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      Late Lutetian Thermal Maximum-Crossing a Thermal Threshold in Earth's Climate System?

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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 long-term numerical solution for the insolation quantities of the Earth

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              An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics.

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                Author and article information

                Journal
                Geochemistry, Geophysics, Geosystems
                Geochem. Geophys. Geosyst.
                Wiley
                15252027
                January 2018
                January 2018
                January 12 2018
                : 19
                : 1
                : 73-82
                Affiliations
                [1 ]MARUM - Center for Marine Environmental Sciences; University of Bremen; Bremen Germany
                [2 ]Faculty of Geosciences; University of Bremen; Bremen Germany
                [3 ]Ocean and Earth Science; University of Southampton, Waterfront Campus, National Oceanography Centre; Southampton UK
                [4 ]Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences; University of Cambridge; Cambridge UK
                [5 ]Astronomie et Systèmes Dynamiques, IMCCE-CNRS UMR8028, Observatoire de Paris; UPMC; Paris France
                [6 ]School of Ocean and Earth Science and Technology; University of Hawai'i at Manoa; Honolulu HI USA
                Article
                10.1002/2017GC007240
                239d3e89-44d7-4ddd-b048-8553c348036c
                © 2018

                http://doi.wiley.com/10.1002/tdm_license_1.1

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