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青藏高原西南部仲巴地区细石器人类活动的时代探讨

李拓宇 伍永秋 杜世松 黄文敏 蒿承智

北京师范大学学报(自然科学版)2016,Vol.52Issue(1):91-96,6.
北京师范大学学报(自然科学版)2016,Vol.52Issue(1):91-96,6.DOI:10.16360/j.cnki.jbnuns.2016.01.018

青藏高原西南部仲巴地区细石器人类活动的时代探讨

Age of Microlith human activities in Zhongba area, southwestern margin of Qinghai-Tibet Plateau

李拓宇 1伍永秋 2杜世松 3黄文敏 1蒿承智2

作者信息

  • 1. 北京师范大学地表过程与资源生态国家重点实验室,100875,北京
  • 2. 北京师范大学防沙治沙教育部工程研究中心,100875,北京
  • 3. 首都师范大学学报编辑部,100048,北京
  • 折叠

摘要

Abstract

Three Microlith relic sites have been found in Zhongba area,southwestern margin of Qinghai-Tibet Plateau.Anaeolian deposit (ZZ)near Microlith relid sites was chosen,accelerator mass spectrometry (AMS) 14 C analysis and optically stimulated luminescence (OSL)of ZZ were used to determine ages,grain size and geochemical parameters were analysed.Relationship between Holocene environment and human activities was reconstructed,the time of Microlith human activities in Zhangba area was determined.It was found that from 8.9 ka BP to 7.3 ka BP,climate was humid,aeolian activity was weak with strong pedogenesis,with relative abundance of natural resources which were good for hunting of Micorlith human.From 7.3 ka BP to 3.8 ka BP,climate was dry,aeolian activity was strong,which was not conducive to human activities.It is therefore concluded that the formation time of Zhongba Microlith relics might be from 8.9-7.3 ka BP.

关键词

全新世/风沙活动/气候变化/仲巴地区/细石器

Key words

Holocene/aeolian activity/climate change/Zhongba area/Microlith

分类

社会科学

引用本文复制引用

李拓宇,伍永秋,杜世松,黄文敏,蒿承智..青藏高原西南部仲巴地区细石器人类活动的时代探讨[J].北京师范大学学报(自然科学版),2016,52(1):91-96,6.

基金项目

国家重点基础研究发展计划基金资助项目(2013CB956001) (2013CB956001)

国家自然科学基金资助项目(41071129) (41071129)

北京师范大学学报(自然科学版)

OA北大核心CSCDCSTPCD

0476-0301

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