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      Stable carbon and oxygen isotope study on benthic foraminifera: Implication for microhabitat preferences and interspecies correlation

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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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            REVISED CARBONATE-WATER ISOTOPIC TEMPERATURE SCALE

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              Pleistocene Temperatures

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                Author and article information

                Contributors
                (View ORCID Profile)
                Journal
                Journal of Earth System Science
                J Earth Syst Sci
                Springer Science and Business Media LLC
                0253-4126
                0973-774X
                July 2017
                July 24 2017
                July 2017
                : 126
                : 5
                Article
                10.1007/s12040-017-0840-0
                fa4c55b8-2f20-4e93-b9d3-788189f0de4c
                © 2017

                http://www.springer.com/tdm

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