Alan E. Brill

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Extreme global warmth and an abrupt negative carbon isotope excursion during the Paleocene–Eocene Thermal Maximum (PETM) have been attributed to a massive release of methane hydrate from sediments on the continental slope [ Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the indicate that the size of the(More)
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