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Chronological reassessment of the Middle to Upper Paleolithic transition and Early Upper Paleolithic cultures in Cantabrian Spain

机译:西班牙坎塔布连对中旧石器时代过渡和早期旧石器时代文化的年代重新评估

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摘要

Methodological advances in dating the Middle to Upper Paleolithic transition provide a better understanding of the replacement of local Neanderthal populations by Anatomically Modern Humans. Today we know that this replacement was not a single, pan-European event, but rather it took place at different times in different regions. Thus, local conditions could have played a role. Iberia represents a significant macro-region to study this process. Northern Atlantic Spain contains evidence of both Mousterian and Early Upper Paleolithic occupations, although most of them are not properly dated, thus hindering the chances of an adequate interpretation. Here we present 46 new radiocarbon dates conducted using ultrafiltration pre-treatment method of anthropogenically manipulated bones from 13 sites in the Cantabrian region containing Mousterian, Aurignacian and Gravettian levels, of which 30 are considered relevant. These dates, alongside previously reported ones, were integrated into a Bayesian age model to reconstruct an absolute timescale for the transitional period. According to it, the Mousterian disappeared in the region by 47.9–45.1ka cal BP, while the Châtelperronian lasted between 42.6k and 41.5ka cal BP. The Mousterian and Châtelperronian did not overlap, indicating that the latter might be either intrusive or an offshoot of the Mousterian. The new chronology also suggests that the Aurignacian appears between 43.3–40.5ka cal BP overlapping with the Châtelperronian, and ended around 34.6–33.1ka cal BP, after the Gravettian had already been established in the region. This evidence indicates that Neanderthals and AMH co-existed <1,000 years, with the caveat that no diagnostic human remains have been found with the latest Mousterian, Châtelperronian or earliest Aurignacian in Cantabrian Spain.
机译:在中古石器时代过渡到上旧石器时代的方法学上的进步提供了对解剖上现代人类替代尼安德特人种群的更好的理解。今天,我们知道这种替代不是一次泛欧事件,而是在不同地区的不同时间发生的。因此,当地条件可能起了作用。伊比利亚是研究这一过程的重要宏观区域。西班牙北大西洋包含穆斯特人和早期旧石器时代职业的证据,尽管其中大多数都未正确标明日期,因此妨碍了进行适当解释的机会。在这里,我们介绍了使用超滤预处理方法对来自坎塔布连地区13个地点的人为操作的骨头进行的46个新的放射性碳数据,这些地点包含穆斯特,奥里尼亚克和格拉维特水平,其中30个被认为是相关的。这些日期与先前报告的日期一起被整合到贝叶斯年龄模型中,以重建过渡时期的绝对时间表。据此,穆斯特人在该地区消失的时间为47.9–45.1ka cal BP,而沙特伯隆人的持续时间为42.6k至41.5ka cal BP。 Mousterian和Châtelperronian没有重叠,表明后者可能是Mousterian的侵入性或分支。新的年表还表明,在该地区已经建立了格拉维特山脉之后,奥里尼亚纪出现在43.3–40.5ka cal BP与Châperperronian重叠,结束于34.6–33.1ka cal BP。该证据表明,尼安德特人和AMH共存了不到1000年,但要注意的是,在西班牙坎塔布连,最新的穆塞特人,沙特勒布朗人或最早的奥里尼亚克人都没有发现可诊断的人类遗骸。

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