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首页> 外文期刊>Quaternary International >Neolithic residential patterns in the southern Caucasus: Radiocarbon analysis of rebuilding cycles of mudbrick architecture at Goytepe, west Azerbaijan
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Neolithic residential patterns in the southern Caucasus: Radiocarbon analysis of rebuilding cycles of mudbrick architecture at Goytepe, west Azerbaijan

机译:高加索南部的新石器时代居住模式:阿塞拜疆西部戈特佩的泥砖建筑重建周期的放射性碳分析

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摘要

Neolithization took place in the southern Caucasus at the beginning of the sixth millennium BC, most likely as part of the expansion of the Neolithic socioeconomy from the Middle East, where the food-production economy had been established at least a few thousand years earlier. However, local adaptation and indigenous cultural development are also likely to have played important roles in this process, by which distinct Neolithic ways of life emerged in the southern Caucasus. This study investigated one possible local aspect of the residential system, referring to archaeological evidence from Goytepe, a major Neolithic settlement of the early sixth millennium BC in Azerbaijan. Using a Bayesian analysis of 45 radiocarbon dates from different occupation levels of this 11 m thick mound, we established a high-resolution chronology of this settlement. Moreover, the analysis of the main trench dates, spanning from ca. 5650 to 5460, revealed a uniquely short rebuilding cycle for mudbrick buildings, an estimated average of 11.4 years, which is far shorter than expected for mudbrick buildings in the Neolithic of the Middle East in general. This finding provides an important piece of evidence for considering a particular type of residential pattern in the Neolithic culture of the southern Caucasus. To test that view, we refer to ethnoarchaeological models and theories of site-formation processes. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:新石器时代发生于公元前六千年初在高加索南部,这很可能是新石器时代社会经济从中东扩张的一部分,那里至少在几千年前就建立了粮食生产经济。但是,当地的适应和土著文化的发展也可能在这一过程中发挥了重要作用,高加索南部出现了新石器时代独特的生活方式。这项研究参考了Goytepe的考古证据,Goytepe是公元前六千年初期在阿塞拜疆的一个主要新石器时代的定居点,研究了居民系统的一个可能的局部方面。通过对这11 m厚丘的不同占领水平的45个放射性碳年代进行贝叶斯分析,我们建立了该沉降的高分辨率年代学。此外,对主要海沟日期的分析,范围从ca.从5650到5460,揭示了泥砖建筑的独特的短重建周期,估计平均为11.4年,这比中东新石器时代的泥砖建筑的预期要短得多。这一发现为考虑高加索南部新石器时代文化中特定类型的居住模式提供了重要的证据。为了检验这种观点,我们参考了民族考古学模型和场所形成过程的理论。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

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