Center for Bioarchaelogical Research, School of Human Evolution and Social Change, Arizona State University, Tempe, AZ, United States of America.
School of Earth and Space Exploration, Arizona State University, Tempe, AZ, United States of America.
PLoS One. 2020 Feb 24;15(2):e0229687. doi: 10.1371/journal.pone.0229687. eCollection 2020.
Radiogenic strontium isotopes (87Sr/86Sr) have long been used in analyses of paleomobility within Mesoamerica. While considerable effort has been expended developing 87Sr/86Sr baseline values across the Maya region, work in central Mexico is primarily focused on the Classic period urban center of Teotihuacan. This study adds to this important dataset by presenting bioavailable 87Sr/86Sr values across central Mexico focusing on the Basin of Mexico. This study therefore serves to expand the utility of strontium isotopes across a wider geographic region. A total of 63 plant and water samples were collected from 13 central Mexican sites and analyzed for 87Sr/86Sr on a Thermo-Finnigan Neptune multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS). These data were analyzed alongside 16 published 87Sr/86Sr values from two additional sites within the region of interest. A five-cluster k-means model was then generated to determine which regions of the Basin of Mexico and greater central Mexico can and cannot be distinguished isotopically using 87Sr/86Sr values. Although the two clusters falling within the Basin of Mexico overlap in their local 87Sr/86Sr ranges, many locations within the Basin are distinguishable using 87Sr/86Sr values at the site-level. This study contributes to paleomobility studies within central Mexico by expanding knowledge of strontium isotope variability within the region, ultimately allowing researchers to detect intra-regional residential mobility and gain a greater understanding of the sociopolitical interactions between the Basin of Mexico and supporting outlying regions of central Mexico.
放射性锶同位素(87Sr/86Sr)长期以来一直被用于分析中美洲古迁移。虽然已经花费了大量精力来开发整个玛雅地区的 87Sr/86Sr 基线值,但墨西哥中部的工作主要集中在特奥蒂瓦坎的古典时期城市中心。本研究通过提供墨西哥中部的生物可用 87Sr/86Sr 值,为这个重要数据集增加了内容,重点是墨西哥盆地。因此,本研究旨在扩大锶同位素在更广泛地理区域的应用。从墨西哥中部的 13 个地点共采集了 63 个植物和水样,并在 Thermo-Finnigan Neptune 多收集电感耦合等离子体质谱仪(MC-ICP-MS)上分析 87Sr/86Sr。这些数据与来自该研究区域内另外两个地点的 16 个已发表的 87Sr/86Sr 值一起进行了分析。然后生成了一个五聚类 k-均值模型,以确定可以和不能使用 87Sr/86Sr 值来区分墨西哥盆地和更大的中墨西哥地区的哪些区域。尽管位于墨西哥盆地内的两个聚类在其局部 87Sr/86Sr 范围内重叠,但在盆地内的许多地点都可以使用 87Sr/86Sr 值在现场水平上进行区分。本研究通过扩展该地区锶同位素变异性方面的知识,为中墨西哥的古迁移研究做出了贡献,最终使研究人员能够检测到区域内的居住迁移,并更好地了解墨西哥盆地与支持中墨西哥外围地区之间的社会政治互动。