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南非新星洞穴中沉积物的年代及相关沉积物

The age of and associated sediments in the Rising Star Cave, South Africa.

作者信息

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

机构信息

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.

出版信息

Elife. 2017 May 9;6:e24231. doi: 10.7554/eLife.24231.

Abstract

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.

摘要

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。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ffd3/5423772/e0652ead0900/elife-24231-fig1.jpg

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