking orbital drivers to climate signatures is not well und...
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University College London (University of London)
2009
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.625191 |