Isotope ratios, IRD and planktonic foraminifera content during marine isotope stage 5 of sediment cores MD99-2303, MD99-2304 and MD95-2010

Variable climatic and oceanographic conditions characterized the last interglacial at high northern latitudes, probably related to changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC). The magnitudes of these changes are comparable to the Holocene variability, and were t...

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Bibliographic Details
Main Authors: Risebrobakken, Bjørg, Dokken, Trond, Jansen, Eystein
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.840727
https://doi.org/10.1594/PANGAEA.840727