The Paleocene-Eocene boundary in ODP Leg 208 sites
The Paleocene-Eocene thermal maximum (PETM) has been attributed to the rapid release of ~2000 * 10**9 metric tons of carbon in the form of methane. In theory, oxidation and ocean absorption of this carbon should have lowerd deep-sea pH, thereby triggering a rapid (<10,000-year) shoaling of the ca...
Main Authors: | , , , , , , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2005
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.772051 https://doi.org/10.1594/PANGAEA.772051 |