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多方法年代测定显示法国罗纳河谷马拉斯岩棚存在 20 万年的中石器时代人类活动遗迹。

Multi-method dating reveals 200 ka of Middle Palaeolithic occupation at Maras rock shelter, Rhône Valley, France.

机构信息

Archéosciences Bordeaux, UMR 6034 CNRS-Université Bordeaux Montaigne, Pessac, France.

Centro Nacional de Investigación Sobre la Evolución Humana, Burgos, Spain.

出版信息

Sci Rep. 2024 Sep 3;14(1):20474. doi: 10.1038/s41598-024-69380-w.

Abstract

The emergence of the Middle Palaeolithic, and its variability over time and space are key questions in the field of prehistoric archaeology. Many sites have been documented in the south-eastern margins of the Massif central and the middle Rhône valley, a migration path that connects Northern Europe with the Mediterranean. Well-dated, long stratigraphic sequences are essential to understand Neanderthals dynamics and demise, and potential interactions with Homo sapiens in the area, such as the one displayed at the Maras rock shelter ("Abri du Maras"). The site is characterised by exceptional preservation of archaeological remains, including bones dated using radiocarbon (C) and teeth using electron spin resonance combined with uranium series (ESR/U-series). Optically stimulated luminescence was used to date the sedimentary deposits. By combining the new ages with previous ones using Bayesian modelling, we are able to clarify the occupation time over a period spanning 200,000 years. Between ca. 250 and 40 ka, the site has been used as a long-term residence by Neanderthals, specifically during three interglacial periods: first during marine isotopic stage (MIS) 7, between 247 ± 34 and 223 ± 33 ka, and then recurrently during MIS 5 (between 127 ± 17 and 90 ± 9 ka) and MIS 3 (up to 39,280 cal BP).

摘要

中更新世的出现及其随时间和空间的变化是史前考古学领域的关键问题。在中央高原东南部和罗纳河谷中部的边缘地带,有许多遗址已经被记录下来,这是一条连接北欧和地中海的迁徙路径。为了了解尼安德特人的动态和灭绝,以及该地区与智人之间的潜在相互作用,如马拉斯岩石避难所(“Maras 洞穴”)所展示的那样,有必要获得经过良好测年的长地层序列。该遗址的特点是考古遗迹保存得非常好,包括使用放射性碳 (C) 对骨骼进行定年和使用电子自旋共振与铀系列 (ESR/U 系列) 对牙齿进行定年。光释光被用于对沉积物进行定年。通过使用贝叶斯模型将新的年龄与以前的年龄结合起来,我们能够澄清在跨越 20 万年的时期内的居住时间。在大约 25 万至 40 千年前,该遗址被尼安德特人用作长期居住地,特别是在三个间冰期期间:第一次是在海洋同位素阶段 (MIS) 7 期间,在 247±34 到 223±33 千年前,然后在 MIS 5(在 127±17 到 90±9 千年前)和 MIS 3(直到 39280 年 cal BP)期间反复出现。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8788/11372155/7fcfe8af06e7/41598_2024_69380_Fig1_HTML.jpg

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