TY  - JOUR
A1  - Dühnforth, Miriam
A1  - Bergner, Andreas G. N.
A1  - Trauth, Martin H.
T1  - Early Holocene water budget of the Nakuru-Elmenteita basin, Central Kenya Rift
Y1  - 2008
UR  - http://www.springerlink.com/content/100294
U6  - https://doi.org/10.1007/s10933-006-9003-z
SN  - 0921-2728
ER  - 
TY  - JOUR
A1  - Trauth, Martin H.
A1  - Maslin, Mark A.
A1  - Deino, Alan L.
A1  - Strecker, Manfred
A1  - Bergner, Andreas G. N.
A1  - Dühnforth, Miriam
T1  - High- and low-latitude forcing of Plio-Pleistocene African climate and human evolution
N2  - 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 2.7 Ma the wet phases appear every 400 kyrs, whereas after 2.7 Ma, the wet phases appear every 800 kyrs, with periods of precessional-forced extreme climate variability at 2.7-2.5 Ma, 1.9-1.7 Ma, and 1.1-0.9 Ma 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 (2.7-2.5 Ma), intensification of the Walker Circulation (1.9-1.7 Ma), and the Mid-Pleistocene Revolution (1.0-0.7 Ma). 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. (C) 2007 Elsevier Ltd. All rights reserved.
Y1  - 2008
U6  - https://doi.org/10.1016/j.jhevol.2006.12.009
ER  -