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      Site U1331: Expedition 320/321

      Expedition 320/321 Scientists

      Proceedings of the IODP

      Integrated Ocean Drilling Program

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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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            Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic

             S. C. Cande,  D. Kent (1995)
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              Heat flow from the Earth's interior: Analysis of the global data set

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                Author and article information

                Journal
                10.2204/iodp.proc.320321.2010
                Proceedings of the IODP
                Integrated Ocean Drilling Program
                1930-1014
                30 October 2010
                10.2204/iodp.proc.320321.103.2010

                This work is licensed under a Creative Commons Attribution 4.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

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                Self URI (journal page): http://publications.iodp.org/

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