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干旱区地理 ›› 2013, Vol. 36 ›› Issue (6): 971-978.

• 地表过程研究 •    下一篇

全新世大暖期对青藏高原东北缘人类活动的影响

侯光良1,赖忠平2,孙永娟2,P.Jeffrey BRANTINGHAM3   

  1. (1    青海师范大学青海省自然地理与环境过程重点实验室, 青海    西宁    810008;2    中国科学院青海盐湖研究所,青海    西宁    810008;3    Department of Anthropology,University of California Los Angeles,Los Angeles,CA 90095,USA)
  • 收稿日期:2012-12-27 修回日期:2013-03-04 出版日期:2013-11-25
  • 作者简介:侯光良(1972-),博士,教授,主要从事环境演变与人类活动研究. Emal:hgl20@163.com
  • 基金资助:

    国家自然科学基金(41161018);教育部人文社会科学研究青年基金项目(10YJCZH041)资助

Impact of the Holocene Climatic Optimum on human activities in the northeastern margin of the Qinghai-Tibetan Plateau

HOU  Guang-liang1,LAI  Zhong-ping2,SUN  Yong-juan2,P.Jeffrey BRANTINGHAM3   

  1. (1   Key Laboratory of Qinghai-Tibetan Plateau Environment and Resource, MOE, School of Life and Geographic Science, Qinghai Normal University, Xining, Qinghai  810008;    2   Qinghai Institute of  Salt  Lakes, Chinese Academy of Sciences, Xining   810008, Qinghai, China;3   Department of Anthropology, University of California Los Angeles, Los Angeles, CA 90095, USA)
  • Received:2012-12-27 Revised:2013-03-04 Online:2013-11-25

摘要: 结合环境演变资料与考古发现,全新世大暖期暖湿的气候条件,促进了青藏高原东北缘古文化的发展。表现在:随着全新世大暖期暖湿环境的到来,人类活动强度大大增强;细石器文化活动模式发生显著改变,由晚更新世末期-全新世早期的短暂宿营式居住模式演变为相对固定的聚落模式;暖期中较好的水热条件,刺激了仰韶、马家窑文化在本区东部河谷地区的扩张,在暖期的6~4 ka BP形成了东部河谷地带马家窑文化,西部高原细石器文化并存的区系格局,两种文化体系在共存中交流,在交流中高原细石器文化掌握了农业种植、使用了陶器,全面推动了高原土著文化进入新石器。

关键词: 全新世大暖期, 青藏高原东北缘, 人类活动

Abstract: By combining climate change data and archaeological discoveries,evidence shows that warm and wet conditions during the Holocene Climatic Optimum promoted the development of ancient cultures along the northeastern margin of the Qinghai-Tibetan Plateau. This scenario is manifested in the following categories:(1) human activities greatly increased along with the warming temperatures during the Holocene Climatic Optimum;(2)the mode of microlithic culture activity changed significantly from the late Pleistocene to the early Holocene as the settlement patterns developed from temporary camps into relatively fixed settlements;(3)the improvement of water resources and climate conditions during the warm period stimulated the expansion of Yangshao and Majiayao Cultures in the Eastern Valley. This included the formation of the Eastern Valley Majiayao Culture that coexisted with the Western Plateau Microlithic Cultures between 6 and 4 ka BP. The two coexisting culture systems participated in exchange during which the Weastern Plateau Microlithic Cultures obtained pottery,agriculture,and Neolithic technologies,promoting their entrance into the Neolithic.

Key words: Holocene Climatic Optimum, the northwest margin of the Qinghai-Tibetan Plateau, human activities

中图分类号: 

  • K871. 11