Dirks Paul Hgm, Roberts Eric M, Hilbert-Wolf Hannah, Kramers Jan D, Hawks John, Dosseto Anthony, Duval Mathieu, Elliott Marina, Evans Mary, Grün Rainer, Hellstrom John, Herries Andy Ir, Joannes-Boyau Renaud, Makhubela Tebogo V, Placzek Christa J, Robbins Jessie, Spandler Carl, Wiersma Jelle, Woodhead Jon, Berger Lee R
Department of Geoscience, James Cook University, Townsville, Australia.
Evolutionary Studies Institute and the National Centre for Excellence in PalaeoSciences, University of the Witwatersrand, Wits, South Africa.
Elife. 2017 May 9;6:e24231. doi: 10.7554/eLife.24231.
New ages for flowstone, sediments and fossil bones from the Dinaledi Chamber are presented. We combined optically stimulated luminescence dating of sediments with U-Th and palaeomagnetic analyses of flowstones to establish that all sediments containing fossils can be allocated to a single stratigraphic entity (sub-unit 3b), interpreted to be deposited between 236 ka and 414 ka. This result has been confirmed independently by dating three teeth with combined U-series and electron spin resonance (US-ESR) dating. Two dating scenarios for the fossils were tested by varying the assumed levels of Rn loss in the encasing sediments: a maximum age scenario provides an average age for the two least altered fossil teeth of 253 +82/-70 ka, whilst a minimum age scenario yields an average age of 200 +70/-61 ka. We consider the maximum age scenario to more closely reflect conditions in the cave, and therefore, the true age of the fossils. By combining the US-ESR maximum age estimate obtained from the teeth, with the U-Th age for the oldest flowstone overlying fossils, we have constrained the depositional age of to a period between 236 ka and 335 ka. These age results demonstrate that a morphologically primitive hominin, survived into the later parts of the Pleistocene in Africa, and indicate a much younger age for the fossils than have previously been hypothesized based on their morphology.
本文给出了迪纳莱迪洞穴内石笋、沉积物和化石骨骼的新年代数据。我们将沉积物的光释光测年与石笋的铀系和古地磁分析相结合,确定所有含有化石的沉积物都可归为一个单一的地层单元(3b亚单元),其沉积时间被推断为23.6万年至41.4万年前。通过对三颗牙齿进行铀系与电子自旋共振联合测年(US-ESR),这一结果得到了独立验证。通过改变包裹沉积物中假设的氡损失水平,测试了两种化石年代测定方案:最大年龄方案得出两颗变化最小的化石牙齿的平均年龄为25.3 +8.2/-7.0万年,而最小年龄方案得出的平均年龄为20.0 +7.0/-6.1万年。我们认为最大年龄方案更能准确反映洞穴内的情况,因此更接近化石的真实年龄。通过将牙齿的US-ESR最大年龄估计值与覆盖化石的最古老石笋的铀钍年龄相结合,我们将化石的沉积年龄限制在23.6万年至33.5万年之间。这些年龄结果表明,一种形态原始的古人类在非洲活到了更新世晚期,并且表明这些化石的年龄比之前根据其形态所假设的要年轻得多。