Paleoceanographic data from ODP Site 986 and core M23071 (GIK23071-3)
The Last Interglacial in the Arctic region is often described as a time with warmer conditions and significantly less summer sea ice than today. The role of Atlantic water (AW) as the main oceanic heat flux agent into the Arctic Ocean remains, however, unclear. Using high-resolution stable isotope a...
Main Authors: | , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2017
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.883805 https://doi.org/10.1594/PANGAEA.883805 |