CO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilization
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/38/10/875/3537085/875.pdf
Reference30 articles.
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3. Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary?;Bice;Paleoceanography,2002
4. Modelling the global carbon cycle with a gas hydrate capacitor: Significance for the latest Paleocene thermal maximum;Dickens,2001
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