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      Dust, volcanic ash, and the evolution of the South Pacific Gyre through the Cenozoic : EVOLUTION OF THE SPG THROUGH CENOZOIC

      , , , , ,

      Paleoceanography

      Wiley-Blackwell

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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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            The chemical composition of subducting sediment and its consequences for the crust and mantle

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              Processes and patterns of oceanic nutrient limitation

               C Moore,  M. Mills,  K. Arrigo (2013)
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                Author and article information

                Journal
                Paleoceanography
                Paleoceanography
                Wiley-Blackwell
                08838305
                August 2015
                August 2015
                : 30
                : 8
                : 1078-1099
                Article
                10.1002/2015PA002829
                © 2015

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

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