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施宁根旧石器时代早期遗址的年代。

The age of the Lower Paleolithic occupation at Schöningen.

作者信息

Richter Daniel, Krbetschek Matthias

机构信息

Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, 04103 Leipzig, Germany; LS Geomorphologie, University of Bayreuth, Universitätsstr. 30, 95447 Bayreuth, Germany.

Sächsische Akademie der Wissenschaften, Forschungsstelle Geochronologie Quartär, Institut für Angewandte Physik, TU Bergakademie Freiberg, Leipziger Straße 23, 09596 Freiberg, Germany; Freiberg Instruments GmbH, Delfterstr. 6, 09599 Freiberg, Germany.

出版信息

J Hum Evol. 2015 Dec;89:46-56. doi: 10.1016/j.jhevol.2015.06.003. Epub 2015 Jul 23.

Abstract

Thermoluminescence (TL) data are presented for eight samples of heated flint collected at the archaeological site of Schöningen 13/I-1 (Cycle I), for which a Holsteinian age is suggested by palynology of stratigraphically similar positions within a cyclic sedimentological model for the Quaternary sequence of Schöningen. Although the fire responsible for the zeroing of the TL-signal cannot be unequivocally attributed to human activities, any time difference between a natural fire and the human occupation is negligible for a site of this antiquity. The weighted mean age of 321 ± 16 ka places the last heating of the flints nominally in the age range of Marine Isotope Stages (MIS) 10 to 8. By inference this data would suggest an attribution of the Holsteinian to MIS 9 and may also serve as a maximum age estimate for the spear site of Schöningen 13/II-4 (Cycle II). Considering the chronometric data available and following an alternative sedimentological model the age of these two sites at Schöningen can be considered as belonging to the same climatic cycle. This suggests an attribution to MIS 9, and by inference provides an age estimate of 337-300 ka for the oldest spears in human history.

摘要

本文展示了在舍宁根13/I-1考古遗址(第一阶段)采集的八个加热燧石样本的热释光(TL)数据。根据舍宁根第四纪序列的循环沉积学模型中地层相似位置的孢粉学研究,推测其年代为霍尔斯坦阶。尽管导致TL信号归零的火灾不能明确归因于人类活动,但对于这样古老的遗址来说,自然火灾与人类居住之间的任何时间差异都可以忽略不计。321±16 ka的加权平均年龄表明燧石的最后一次加热名义上处于海洋同位素阶段(MIS)10至8的年龄范围内。由此推断,这些数据表明霍尔斯坦阶可归因于MIS 9,也可作为舍宁根13/II-4(第二阶段)矛遗址的最大年龄估计。考虑到现有的年代测定数据,并遵循另一种沉积学模型,舍宁根这两个遗址的年代可被视为属于同一气候周期。这表明可归因于MIS 9,由此推断,为人类历史上最古老的矛提供了337 - 300 ka的年龄估计。

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