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冰川冻土 ›› 2017, Vol. 39 ›› Issue (5): 957-966.doi: 10.7522/j.issn.1000-0240.2017.0106

• 冰冻圈与全球变化 • 上一篇    下一篇

MIS 3时期青藏高原东南部稻城古冰帽冰进事件研究

张志刚1,2, 王建1, 何元庆2, 何则3, 齐翠姗2,4, 李盼盼2,4   

  1. 1. 南京师范大学 地理科学学院, 江苏 南京 210023;
    2. 中国科学院 西北生态环境资源研究院 冰冻圈科学国家重点实验室, 甘肃 兰州 730000;
    3. 中国科学院 地理科学与资源研究所, 北京 100101;
    4. 兰州大学 资源环境学院, 甘肃 兰州 730000
  • 收稿日期:2017-03-02 修回日期:2017-09-25 出版日期:2017-10-25 发布日期:2018-01-27
  • 通讯作者: 王建,E-mail:jwang169@vip.sina.com E-mail:jwang169@vip.sina.com
  • 作者简介:张志刚(1984-),男,山西忻州人,讲师,2014年在南京师范大学获博士学位,从事冰川地貌宇生核素年代学研究.E-mail:zhangzhigang840620@126.com
  • 基金资助:
    国家自然科学基金项目(41503054);中国博士后科学基金项目(2015M582728);中国科学院重点部署项目(KJZD-EW-G03-04)资助

MIS 3 glacial advance of the paleo-Daocheng Ice Cap, southestern Qinghai-Tibet Plateau

ZHANG Zhigang1,2, WANG Jian1, HE Yuanqing2, HE Ze3, QI Cuishan2,4, LI Panpan2,4   

  1. 1. School of Geographical Sciences, Nanjing Normal University, Nanjing 210023, China;
    2. State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment, Chinese Academy of Sciences, Lanzhou 730000, China;
    3. Institute of Geographic Science and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
    4. College of Earth Environmental Sciences, Lanzhou University, Lanzhou 730000, China
  • Received:2017-03-02 Revised:2017-09-25 Online:2017-10-25 Published:2018-01-27

摘要: 深海氧同位素3阶段(Marine Isotope Stage 3,MIS 3)是全球气候演化过程中特殊的时期,对深入认识区域古气候、古环境演变具有重要意义。青藏高原东南部稻城古冰帽是第四纪冰川作用历史和古气候研究的理想区域,许多学者在该区进行了冰川地貌学和年代学研究。目前,该区域在MIS 3阶段是否存在冰川前进事件仍存在争论。现着重从洞穴石笋、高原冰芯、海洋沉积、古湖孢粉等记录来总结我国MIS 3阶段的气候环境状况,并搜集高原及周边地区MIS 3阶段冰进事件的记录,结合稻城古冰帽区已发表的MIS 3阶段的年代数据来探讨稻城古冰帽区MIS 3阶段的冰川前进的可能性。结果表明:稻城古冰帽区MIS 3阶段(43~53 ka)发生了大规模冰进事件,这可能是由于该冰帽区处于相对冷湿环境且受到了西南季风的影响。本研究可为区域气候重建与环境演变提供新的依据。

关键词: 青藏高原, 稻城古冰帽, MIS 3, 宇生核素

Abstract: The MIS 3 (Marine Isotope Stage 3) was a special period during the past global climate evolution process. It is important for getting more details about MIS 3 for deeply understanding the regional change of paleo-climate and paleo-environment. The paleo-Daocheng Ice Cap is situated in the southeastern Tibetan Plateau, where the glacial remnants (including the oldest moraines in the Hengduan Mountains) have been well preserved, which provides a natural laboratory to study the glacial history and climate change during Quaternary. Although there has been a lot of work in this area, consensus has not reached on the time of the maximum glaciation and whether glacier advance during MIS 3. In this paper, the possibility of MIS 3 glacial advance in paleo-Daocheng Ice Cap is explored based on the climatic records (stalagmites, ice cores, marine sediments and pollen data) and the dating data of glacial advance in the plateau (include the paleo-Daocheng Ice Cap) and around areas during MIS 3. The results showed that glaciers had advanced during 43~53 ka (MIS 3). This research will provide new data for climate and environment reconstruction.

Key words: Tibetan Plateau, paleo-Daocheng Ice Cap, Marine Isotope Stage 3, cosmogenic nuclides

中图分类号: 

  • P512.4