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      Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

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          Long-Term Variations of Daily Insolation and Quaternary Climatic Changes

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            Plio-Pleistocene African climate.

            Marine records of African climate variability document a shift toward more arid conditions after 2.8 million years ago (Ma), evidently resulting from remote forcing by cold North Atlantic sea-surface temperatures associated with the onset of Northern Hemisphere glacial cycles. African climate before 2.8 Ma was regulated by low-latitude insolation forcing of monsoonal climate due to Earth orbital precession. Major steps in the evolution of African hominids and other vertebrates are coincident with shifts to more arid, open conditions near 2.8 Ma, 1.7 Ma, and 1.0 Ma, suggesting that some Pliocene (Plio)-Pleistocene speciation events may have been climatically mediated.
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              On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch Forcing

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                Author and article information

                Journal
                Nature
                Nature
                Springer Nature
                0028-0836
                1476-4687
                June 1999
                June 1999
                : 399
                : 6735
                : 429-436
                Article
                10.1038/20859
                a59f0195-c241-48dd-a8e8-009e87271a01
                © 1999

                http://www.springer.com/tdm

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