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      A 26 million year gap in the central Arctic record at the greenhouse-icehouse transition: Looking for clues : ∼26 MA GAP IN THE ARCTIC CENOZOIC RECORD

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          Most cited references29

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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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            Some remarks on the development of sedimentary basins

            D MCKENZIE (1978)
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              Distributional variations in marine crenarchaeotal membrane lipids: a new tool for reconstructing ancient sea water temperatures?

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                Author and article information

                Journal
                Paleoceanography
                Paleoceanography
                American Geophysical Union (AGU)
                08838305
                March 2008
                March 29 2008
                : 23
                : 1
                : n/a
                Article
                10.1029/2007PA001477
                97540ea9-e159-421f-87d9-e5d3c5188c71
                © 2008

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

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