| Literature DB >> 19683788 |
Morris B Sutton1, Travis Rayne Pickering, Robyn Pickering, C K Brain, Ronald J Clarke, Jason L Heaton, Kathleen Kuman.
Abstract
We report on new research at Swartkrans Cave, South Africa, that provides evidence of two previously unrealized artifact- and fossil-bearing deposits. These deposits underlie a speleothem dated by the uranium-thorium disequilibrium technique to 110,000+/-1,980 years old, the first tightly constrained, geochronological date available for the site. Recovered fauna from the two underlying deposits-including, prominently, the dental remains of Paranthropus (Australopithecus) robustus from the uppermost layer (Talus Cone Deposit)-indicate a significantly older, late Pliocene or early Pleistocene age for these units. The lowest unit (LB East Extension) is inferred to be an eastward extension of the well-known Lower Bank of Member 1, the earliest surviving infill represented at the site. The date acquired from the speleothem also sets the maximum age of a rich Middle Stone Age lithic assemblage.Entities:
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Year: 2009 PMID: 19683788 DOI: 10.1016/j.jhevol.2009.05.014
Source DB: PubMed Journal: J Hum Evol ISSN: 0047-2484 Impact factor: 3.895