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中国北方水洞沟地点 1 号发掘 1963 年出土的大型叶片组合内的组合内变化,以及区域变化的背景。

Intra-assemblage variation in the macro-blade assemblage from the 1963 excavation at Shuidonggou locality 1, northern China, in the context of regional variation.

机构信息

Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China.

CAS Center for Excellence in Life and Paleoenvironment, Beijing, China.

出版信息

PLoS One. 2020 Jun 15;15(6):e0234576. doi: 10.1371/journal.pone.0234576. eCollection 2020.

Abstract

The emergence of the Upper Paleolithic and regional variability in early Upper Paleolithic industries are prominent topics in Paleolithic archaeology, with special relevance to the dispersal and differentiation of early modern human cultures across Eurasia. The so-called Initial Upper Paleolithic (IUP) has been considered a key element in the emergence of the Upper Paleolithic in northern Asia. Here, we examine the intra-assemblage variation in the collection from the 1963 excavation at Shuidonggou locality 1, a major IUP site in northern China. We combine technological and quantitative attribute analyses to investigate the variety of core reduction sequences and tool manufacture behaviors at the site. A range of core reduction sequences have been documented at Shuidonggou locality 1, including both simple core reduction and prepared core reduction yielding laminar (blade-like) products. The simple core reduction component may due to mixed non-IUP assemblages from different archaeological layers. Among the laminar core reduction sequences, the main strategy involves asymmetrical exploitation of the broad face of core blank, producing blades and elongate flakes, and resembling a recurrent Levallois blade method sensu lato. We compare Shuidonggou laminar blank production with that of IUP assemblages in the Siberian Altai, northern Mongolia, and the Transbaikal region. The comparison demonstrates a general consistency to the basic blank production in IUP assemblages across northern Asia, with some regional variation. The results suggest a multi-directional model of diffusion of the IUP in northeast Asia.

摘要

旧石器时代考古学中一个突出的话题是旧石器时代晚期的出现以及早期旧石器时代晚期工业的地域差异,这与早期现代人文化在欧亚大陆的传播和分化有着特殊的关系。所谓的初始旧石器时代(IUP)被认为是北亚旧石器时代晚期出现的关键因素。在这里,我们研究了中国北方主要的 IUP 遗址——水洞沟 1 号地点 1963 年发掘出土的遗物组合中的内在变化。我们结合技术和定量属性分析,研究了该遗址核心减少序列和工具制造行为的多样性。水洞沟 1 号地点记录了一系列核心减少序列,包括简单核心减少和准备核心减少,产生层状(片状)产品。简单核心减少的组成部分可能是由于不同考古层的非 IUP 组合混合造成的。在层状核心减少序列中,主要策略是不对称地利用核心毛坯的宽面,生产出叶片和拉长的薄片,类似于广义的勒瓦娄哇技术。我们将水洞沟的层状毛坯生产与西伯利亚阿尔泰山、蒙古北部和外贝加尔地区的 IUP 组合进行了比较。比较表明,整个北亚的 IUP 组合在基本毛坯生产方面具有普遍的一致性,但也存在一些区域差异。结果表明,IUP 在东北亚的扩散是一个多方向的模式。

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