玉龙雪山冰川沉积序列OSL定年

doi:10.7522/j.issn.1000-0240.2016.0180

冰川冻土 ›› 2016, Vol. 38 ›› Issue (6): 1544-1552.doi: 10.7522/j.issn.1000-0240.2016.0180

玉龙雪山冰川沉积序列OSL定年

何则^1,2, 何元庆^1,3,5, 张志刚^3,1, 和丽华⁴, 齐翠姗^5,1, 刘婧^1,2

1. 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;
2. 中国科学院大学, 北京 100049;
3. 南京师范大学地理科学学院, 江苏南京 210023;
4. 玉龙雪山省级旅游开发区管理委员会, 云南丽江 674100;
5. 兰州大学资源环境学院, 甘肃兰州 730000

收稿日期:2016-07-16 修回日期:2016-11-10 出版日期:2016-12-25 发布日期:2017-04-06
通讯作者: 何元庆,E-mail:yqhe@lzb.ac.cn;张志刚,E-mail:zhangzhigang840620@126.com E-mail:yqhe@lzb.ac.cn;zhangzhigang840620@126.com
作者简介:何则(1992-),男,陕西宝鸡人,2014年在西北大学获学士学位,现为中国科学院西北生态环境资源研究院在读硕士研究生,主要从事冰川地貌与地质公园规划研究.E-mail:heze@lzb.ac.cn
基金资助:
国家重大科学计划研究项目（2013CBA01801）；中科院重点部署项目（KJZD-EW-G03-04）；国家自然科学基金项目（41503054；41273010）；丽江玉龙雪山省级旅游开发区管理委员会委托项目；冰冻圈科学国家重点实验室自主课题（SKLCS-ZZ-2016）；中国博士后科学基金面上项目（2015M582728）资助

OSL dating of the Quaternary glacial sedimentary sequences at Mt. Yulong, China

HE Ze^1,2, HE Yuanqing^1,3,5, ZHANG Zhigang^3,1, HE Lihua⁴, QI Cuishan^5,1, LIU Jing^1,2

1. State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China;
3. School of Geographical Sciences, Nanjing Normal University, Nanjing 210023, China;
4. Committee of Provincial Tourism Development and Management in Yulong Snow Mountain, Lijiang 674100, China;
5. College of Earth Environmental Sciences, Lanzhou University, Lanzhou 730000, China

Received:2016-07-16 Revised:2016-11-10 Online:2016-12-25 Published:2017-04-06

摘要/Abstract

摘要：

位于青藏高原东南缘的玉龙雪山分布有欧亚大陆纬度最低的海洋型冰川，其主峰及周边地区保存了大量清晰完整的第四纪冰川遗迹。研究该区第四纪冰川作用遗迹及其冰川作用史，具有重要的理论与实际价值。应用光释光（OSL）测年技术对玉龙雪山冰川沉积物进行了定年，结合前人研究资料，重建玉龙雪山冰川作用史。研究结果表明：玉龙雪山东麓的末次冰期冰碛物主要形成于晚更新世末次冰期最盛时期，其平均年代约在25ka，西麓末次冰期冰碛物形成年代约为50ka，对应于深海氧同位素3阶段中期（MIS3b）。而倒数第二次冰期的年代在240ka左右，处于中更新世晚期，对应于MIS8阶段，当时玉龙雪山存在多条复式山谷冰川。该研究可为玉龙雪山第四纪冰川作用历史的重新认识以及光释光测年技术在该区的应用提供基础资料。

关键词: 冰川地貌, OSL, 末次冰盛期, 倒数第二次冰期, 玉龙雪山

Abstract:

The Mt. Yulong is situated in the southeast of the Tibetan Plateau, where the well preserved glacial remnants (including the lowest latitude moraines in the northern hemisphere) provide a natural laboratory to study the Quaternary glacial and the past global climate evolution process. Getting more details about these glacial remnants is important for deeply understanding the regional change of paleo-climate and paleo-environment, as well as the development and utilization of the glacial tills. However, because of shortage of dating records and controversy of climate background, there are no consensus about how many times of glacier advance during the Quaternary. In this paper, OSL dating techniques was used on the glacial sediments at Mt. Yulong. OSL dating data and evidences from geomorphology and stratigraphy reveal that glaciers had advanced during local last glacial maximum (~25 ka) at east side and mid-MIS 3b (~50 ka) at west side of the Mt. Yulong. The Penultimate Glaciation had appeared at ~240 ka in late Middle Pleistocene, corresponding to MIS 8. At that time, there were multiple composite valley glaciers at Mt. Yulong.

Key words: glacial geomorphology, OSL, Last Glacial Maximum, Penultimate Glaciation, Mt. Yulong

中图分类号:

P343.6

何则, 何元庆, 张志刚, 和丽华, 齐翠姗, 刘婧. 玉龙雪山冰川沉积序列OSL定年[J]. 冰川冻土, 2016, 38(6): 1544-1552.

HE Ze, HE Yuanqing, ZHANG Zhigang, HE Lihua, QI Cuishan, LIU Jing. OSL dating of the Quaternary glacial sedimentary sequences at Mt. Yulong, China[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2016, 38(6): 1544-1552.

参考文献

[1] Shi Yafeng, Cui Zhijiu, Su Zhen. The quaternary glaciations and environmental variations in China[M]. Shijiazhuang:Hebei Science and Technology Publishing House, 2006.[施雅风, 崔之久, 苏珍. 中国第四纪冰川与环境变化[M]. 石家庄:河北科学技术出版社, 2006.]

[2] Li Jijun, Shu Qiang, Zhou Shangzhe, et al. Review and prospects of quaternary glaciation research in China[J]. Journal of Glaciology and Geocrylolgy, 2004, 26(3):235-243.[李吉均, 舒强, 周尚哲, 等. 中国第四纪冰川研究的回顾与展望[J]. 冰川冻土, 2004, 26(3):235-243.]

[3] Heyman J, Stroeven A P, Caffee M W, et al. Palaeoglaciology of Bayan Har Shan, NE Tibetan Plateau:exposure ages reveal a missing LGM expansion[J]. Quaternary Science Reviews, 2011, 30:1988-2011.

[4] Fu Ping, Heyman J, H ttestrand C, et al. Glacial geomorphology of the Shaluli Shan, southeastern Tibetan Plateau[J]. Journal of Maps, 2012, 8(1):48-55.

[5] Cui Zhijiu, Wu Yongqiu, Liu Gengnian, et al. On Kunlun-Yellow River tectonic movement[J]. Science in China (Series D:Earth Sciences), 1998, 28(1):53-59.[崔之久, 伍永秋, 刘耕年, 等. 关于"昆仑-黄河运动"[J]. 中国科学(D辑:地球科学), 1998, 28(1):53-59.]

[6] Cui Zhijiu, Chen Yixin, Zhang Wei, et al. Research history, glacial chronology and origins of Quaternary glaciations in China[J]. Quaternary Sciences, 2011, 31(5):749-764.[崔之久, 陈艺鑫, 张威, 等. 中国第四纪冰期历史、特征及成因探讨[J]. 第四纪研究, 2011, 31(5):749-764.]

[7] Shi Yafeng. Evolution of the Cryosphere in the Tibetan Plateau, China, and its relationship with the global change in the mid Quaternary[J]. Journal of Glaciology and Geocrylolgy, 1998, 20(3):197-208.[施雅风. 第四纪中期青藏高原冰冻圈的演化及其与全球变化的联系[J]. 冰川冻土, 1998, 20(3):197-208.]

[8] Zhou Shangzhe, Wang Xiaoli, Wang Jie, et al. A preliminary study on timing of the oldest Pleistocene glaciation in Qinghai-Tibetan Plateau[J]. Quaternary International, 2006, 154:44-51.

[9] Jiang Heli, Zhao Jingdong, Yin Xiufeng, et al. New OSL chronology of the last glaciation in Kanas River Vally, Altay Mountains, China[J]. Journal of Glaciology and Geocrylolgy, 2012, 34(2):304-310.[江合理, 赵井东, 殷秀峰, 等. 阿尔泰山喀纳斯河流域末次冰期OSL年代学新证[J]. 冰川冻土, 2012, 34(2):304-310.]

[10] Zhao Jingdong, Wang Jie, Shangguan Donghui. Sequences of quaternary glacial sediments and their preparatory chronology in the Tomur River Valley, Tianshan Mountain[J]. Journal of Glaciology and Geocrylolgy, 2009, 31(4):628-633.[赵井东, 王杰, 上官冬辉. 天山托木尔河流域第四纪冰川沉积序列及其初步年代学[J]. 冰川冻土, 2009, 31(4):628-633.]

[11] Lai Zhongping, Ou Xianjiao. Basic procedures of optically stimulated luminescence (OSL) dating[J]. Progress in Geography, 2013, 32(5):683-693.[赖忠平, 欧先交. 光释光测年基本流程[J]. 地理科学进展, 2013, 32(5):683-693.]

[12] Liu Gengnian, Chen Yixin, Zhang Mei, et al. Glacial landform chronology and environment reconstruction of PeikuGangri, Himalayas[J]. Journal of Glaciology and Geocrylolgy, 2011, 33(5):959-970.[刘耕年, 陈艺鑫, 张梅, 等. 喜马拉雅山佩枯岗日冰川地貌的年代学, 平衡线高度和气候研究[J]. 冰川冻土, 2011, 33(5):959-970.]

[13] Zhou Shangzhe. New advance in study of Alpine Glaciations[J]. Journal of Glaciology and Geocrylolgy, 2012, 34(5):1127-1133.[周尚哲. 阿尔卑斯山地区第四纪冰川最新研究[J]. 冰川冻土, 2012, 34(5):1127-1133.]

[14] Zhao Xitao, Qu Yongxin, Li Tiesong. Pleitocene glaciations along the eastern foot of the Yulong Mountains[J]. Journal of Glaciology and Geocrylolgy, 1999, 21(3):242-248.[赵希涛, 曲永新, 李铁松. 玉龙山东麓更新世冰川作用[J]. 冰川冻土, 1999, 21(3):242-248.]

[15] Ou Xianjiao, Zeng Lanhua, Long Hao, et al. Applicability of OSL dating the quartz from the tills of last glacial in the Hengduan Mountains[J]. Journal of Glaciology and Geocryology, 2011, 33(1):110-117.[欧先交, 曾兰华, 隆浩, 等. 横断山地区末次冰期冰碛物石英光释光测年的适应性[J]. 冰川冻土, 2011, 33(1):110-117.]

[16] Shi Yafeng, Zhao Jingdong, Wang Jie. New understanding of quaternary glaciations in China[M]. Shanghai:Shanghai Popular Science Press, 2011:5-28.[施雅风, 赵井东, 王杰. 中国第四纪冰川新论[M]. 上海:上海科学普及出版社, 2011:5-28.]

[17] Ren Meie, Liu Zhenzhong, Yong Wanli, et al. A primary study on Lijiang and Yulong Mountains[J]. Journal of Yunnan University (Natural Sciences), 1957, 4:9-18.[任美锷, 刘振中, 雍万里, 等. 丽江和玉龙山地貌的初步研究[J]. 云南大学学报(自然科学版), 1957, 4:9-18.]

[18] Ives J D, Zhang Y. Glaciation of the Yulongxue Shan, Northwestern Yunnan Province, People's Republic of China (Vergletscherung des Yulongxue Shan, Nordwest-Yunnan, Volksrepublik China)[J]. Erdkunde, 1993:165-176.

[19] The First Brigade for Regional Geological Survey in Bureau of Geology, Yunnan Province. The regional geological survey of the People's Republic of China (1:200,000) #Lijiang(G-47-XI) (Geological section)[M]. Kunming:Bureau of Geology, 1977.[云南省地质局第一区域地质调查大队. 中华人民共和国区域地质调查报告(1:20万)#丽江幅(G-47-XI)(地质部分)[M]. 昆明:云南省地质局, 1977.]

[20] Ming Qingzhong, Jing Cairui. Neotectonic movement in the Yulong Mountains[J]. Journal of Central China Nomal University (Natural Science Edition), 1991(2):224-228.[明庆忠, 景才瑞. 滇西北玉龙山新构造运动研究[J]. 华中师范大学学报(自然科学版), 1991(2):224-228.]

[21] Xie Youyu, Cui Zhijiu. Yulong Mountain at north of yunnan province[M]//Shi Yafeng, Cui Zhijiu, Li Jijun, et al. The problems of quaternary glacier and environment in the east China. Beijing:Science Publishing House, 1989:106-119.[谢又予, 崔之久. 滇北玉龙山[M]//施雅风, 崔之久, 李吉均, 等. 中国东部第四纪冰川与环境问题. 北京:科学出版社, 1989:106-119.]

[22] Zheng Benxing. Quaternary glaciation and glacier evolution in the Yulong Mount, Ynnan[J]. Journal of Glaciology and Geocrylolgy, 2000(1):53-61.[郑本兴. 云南玉龙雪山第四纪冰期与冰川演化模式[J]. 冰川冻土, 2000(1):53-61.]

[23] Zhao Xitao, Zhang Yongshuang, Qu Yongxin, et al. Pleistocene glaciations along the western foot of the Yulong Mountains and their relationship with the formation and development of the Jinsha River[J]. Quaternary Sciences, 2007, 27(1):35-44.[赵希涛, 张永双, 曲永新, 等. 玉龙山西麓更新世冰川作用及其与金沙江河谷发育的关系[J]. 第四纪研究, 2007, 27(1):37-46.]

[24] Xin Huijuan, He Yuanqing, Zhang Tao, et al. The features of climate variation and glacier response in Mt.Yulong, southeastern Tibetan Plateau[J]. Advances in Earth Science, 2013, 28(11):1257-1268.[辛惠娟, 何元庆, 张涛, 等. 青藏高原东南缘丽江玉龙雪山气候变化特征及其对冰川变化的影响[J]. 地球科学进展, 2013, 28(11):1257-1268.]

[25] He Yuanqing, Zhang Zhonglin, Wilfred H T, et al. Changing features of climate and glaciers in China's monsoonal temperate glacier region[J]. Journal of Geophysical Research, 2003, 108(D17):4530-4536.

[26] Li Zongxing, He Yuanqing, Jia Wenxiong, et al. Response of the glaciers-runoff system in a typical temperate-glacier, Hailuogou glacier in Mt.Gongga of China, to global change[J]. Scientia Geographica Sinica, 2008, 28(2):229-234.[李宗省, 何元庆, 贾文雄, 等. 中国海洋型冰川区"冰川-径流"系统的全球变化敏感性研究[J]. 地理科学, 2008, 28(2):229-234.]

[27] Zhang Ningning, He Yuanqing, Pang Hongxi, et al. The causes of glacier collapse in Mt.Yulong[J]. Journal of Mountain Sciences, 2007, 25(4):412-418.[张宁宁, 何元庆, 庞洪喜, 等. 玉龙雪山冰川崩塌的原因[J]. 山地学报, 2007, 25(4):412-418.]

[28] Li Zongxing, He Yuanqing, Pu Tao, et al. Changes of climate, glacier sand runoff in China's monsoonal temperate glacier region during the last several decades[J]. Quaternary International, 2009. doi:10.1016/j.quaint.2009.05.010.

[29] Li Zongxing, He Yuanqing, Wang Shijin, et al. The analysis on changes of some monsoonal temperate glaciers in Mt.Hengduan region during 1900-2007[J]. Acta Geographica Sinica, 2009, 64(11):1319-1330.[李宗省, 何元庆, 王世金, 等. 1900-2007年横断山区部分海洋型冰川的变化[J]. 地理学报, 2009, 64(11):1319-1330.]

[30] Kong P, Na C, Fink D, et al. Moraine dam related to late Quaternary glaciation in the Yulong Mountains, southwest China, and impacts on the Jinsha River[J]. Quaternary Science Reviews, 2009, 28(27):3224-3235.

[31] Gillespie A, Molnar P. Asynchronous maximum advances of mountain and continental glaciers[J]. Reviews of Geophysics, 1995, 33(3):311-364.

[32] Phillips W M, Sloan V F, Shroder J F, et al. Asynchronous glaciation at Nanga Parbat, northwestern Himalaya Mountains, Pakistan[J]. Geology, 2000, 28(5):431-434.

[33] Owen L A, Finkel R C, Caffee M W. A note on the extent of glaciation throughout the Himalaya during the global Last Glacial Maximum[J]. Quaternary Science Reviews, 2002, 21(1):147-157.

[34] Shi Yafeng, Yao Tandong. MIS 3b (54-44 ka BP) cold perid and glacial advance in middle and low latitudes[J]. Journal of Glaciology and Geocryology, 2002, 24(1):1-9.[施雅风, 姚檀栋. 中纬度MIS 3b(54-44 ka BP)冷期与冰川前进[J]. 冰川冻土, 2002, 24(1):1-9.]

[35] Zhao Jingdong, Zhou Shangzhe, Liu Shiyin, et al. A preliminary study of the glacier advance in MIS3b in the western regions of China[J]. Journal of Glaciology and Geocryology, 2007, 29(2):233-241.[赵井东, 周尚哲, 刘时银, 等. 中国西部山岳冰川MIS3b冰进初步探讨[J]. 冰川冻土, 2007, 29(2):233-241.]

[36] Wang Jie. Glacial advance in the Qinghai-Xizang Plateau and peripheral mountains during the mid-MIS 3[J]. Quaternary Sciences, 2010, 30(5):1055-1065.[王杰. 青藏高原及周边地区MIS 3中期冰进探讨[J]. 第四纪研究, 2010, 30(5):1055-1065.]

[37] Xu Liubing, Ou Xianjiao, Lai Zhongping, et al. Timing and style of late pleistocene glaciation in the Queer Shan, northern Hengduan Mountains in the eastern Tibetan Plateau[J]. Journal Quaternary Science, 2010, 25:957-966.

[38] Zhang Wei, Liu Beibei, Li Yonghua, et al. Quaternary glacier development and environmental evolution in Qianhu Mountain, northwestern Yunnan Province[J]. Acta Geographica Sinica, 2012, 67(5):658-670.[张威, 刘蓓蓓, 李永化, 等. 云南千湖山第四纪冰川发育特点与环境变化[J]. 地理学报, 2012, 67(5):658-670.]

[39] Zhang Wei, Cui Zhijiu, Li Yonghua, et al. Quaternary glacier development and the relationship between the climate change and tectonic uplift in the Helan Mountain[J]. Chinese Science Bulletin, 2012, 57(25):2390-2402.[张威, 崔之久, 李永化, 等. 贺兰山第四纪冰川特征及其与气候和构造之间的耦合关系[J]. 科学通报, 2012, 57(25):2390-2402.]

[40] Chen Yixin, Li Yingkui, Wang Yueyan, et al. Late Quaternary glacial history of the Karlik Range, easternmost TianShan, derived from ¹⁰Be surface exposure and optically stimulated luminescence datings[J]. Quaternary Science Reviews, 2015, 115:17-27.

[41] Zhang Wei, Liu Beibei. Features of the glaciation during the last Glaciation cycle in northwestern Yunnan Province[J]. Journal of Glaciology and Geocryology, 2014, 36(1):30-37.[张威, 刘蓓蓓. 滇西北山地末次冰期冰川发育及其基本特征[J]. 冰川冻土, 2014, 36(1):30-37.]

玉龙雪山冰川沉积序列OSL定年

OSL dating of the Quaternary glacial sedimentary sequences at Mt. Yulong, China

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	齐翠姗, 何元庆, 王世金, 何则, 石晓非, 史晓宜. 玉龙雪山国家地质公园地质遗迹资源类型划分及其综合评价[J]. 冰川冻土, 2018, 40(1): 186-196.
[2]	燕兴国, 何元庆, 张松林, 牛贺文, 朱国峰, 王世金, 蒲涛, 史晓宜, 石晓非, 齐翠姗. 玉龙雪山白水河1号冰川消融期表面流速特征分析[J]. 冰川冻土, 2017, 39(6): 1212-1220.
[3]	王乃昂, 戴霜, 张律吕, 余莺潇, 于昕冉, 田璐, 尹丽颖. 第四纪冰川遗迹的判别标准与方法问题——兼论蒙山巨砾堆积堤之成因[J]. 冰川冻土, 2017, 39(6): 1289-1297.
[4]	王乃昂, 赵井东, 余莺潇, 于昕冉, 张文佳. 渐趋完善的第四纪冰川研究范式——记第四届中国第四纪冰川与环境变化研讨会[J]. 冰川冻土, 2017, 39(5): 1029-1038.
[5]	张威, 柴乐. 他念他翁山中段第四纪冰川作用ESR定年初步研究[J]. 冰川冻土, 2016, 38(5): 1281-1291.
[6]	伍云飞, 赵井东, 郑辉军. 东帕米尔高原喀拉库勒湖的成因及其年代[J]. 冰川冻土, 2016, 38(1): 100-106.
[7]	温华春, 赖忠平, Michael E. Brookfield, I. Peter Martini, 欧先交. 北美五大湖区晚更新世劳伦泰德冰盖演化年代学综述及石英光释光测年的初步尝试[J]. 冰川冻土, 2015, 37(3): 711-722.
[8]	戚帮申, 胡道功, 赵希涛, 张绪教, 张耀玲, 杨肖肖, 赵珍, 高雪咪. 青海湖北岸原生砂楔的发现及其古气候意义[J]. 冰川冻土, 2014, 36(6): 1412-1419.
[9]	牛贺文, 何元庆. 玉龙雪山地区大气降水中粉尘颗粒物特征研究[J]. 冰川冻土, 2014, 36(1): 71-79.
[10]	殷秀峰, 赵井东, 伍云飞. 东天山黑沟流域冰川沉积序列及OSL测年研究[J]. 冰川冻土, 2014, 36(1): 63-70.
[11]	赵井东, 王杰, 沈永平, 殷秀峰, 伍云飞. 西秦岭迭山西北部冰川地貌分布及其特征[J]. 冰川冻土, 2013, 35(4): 841-847.
[12]	赵井东, 王杰, 殷秀峰. 中国第四纪冰川研究的现状与争议——兼记首届“中国第四纪冰川与环境变化”研讨会[J]. 冰川冻土, 2013, 35(1): 119-125.
[13]	江合理, 赵井东, 殷秀峰, 李忠勤, 康剑, 孙吉舟. 阿尔泰山喀纳斯河流域末次冰期OSL年代学新证[J]. 冰川冻土, 2012, (2): 304-310.
[14]	杨岁桥, 杨建平, 王世金, 谭春萍, 刘俊峰. 生态-经济系统对冰冻圈变化的适应能力评价——以玉龙雪山地区为例[J]. 冰川冻土, 2012, (2): 485-493.
[15]	刘耕年;Li Yingkui;陈艺鑫;张梅;李川川;孔屏;Harbor J.;Caffee M.W. . 喜马拉雅山佩枯岗日冰川地貌的年代学、平衡线高度和气候研究 [J]. 冰川冻土, 2011, 33(5): 959-970.