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      Changes in the depth habitat of the Oligocene planktic foraminifera (Dentoglobigerina venezuelana) induced by thermocline deepening in the eastern equatorial Pacific : Depth Habitat ofD. Venezuelana

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      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 distribution of 13C of ΣCO2 in the world oceans

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              Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin

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                Author and article information

                Journal
                Paleoceanography
                Paleoceanography
                Wiley-Blackwell
                08838305
                June 2016
                June 15 2016
                : 31
                : 6
                : 715-731
                Article
                10.1002/2016PA002950
                ef8d0ff2-61f0-433c-94a0-7548c9b60a38
                © 2016

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

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