Evidence for the oldest Middle Palaeolithic cave occupation in the Romanian Carpathians

IF 1.9 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
Christoph Schmidt, Daniel Veres, George Murătoreanu, Marian Cosac, Loredana Niţă, Ştefan Vasile, Gabriel Sebastian Şerbănescu, Iuliana-Elisabeta Bartok
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Abstract

The Middle and Upper Palaeolithic sites in the Carpathians and Danube lowlands constitute key contexts for tracing the dispersal of Homo sapiens into central-western Europe and the replacement of Homo neanderthalensis. Surprisingly, the Romanian archaeological inventory lacks transitional technologies and only a few sites have been systematically excavated and numerically dated, explaining the incomplete understanding of the Middle Palaeolithic and hence Neanderthal population dynamics. Here we present new age constraints for the Abri 122/1200 and Peștera Mare caves in the Romanian Carpathians, obtained by radiocarbon dating of charcoal and bone and by optically stimulated luminescence (OSL) dating of cave sediments. Methodological issues and the method's upper limit cause grossly underestimated radiocarbon ages for charcoal from Abri 122/1200 and provide only minimum ages (>41–60 14C ka  bp) for bones from Peștera Mare cave. However, the OSL ages suggest Middle Palaeolithic cave occupation in the Carpathians since early Marine Isotopic Stage (MIS) 7 and lasting at least until MIS 5. These ages reinforce the vast potential of Carpathian cave sites in solidifying our understanding of Neanderthal dynamics in the region and their habitats. We discuss the reliability of this new chronology and the archaeological implications for the Middle Palaeolithic of neighbouring areas.

Abstract Image

罗马尼亚喀尔巴阡山脉最古老的旧石器时代中期洞穴居住证据
位于喀尔巴阡山脉和多瑙河低地的旧石器时代中晚期遗址构成了追踪智人向西欧中部扩散和尼安德特人取代的关键背景。令人惊讶的是,罗马尼亚的考古清单缺乏过渡技术,只有少数遗址被系统地挖掘和计算出年代,这解释了对旧石器时代中期和尼安德特人人口动态的不完整理解。在这里,我们提出了罗马尼亚喀尔巴阡山脉的Abri 122/1200和Peștera Mare洞穴的新年龄限制,这些洞穴是通过对木炭和骨头的放射性碳定年以及对洞穴沉积物的光学激发发光(OSL)定年获得的。方法问题和方法的上限导致严重低估了Abri 122/1200木炭的放射性碳年龄,并且只提供了Peștera Mare洞穴骨骼的最小年龄(> 41-60 14C ka bp)。然而,OSL年龄表明,喀尔巴阡山脉中旧石器时代的洞穴活动从早期海洋同位素阶段(MIS) 7开始,至少持续到MIS 5。这些年代强化了喀尔巴阡洞穴遗址的巨大潜力,巩固了我们对该地区尼安德特人动态及其栖息地的理解。我们讨论了这个新的年表的可靠性和考古意义的中期旧石器时代的邻近地区。
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来源期刊
Journal of Quaternary Science
Journal of Quaternary Science 地学-地球科学综合
CiteScore
4.70
自引率
8.70%
发文量
82
审稿时长
6-12 weeks
期刊介绍: The Journal of Quaternary Science publishes original papers on any field of Quaternary research, and aims to promote a wider appreciation and deeper understanding of the earth''s history during the last 2.58 million years. Papers from a wide range of disciplines appear in JQS including, for example, Archaeology, Botany, Climatology, Geochemistry, Geochronology, Geology, Geomorphology, Geophysics, Glaciology, Limnology, Oceanography, Palaeoceanography, Palaeoclimatology, Palaeoecology, Palaeontology, Soil Science and Zoology. The journal particularly welcomes papers reporting the results of interdisciplinary or multidisciplinary research which are of wide international interest to Quaternary scientists. Short communications and correspondence relating to views and information contained in JQS may also be considered for publication.
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