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Age estimates for hominin fossils and the onset of the Upper Palaeolithic at Denisova Cave

机译:人参化石的年龄估计和Denisova洞穴上古旧石器时代的开始

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Denisova Cave in the Siberian Altai (Russia) is a key site for understanding the complex relationships between hominin groups that inhabited Eurasia in the Middle and Late Pleistocene epoch. DNA sequenced from human remains found at this site has revealed the presence of a hitherto unknown hominin group, the Denisovans(1,2), and high-coverage genomes from both Neanderthal and Denisovan fossils provide evidence for admixture between these two populations(3). Determining the age of these fossils is important if we are to understand the nature of hominin interaction, and aspects of their cultural and subsistence adaptations. Here we present 50 radiocarbon determinations from the late Middle and Upper Palaeolithic layers of the site. We also report three direct dates for hominin fragments and obtain a mitochondrial DNA sequence for one of them. We apply a Bayesian age modelling approach that combines chronometric (radiocarbon, uranium series and optical ages), stratigraphic and genetic data to calculate probabilistically the age of the human fossils at the site. Our modelled estimate for the age of the oldest Denisovan fossil suggests that this group was present at the site as early as 195,000 years ago (at 95.4% probability). All Neanderthal fossils-as well as Denisova 11, the daughter of a Neanderthal and a Denisovan(4)-date to between 80,000 and 140,000 years ago. The youngest Denisovan dates to 52,000-76,000 years ago. Direct radiocarbon dating of Upper Palaeolithic tooth pendants and bone points yielded the earliest evidence for the production of these artefacts in northern Eurasia, between 43,000 and 49,000 calibrated years before present (taken as ad 1950). On the basis of current archaeological evidence, it may be assumed that these artefacts are associated with the Denisovan population. It is not currently possible to determine whether anatomically modern humans were involved in their production, as modern-human fossil and genetic evidence of such antiquity has not yet been identified in the Altai region.
机译:西伯利亚阿尔泰(俄罗斯)的Denisova洞穴是了解中更新世末期居住在欧亚大陆的人种群体之间复杂关系的重要场所。从在此位置发现的人类遗体测序的DNA揭示了迄今未知的人类素组Denisovans(1,2)的存在,尼安德特人和Denisovan化石的高覆盖率基因组为这两个种群之间的混合提供了证据(3) 。如果我们要了解人参相互作用的性质以及其文化和生存适应的方面,确定这些化石的年龄很重要。在这里,我们介绍了该地点中晚期和旧石器时代晚期层的50个放射性碳测定值。我们还报告了人参片段的三个直接日期,并为其中一个获得了线粒体DNA序列。我们采用贝叶斯年龄建模方法,该方法结合了测时(放射性碳,铀系列和光学年龄),地层和遗传数据,以概率方式计算了该地点化石的年龄。我们对最古老的Denisovan化石的年龄进行的模型估算表明,该组最早出现在195,000年前(占95.4%的概率)。所有尼安德特人化石-以及尼安德特人和Denisovan(4)的女儿Denisova 11-都可以追溯到80,000到140,000年前。最年轻的Denisovan可以追溯到52,000-76,000年前。上古石器时代的牙齿挂件和骨尖的直接放射性碳测年提供了最早的证据,证明了在欧亚大陆北部出现这些人工制品的时间,经过校准的年数在43,000至49,000之间(取自公元1950年)。根据当前的考古证据,可以假定这些文物与Denisovan种群有关。目前尚无法确定解剖学上是否涉及现代人类的生产,因为在阿尔泰地区尚未发现此类古代的现代人类化石和遗传证据。

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