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The Palaeolithic cave of Kalamakia (Mani Peninsula) Greece: new insights on the palaeoenvironment using microvertebrates and mesowear analysis of ruminant teeth

机译:希腊卡拉马基亚(马尼半岛)的旧石器时代洞穴:利用微脊椎动物和反刍动物的细观磨损分析对古环境的新见解

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摘要

In the present study, results from the examination of mammalian teeth from the cave of Kalamakia with modern techniques, as well as a qualitative overview of the microvertebrate and lithic material, are presented together with a revision of previous related work done for the site, in order to assess the palaeoenvironmental conditions in the area and the role they played in the Neanderthal's repeated occupation of the cave. Geometric morphometrics analyses performed on the first lower molars of spp. individuals revealed persistent populations of the subgenus Terricola, in which the presence of and are continuous through the stratigraphic units. Mesowear analyses performed on ruminant teeth showed no significant variation in toothwear through time, except for relatively elevated levels of dietary abrasion for the more recent samples. The study of the lithics revealed that Neanderthals visited the cave in alternating short and more permanent episodes of occupation, with the human occupants exhibiting special concern for raw material economy, while exploiting poor raw materials for the construction of their tools. The overview of the microvertebrate remains showed a growing trend towards the upper stratigraphic units, where taxa typical of temperate climate, open woodland and shrubland become more dominant. These results, along with observations derived from previous studies, suggest that temperate climate and open environment were the factors that mainly contributed to making the cave of Kalamakia attractive as a habitation site to the humans of the area.
机译:在本研究中,呈现了采用现代技术对卡拉马基亚洞中的哺乳动物牙齿进行检查的结果,以及对微脊椎动物和石质材料的定性概述,以及对该地点先前所做的相关工作的修订。目的是评估该地区的古环境状况,以及它们在尼安德特人对洞穴的反复占领中所扮演的角色。在spp的第一个较低的臼齿上进行几何形态计量学分析。个体揭示了Terricola属的持续种群,其中地层单元的存在是连续的。在反刍动物牙齿上进行的Mesowear分析表明,随时间的推移,牙齿磨损无显着变化,但最新样本的饮食磨损水平相对较高。对石器的研究表明,尼安德特人以短暂而又永久的占领交替来到洞穴,人类居住者对原材料的经济表现出特别的关注,同时利用不良的原材料来建造工具。微脊椎动物遗骸的概述显示出向上层地层单位发展的趋势,在该地区上层典型的是温带气候,开阔的林地和灌木林。这些结果以及先前研究得出的观察结果表明,温带气候和开放环境是主要因素,使卡拉马基亚洞穴成为该地区人类的栖息地。

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