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在匈牙利大平原,史前农民的饮食变化历经 5000 年。

5000 years of dietary variations of prehistoric farmers in the Great Hungarian Plain.

机构信息

School of Archaeology, University College Dublin, Dublin, Ireland.

Earth Institute, University College Dublin, Dublin, Ireland.

出版信息

PLoS One. 2018 May 10;13(5):e0197214. doi: 10.1371/journal.pone.0197214. eCollection 2018.

Abstract

The development of farming was a catalyst for the evolution of the human diet from the varied subsistence practices of hunter-gatherers to the more globalised food economy we depend upon today. Although there has been considerable research into the dietary changes associated with the initial spread of farming, less attention has been given to how dietary choices continued to develop during subsequent millennia. A paleogenomic time transect for 5 millennia of human occupation in the Great Hungarian Plain spanning from the advent of the Neolithic to the Iron Age, showed major genomic turnovers. Here we assess where these genetic turnovers are associated with corresponding dietary shifts, by examining the carbon and nitrogen stable isotope ratios of 52 individuals. Results provide evidence that early Neolithic individuals, which were genetically characterised as Mesolithic hunter-gatherers, relied on wild resources to a greater extent than those whose genomic attributes were of typical Neolithic European farmers. Other Neolithic individuals and those from the Copper Age to Bronze Age periods relied mostly on terrestrial C3 plant resources. We also report a carbon isotopic ratio typical of C4 plants, which may indicate millet consumption in the Late Bronze Age, despite suggestions of the crop's earlier arrival in Europe during the Neolithic.

摘要

农业的发展是人类饮食从狩猎采集者多样化的生存方式向我们今天所依赖的更全球化的粮食经济转变的催化剂。尽管人们已经对与农业最初传播相关的饮食变化进行了大量研究,但对于在随后的几千年里饮食选择如何继续发展,关注较少。对匈牙利大平原上 5000 年人类居住的古基因组时间剖面的研究,跨越了从新石器时代到铁器时代,显示出主要的基因组更替。在这里,我们通过检查 52 个人的碳和氮稳定同位素比值,评估这些遗传更替与相应饮食变化的关联。研究结果表明,早期的新石器时代个体在遗传上被认为是旧石器时代的狩猎采集者,他们比那些具有典型新石器时代欧洲农民遗传特征的个体更依赖于野生资源。其他新石器时代的个体和铜器时代到青铜时代的个体主要依赖于陆地 C3 植物资源。我们还报告了一个典型的 C4 植物的碳同位素比值,这可能表明在青铜时代晚期有小米的消费,尽管有迹象表明这种作物在新石器时代更早地传入欧洲。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9925/5944993/497d273bce42/pone.0197214.g001.jpg

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