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      Carbon cycling and chronology of climate warming during the Palaeocene/Eocene transition

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      Nature
      Springer Nature

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          Long-Term Variations of Daily Insolation and Quaternary Climatic Changes

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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
                Nature
                Nature
                Springer Nature
                0028-0836
                October 21 1999
                October 21 1999
                : 401
                : 6755
                : 775-778
                Article
                10.1038/44545
                13565e2e-c7cb-4065-8065-5d7de903b05f
                © 1999
                History

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