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      Reduced continental weathering and marine calcification linked to late Neogene decline in atmospheric CO2

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      Nature Geoscience
      Springer Science and Business Media LLC

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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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            A negative feedback mechanism for the long-term stabilization of Earth's surface temperature

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              The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years

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                Author and article information

                Journal
                Nature Geoscience
                Nat. Geosci.
                Springer Science and Business Media LLC
                1752-0894
                1752-0908
                September 23 2019
                Article
                10.1038/s41561-019-0450-3
                ea9d02b8-2b27-4ba1-9f32-e4f8bed6df32
                © 2019

                http://www.springer.com/tdm

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