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Isotope values of the bioavailable strontium in inland southwestern Sweden—A baseline for mobility studies

机译:瑞典西南内陆的生物利用锶的同位素值—迁移率研究的基准

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摘要

The inland area of southwestern Sweden is well known for its well-preserved archaeological animal and human remains dating back to the Mesolithic and Neolithic (10000–4000 and 4000–1700 BC). They allow application of multiple bioarchaeological methods, giving insights into various and complementary aspects of prehistoric human life, as well as economic and social structures. One important aspect concerns human mobility and its relation to social networks and to circulation of objects. Here, strontium isotope analysis plays a crucial role. The present study aims to construct a strontium isotope baseline of southwestern Sweden with considerably greater coverage and higher resolution than previously published data. As the region has been affected by glacial events, the relation between bedrock geology and isotope signals of the bioavailable strontium in such areas is given special attention. We determined strontium isotope ratios for 61 water and five archaeological animal samples, and combined the data with previous measurements of two water and 21 non-domestic faunal samples. The results reveal a complex pattern. Several areas with distinct baseline ranges can be distinguished, although with overlaps between some of them. Overall, the bioavailable strontium isotope signals mirror the basement geology of the region. The highest ratios occur in the geologically oldest eastern parts of the Precambrian terrain, while lower ratios are found in the western part, and the lowest ratios occur in the youngest Paleozoic areas. At the same time, there are minor deviations compared to the underlying bedrock, due to glacial transport, overlying sediments, and local intrusions of younger rocks. The background data set now available allows for more nuanced and detailed interpretations of human and animal mobility in the region, in particular by identification of subregions with differing strontium isotope ratios within the Precambrian province. Also, we can now identify long distance mobility with greater confidence.
机译:瑞典西南部的内陆地区以保存完好的考古动物和人类遗骸而闻名,可追溯至中石器时代和新石器时代(公元前10000-4000年和4000-1700年)。它们允许应用多种生物考古方法,从而深入了解史前人类生活的各个方面和互补方面以及经济和社会结构。一个重要方面涉及人类流动性及其与社交网络和物体流通的关系。在这里,锶同位素分析起着至关重要的作用。本研究旨在构建瑞典西南部的锶同位素基线,其覆盖范围和分辨率比以前公布的数据高得多。由于该地区受到冰川事件的影响,因此在这些地区中,基岩地质与生物可利用锶同位素信号之间的关系受到特别关注。我们确定了61种水和5种考古动物样品中锶的同位素比率,并将这些数据与2种水和21种非家畜动物样品的先前测量值结合在一起。结果揭示了一个复杂的模式。可以区分基线范围不同的几个区域,尽管其中一些区域重叠。总体而言,可生物利用的锶同位素信号反映了该地区地下室的地质情况。比率最高的发生在前寒武纪地形中地质最古老的东部,而比率较低的发生在西部,而比率最低的发生在最年轻的古生代地区。同时,由于冰川运移,上覆沉积物和较年轻岩石的局部侵入,与下伏基岩相比存在较小偏差。现在可用的背景数据集可对该地区的人类和动物活动性进行更细致和详细的解释,特别是通过识别前寒武纪省内锶同位素比率不同的次区域。而且,我们现在可以更有信心地确定远距离移动性。

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