Great Lakes Range, Museum of Anthropological Archaeology, University of Michigan, Ann Arbor, Michigan, United States of America.
Museum of Anthropological Archaeology, University of Michigan, Ann Arbor, Michigan, United States of America.
PLoS One. 2024 May 29;19(5):e0302255. doi: 10.1371/journal.pone.0302255. eCollection 2024.
The Belson site is located on an outwash plain draining the Early Algonquin stage of the central Great Lakes (coinciding with the Older Dryas stadial period around 14,000 Cal B.P) southwest across Lower Michigan into the Ohio tributaries. By 13,000 Cal B.P the St. Joseph River had incised multiple channels into this plain. On a terrace just north of a now-abandoned channel, a detailed surface study by Talbot from 2005-2018 showed several flake clusters largely of Attica chert, procured about 235 km southwest of Belson. A study of the surface sample was published by the authors in 2021 and indicated that the points were made with the Clovis technological pattern. Excavations in 2020-21 revealed hundreds of buried flakes and multiple tools in the lower, less-disturbed terrace sediment. Plotting of this material indicates successive occupations below the ploughed deposit and covering more than 30 m2. The buried assemblages are similar to the published surface assemblage with the addition of more small scrapers and manufacturing debris. Several of the buried tools have traces of proteins from a range of mammals, suggesting a broad-spectrum subsistence strategy. The documentation of a succession of little disturbed deposits with precisely recorded micro-debris will allow for testing of models describing settlement choice and developing dynamics of internal site organization. Initial analysis of recovered data provides support for an 'outcrop centered' model where high-quality chert outcrops serve as central places on the landscape. Samples of sediment and charcoal for identification and dating await study.
贝尔森遗址位于一个冲积平原上,该平原位于密歇根州西南部,由早期阿尔冈昆阶(与约 14000 年前的 Older Dryas 冰期相对应)的中央大湖区排水,流入俄亥俄支流。到 13000 年前,圣约瑟夫河已经在这片平原上切入了多个河道。在一个现已废弃的河道以北的梯田上,塔尔博特 2005-2018 年的详细地表研究显示,有几个石片集群主要是阿提卡燧石,这些燧石是从贝尔森西南约 235 公里处采集的。作者在 2021 年发表了对地表样本的研究,表明这些石片是用克洛维斯技术模式制作的。2020-21 年的挖掘揭示了数百个埋藏的石片和多个工具,位于较低、受干扰较小的梯田沉积物中。对这些材料的绘图表明,在被耕种的沉积物以下有连续的居住点,覆盖面积超过 30 平方米。埋藏的组合与已发表的地表组合相似,增加了更多的小型刮刀和制造废料。一些埋藏的工具上有来自多种哺乳动物的蛋白质痕迹,表明存在广泛的生存策略。对一系列受干扰较小的沉积物的详细记录和微碎片的记录,将允许测试描述定居点选择和内部地点组织发展动态的模型。对回收数据的初步分析为“露头中心”模型提供了支持,在该模型中,高质量的燧石露头作为景观上的中心地点。用于鉴定和年代测定的沉积物和木炭样本有待研究。