中西伯利亚旧石器晚期的细石器文化———兼谈与中国北方的联系

权乾坤, 阿尔杰米耶夫·叶甫盖尼, 武仙竹. 中西伯利亚旧石器晚期的细石器文化———兼谈与中国北方的联系[J]. 第四纪研究, 2017, 37(4): 797-804. doi: 10.11928/j.issn.1001-7410.2017.04.12
引用本文: 权乾坤, 阿尔杰米耶夫·叶甫盖尼, 武仙竹. 中西伯利亚旧石器晚期的细石器文化———兼谈与中国北方的联系[J]. 第四纪研究, 2017, 37(4): 797-804. doi: 10.11928/j.issn.1001-7410.2017.04.12
权乾坤, 阿尔杰米耶夫·叶甫盖尼, 武仙竹. 中西伯利亚旧石器晚期的细石器文化———兼谈与中国北方的联系[J]. 第四纪研究, 2017, 37(4): 797-804. doi: 10.11928/j.issn.1001-7410.2017.04.12 Quan Qiankun, Artemyev Ye, Wu Xianzhu. CENTRAL SIBERIAN LATE PALEOLITHIC MICROLITHIC CULTURE——AND TALK WITH THE LINK IN NORTHERN CHINA[J]. Quaternary Sciences, 2017, 37(4): 797-804. doi: 10.11928/j.issn.1001-7410.2017.04.12
Citation: Quan Qiankun, Artemyev Ye, Wu Xianzhu. CENTRAL SIBERIAN LATE PALEOLITHIC MICROLITHIC CULTURE——AND TALK WITH THE LINK IN NORTHERN CHINA[J]. Quaternary Sciences, 2017, 37(4): 797-804. doi: 10.11928/j.issn.1001-7410.2017.04.12

中西伯利亚旧石器晚期的细石器文化———兼谈与中国北方的联系

  • 基金项目:

    重庆市社会科学规划项目"长江三峡地区旧石器文化资源及价值研究"(批准号:2016YBLS102)资助

详细信息
    作者简介:

    权乾坤  男  31岁  俄罗斯西伯利亚联邦大学博士研究生  旧石器考古专业  E-mail:jeffqqk@gmail.com

  • 中图分类号: K876.2;K871.11

CENTRAL SIBERIAN LATE PALEOLITHIC MICROLITHIC CULTURE——AND TALK WITH THE LINK IN NORTHERN CHINA

  • 俄罗斯中西伯利亚叶尼塞河流域,保存有丰富的旧石器时代古文化遗址。其中旧石器时代晚期含有细石器的古文化遗址有43处,出土细石器标本近2000件。本文通过中西伯利亚地区细石器文化材料的全面整理,对其从14C测年、地层学相对年代分析等进行时代早晚排序,全面介绍该地区细石器文化遗址的时空分布规律。总体观察中西伯利亚地区细石器文化概貌,重点介绍了卡缅内洛克(Каменный)遗址、利斯特文卡遗址(Лиственка)遗址细石器。通过中西伯利亚地区所出土细石器与中国北方地区细石器文化的初步对比,认识到中国北方地区和中西伯利亚地区细石叶工业技术上具有密切文化传统关系,均在旧石器时代晚期同时出现选择优质石料生产细石器的工业传统;但二者之间也存在有一定的区域差异性,如中国北方地区细石器组合中以细石核和尖状器比例较高,而中西伯利亚地区细石器组合中则以细石叶比例较高。这些区域差异性可能是不同地点石质材料和生产方式差异所产生,但也可能是不同经济形态(畜牧经济、渔猎解决、农业经济)在生产工具上的体现。如果用技术扩散和文化传播的视角看(均存在间接打击法生产的细石器;细石器各种类型均存在,只是在石器组合中所占比例不同),在旧石器时代晚期时,中国北方地区和西伯利亚地区旧石器工业生产,正出现标准化、趋同化发展现象。进一步加强西伯利亚地区和中国北方地区旧石器文化文化关系的研究,对探讨早期人类对不同环境的适应性及其生活方式、人类迁徙与区域文化交流等,具有非常重要的学术价值。

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  • 图 1 

    卡缅内洛克遗址细石叶石核

    Figure 1. 

    Microcores from Kamennyylog site

    图 2 

    利斯特文卡遗址细石叶石核-(地表采集)

    Figure 2. 

    Microcores form Listvenka site

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出版历程
收稿日期:  2017-02-05
修回日期:  2017-05-10
刊出日期:  2017-07-30

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