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...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2014
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.840727 https://doi.org/10.1594/PANGAEA.840727 |