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爱沙尼亚考古动物学材料的多同位素分析(约公元 200-1800 年):食物网和地理区域之间的变化。

Multi-isotopic analysis of zooarchaeological material from Estonia (ca. 200-1800 CE): Variation among food webs and geographical regions.

机构信息

Archaeological Research Collection, Tallinn University, Tallinn, Estonia.

Institute of History and Archaeology, University of Tartu, Tartu, Estonia.

出版信息

PLoS One. 2022 Dec 27;17(12):e0279583. doi: 10.1371/journal.pone.0279583. eCollection 2022.

Abstract

To better comprehend the dietary practices of past populations in the Eastern Baltic region we have created temporally and geographically restricted baselines for the time period of 200-1800 CE. In this multi-isotopic analysis, we report new δ13C, δ15N and δ34S values for 251 faunal bone collagen samples from various archaeological contexts in Estonia representing the most comprehensive set of Iron Age, Medieval and Early Modern Period faunal stable isotope values to date. The results map out the local carbon and nitrogen baselines and define isotopic ranges of local terrestrial, avian and aquatic fauna. We also demonstrate the potential application of sulfur stable isotope analysis in archaeological research. The results demonstrate a clear distinction between δ13C and δ34S values of marine and terrestrial species, however, freshwater fish display notable overlaps with both marine and terrestrial ranges for both δ13C and δ34S values. Herbivores show variation in δ34S values when grouped by region, explained by differences in the local biotopes. This study is the first attempt to connect the Eastern Baltic isotopic baselines and provides more detailed temporal and geographical references to study the local ecologies and interpret the human data.

摘要

为了更好地理解东波罗的海地区过去人群的饮食行为,我们为公元 200-1800 年期间创建了时间和地理上受限的基线。在这项多稳定同位素分析中,我们报告了来自爱沙尼亚不同考古背景的 251 个动物骨骼胶原样本的新的 δ13C、δ15N 和 δ34S 值,这是迄今为止针对铁器时代、中世纪和早期现代时期动物稳定同位素值最全面的数据集。结果描绘了当地的碳和氮基线,并定义了当地陆地、鸟类和水生动物群的同位素范围。我们还展示了硫稳定同位素分析在考古研究中的潜在应用。结果表明,海洋和陆地物种的 δ13C 和 δ34S 值之间存在明显差异,然而,淡水鱼类的 δ13C 和 δ34S 值与海洋和陆地范围都有显著重叠。当按地区分组时,食草动物的 δ34S 值存在差异,这是由当地生物区系的差异造成的。这项研究首次尝试将东波罗的海的同位素基线联系起来,并提供更详细的时间和地理参考,以研究当地生态系统并解释人类数据。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/df16/9794088/27a71dbbd1da/pone.0279583.g001.jpg

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