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Testing the impact of diagenesis on theδ18O andδ13C of benthic foraminiferal calcite from a sediment burial depth transect in the equatorial Pacific : DIAGENESIS IN BENTHIC FORAMINIFERA

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Paleoceanography

Wiley-Blackwell

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      The operated Markov´s chains in economy (discrete chains of Markov with the income)

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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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          Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates

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            Author and article information

            Journal
            Paleoceanography
            Paleoceanography
            Wiley-Blackwell
            08838305
            September 2013
            September 2013
            : 28
            : 3
            : 468-480
            10.1002/palo.20045
            © 2013

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

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