Identifying Local Learning Communities During the Terminal Palaeolithic in the Southern Levant: Multi-scale 3-D Analysis of Flint Cores

Q1 Social Sciences
Francesco Valletta, Itamar Dag, L. Grosman
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引用次数: 6

Abstract

A methodology for identifying prehistoric local learning communities is proposed. We wish to test possible relationships among communities based on continuity and variability in lithic reduction sequence technological traits with different visibility and malleability. Quantitative features reflecting different technological traits are measured on 3-D models of flint cores in different scales: the ratio between core thickness and reduction surface width, the angle between subsequent bands of production blank scars to the relative striking platform, and the average curvature of the ridge between each blank scar striking platform pair. Continuity and variability in these features are used to establish the relations among lithic assemblages on different hierarchical levels: local learning communities and geographically widespread cultural lineages. The Late Upper Palaeolithic and the Epipalaeolithic of the Southern Levant (ca. 27,000–15,000 cal BP) provide an opportunity to test our method. A progressive increase in territoriality is hypothesized throughout this timespan, yet the precise timing and modes of this phenomenon need to be defined. The present study analyzes six core assemblages attributed to different cultural entities, representing chronologically separated occupations of the Ein Gev area and the coastal Sharon Plain. Continuity in technological traits between the Atlitian (ca. 27,000–26,000 cal BP) and Nizzanan (ca. 20,000–18,500 cal BP) occupations of the Ein Gev area suggests that the same learning community repeatedly settled there during a long time span. Two geographically separate learning communities were defined in the study areas within the Kebaran cultural entity (ca. 24,000–18,000 cal BP); the group occupying the Ein Gev area possibly continued to settle there during the Geometric Kebaran (ca. 18,000–15,000 cal BP). Continuity in more conservative traits of the reduction sequence allows to tie these two communities to the same cultural lineage. The ability to track prehistoric learning communities based on quantitative features helps increase the objectivity and the resolution in the reconstruction of past cultural dynamics.
识别南黎凡特旧石器时代晚期的当地学习社区:弗林特岩芯的多尺度三维分析
提出了一种识别史前地方学习社区的方法。我们希望基于具有不同可见性和延展性的岩屑还原序列技术特征的连续性和可变性来测试群落之间的可能关系。在不同尺度的燧石岩心三维模型上测量了反映不同技术特征的定量特征:岩心厚度与压下表面宽度之间的比率、后续生产毛坯疤痕带与相对打击平台之间的角度,以及每个毛坯疤痕打击平台对之间的山脊平均曲率。这些特征的连续性和可变性被用来建立不同等级的石器组合之间的关系:当地的学习社区和地理上广泛分布的文化谱系。旧石器时代晚期和南黎凡特旧石器时代末期(约27000–15000 cal BP)为测试我们的方法提供了机会。假设在整个时间跨度内,领土面积会逐渐增加,但这种现象的确切时间和模式需要确定。本研究分析了属于不同文化实体的六个核心组合,代表了埃因盖夫地区和沿海沙龙平原按时间顺序分离的职业。埃因盖夫地区的Atlitian(约27000–26000 cal BP)和Nizzanan(约20000–18500 cal BP)职业之间技术特征的连续性表明,同一学习群体在很长一段时间内反复定居在那里。在Kebaran文化实体内的研究区域中定义了两个地理上独立的学习社区(约24000–18000 cal BP);在Geometric Kebaran时期(约18000–15000 cal BP),占领Ein Gev地区的群体可能继续在那里定居。还原序列中更保守的特征的连续性允许将这两个群体与同一文化谱系联系起来。基于数量特征跟踪史前学习社区的能力有助于提高重建过去文化动态的客观性和分辨率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
5.50
自引率
0.00%
发文量
12
审稿时长
19 weeks
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