Swiss Bell Beaker population dynamics: eastern or southern influences?
Swiss Bell Beaker population dynamics: eastern or southern influences?
复制标题
瑞士贝尔烧杯种群动态：东部还是南部影响？
DOI：
10.1007/s12520-010-0037-9
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发表时间：
2010
影响因子：
2.2
通讯作者：
M. Besse
中科院分区：
文献类型：
--
作者：
J. Desideri;M. Besse
贝尔烧杯复杂的定义，首先是由陶瓷风格在公元前3000年广泛传播到欧洲。它特别大的地理分布引起了不同的解释：一个独特的人口入侵欧洲，长途交换的声望商品，并没有一个真实的贝尔烧杯人口只有其文化成分的扩散。对于瑞士来说，钟形烧杯时期可能是在地中海地区和中欧的影响下发展起来的。生物人类学使得检验第一种假设成为可能，即文化的传播是通过人口迁移实现的。在这里，选择分析牙科非计量学。我们以前的研究牙科nonmetrics支持的想法，为瑞士，在新石器时代中期人口的一定的和谐，和流动性或适度的人口贡献开始在新石器时代的最后，并继续在钟形烧杯时期更激烈。这里的目的是确定在瑞士西部新石器时代结束时人口贡献的来源，更具体地说，在钟形烧杯时期。为了做到这一点，我们比较了瑞士前钟形烧杯，钟形烧杯，和后钟形烧杯人口的牙齿形态，发现不仅在东部地区（捷克共和国和匈牙利），而且在南部地区（法国南部和北方西班牙）的同时代人群。我们现在可以证明，在瑞士西部新石器时代结束时，外部人口影响的轴线显然是南部。
The Bell Beaker complex is defined, above all, by a ceramic style widespread across Europe during the 3rd millennium BC. Its particularly large geographic distribution has provoked different interpretations: a unique population invading Europe, the long-distance exchange of prestige goods, and the absence of a real Bell Beaker population with only the diffusion of its cultural components. For Switzerland, the Bell Beaker period would have developed following influences varying in significance from both the Mediterranean region and Central Europe. Bioanthropology makes it possible to test the first of these hypotheses, which proposes the diffusion of a culture by population displacement. Here, the choice was made to analyze dental nonmetrics. Our previous research on dental nonmetrics supports the idea, for Switzerland, of a certain harmony in Middle Neolithic populations, and the mobility or a moderate population contribution beginning in the Final Neolithic and continuing more intensely during the Bell Beaker period. The aim here is to identify the provenance of the population contribution at the end of the western Swiss Neolithic, and more specifically during the Bell Beaker period. To do so, we have compared the dental morphology of Swiss pre-Bell Beaker, Bell Beaker, and post-Bell Beaker populations with that of contemporaneous populations found not only in the eastern sphere (Czech Republic and Hungary), but also in the southern sphere (southern France and northern Spain). We are now able to demonstrate that the axis for external population influences at the end of the western Swiss Neolithic is clearly southern.