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      Orbital climate forcing of δ13C excursions in the late Paleocene-early Eocene (chrons C24n-C25n) : ORBITAL FORCING OF CARBON ISOTOPES

      , , ,
      Paleoceanography
      American Geophysical Union (AGU)

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          Trends, rhythms, and aberrations in global climate 65 Ma to present.

          Since 65 million years ago (Ma), Earth's climate has undergone a significant and complex evolution, the finer details of which are now coming to light through investigations of deep-sea sediment cores. This evolution includes gradual trends of warming and cooling driven by tectonic processes on time scales of 10(5) to 10(7) years, rhythmic or periodic cycles driven by orbital processes with 10(4)- to 10(6)-year cyclicity, and rare rapid aberrant shifts and extreme climate transients with durations of 10(3) to 10(5) years. Here, recent progress in defining the evolution of global climate over the Cenozoic Era is reviewed. We focus primarily on the periodic and anomalous components of variability over the early portion of this era, as constrained by the latest generation of deep-sea isotope records. We also consider how this improved perspective has led to the recognition of previously unforeseen mechanisms for altering climate.
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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
                Paleoceanography
                Paleoceanography
                American Geophysical Union (AGU)
                08838305
                December 2003
                December 2003
                : 18
                : 4
                : n/a
                Article
                10.1029/2003PA000909
                85438ca9-932e-4bb9-a423-52102b091ee5
                © 2003

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

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