Terrestrial records for the Middle Pleistocene of Southern Africa are sparse and mostly fragmentary because the landscape was largely devoid of suitable depositories. Fortunately, one continuous lacustrine sequence, that of the Tswaing impact crater near Pretoria, South Africa (Fig. 1), spans the period from ~200 kyr to the present. Recent analyses of marine cores off the west coast of Southern Africa have, in addition, vouchsafed important proxy evidence of palaeo-wind regimes, periods of aridity and terrestrial flora.A generalised, but largely consistent, picture of palaeoenvironmental fluctuations during Isotope Stage 6 can therefore be drawn.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Similar content being viewed by others
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2004 Springer
About this chapter
Cite this chapter
Partridge, T.C., Scott, L., Schneider, R.R. (2004). Between Agulhas and Benguela: responses of Southern African climates of the Late Pleistocene to Current Fluxes, Orbital Precession and the Extent of the Circum-Antarctic Vortex. In: Battarbee, R.W., Gasse, F., Stickley, C.E. (eds) Past Climate Variability through Europe and Africa. Developments in Paleoenvironmental Research, vol 6. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-2121-3_4
Download citation
DOI: https://doi.org/10.1007/978-1-4020-2121-3_4
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-2120-6
Online ISBN: 978-1-4020-2121-3
eBook Packages: Springer Book Archive