Department of Integrated Biosciences, Graduate School of Frontier Sciences, University of Tokyo, Kashiwa, Chiba 277-8562, Japan.
Am J Phys Anthropol. 2010 Sep;143(1):31-40. doi: 10.1002/ajpa.21287.
Nitrogen stable isotopes analysis of individual bone collagen amino acids was applied to archeological samples as a new tool for assessing the composition of ancient human diets and calibrating radiocarbon dates. We used this technique to investigate human and faunal samples from the Kitakogane shell midden in Hokkaido, Japan (5,300-6,000 cal BP). Using compound-specific nitrogen isotope analysis of individual amino acids, we aimed to estimate i) the quantitative contribution of marine and terrestrial protein to the human diet, and ii) the mean trophic level (TL) from which dietary protein was derived from marine ecosystems. Data were interpreted with reference to the amino acid trophic level (TL(AA)) model, which uses empirical amino acid delta(15)N from modern marine fauna to construct mathematical equations that predict the trophic position of organisms. The TL(AA) model produced realistic TL estimates for the Kitakogane marine animals. However, this model was not appropriate for the interpretation of human amino acid delta(15)N, as dietary protein is derived from both marine and terrestrial environments. Hence, we developed a series of relevant equations that considered the consumption of dietary resources from both ecosystems. Using these equations, the mean percentage of marine protein in the Kitakogane human diet was estimated to be 74%. Although this study is one of the first systematic investigations of amino acid delta(15)N in archeological bone collagen, we believe that this technique is extremely useful for TL reconstruction, palaeodietary interpretation, and the correction of marine reservoir effects for radiocarbon dating.
氮稳定同位素分析个体骨胶原氨基酸被应用于考古样本,作为评估古代人类饮食组成和校准放射性碳年代的新工具。我们使用这项技术研究了日本北海道北小樽贝壳堆积遗址的人类和动物样本(5300-6000 cal BP)。通过对个体氨基酸的复合特异性氮同位素分析,我们旨在估算:i)海洋和陆地蛋白质对人类饮食的定量贡献;ii)人类饮食中的蛋白质来源于海洋生态系统的平均营养级(TL)。数据的解释参考了氨基酸营养级(TL(AA))模型,该模型利用现代海洋动物的氨基酸 δ15N 数据构建数学方程,预测生物体的营养位置。TL(AA) 模型为北小樽的海洋动物提供了合理的 TL 估计值。然而,由于人类的饮食蛋白质既来自海洋又来自陆地,因此该模型不适用于解释人类的氨基酸 δ15N。因此,我们开发了一系列相关的方程,考虑了来自这两个生态系统的饮食资源的消耗。使用这些方程,估计北小樽人类饮食中海洋蛋白质的平均百分比为 74%。尽管这是考古骨骼胶原中首次系统研究氨基酸 δ15N 的研究之一,但我们认为该技术对于 TL 重建、古食谱解释以及放射性碳测年的海洋碳库效应校正非常有用。