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首页> 外文期刊>Quaternary International >Emine-Bair-Khosar Cave in the Crimea, a huge bone accumulation of Late Pleistocene fauna
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Emine-Bair-Khosar Cave in the Crimea, a huge bone accumulation of Late Pleistocene fauna

机译:克里米亚的Emine-Bair-Khosar洞穴,晚更新世动物的巨大骨骼堆积

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摘要

The Crimean Mountains are well known from the abundance of Middle and Late Palaeolithic sites and palaeontological remains recovered from cultural layers in caves and rockshelters. The fossil-bearing deposits of Emine-Bair-Khosar Cave, located at the elevation of 1000 m on the Chatyrdag Plateau, yielded a very diverse and numerous vertebrate remains that widen the knowledge of Late Pleistocene faunal diversity in the Crimea. The assemblage comprised in total almost 50 species of vertebrates. Studies included geomorphological, geological and stratigraphic analyses as well AMS ~(14)C dating. Faunal remains were present in ten palaeontological sites. The main bone accumulation (section Ba2) was deposited during Middle Valdai or Vytachiv (MIS 3) interstadial, and including a long time gap, to the end of the Pleistocene and the Holocene. Comparison of the Emine-Bair-Khosar fauna with vertebrate faunas of other Crimean sites showed a remarkable stability in the faunal composition and frequency during the whole MIS 3 interstadial. Steppe and other open-country species dominated in the compared assemblages, while boreal-tundra species were far less numerous. Inhabitants of forests, including red deer and some rodents, were stable members of fossil assemblages.
机译:克里米亚山脉以中,晚期旧石器时代遗址的丰富而闻名,古生物学遗迹可从洞穴和石棚中的文化层中回收。位于Chatyrdag高原海拔1000 m的Emine-Bair-Khosar洞穴的化石沉积物产生了非常多样的脊椎动物遗骸,拓宽了克里米亚晚更新世动物群多样性的知识。该组合总共包括近50种脊椎动物。研究包括地貌,地质和地层分析以及AMS〜(14)C测年。在十个古生物学遗址中存在动物遗骸。主要的骨堆积(截面Ba2)是在中瓦尔代或维塔希夫(MIS 3)间期沉积的,包括很长的时间间隔,直到更新世和全新世末期。将Emine-Bair-Khosar动物群与其他克里米亚半岛站点的脊椎动物区系进行比较表明,在整个MIS 3陆间期,动物区系组成和频率都具有显着的稳定性。在比较的种群中,草原和其他野外物种占主导地位,而寒带苔原物种则少得多。森林居民,包括马鹿和一些啮齿动物,是化石组合的稳定成员。

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  • 来源
    《Quaternary International》 |2013年第23期|151-160|共10页
  • 作者单位

    Department of Physical Geography and Natural Management, Geographical Faculty, Chernivtsi Yuriy Fedkovych National University, Kotsubynskogo 2, 58012 Chernivtsi, Ukraine,Ukrainian Institute of Speleology and Karstology, 4 Prospect Vemadskogo, Simferopol 95007, Ukraine;

    Department of Palaeozoology, Zoological Institute, University of Wroclaw, Sienkiewicza 21, 50-335 Wroclaw, Poland;

    Department of Palaeozoology, Zoological Institute, University of Wroclaw, Sienkiewicza 21, 50-335 Wroclaw, Poland;

    Palaeontological Museum, National Museum of Natural History, Str. Bogdan Khmelnytskyi 75, Kyjiv 01030, Ukraine;

    Department of Palaeozoology, Zoological Institute, University of Wroclaw, Sienkiewicza 21, 50-335 Wroclaw, Poland;

    Department of Natural Sciences, Transylvanian Museum Society (EME), 2-4 Napoca Street, Cluj-Napoca 400009, Romania;

    Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Slawkowska 17, 30-611 Krakow, Poland;

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