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Late Quaternary lake-level fluctuations in the Mababe Depression: Middle Kalahari palaeolakes and the role of Zambezi inflows

Published online by Cambridge University Press:  20 January 2017

S.L. Burrough  and
D.S.G. Thomas
S.L. Burrough*
Affiliation:
Oxford University Centre for the Environment School of Geography, University of Oxford, South Parks Road, Oxford, OX1 3QY, UK
D.S.G. Thomas
Affiliation:
Oxford University Centre for the Environment School of Geography, University of Oxford, South Parks Road, Oxford, OX1 3QY, UK Visiting Professor, Department of Environmental and Geographical Science, University of Cape Town, Rondebosch 7701, South Africa
*
*Corresponding author.E-mail address:[email protected] (D.S.G. Thomas).
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Abstract

A systematic drilling and optical dating programme on Middle Kalahari beach ridge (relict shoreline) sediments has enabled the identification of multiple episodes of lake high stands of an extensive palaeolake system at the terminus of the Okavango Delta, northern Botswana. This paper presents 23 ages from the Mababe Depression and establishes four shoreline construction phases in the late Quaternary coeval with other sub-basin lake high stands (Lake Ngami). These synchronous lake phases result from a coalescence of the sub-basins into a unified palaeolake, Lake Thamalakane, covering an area of ∼ 32,000 km2. Six additional ages are also presented from the Chobe enclave to the north of the basin where shoreline ridges were emplaced at the same time as Lake Thamalakane phases. This suggests that increased flow in the Chobe and Zambezi system significantly contributed to the Middle Kalahari lake phases in both the post-glacial and Holocene periods. The integration of these new data and their compatibility with other regional and tropical palaeo-archives is discussed in the light of understanding Quaternary climate drivers within the Kalahari.

Keywords

Palaeolake ThamalakaneKalahariMababe DepressionOSL dating
Type
Original Articles
Information
Quaternary Research , Volume 69 , Issue 3 , May 2008 , pp. 388 - 403
Copyright
University of Washington

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