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      The chacma baboon (Papio ursinus) through time: a model of potential core habitat regions during a glacial–interglacial cycle

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          Very high resolution interpolated climate surfaces for global land areas

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            The Last Glacial Maximum.

            We used 5704 14C, 10Be, and 3He ages that span the interval from 10,000 to 50,000 years ago (10 to 50 ka) to constrain the timing of the Last Glacial Maximum (LGM) in terms of global ice-sheet and mountain-glacier extent. Growth of the ice sheets to their maximum positions occurred between 33.0 and 26.5 ka in response to climate forcing from decreases in northern summer insolation, tropical Pacific sea surface temperatures, and atmospheric CO2. Nearly all ice sheets were at their LGM positions from 26.5 ka to 19 to 20 ka, corresponding to minima in these forcings. The onset of Northern Hemisphere deglaciation 19 to 20 ka was induced by an increase in northern summer insolation, providing the source for an abrupt rise in sea level. The onset of deglaciation of the West Antarctic Ice Sheet occurred between 14 and 15 ka, consistent with evidence that this was the primary source for an abrupt rise in sea level approximately 14.5 ka.
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              Results of PMIP2 coupled simulations of the Mid-Holocene and Last Glacial Maximum – Part 1: experiments and large-scale features

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                Author and article information

                Journal
                Evolutionary Ecology
                Evol Ecol
                Springer Science and Business Media LLC
                0269-7653
                1573-8477
                August 2016
                April 25 2016
                August 2016
                : 30
                : 4
                : 755-782
                10.1007/s10682-016-9833-8
                © 2016

                http://www.springer.com/tdm

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