Geochemical investigations of sediment profiles in the Norwegian-Greenland Sea
High-, i.e. 15-140-yr-resolution climate records from sediment cores 23071, 23074, and PS2644 from the Nordic Seas were used to recon:;truct changes in the surface and deep water circulation during marine isotope stages 1-5.1, i.e. the last 82 000 yr. From this the causal links between the paleocean...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2011
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.771756 https://doi.org/10.1594/PANGAEA.771756 |