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Paleoenvironment of the Fore-Baikal region in the Karginian interstadial: Results of the interdisciplinary studies of the Bol'shoj Naryn site

机译:Karginian际地带中前贝加尔湖地区的古环境:Bol'shoj Naryn遗址的跨学科研究结果

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摘要

As a result of integrated researches on two Paleolithic sites of the Fore-Baikal region-Bol'shoj Naryn and Gerasimov's, the first representative mammal fauna of the Karginian interstadial been dated and characterized. That provided the basis for reconstructing the paleoenvironments in the Fore-Baikal region during MIS 3. The species composition of the faunal remains recovered from the Bol'shoj Naryn site in the course of five-year excavations since 2003 was examined in details. Since 2010, the cultural layer was studied layer-by-layer (at 5 cm intervals), all the artifacts and faunal remains (of mollusks, birds, and mammals) being described. In addition, the lower, middle and upper parts of cultural layer were sampled for palynological analysis. The geological and paleontological data thus obtained suggest a moderately cold and humid climate in the Fore-Baikal region during MIS 3, with predominant open landscapes of steppes and relatively limited areas under taiga forest, tundra, and wetlands. There are abundant data on significant environmental changes in the Fore-Baikal region during MIS 3 previously obtained by investigators, such as pollen spectra recovered from the Lake Kotokel bottom sediments or faunal remains (including small mammals) excavated from the Bol'shoj Naryn site. The present study, however, differs from the earlier ones in that it included multidisciplinary analysis of a large number of faunal and floral remains recovered from the same section and characterizing the same region. The data thus obtained from the Bol'shoj Naryn site are extremely important for better understanding of the Late Pleistocene environments of the Fore-Baikal region.
机译:由于对前贝加尔河地区的两个旧石器时代遗址进行了综合研究-博尔肖伊·纳林和格拉西莫夫的遗址,确定了Karginian交错带的第一个代表性哺乳动物区系的年代并进行了特征化。这为在MIS 3期间重建贝加尔湖前地区的古环境提供了基础。详细检查了自2003年以来五年发掘过程中从Bol'shoj Naryn遗址回收的动物群的物种组成。自2010年以来,对文化层进行了逐层研究(每隔5厘米),描述了所有的人工制品和动物遗骸(软体动物,鸟类和哺乳动物)。此外,对文化层的下部,中部和上部进行了采样,以进行孢粉分析。如此获得的地质和古生物学数据表明,MIS 3期间前贝加尔湖地区出现了中冷和潮湿的气候,主要是开阔的草原景观,以及针叶林,苔原和湿地以下相对有限的区域。研究人员先前获得的有关MIS 3期间前贝加尔湖地区重大环境变化的大量数据,例如从科托克尔湖底部沉积物或从博尔绍伊·纳林遗址发掘的动物遗体(包括小型哺乳动物)中回收的花粉光谱。但是,本研究与早期研究的不同之处在于,该研究包括对从同一区域回收并表征同一区域的大量动植物和花卉残骸的多学科分析。因此,从Bol'shoj Naryn站点获得的数据对于更好地了解贝加尔湖前区的晚更新世环境极为重要。

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  • 来源
    《Quaternary International》 |2014年第30期|146-155|共10页
  • 作者单位

    Department of Archaeology and Ethnology, Faculty of Letters, Keio University, Tokyo, Japan;

    Geological Institute, Siberian Branch (SB), Russian Academy of Sciences (RUS), Ulan-Ude, Russia;

    Geological Institute, RAS, Moscow, Russia;

    Institute of Geology, Ufa Scientific Centre, RAS, Ufa, Russia;

    Institute of Geology, Ufa Scientific Centre, RAS, Ufa, Russia;

    The University Museum, The University of Tokyo, Tokyo Japan;

    Tokoro Research Laboratory, The University of Tokyo, Kitami, Japan;

    Center for Ainu and Indigenous Studies, Hokkaido University, Sapporo, Japan;

    Center for Ainu and Indigenous Studies, Hokkaido University, Sapporo, Japan;

    Department of Archaeology and Ethnology, Faculty of History, Irkutsk State University, Irkutsk, Russia;

    Department of Archaeology and Ethnology, Faculty of History, Irkutsk State University, Irkutsk, Russia;

    Krasnoyarsk Regional Natural Museum, Krasnoyarsk, Russia;

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