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      The Paleocene–Eocene transition at Mead Stream, New Zealand: a southern Pacific record of early Cenozoic global change

      , , , ,
      Palaeogeography, Palaeoclimatology, Palaeoecology
      Elsevier BV

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

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              Interpreting carbon-isotope excursions: carbonates and organic matter

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                Author and article information

                Journal
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Elsevier BV
                00310182
                January 2005
                January 2005
                : 215
                : 3-4
                : 313-343
                Article
                10.1016/j.palaeo.2004.09.011
                14d29cd6-5b46-43ec-916e-fd04ffacf180
                © 2005

                http://www.elsevier.com/tdm/userlicense/1.0/

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