An abyssal carbonate compensation depth overshoot in the aftermath of the Paleocene-Eocene Thermal Maximum
During the Paleocene-Eocene Thermal Maximum (PETM) about 56 million years ago, thousands of petagrams of carbon were released into the atmosphere and ocean in just a few thousand years, followed by a gradual sequestration over approximately 200,000 years. If silicate weathering is one of the key neg...
| Main Authors: | , , , , , , , , , , , |
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| Format: | Journal article |
| Published: |
Nature Publishing Group
2016
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