1. Tufas indicate prolonged periods of water availability linked to human occupation in the southern Kalahari
- Author
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Zerboni, A, von der Meden, J, Pickering, R, Schoville, BJ, Green, H, Weij, R, Hellstrom, J, Greig, A, Woodhead, J, Khumalo, W, Wilkins, J, Zerboni, A, von der Meden, J, Pickering, R, Schoville, BJ, Green, H, Weij, R, Hellstrom, J, Greig, A, Woodhead, J, Khumalo, W, and Wilkins, J
- Abstract
Detailed, well-dated palaeoclimate and archaeological records are critical for understanding the impact of environmental change on human evolution. Ga-Mohana Hill, in the southern Kalahari, South Africa, preserves a Pleistocene archaeological sequence. Relict tufas at the site are evidence of past flowing streams, waterfalls, and shallow pools. Here, we use laser ablation screening to target material suitable for uranium-thorium dating. We obtained 33 ages covering the last 110 thousand years (ka) and identify five tufa formation episodes at 114-100 ka, 73-48 ka, 44-32 ka, 15-6 ka, and ~3 ka. Three tufa episodes are coincident with the archaeological units at Ga-Mohana Hill dating to ~105 ka, ~31 ka, and ~15 ka. Based on our data and the coincidence of dated layers from other local records, we argue that in the southern Kalahari, from ~240 ka to ~71 ka wet phases and human occupation are coupled, but by ~20 ka during the Last Glacial Maximum (LGM), they are decoupled.
- Published
- 2022