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

      , , ,
      Paleoceanography
      American Geophysical Union (AGU)

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

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            Gas hydrates-geological perspective and global change

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              Evolution of Early Cenozoic marine temperatures

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                Author and article information

                Journal
                Paleoceanography
                Paleoceanography
                American Geophysical Union (AGU)
                08838305
                December 1995
                December 1995
                : 10
                : 6
                : 965-971
                Article
                10.1029/95PA02087
                ef72baa7-a5f1-4ca7-ac7b-e95efcda8f18
                © 1995

                http://doi.wiley.com/10.1002/tdm_license_1.1

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