晚更新世以来西藏古人类迁移与气候变化关系
收稿日期: 2003-09-10
修回日期: 2003-11-20
网络出版日期: 2004-03-25
基金资助
国家社会科学基金资助项目(02BJY031)
Relationship between the Ancients Migration and Climate Change in the Later Period of Late Pleistocene in Tibet
Received date: 2003-09-10
Revised date: 2003-11-20
Online published: 2004-03-25
Supported by
National Social Science Foundation of China, No.02BJY031
根据西藏地区50 KaBP以来18处古人类遗址的发掘资料，整理西藏旧石器中期以来石陶文化的特征，提出了一个“晚更新世以来西藏古人类三次迁移”假说，即五万年以来西藏古文化发生过三次迁移与融合：第一次，50KaBP~10KaBP，居住在藏南定日苏热一带的旧石器古人类向藏北迁移与扩展，形成了藏北旧石器与中石器文化区；第二次，6 KaBP~3.6 KaBP，居住在藏北申扎、双湖一带的中石器古人类沿唐古拉山南麓向东迁移，形成了新石器早期著名的昌都卡若文化，而生活于普兰霍尔的中石器古人类则沿雅鲁藏布江流域向东迁移，形成了林芝文化；第三次，3 KaBP~2.2 KaBP，居住于昌都和林芝的古人类向拉萨和山南一带迁移，促进了藏南新石器晚期文化的繁荣和以雅隆为主的藏文明的兴起，气候变化是这三次文化变迁的主因。
关键词： 西藏；古文化；气候变化； 更新世
王建林,熊伟 . 晚更新世以来西藏古人类迁移与气候变化关系[J]. 地理学报, 2004 , 59(2) : 174 -182 . DOI: 10.11821/xb200402002
Based on examinations of the culture characters from late Paleolithic age to late Neolithic age by math method, we discover three times large-scale ancients remove in history. First, about 50 KaBP-10 KaBP, the southern ancients removed to the north of Tibet. Second, about 6 KaBP-3.6 KaBP, the northern ancients removed to east of Tibet. Third, about 3 KaBP-2.2 KaBP, the eastern ancients removed to the middle part of Tibet. The remove laid the foundation for the formation of later culture in Tibet. We also discover that the climate is the main cause of the ancients' remove. The consequence of the great remove is a fusion of different cultures which produced a new culture, because the migrants served as the crowed is only carrier of the information about the technique and the experience before the appearance of the writing system. Thus the information is expressed by population. We give the method to study the culture remove and change by determining a more similar culture with the given culture via the similar coefficient. Finally, whether or not paleoanthropologic character, especially, the features of are identical between the two cultures.
Key words： Tibet; culture of ancients; climate change
[1] Hou Shizhu. The Archaeological Outline in Tibet. Lhasa: Tibet People's Publishing House, 1991. 15-195.
[侯石柱. 西藏考古大纲. 拉萨: 西藏人民出版社, 1991. 15-195.]
[2] An Zhimin, Yin Zesheng, Li Bingyuan. The Later Paleolithic and Slender Paleolithic of Shengzha and Shuanghu in North Tibet. Archaeology, 1979, (6): 481-491.
[安志敏, 尹泽生, 李炳元. 藏北申扎、双湖的旧石器和细石器. 考古, 1979, (6): 481-491.]
[3] Li Bingyuan, Wang Fubao, Zhang Qingsong. The Quaternary Geology in Tibet. Beijing: Science Press, 1983. 15-109.
[李炳元, 王富葆, 张青松. 西藏第四纪地质. 北京: 科学出版社, 1983. 15-109.]
[4] Gao Youxi, Jiang Shikui, Zhang Yiguang et al. Climate in Tibet. Beijing: Science Press, 1984. 1-32.
[高由禧, 蒋世逵, 张宜光 等. 西藏气候. 北京: 科学出版社, 1984. 1-32.]
[5] Integrated Scientific Suvrey Team of Qinghai-Tibet Plateau, CAS. Ancient Living Things in Tibet. Beijing: Science Press, 1984. 54-75.
[中国科学院青藏高原综合考察队. 西藏古生物. 北京, 科学出版社, 1984. 54-75.]
[6] Yu Xiulin, Ren Xuesong. Multivariate Statistical Analysis. Beijing: Science Press, 1999. 101-114.
[于秀林, 任雪松. 多元统计分析. 北京: 科学出版社, 1999. 101-114.]
[7] Huang Cixuan, Zhang Qingsong. A preliminary study of paleovegetation and paleoclimate in the later period of late Pleistocene in the Bangongco lake region of Tibet. Journal of Natural Resources, 1989, 4(3): 247-253.
[黄赐璇, 张青松. 西藏日土县班公错地区晚更新世晚期植物群与古气候探讨. 自然资源学报, 1989, 4(3): 247-253.]
[8] Xiong Heigang, Zhong Wei, Tashpolat-Tiyip et al. The coupling relationship between the nature and the man in south edge of Tarim Basin. Acta Geographica Sinica, 2000, 55(2): 191-199.
[熊黑钢, 钟巍, 塔西甫拉提 等. 塔里木盆地南缘自然与人文历史变迁的耦合关系. 地理学报, 2000, 55(22): 191-199.]
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