Constraints on ocean circulation at the Paleocene–Eocene Thermal Maximum from neodymium isotopes
Global warming during the Paleocene–Eocene Thermal Maximum (PETM) ∼ 55 million years ago (Ma) coincided with a massive release of carbon to the ocean–atmosphere system, as indicated by carbon isotopic data. Previous studies have argued for a role of changing ocean circulation, possibly as a trigge...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2016-04-01
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| Series: | Climate of the Past |
| Online Access: | http://www.clim-past.net/12/837/2016/cp-12-837-2016.pdf |