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首页> 外文期刊>Quaternary International >Were European steppe bison migratory? ~(18)O,~(13)C and Sr intra-tooth isotopic variations applied to a palaeoethological reconstruction
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Were European steppe bison migratory? ~(18)O,~(13)C and Sr intra-tooth isotopic variations applied to a palaeoethological reconstruction

机译:欧洲草原野牛会迁徙吗? 〜(18)O,〜(13)C和Sr齿内同位素变异应用于古人类学重建

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This paper focuses on the palaeoethological study of steppe bison {Bison priscus), a Eurasiatic species that disappeared at the end of the Pleistocene. In the Southern steppe of Eastern Europe, this large bovid seems to have been a keystone species during the late Pleistocene, where it is omnipresent in archaeozoological assemblages and can constitute spectacular bone accumulations. Based on the principles of actualism, which assume that modern animal biology and their behavioural adaptations can be applied to the past, different models of bison palaeoethological reconstructions have been proposed to explain this important occurrence of bison in East European archaeological records. Considering the variability of extant bison behaviour, it appeared necessary to undertake a direct reconstruction of the behaviour of fossil bison, to assess how they were targeted. In order to reconstruct steppe bison ecology and habits stable isotope analyses were conducted of tooth enamel carbonate of 25 individuals from Amvrosievka, a Late Pleistocene (~ 18,500 BP) archaeological site complex from Eastern Ukraine. Intra- and inter-individual variations in the stable oxygen, carbon and strontium isotope composition of tooth enamel were analysed to reconstruct the feeding behaviour and seasonal movements of steppe bison. This is the first large scale multi-proxy study of its kind for a Pleistocene cohort. The results show that bison δ~(13)C values are wholly consistent with an exclusively C_3 plant diet, typical of steppe/grassland environments, with a likely consumption of lichen during the cold season. δ~(18)O, δ~(13)C and ~(87)Sr/~(86)Sr values are typical of sedentary bison herds, with limited inter-seasonal movement. These results challenge the previous assumption that Pleistocene bison of the East European steppe were migratory, demonstrating instead that they occupied limited ranges, with no long distance seasonal movement, and that they occasionally incorporated low nutrient foods in their diet. These new palaeobiological results confirm the ecological and behavioural plasticity of bison and have important implications for archaeologists studying hunter-gatherers since human acquisition strategies are directly related to the social, seasonal and spatial behaviour of prey species. This research demonstrates that direct reconstructions of the eco-ethology of fossil prey species are essential, therefore, before attempting to make inferences about the hunting tactics and subsistence strategies developed by Prehistoric hunters.
机译:本文着重研究草原野牛(Bison priscus)的古人类学研究,该草原是一种在更新世末期消失的欧亚物种。在东欧南部的草原上,这种巨大的牛津似乎是更新世晚期的基石物种,在考古学研究中无处不在,可以构成壮观的骨骼堆积。基于现实主义的原理(假定现代动物生物学及其行为适应可以应用于过去),提出了不同的野牛古生态重建模型来解释东欧考古记录中这种重要的野牛发生情况。考虑到现存野牛行为的可变性,似乎有必要对化石野牛的行为进行直接重建,以评估其目标。为了重建草原野牛的生态学和生活习性,对来自乌克兰东部晚更新世(〜18,500 BP)考古遗址Amvrosievka的25个人的牙釉质碳酸盐进行了同位素分析。分析了牙釉质中稳定的氧,碳和锶同位素组成的个体内和个体间差异,以重建草原野牛的摄食行为和季节性运动。这是针对更新世的同类研究中的首次大规模多代理研究。结果表明,野牛的δ〜(13)C值与草原/草地环境典型的仅C_3植物饮食完全一致,在寒冷季节可能会消耗地衣。久坐的野牛群的δ〜(18)O,δ〜(13)C和〜(87)Sr /〜(86)Sr值是典型的,且季节间运动有限。这些结果挑战了以前的假设,即东欧草原的更新世野牛具有迁徙性,这表明它们占据了有限的范围,没有长距离的季节性运动,并且偶尔在饮食中掺入了低营养的食物。这些新的古生物学结果证实了野牛的生态和行为可塑性,并且由于人类的获取策略与猎物的社会,季节和空间行为直接相关,因此对研究猎人-采集者的考古学家具有重要意义。这项研究表明,直接重建化石猎物物种的生态伦理学至关重要,因此,在试图对史前猎人制定的狩猎策略和生存策略做出推断之前。

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  • 来源
    《Quaternary International》 |2012年第31期|p.106-119|共14页
  • 作者单位

    Department of Anthropology, University of Montreal, C.P. 6128, Succ. Centre-ville, Montreal, Quebec H3C 3J7, Canada,Department of Prehistory, National Museum of Natural History, UMR 7194 CNRS. 1 r. Panhard, 75013 Paris, France;

    Department of Geosciences, Biogeology, University of Tubingen, Hdlderlinstr. 12, 72074 Tubingen, Germany;

    Department of Anthropology, University of Montreal, C.P. 6128, Succ. Centre-ville, Montreal, Quebec H3C 3J7, Canada;

    Department of Geosciences, Biogeology, University of Tubingen, Hdlderlinstr. 12, 72074 Tubingen, Germany;

    Department of Prehistory, National Museum of Natural History, UMR 7194 CNRS. 1 r. Panhard, 75013 Paris, France;

    Department of Stone Age, Institute of Archaeology, National Ukrainian Academy of Science, 12 Geroiv Stalingrada Ave., 04210 Kyiv - 210, Ukraine;

    Department of Prehistory, National Museum of Natural History, UMR 7194 CNRS. 1 r. Panhard, 75013 Paris, France;

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