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      Release of methane from a volcanic basin as a mechanism for initial Eocene global warming

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          Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene

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            Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene

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              Large igneous provinces and mass extinctions

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                Author and article information

                Journal
                Nature
                Nature
                Springer Nature
                0028-0836
                1476-4679
                June 3 2004
                June 3 2004
                : 429
                : 6991
                : 542-545
                Article
                10.1038/nature02566
                15175747
                b029289c-afc2-48b1-be59-9f3d70f51f39
                © 2004
                History

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