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High- and low-latitude forcing of Plio-Pleistocene East African climate and human evolution.

Trauth MH, Maslin MA, Deino AL, Strecker MR, Bergner AG, Dühnforth M

Institut für Geowissenschaften, Universität Potsdam, POB 601553, D-14415 Potsdam, Germany.

The late Cenozoic climate of East Africa is punctuated by episodes of short, alternating periods of extreme wetness and aridity, superimposed on a regime of subdued moisture availability exhibiting a long-term drying trend. These periods of extreme climate variability appear to correlate with maxima in the 400-thousand-year (kyr) component of the Earth's eccentricity cycle. Prior to 2.7Ma the wet phases appear every 400kyrs, whereas after 2.7Ma, the wet phases appear every 800kyrs, with periods of precessional-forced extreme climate variability at 2.7-2.5Ma, 1.9-1.7Ma, and 1.1-0.9Ma before present. The last three major lake phases occur at the times of major global climatic transitions, such as the onset of Northern Hemisphere Glaciation (2.7-2.5Ma), intensification of the Walker Circulation (1.9-1.7Ma), and the Mid-Pleistocene Revolution (1.0-0.7Ma). High-latitude forcing is required to compress the Intertropical Convergence Zone so that East Africa becomes locally sensitive to precessional forcing, resulting in rapid shifts from wet to dry conditions. These periods of extreme climate variability may have provided a catalyst for evolutionary change and driven key speciation and dispersal events amongst mammals and hominins in East Africa.

Published 6 November 2007 in J Hum Evol, 53(5): 475-86.
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