Oxford Radiocarbon Accelerator Unit, University of Oxford, Oxford OX1 3QY, United Kingdom.
Department of Archaeology, University of Southampton, Southampton SO17 1BF, United Kingdom.
Proc Natl Acad Sci U S A. 2023 May 16;120(20):e2204501120. doi: 10.1073/pnas.2204501120. Epub 2023 May 8.
Understanding mobility and landscape use is important in reconstructing subsistence behavior, range, and group size, and it may contribute to our understanding of phenomena such as the dynamics of biological and cultural interactions between distinct populations of Upper Pleistocene humans. However, studies using traditional strontium isotope analysis are generally limited to identifying locations of childhood residence or nonlocal individuals and lack the sampling resolution to detect movement over short timescales. Here, using an optimized methodology, we present highly spatially resolved Sr/Sr measurements made by laser ablation multicollector inductively coupled plasma mass spectrometry along the growth axis of the enamel of two marine isotope stage 5b, Middle Paleolithic Neanderthal teeth (Gruta da Oliveira), a Tardiglacial, Late Magdalenian human tooth (Galeria da Cisterna), and associated contemporaneous fauna from the Almonda karst system, Torres Novas, Portugal. Strontium isotope mapping of the region shows extreme variation in Sr/Sr, with values ranging from 0.7080 to 0.7160 over a distance of c. 50 km, allowing short-distance (and arguably short-duration) movement to be detected. We find that the early Middle Paleolithic individuals roamed across a subsistence territory of approximately 600 km, while the Late Magdalenian individual parsimoniously fits a pattern of limited, probably seasonal movement along the right bank of the 20-km-long Almonda River valley, between mouth and spring, exploiting a smaller territory of approximately 300 km. We argue that the differences in territory size are due to an increase in population density during the Late Upper Paleolithic.
了解移动性和景观利用对于重建生存行为、范围和群体规模非常重要,它可能有助于我们理解上更新世人类不同群体之间生物和文化相互作用的动态等现象。然而,使用传统锶同位素分析的研究通常仅限于识别儿童时期居住地或非本地个体的位置,并且缺乏检测短时间尺度内运动的采样分辨率。在这里,我们使用优化的方法,沿着两个海洋同位素阶段 5b、中更新世尼安德特人牙齿(Gruta da Oliveira)、冰川期晚期、马格达林晚期人类牙齿(Galeria da Cisterna)的釉质生长轴,以及来自葡萄牙托雷斯诺瓦斯杏仁洞系统的相关同期动物群,进行了激光烧蚀多接收电感耦合等离子体质谱法的高度空间分辨率 Sr/Sr 测量。该地区的锶同位素映射显示 Sr/Sr 存在极端变化,在 50 公里的距离内,值从 0.7080 到 0.7160 不等,允许检测到短距离(可以说是短时间)的运动。我们发现,早期中更新世个体在大约 600 公里的生存领域中漫游,而马格达林晚期个体则合理地符合沿 20 公里长的 Almonda 河谷右岸、河口和泉之间进行有限、可能季节性运动的模式,利用大约 300 公里的较小领地。我们认为,领地规模的差异是由于晚更新世人口密度的增加所致。