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Orbitally-paced climate evolution during the middle Miocene “Monterey” carbon-isotope excursion

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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 use of fast Fourier transform for the estimation of power spectra: A method based on time averaging over short, modified periodograms

         Ryan Welch (1967)
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          Macintosh Program performs time-series analysis

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            Author and article information

            Journal
            Earth and Planetary Science Letters
            Earth and Planetary Science Letters
            Elsevier BV
            0012821X
            September 2007
            September 2007
            : 261
            : 3-4
            : 534-550
            10.1016/j.epsl.2007.07.026
            © 2007

            http://www.elsevier.com/tdm/userlicense/1.0/

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