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从典型的西欧阿舍利晚期石器工艺到中更新世晚期卡恩德拉阿罗格(法国东比利牛斯省)沉积单元 D 中的微加工工艺的转变。

The shift from typical Western European Late Acheulian to microproduction in unit 'D' of the late Middle Pleistocene deposits of the Caune de l'Arago (Pyrénées-Orientales, France).

机构信息

Institut Català de Paleoecologia Humana i Evolució Social (IPHES), Zona Educacional 4, Campus Sescelades URV (Edifici W3), 43007, Tarragona, Spain; Universitat Rovira i Virgili (URV), Àrea de Prehistòria, Avinguda de Catalunya 35, 43002, Tarragona, Spain.

Muséum National d'Histoire Naturelle (MNHN), UMR 7194 CNRS, UVPD-HNHP, EPCC-Centre Européen de Recherches Préhistoriques-Tautavel, 66720, Tautavel, France.

出版信息

J Hum Evol. 2019 Oct;135:102650. doi: 10.1016/j.jhevol.2019.102650. Epub 2019 Aug 28.

Abstract

Stratigraphic Unit D levels of the Caune de l'Arago (Pyrénées-Orientales, France), situated in the upper part of the depositional sequence of Ensemble Stratigraphique III (ES III), has yielded a rich Acheulian archeopaleontological record dated to the Middle Pleistocene. The site's infill, dated from 690 to 90 ka, encloses a thick cultural sequence comprising some of the oldest evidence of Acheulian documented so far in Western Europe (Unit P levels). The deposits contain successive occupation layers with abundant faunal remains, stone artifacts, and sometimes hominin remains attributed to Homo erectus tautavelensis. The Unit D levels are chronostratigraphically positioned at the top of the ES III sequence, accumulated at the end of Marine Isotope Stage (MIS) 12. The Unit D lithic assemblage shows no evidence of Levallois knapping strategies. Rather, its features indicate a trend towards microproduction that continues into subsequent occupational phases, apparently marking a local expression of the transition from the Lower to the Middle Paleolithic. Remarkably, tiny discoid and multidirectional type cores, predominantly knapped from small-sized quartz pebbles, characterize the Unit D lithic assemblage. Experimental work presented here demonstrates the likelihood that, despite the small size of the cores and the recalcitrant crystalline materials from which they were knapped, flake production can be carried out with free-hand hard hammer techniques. We explore behavioral aspects gleaned from Unit D cultural material, contrasting them with microlithic praxis observed elsewhere in Europe and the Near East in a similar timeframe.

摘要

法国东比利牛斯省的卡内德阿罗格(Caune de l'Arago)的地层单元 D 层,位于沉积序列综合地层 III(ES III)的上部,出土了丰富的中更新世阿舍利古考古记录。该遗址的填充物可追溯到 69 到 90 千年前,其中包含了一层厚厚的文化层,其中包含了迄今为止在西欧记录的最古老的阿舍利文化证据(P 层)。这些沉积物包含了连续的居住层,其中有大量的动物遗骸、石器,有时还有被归为直立人图太威亚种的人类遗骸。地层单元 D 在年代地层学上位于 ES III 序列的顶部,堆积在海洋同位素阶段 12 的末期。地层单元 D 的石器组合没有证据表明存在勒瓦娄哇技术。相反,其特征表明存在向微观生产的趋势,这种趋势一直延续到随后的居住阶段,显然标志着从旧石器时代早期到中期的过渡在当地的表现。值得注意的是,地层单元 D 的石器组合以微小的盘状和多向型石核为特征,主要是用小型石英卵石制成。这里展示的实验工作表明,尽管核心很小,且它们是由难加工的结晶材料制成,但仍可以使用手工硬锤技术进行石片生产。我们探讨了从地层单元 D 的文化材料中得出的行为方面,将其与在类似时间范围内在欧洲和近东其他地方观察到的微石器实践进行了对比。

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