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Several distinct wet periods since 420 ka in the Namib Desert inferred from U-series dates of speleothems

Published online by Cambridge University Press:  20 January 2017

Mebus A. Geyh  and
Klaus Heine
Mebus A. Geyh*
Affiliation:
University of Marburg, Germany
Klaus Heine
Affiliation:
Institute of Geography, Regensburg University, Germany
*
*Corresponding author at: Rübeland 12, 29308 Winsen (Aller), Germany. Tel.: + 49 5146 987123. E-mail address:mebus.geyh@t-online.de (M.A. Geyh).
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Abstract

The scarcity of numerical dates of the arid areas in southern Africa is a challenge for reconstructing paleoclimate. This paper presents a chronological reconstruction in the central part of the Namib Desert, Namibia, for the last 420,000 yr. It is based on 230Th/U dates (TIMS) from a large stalagmite and a thick flowstone layer in a small cave located in the hyper-arid central Namib Desert. The results provide for the first time evidence of three or possibly four succeeding wet periods of decreasing intensity since 420 ka through which speleothem deposited at approximately 420–385 ka, 230–207 ka and 120–117 ka following the 100-ka Milankovitch cycle. Speleothem growth was not recorded for the Holocene. These wet periods interrupted the predominantly dry climate of the Namib Desert and coincided with wet phases in deserts of the northern hemisphere in the Murzuq Basin, Sahara, the Negev, Israel, the Nafud Desert, Saudi Arabia, and the arid northern Oman, Arabian Peninsula.

Keywords

Namib DesertSpeleothems230Th/U datingMiddle/Late PleistocenePaleoclimatePaleoprecipitationMilankovitch forcing
Type
Research Article
Information
Quaternary Research , Volume 81 , Issue 2 , March 2014 , pp. 381 - 391
Copyright
University of Washington

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