Increased export production during recovery from the Paleocene–Eocene thermal maximum constrained by sedimentary Ba isotopes
The Paleocene–Eocene thermal maximum (PETM; ∼56 Ma) was a transient global warming event associated with a huge perturbation to the global carbon cycle. Changes in marine biological productivity may have contributed to the rapid recovery from this climate change event, by driving the burial of inorg...
| Main Authors: | , , , |
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| Format: | Journal article |
| Published: |
Elsevier
2019
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