Blog
About

  • Record: found
  • Abstract: not found
  • Article: not found

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

Read this article at

ScienceOpenPublisher
Bookmark
      There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

      Abstract

      Related collections

      Most cited references 35

      • Record: found
      • Abstract: not found
      • Article: not found

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

       J P Kennett,  L. Stott (1991)
        Bookmark
        • Record: found
        • Abstract: not found
        • Article: not found

        Tertiary oxygen isotope synthesis, sea level history, and continental margin erosion

          Bookmark
          • Record: found
          • Abstract: not found
          • Article: not found

          Evolution of Early Cenozoic marine temperatures

            Bookmark

            Author and article information

            Journal
            Paleoceanography
            Paleoceanography
            American Geophysical Union (AGU)
            08838305
            December 1995
            December 1995
            : 10
            : 6
            : 965-971
            10.1029/95PA02087
            © 1995

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

            Product
            Self URI (article page): http://doi.wiley.com/10.1029/95PA02087

            Comments

            Comment on this article