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      Response of oceanic organisms to abiotic events in the Paleogene

      Oceanology
      Pleiades Publishing Ltd

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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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              Evolution of Cenozoic seaways in the circum-Antarctic region

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                Author and article information

                Journal
                Oceanology
                Oceanology
                Pleiades Publishing Ltd
                0001-4370
                1531-8508
                June 2009
                July 1 2009
                June 2009
                : 49
                : 3
                : 385-395
                Article
                10.1134/S0001437009030114
                38868d9d-7185-459a-9f39-b4796e8875a5
                © 2009

                http://www.springer.com/tdm

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