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Mobility of middle Holocene foragers in the Cis-Baikal region, Siberia: Individual life history approach, strontium ratios, rare earth and trace elements

机译:西伯利亚顺西贝加尔湖地区中全新世觅食者的流动性:个人生活史方法,锶比,稀土和微量元素

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Previous geochemical work conducted on the materials from the Khuzhir-Nuge ⅩⅣ cemetery on Lake Baikal, Siberia, has demonstrated the effectiveness of using ~(87)Sr/~(86)Sr ratio analysis in interpreting mobility patterns among Early Bronze Age hunter-gatherer groups. The research reported here focuses on six small cemeteries representing the Little Sea and Upper Lena micro-regions as well the Early Neolithic (EN: ca. 8000-7200 cal BP) and Early Bronze Age (EBA: ca. 5200-3400 cal BP) periods, thus expanding both the geographic and chronological scope of the previous work. The reference collection of environmental samples, to document bioavailability of the measured geochemical tracers, was also expanded substantially by inclusion of samples of modern plants and water from Lake Baikal and a number of surrounding rivers. First, second, and third molars of 14 adult individuals were tested for ~(87)Sr/~(86)Sr ratios as well as rare earth and trace element concentrations using LA-ICP-MS. Each human tooth was micro-sampled at four locations along the crown enamel thus providing data of higher temporal resolution relative to a single sampling locus. Geochemical signatures for water, plant and animal bone samples were found to be far more variable across the region than predicted based on the age and type of geologic formations. ~(87)Sr/~(86)Sr ratios for cultural micro-regions proved to overlap significantly and required trace element data to identify more discrete geochemical groups. The level of hunter-gatherer mobility between and within the analyzed micro-regions was found to be significant with individuals recovered from the Upper Lena showing contact with the Little Sea micro-region along the northwest coast of the lake.
机译:先前对西伯利亚贝加尔湖Khuzhir-NugeⅩⅣ墓地的材料进行的地球化学研究表明,使用〜(87)Sr /〜(86)Sr比分析来解释早期青铜时代猎人-采集者的迁移模式是有效的组。这里报道的研究集中在代表小海和上莉娜微区的六个小公墓以及新石器时代早期(EN:大约8000-7200 cal BP)和青铜时代早期(EBA:大约5200-3400 cal BP)时间,从而扩大了以前工作的地理和时间范围。通过记录来自贝加尔湖和许多周围河流的现代植物和水的样品,也大大扩展了用于记录所测地球化学示踪剂生物利用度的环境样品的参考收藏。使用LA-ICP-MS测试了14名成年个体的第一,第二和第三臼齿的〜(87)Sr /〜(86)Sr比以及稀土和痕量元素的浓度。在沿牙釉质的四个位置对每个人的牙齿进行了微采样,从而提供了相对于单个采样位置而言更高的时间分辨率的数据。发现水,植物和动物骨骼样品的地球化学特征在整个地区的变化远比根据年龄和地质构造类型所预测的要大。文化微区的〜(87)Sr /〜(86)Sr比被证明有明显的重叠,需要微量元素数据来识别更多离散的地球化学组。发现在分析的微区域之间和之内的猎人-采集者的流动水平很重要,从上莉娜(Lena)回收的个体显示出与沿湖西北海岸的小海微区域接触。

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