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Microbotanical evidence for the spread of cereal use during the Mesolithic-Neolithic transition in the Southeastern Europe (Danube Gorges): Data from dental calculus analysis

机译:在欧洲东南部(多瑙河峡谷)中的岩石新石器时代过渡期间谷物用途的微胆管证据:来自牙科微积分分析的数据

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Research increasingly suggests that natural and social environments shaped the Neolithic expansion of the farming niche into Europe. The Danube Gorges, on account of its position between the Mediterranean and more temperate regions and the presence of archaeological sites with continuous Mesolithic and Neolithic layers of occupation associated with vast burial grounds is ideal for studying the modality of Neolithization. Previous dietary stable isotope (carbon, nitrogen, and sulphur) studies in the Central Balkan area indicate that many Neolithic humans remained reliant on foraged aquatic resources in the Gorges. Until now, there is no unambiguous evidence of cereal consumption in this region. The possibility that the rich aquatic resources of the Danube river habitats within Central Balkans influenced diet and thus delayed uptake of Neolithic cultigens is unanswered. The extensive skeletal record from sites in the Danube Gorges (Central Balkans) with its long temporal sequence, provides the opportunity to reconstruct plant use during Mesolithic and the Neolithic. To assess when cereals and possibly cultivated plants spread to the region, we analysed the microbotanical remains (starch grains and phytoliths) entrapped in the dental calculus of 81 individuals dating from 9100 to 5500 cal BC, recovered from five sites in the Danube Gorges. This study marks the largest study of dental calculus from this period so far conducted. Added to this, we present new radiocarbon dates (n = 17), bone collagen stable isotope data (delta C-13 and delta N-15; n = 5) and data on caries frequency. This dietary study identifies that the growing of crops commenced in the Early Neolithic circa 6000 cal BC and was brought by farming migrants of north-western Anatolian ancestry into the Danube Gorges. Despite bringing a Neolithic agm-pastoral subsistence practices and cultural novelties in the Gorges, these migrants and their descendants adopted some of the local dietary and cultural traditions, suggesting a mosaic pattern of Neolithization. The resulting data provides a better understanding of the tempo and spread of cereal agriculture practices and the role of cereals in the diet of Danube Gorges inhabitants.
机译:越来越多的研究表明,自然和社会环境决定了新石器时代农业生态位向欧洲的扩张。多瑙河峡谷位于地中海和更温和的地区之间,并且存在着考古遗址,这些遗址具有连续的中石器时代和新石器时代的占领层,以及广阔的墓地,因此是研究新石器时代形态的理想之地。此前在巴尔干半岛中部地区进行的饮食稳定同位素(碳、氮和硫)研究表明,许多新石器时代的人类仍然依赖于峡谷中的觅食水生资源。到目前为止,还没有明确的证据表明该地区有谷物消费。巴尔干半岛中部多瑙河栖息地丰富的水资源可能会影响饮食,从而推迟新石器时代文化的吸收,这一点尚未得到解答。多瑙河峡谷(巴尔干半岛中部)遗址的大量骨骼记录及其漫长的时间序列,为重建中石器时代和新石器时代的植物用途提供了机会。为了评估谷物和可能种植的植物何时传播到该地区,我们分析了从多瑙河峡谷的五个地点采集的81个个体的牙石中残留的微生物遗骸(淀粉粒和植硅体),这些遗骸的年龄为公元前9100至5500 cal。这项研究标志着迄今为止对牙石进行的最大规模的研究。除此之外,我们还提供了新的放射性碳年代(n=17)、骨胶原蛋白稳定同位素数据(δC-13和δn-15;n=5)和龋齿频率数据。这项饮食研究表明,作物的生长始于约公元前6000年的新石器时代早期,由安纳托利亚西北部祖先的农业移民带入多瑙河峡谷。尽管这些移民及其后代在三峡带来了新石器时代的农耕生活方式和文化新奇,但他们还是采纳了当地的一些饮食和文化传统,这表明了新石器时代的马赛克模式。由此产生的数据可以更好地了解谷物农业实践的节奏和传播,以及谷物在多瑙河峡谷居民饮食中的作用。

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