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对人类骨骼磷酸盐的氧同位素分析证明了考古群体中的断奶年龄。

Oxygen isotope analysis of human bone phosphate evidences weaning age in archaeological populations.

作者信息

Britton Kate, Fuller Benjamin T, Tütken Thomas, Mays Simon, Richards Michael P

机构信息

Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, 04103, Leipzig, Germany.

Department of Archaeology, University of Aberdeen, St. Mary's Building, Aberdeen, Scotland AB24 3UF, UK.

出版信息

Am J Phys Anthropol. 2015 Jun;157(2):226-41. doi: 10.1002/ajpa.22704. Epub 2015 Feb 11.

DOI:10.1002/ajpa.22704
PMID:25677569
Abstract

Here we report bone phosphate oxygen (δ(18)Op) values from perinates/neonates and infants (<3.5 years; n = 32); children (4-12 years; n = 12); unsexed juveniles (16-18 years; n = 2); and adult bones (n = 17) from Wharram Percy, North Yorkshire, England, in order to explore the potential of this method to investigate patterns of past breastfeeding and weaning. In prior studies, δ(15)N and δ(13)C analyses of bone collagen have been utilized to explore weaning age in this large and well-studied assemblage, rendering this material highly appropriate for the testing and development of this alternative method targeting the inorganic phase of bone. Data produced reveal (18)O-enrichment in the youngest perinatal/neonatal and infant samples, and an association between age and bone δ(18)Op (and previously-published δ(15)N values), with high values in both these isotope systems likely due to breastfeeding. After the age of 2-3 years, δ(18)Op values are lower, and all children between the ages of 4 and 12, along with the vast majority of sub-adults and adults sampled (aged 16 to >50 years), have δ(18)Op values consistent with the consumption of local modern drinking water. The implications of this study for the reconstruction of weaning practices in archaeological populations are discussed, including variations observed with bone δ(15)Ncoll and δ(18)Op co-analysis and the influence of culturally-modified drinking water and seasonality. The use of this method to explore human mobility and palaeoclimatic conditions are also discussed with reference to the data presented.

摘要

在此,我们报告了来自英格兰北约克郡沃勒姆·珀西的围产期/新生儿、婴儿(小于3.5岁;n = 32)、儿童(4 - 12岁;n = 12)、未区分性别的青少年(16 - 18岁;n = 2)以及成人骨骼(n = 17)的骨磷酸盐氧(δ(18)Op)值,以便探究该方法在研究过去母乳喂养和断奶模式方面的潜力。在先前的研究中,已利用骨胶原蛋白的δ(15)N和δ(13)C分析来探究这个经过大量深入研究的群体的断奶年龄,这使得该材料非常适合用于测试和开发这种针对骨无机相的替代方法。所产生的数据显示,最年幼的围产期/新生儿和婴儿样本中存在(18)O富集现象,并且年龄与骨δ(18)Op(以及先前公布的δ(15)N值)之间存在关联,这两种同位素系统中的高值可能是由于母乳喂养所致。在2 - 3岁之后,δ(18)Op值较低,所有4至12岁的儿童以及绝大多数抽样的亚成年人和成年人(年龄在16岁至50岁以上)的δ(18)Op值与当地现代饮用水的消耗情况一致。本文讨论了这项研究对于重建考古人群断奶习俗的意义,包括在骨δ(15)Ncoll和δ(18)Op联合分析中观察到的变化以及文化改良饮用水和季节性的影响。还结合所呈现的数据讨论了使用这种方法来探究人类流动性和古气候条件的情况。

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