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      Ocean overturning since the Late Cretaceous: Inferences from a new benthic foraminiferal isotope compilation : BENTHIC ISOTOPE COMPILATION

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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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              An analysis of the variation of ocean floor bathymetry and heat flow with age

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                Author and article information

                Journal
                Paleoceanography
                Paleoceanography
                American Geophysical Union (AGU)
                08838305
                December 2009
                December 2009
                December 23 2009
                : 24
                : 4
                Affiliations
                [1 ]Department of Geological Sciences; University of Oregon; Eugene Oregon USA
                [2 ]Geophysical Fluid Dynamics Laboratory; NOAA; Princeton New Jersey USA
                [3 ]Department of Earth and Planetary Sciences; Rutgers University; Piscataway New Jersey USA
                [4 ]Department of Earth and Environmental Sciences; Rensselaer Polytechnic Institute; Troy New York USA
                Article
                10.1029/2008PA001683
                6f53e1b8-8583-471c-9be8-f2ffa8b0c882
                © 2009
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