Adler Daniel S, Bar-Yosef Ofer, Belfer-Cohen Anna, Tushabramishvili Nicholas, Boaretto E, Mercier N, Valladas H, Rink W J
Department of Anthropology, 354 Mansfield Road, Unit 2176, University of Connecticut, Storrs, CT 06269-2176, USA.
J Hum Evol. 2008 Nov;55(5):817-33. doi: 10.1016/j.jhevol.2008.08.010. Epub 2008 Oct 18.
This paper considers the recent radiometric dating (14C-AMS, TL, ESR) of 76 late Middle and early Upper Paleolithic samples from Ortvale Klde Rockshelter, located in the Republic of Georgia. We present a critical evaluation of each date based on its stratigraphic and archaeological context, its pretreatment and contamination history, and its resulting accuracy and precision, the goal being to establish a sound chronology for the site. Only by systematically identifying aberrant dates within a data set and isolating them from further analysis can we hope to understand cultural and biological phenomena on an accurate temporal scale. Based on the strict discard protocol outlined here, we omit 25% of the dated samples from the analysis. The remaining data speak to the lengthy tenure of Neandertals in the region, but also to their relatively rapid demise and the establishment of modern human populations approximately 38-34 ka 14C BP (42-39 kacalBP(Hulu)). We compare these chronometric data with those from the neighboring sites of Bronze and Dzudzuana caves, as well as Mezmaiskaya Cave, located in the northern Caucasus. While the lack of key contextual information limit our ability to subject these other data sets to the same critical evaluation procedure, they provide the first interregional temporal assessment of the Middle to Upper Paleolithic "transition," the results of which suggest an initial expansion of modern humans into the southern Caucasus followed by expansion along the Black Sea coast and into the northern Caucasus.
本文探讨了对来自格鲁吉亚共和国奥尔塔莱·克莱德岩厦的76个旧石器时代中晚期和晚期旧石器时代早期样本的近期放射性测年(14C-AMS、热释光、电子自旋共振)。我们基于每个测年数据的地层和考古背景、预处理和污染历史以及其结果的准确性和精确性进行批判性评估,目的是为该遗址建立一个可靠的年代学。只有通过系统地识别数据集中异常的测年数据并将它们从进一步分析中分离出来,我们才有希望在准确的时间尺度上理解文化和生物现象。基于此处概述的严格舍弃方案,我们在分析中排除了25%的测年样本。其余数据表明尼安德特人在该地区长期存在,但也表明他们相对迅速地灭绝以及现代人类群体大约在距今14C 38 - 34 ka(校正后距今42 - 39 ka(葫芦校准曲线))时的建立。我们将这些计时数据与来自邻近的青铜洞和祖祖阿纳洞以及位于北高加索的梅兹迈斯卡亚洞的数据进行比较。虽然缺乏关键的背景信息限制了我们对这些其他数据集进行相同批判性评估程序的能力,但它们提供了旧石器时代中期到晚期“过渡”的首次区域间时间评估,其结果表明现代人类最初向高加索南部扩张,随后沿着黑海海岸扩张并进入北高加索。