Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximum
Author:
Publisher
Proceedings of the National Academy of Sciences
Subject
Multidisciplinary
Reference65 articles.
1. Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene
2. Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene
3. Rapid Acidification of the Ocean During the Paleocene-Eocene Thermal Maximum
4. Causes of the .DELTA.13C anomalies of carbonates and a new paradigm 'Gas-Hydrate Hypothesis'.
5. Uncorking the bottle: What triggered the Paleocene/Eocene thermal maximum methane release?
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