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      Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximum

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      Proceedings of the National Academy of Sciences
      Proceedings of the National Academy of Sciences

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          REVISED CARBONATE-WATER ISOTOPIC TEMPERATURE SCALE

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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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                Author and article information

                Journal
                Proceedings of the National Academy of Sciences
                Proceedings of the National Academy of Sciences
                Proceedings of the National Academy of Sciences
                0027-8424
                1091-6490
                October 01 2013
                September 16 2013
                : 110
                : 40
                : 15908-15913
                Article
                10.1073/pnas.1309188110
                056c45d3-bd03-493b-b904-938891a35a09
                © 2013
                History

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