Cosmogenic nuclide dating of Australopithecus at Sterkfontein, South
Africa
Sterkfontein is the most prolific single source of Australopithecus
fossils, the vast majority of which were recovered from Member 4, a
cave breccia now exposed by erosion and weathering at the landscape
surface. A few other Australopithecus fossils, including the StW 573 skeleton, come from subterranean deposits [T. C. Partridge et al.,
Science 300, 607–612 (2003); R. J. Clarke, K. Kuman, J. Hum. Evol.
134, 102634 (2019)]. Here, we report a cosmogenic nuclide isochron
burial date of 3.41 +/- 0.11 million years (My) within the lower
middle part of Member 4, and simple burial dates of 3.49 +/- 0.19 My
in the upper middle part of Member 4 and 3.61 +/- 0.09 My in Jacovec
Cavern. Together with a previously published isochron burial date of
3.67 +/- 0.16 My for StW 573 [D. E. Granger et al., Nature 522, 85–88 (2015)], these results place nearly the entire Australopithecus
assemblage at Sterkfontein in the mid-Pliocene, contemporaneous with Australopithecus afarensis in East Africa. Our ages for the
fossil-bearing breccia in Member 4 are considerably older than the
previous ages of ca. 2.1 to 2.6 My interpreted from flowstones
associated with the same deposit. We show that these previously dated flowstones are stratigraphically intrusive within Member 4 and that
they therefore underestimate the true age of the fossils.
https://www.pnas.org/doi/full/10.1073/pnas.2123516119
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