MIS 3时期青藏高原东南部稻城古冰帽冰进事件研究
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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。
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 newdata for climate and environment reconstruction.
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 newdata for climate and environment reconstruction.
引文
[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 Geocryology,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.Paleoglaciation of the Tibetan Plateau and surrounding mountains based on exposure ages and ELA depression estimates[J].Quaternary Science Review s,2014,91(3):30-41.
[4]Fu Ping,Heyman J,H ttestrand C,et al.Glacial geomorphology of the Shaluli Shan,southeastern Tibetan Plateau[J].Journal of M aps,2012,8(1):48-55.
[5]Cui Zhijiu,Wu Yongqiu,Liu Gengnian,et al.On KunlunY ello w River tectonic movement[J].Science in China:Series D Earth Sciences,1998,41(6):592-600.[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 w ith the global change in the M id Quaternary[J].Journal of Glaciology and Geocryology,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 QinghaiTibetan Plateau[J].Quaternary International,2006,154(5):44-51.
[9]Xia Zhengkai,Liu Decheng,Wang Youping,et al.Environmental background of human activities during M IS 3 stage recorded in the Zhijidong cave site,Zhengzhou[J].Quaternary Sciences,2008,28(1):96-102.[夏正楷,刘德成,王幼平,等.郑州织机洞遗址MIS 3阶段古人类活动的环境背景[J].第四纪研究,2008,28(1):96-102.]
[10]Li Xiaoli,Zhang Shuangquan,Wei Mingrui,et al.Environmental background of human occupation at Zhoukoudian Tianyuan cave[J].M arine Geology and Quaternary Geology,2009,29(3):133-140.[李潇丽,张双权,魏明瑞,等.周口店田园洞MIS 3阶段古人类生存环境[J].海洋地质与第四纪地质,2009,29(3):133-140.]
[11]Wang Yongjin,Wu Jiangying,Wu Jinquan,et al.Correlation betw een high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the Last Glaciation[J].Science in China:Series D Earth Sciences,2001,44(1):14-23.[汪永进,吴江滢,吴金全,等.末次冰期南京石笋高分辨率气候记录与GRIP冰芯对比[J].中国科学:D辑地球科学,2000,30(5):533-539.]
[12]Zhang Meiliang,Lin Yushi,Feng Yumei,et al.The records of paleoclimate change from a stalagmite of Dongge cave in the preiod of 42.0 ka BP to 65.0 ka BP in Libo[J].Guangxi Sciences,2004,11(3):218-220.[张美良,林玉石,冯玉梅,等.贵州荔波42.0~65.0 ka BP气候变化的石笋记录[J].广西科学,2004,11(3):218-220.]
[13]Yao Tandong,Thompson L G,Shi Yafeng,et al.Climate variation since the Last Interglaciation recorded in the Guliya ice core[J].Science in China:Series D Earth Sciences,1997,40(6):662-668.[姚檀栋,Thompson L G,施雅风,等.古里雅冰芯中末次间冰期以来气候变化记录研究[J].中国科学:D辑地球科学,1997,27(5):447-452.]
[14]Yang Wenyu,Huang Baoqi,Xiao Jie,et al.Environmental changes of surface sea recorded in planktonic foram in ifera during M IS 3 in the w estern South China Sea[J].Quaternary Sciences,2008,28(3):437-446.[杨文瑜,黄宝琦,肖洁,等.南海西部浮游有孔虫记录的MIS 3期表层海洋环境变化[J].第四纪研究,2008,28(3):437-446.]
[15]Zheng Hongbo,Yang Wenguang,He Juan,et al.Marine isotope stage 3(M IS 3)of South China Sea[J].Quaternary Sciences,2008,28(1):69-78.[郑洪波,杨文光,贺娟,等.南海的氧同位素3期[J].第四纪研究,2008,28(1):69-78.]
[16]Du Jianghui,Huang Baoqi.Variations in upper water structure during M IS 3 from the w estern South China Sea[J].Chinese Science Bulletin,2010,55(3):301-307.
[17]Niu Yaocheng,Zhang Yiyuan,Du Jianghui,et al.Variations in paleoproductivity recorded by benthic foraminifera during M IS 3from the w estern South China Sea[J].M arine Geology and Quaternary Geology,2011,31(1):85-92.[钮耀诚,张译元,杜江辉,等.南海西部MIS 3期底栖有孔虫的生产力变化[J].海洋地质与第四纪地质,2011,31(1):85-92.]
[18]Chen Xiaoyun,Wu Naiqin.Relatively warm-humid climate recorded by mollusk species in the Chinese Loess Plateau during M IS 3 and its possible forcing mechanism[J].Quaternary Sciences,2008,28(1):154-161.[陈晓云,吴乃琴.黄土高原M IS 3时期蜗牛化石记录的温湿气候及其成因机制探讨[J].第四纪研究,2008,28(1):154-161.]
[19]Zhai Xinwei,Li Fuqiang,Wu Song,et al.Huining MIS 3 stage climate change based on the loess grain size record[J].Arid Land Geography,2013,36(5):773-780.[翟新伟,李富强,吴松.会宁剖面黄土粒度记录的MIS 3阶段气候变化研究[J].干旱区地理,2013,36(5):773-780.]
[20]Wu Jinglu,Wang Sumin,Pan Hongxi,et al.Climatic variations in the past 140 ka recorded in core RM,east Qinghai-Xizang Plateau[J].Science in China:Series D Earth Sciences,1997,40(4):443-448.[吴敬禄,王苏民,潘红玺,等.青藏高原东部RM孔140 ka以来湖泊碳酸盐同位素记录的古气候特征[J].中国科学:D辑地球科学,1997,27(3):255-259.]
[21]Wu Jinglu,Wang Sumin,Shi Yafeng,et al.Temperature estimation by oxygen-stable record over the past 200 ka in Zoige Basin[J].Science in China:Series D Earth Sciences,2000,43(6):577-586.[吴敬禄,王苏民,施雅风,等.若尔盖盆地200 ka以来氧同位素记录的古温度定量研究[J].中国科学:D辑地球科学,2000,30(1):73-80.]
[22]Li Shijie,Zhang Hongliang,Shi Yafeng,et al.A high resolution M IS 3 environmental change record derived from lacustrine deposit of Tianshuihai Lake,Qinghai-Tibet Plateau[J].Quaternary Sciences,2008,28(1):121-131.[李世杰,张宏亮,施雅风,等.青藏高原甜水海盆地MIS 3阶段湖泊与环境变化[J].第四纪研究,2008,28(1):122-131.]
[23]Yang Xiangdong,Wang Sumin,Tong Guobang,et al.The late Pleistocene pollen record in the lake sediments from ancient Heqing Lake and its significance for palaeoclimate[J].Quaternary Sciences,1998,18(4):335-342.[羊向东,王苏民,童国榜,等.云南鹤庆古湖晚更新世的孢粉记录及其古气候学意义[J].第四纪研究,1998,18(4):335-342.]
[24]Zhao Zengyou,Yuan Daoxian,Shi Shengqiang,et al.MIS3b vegetation and climate changes based on pollen and charcoal on Qianxi Plateau[J].Acta Ecologica Sinica,2012,32(15):4811-4818.[赵增友,袁道先,石胜强,等.孢粉、炭屑揭示的黔西高原MIS3b期间古植被、古气候演变[J].生态学报,2012,32(15):4811-4818.]
[25]van Andel T H.The climate and landscape of the middle part of the Weichselian Glaciation in Europe:the stage 3 project[J].Quaternary Research,2002,57(1):2-8.
[26]Zhang Zhigang,Wang Jian,Xu Xiaobin,et al.Cosmogenic isotope10Be dating for Kuzhaori moraine in Daocheng Ice Cap[J].M arine Geology and Quaternary Geology,2012,32(1):85-91.[张志刚,王建,徐孝彬,等.稻城冰帽库照日冰碛垄的宇生核素10Be年代测定[J].海洋地质与第四纪地质,2012,32(1):85-91.]
[27]Zhang Zhigang,Wang Jian,Xu Xiaobin,et al.Cosmogenic10Be and26Al chronology of the Last Glaciation of the PalaeoDaocheng Ice Cap,southeastern Qinghai-Tibetan Plateau[J].Acta Geologica Sinica,2015,89(2):575-584.
[28]Wang Jian,Zhang Zhigang,Xu Xiaobin,et al.Cosmogenic isotopes dating of Quaternary glacial activity of the Paleo-Daocheng Ice Cap,on the southeastern part of the Qinghai-Xizang Plateau[J].Quaternary Sciences,2012,32(3):394-402.[王建,张志刚,徐孝彬,等.青藏高原东南部稻城古冰帽南缘第四纪冰川活动的宇生核素年代研究[J].第四纪研究,2012,32(3):394-402.]
[29]Xu Liubing,Zhou Shangzhe,Cui Jianxin,et al.Dating of the Pleistocene glaciations around the Daocheng Ice Cap[J].Journal of Glaciology and Geocryology,2004,26(5):528-534.[许刘兵,周尚哲,崔建新,等.稻城冰帽区更新世冰川测年研究[J].冰川冻土,2004,26(5):528-534.]
[30]Xu Liubing,Zhou Shangzhe.Quaternary glaciations recorded by glacial and fluvial landforms in the Shaluli M ountains,Southeastern Tibetan Plateau[J].Gemorphology,2009,103(2):268-275.
[31]Fu Ping,Stroeven A P,Harbor J M,et al.Paleoglaciation of Shaluli Shan,Southeastern Tibetan Plateau[J].Quaternary Science Review s,2013,64(433):121-135.
[32]Zheng Benxing,Ma Qiuhua.A study on the geomorphological characteristics and glaciations in Paleo-Daocheng Ice Cap,w estern Sichuan[J].Journal of Glaciology and Geocryology,1995,17(1):23-32.[郑本兴,马秋华.川西稻城古冰帽的地貌特征与冰期探讨[J].冰川冻土,1995,17(1):23-32.]
[33]Lin Zhenyao,Wu Xiangding.A study on the path of moisture transportation in the Tibetan Plateau[J].Geographical Research,1990,9(3):33-40.[林振耀,吴祥定.青藏高原水气输送路径的探讨[J].地理研究,1999,9(3):33-40.]
[34]Gou Xiaohua,Yang Tao,Gao Linlin,et al.A 457-year reconstruction of precipitation in the southeastern Qinghai-Tibet Plateau[J].Chinese Science Bulletin,2013,58(10):1107-1114.
[35]Luo Laixing,Yang Yichou.An approach of geomorphological formation in the region of West Sichuan and North Yunnan[C]//Geographical Bulletin No.5.Beijing:Science Press,1963:1-58.[罗来兴,杨逸畴.川西滇北地貌形成的探讨[C]//地理集刊5号.北京:科学出版社,1963:1-58.]
[36]Yao Tandong,Feng Zhaodong,Li Jijun.The basic features of Daocheng ancient ice cap[C]//Studies in Qinghai-Xizang(Tibet)Plateau special issue of Hengduan M ountains scientific expedition(1).Kunming:Yunnan People's Publishing House,1983:132-139.[姚檀栋,冯兆东,李吉均.稻城古冰帽的基本特征[C]//青藏高原研究横断山考察专集(一).昆明:云南人民出版社,1983:132-139.]
[37]Li Jijun,Yao Tandong,Feng Zhaodong.The development model of the Daocheng former ice cap[C]//Studies in Qinghai-Xizang(Tibet)Plateau special issue of Hengduan Mountains scientific expedition(2).Beijing:Beijing Science and Technology Press,1986:271.[李吉均,姚檀栋,冯兆东.稻城古冰帽发育模式[C]//青藏高原研究横断山考察专集(二).北京:北京科学技术出版社,1986:271.]
[38]Li Jijun,Feng Zhaodong,Zhou Shangzhe.The vestiges of Quaternary glaciation in the Hengduan M ountains region[M]//Glacier in the Hengduan M ountains region.Beijing:Science Press,1996:157-173.[李吉均,冯兆东,周尚哲.横断山第四纪冰川作用遗迹[M]//横断山冰川.北京:科学出版社,1996:157-173.]
[39]Zhou Shangzhe,Xu Liubing,Cui Jianxin,et al.Geomorphologic evolution and environmental changes in the Shaluli M ountain region during the Quaternary[J].Chinese Science Bulletin,2005,50(1):52-57.
[40]Schfer J M,Tschudi S,Zhao Zhizhong,et al.The limited influence of glaciations in Tibet on global climate over the past170 000 yr[J].Earth and Planetary Science Letters,2002,194:287-297.
[41]Wang Jian,Raisbeck G,Xu Xiaobin,et al.In situ cosmogenic10Be dating of the Quaternary glaciations in the southern Shaluli M ountain on the Southeastern Tibetan Plateau[J].Science in China:Series D Earth Sciences,2006,49(12):1291-1298.
[42]Shi Yafeng,Yao Tandong.MIS 3b(54~44 ka BP)cold period 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.]
[43]Zhen Zhiguo,Zhong Wei,Xue Jibin,et al.Progress in the studies of climatic features in different areas of China during the M IS-3[J].Journal of Glaciology and Geocryology,2008,30(5):814-824.[甄治国,钟巍,薛积彬,等.中国不同区域M IS-3时期气候特征研究进展[J].冰川冻土,2008,30(5):814-824.]
[44]Fang Xiaomin,Lu Liangqing,Mason J A,et al.Pedogenic response to millennial summer monsoon enhancements on the Tibetan Plateau[J].Quaternary International,2003,106(2):79-88.
[45]Yao Jing,Yu Hongjun,Xu Xingyong,et al.Paleoenvironmental changes during the late Quaternary as inferred from foraminifera assemblages in the Laizhou Bay[J].Acta Oceanologica Sinica,2014,33(10):10-18.
[46]Zhao Yan,Yu Zicheng,Herzschuh U,et al.Vegetation and climate change during M arine Isotope Stage 3 in China[J].Chinses Science Bulletin,2014,59(33):4444-4455.
[47]Gillespie A,Molnar P.Asynchronous maximum advances of mountain and continental glaciers[J].Review s of Geophysics,1995,33(3):311-364.
[48]Phillips W M,Sloan V F,Shroder J F J,et al.Asynchronous glaciation at Nanga Parbat,northw estern Himalaya M ountains,Pakistan[J].Geology,2000,28(5):431-434.
[49]Owen L A,Finkel R C,Caffee M W.A note on the extent of glaciation throughout the Himalaya during the global Last Glacial M aximum[J].Quaternary Science Review s,2002,21(1):147-157.
[50]Zhao Jingdong,Zhou Shangzhe,Liu Shiyin,et al.A preliminary study of the glacier advance in M IS3b in the w estern 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.]
[51]Wang Jie.Glacial advance in the Qinghai-Xizang Plateau and peripheral mountains during the mid-M IS 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.]
[52]Finkel R C,Owen L A,Barnard P L,et al.Beryllium-10 dating of M ount Everest moraines indicates a strong monsoonal influence and glacial synchroneity throughout the Himalaya[J].Geology,2003,31:561-564.
[53]Zech W,Glaser B,Abramowski U,et al.Reconstruction of the Late Quaternary Glaciation of the M acha Khola valley(Gorkha Himal,Nepal)using relative and absolute(14C,10Be,dendrochronology)dating techniques[J].Quaternary Science Review s,2003,22(21):2253-2265.
[54]Owen L A,Caffee M W,Bovard K R,et al.Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen:Ladakh Range,northern India[J].Geological Society of America Bulletin,2006,118(3):383-392.
[55]Owen L A,Robinson R,Benn D I,et al.Quaternary glaciation of M ount Everest[J].Quaternary Science Review s,2009,28(15):1412-1433.
[56]Dortch J M,Owen L A,Caffee M W.Quaternary glaciation in the Nubra and Shyok valley confluence,northernmost Ladakh,India[J].Quaternary Research,2010,74(1):132-144.
[57]Owen L A,Yi Chaolu,Finkel R C,et al.Quaternary glaciation of Gurla M andhata(Naimon'anyi)[J].Quaternary Science Review s,2010,29(15):1817-1830.
[58]Hedrick K A,Seong Y B,Owen LA,et al.Towards defining the transition in style and timing of Quaternary glaciation betw een the monsoon-influenced Greater Himalaya and the semi-arid Transhimalaya of Northern India[J].Quaternary International,2011,236(1):21-33.
[59]Owen L A,Finkel R C,Caffee M W,et al.Timing of multiple Late Quaternary glaciations in the Hunza Valley,Karakoram M ountains,northern Pakistan:defined by cosmogenic radionuclide dating of moraines[J].Geological Society of America Bulletin,2002,114(5):593-604.
[60]Owen L A,Finkel R C,Ma Haizhou,et al.Timing and style of Late Quaternary glaciation in northeastern Tibet[J].Geological Society of America Bulletin,2003,115(11):1356-1364.
[61]Owen L A,Finkel R C,Ma Haizhou,et al.Late Quaternary landscape evolution in the Kunlun M ountains and Qaidam Basin,Northern Tibet:a framew ork for examining the links betw een glaciation,lake level changes and alluvial fan formation[J].Quaternary International,2006,154(5):73-86.
[62]Abramowski U,Bergau A,Seebach D,et al.Pleistocene glaciations of Central Asia:results from10Be surface exposure ages of erratic boulders from the Pamir(Tajikistan)and the Alay-Turkestan range(Kyrgyzstan)[J].Quaternary Science Review s,2006,25(9):1080-1096.
[63]Koppes M,Gillespie A R,Burke R M,et al.Late Quaternary glaciation in the Kyrgyz Tien Shan[J].Quaternary Science Review s,2008,27(7/8):846-866.
[64]Li Yingkui,Liu Gengnian,Chen Yixin,et al.Timing and extent of Quaternary glaciations in the Tianger Range,eastern Tian Shan,China,investigated using10Be surface exposure dating[J].Quaternary Science Reviews,2014,98:7-23.
[65]Owen L A,Finkel R C,Barnard P L,et al.Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by10Be cosmogenic radionuclide surface exposure dating[J].Quaternary Science Review s,2005,24:1391-1411.
[66]Colgan P M,Munroe J S,Zhou Shangzhe.Cosmogenic radionuclide evidence for the limited extent of Last Glacial M aximum glaciers in the Tanggula Shan of the central Tibetan Plateau[J].Quaternary Research,2006,65(2):336-339.
[67]Dong Guocheng,Yi Chaolu,Caffee M.10Be dating of boulders on moraines from the last glacial period in the Nyainqentanglha M ountains,Tibet[J].Science China:Series D Earth Sciences,2014,57(2):221-231.
[68]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 Review s,2011,30(15/16):1988-2001.
[69]Wang Jie,Kassab C,Harbor J M,et al.Cosmogenic nuclide constraints on late Quaternary glacial chronology on the Dalijia Shan,northeastern Tibetan Plateau[J].Quaternary Research,2013,79(3):439-451.
[70]Zech R,Abramowski U,Glaser B,et al.Late Quaternary glacier and climate history of the Pamir M ountains derived from cosmogenic10Be exposure ages[J].Quaternary Research,2005,64(2):212-220.
[71]Xu Liubing,Ou Xianjiao,Lai Zhongping,et al.Timing and style of Late Pleistocene glaciation in the Queer Shan,northern Hengduan M ountains in the eastern Tibetan Plateau[J].Journal Quaternary Science,2010,25(6):957-966.
[72]Wang Jie,Zhou Shangzhe,Zhao Jingdong,et al.Quaternary glacial geomorphology and glaciations of Kongur M ountain,eastern Pamir,China[J].Science in China:Series D Earth Sciences,2011,54(4):591-602.[王杰,周尚哲,赵井东,等.东帕米尔公格尔山地区第四纪冰川地貌与冰期[J].中国科学:D辑地球科学,2011,41(3):350-361.]
[73]Wang Jie,Pan Baotian,Zhang Guoliang,et al.Late Quaternary glacial chronology on the eastern slope of Gongga M ountain,eastern Tibetan Plateau,China[J].Science China:Series D Earth Sciences,2012,56(3):354-365.[王杰,潘保田,张国梁,等.贡嘎山东坡中更新世晚期以来冰川作用年代学研究[J].中国科学:D辑地球科学,2012,42(12):1889-1900.]
[74]Jiang Heli,Zhao Jingdong,Yin Xiufeng,et al.New OSL Chronology of the Last Glaciation in Kanas River Valley,Altay M ountains,China[J].Journal of Glaciology and Geocryology,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.]
[75]Zhang Wei,Liu Beibei,Li Yonghua,et al.Quaternary glacier development and environmental evolution in Qianhu M ountain,Northw estern 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.]
[76]Zhang Wei,Cui Zhijiu,Li Yonghua,et al.Quaternary glacier development and the relationship betw een the climate change and tectonic uplift in the Helan M ountain[J].Chinese Science Bulletin,2012,57(34):4491-4504.[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.]
[77]Zhang Wei,Chai Le.The preliminary study of the Quaternary glacier in middle part of the Tenasserim Chain w ith ESR dating method[J].Journal of Glaciology and Geocryology,2016,38(5):1281-1291.[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.]
[78]Chen Yixin,Li Yingkui,Wang Yueyan,et al.Late Quaternary glacial history of the Karlik Range,easternmost Tian Shan,derived from10Be surface exposure and optically stimulated luminescence datings[J].Quaternary Science Review s,2015,115:17-27.
[79]Liu Beibei,Zhang Wei,Cui Zhijiu,et al.Climate-tectonics coupling effect on Late Quaternary glaciation in the M ayaxue Shan,Gansu Province[J].Journal of Glaciology and Geocryology,2015,37(3):701-710.[刘蓓蓓,张威,崔之久,等.青藏高原东北缘玛雅雪山晚第四纪冰川发育的气候和构造耦合[J].冰川冻土,2015,37(3):701-710.]
[80]He Ze,He Yuanqing,Zhang Zhigang,et al.OSL dating of the Quaternary glacial sedimentary sequences at M t.Yulong,China[J].Journal of Glaciology and Geocryology,2016,38(6):1544-1552.[何则,何元庆,张志刚,等.玉龙雪山冰川沉积序列OSL定年[J].冰川冻土,2016,38(6):1544-1552.]
[81]Bi Weili,Yi Chaolu.Review of ESR dating technique in Quaternary glacial chronology[J].Journal of Glaciology and Geocryology,2016,38(5):1292-1299.[毕伟力,易朝路.ESR测年技术在第四纪冰川年代学中的研究综述[J].冰川冻土,2016,38(5):1292-1299.]
[82]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.]
[83]Wang Jie,Cui Hang,Harbor J M,et al.Mid-MIS3 climate inferred from reconstructing the Dalijia Shan ice cap,north-eastern Tibetan Plateau[J].Journal of Quaternary Science,2015,30(6):558-568.
[2]Li Jijun,Shu Qiang,Zhou Shangzhe,et al.Review and prospects of Quaternary glaciation research in China[J].Journal of Glaciology and Geocryology,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.Paleoglaciation of the Tibetan Plateau and surrounding mountains based on exposure ages and ELA depression estimates[J].Quaternary Science Review s,2014,91(3):30-41.
[4]Fu Ping,Heyman J,H ttestrand C,et al.Glacial geomorphology of the Shaluli Shan,southeastern Tibetan Plateau[J].Journal of M aps,2012,8(1):48-55.
[5]Cui Zhijiu,Wu Yongqiu,Liu Gengnian,et al.On KunlunY ello w River tectonic movement[J].Science in China:Series D Earth Sciences,1998,41(6):592-600.[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 w ith the global change in the M id Quaternary[J].Journal of Glaciology and Geocryology,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 QinghaiTibetan Plateau[J].Quaternary International,2006,154(5):44-51.
[9]Xia Zhengkai,Liu Decheng,Wang Youping,et al.Environmental background of human activities during M IS 3 stage recorded in the Zhijidong cave site,Zhengzhou[J].Quaternary Sciences,2008,28(1):96-102.[夏正楷,刘德成,王幼平,等.郑州织机洞遗址MIS 3阶段古人类活动的环境背景[J].第四纪研究,2008,28(1):96-102.]
[10]Li Xiaoli,Zhang Shuangquan,Wei Mingrui,et al.Environmental background of human occupation at Zhoukoudian Tianyuan cave[J].M arine Geology and Quaternary Geology,2009,29(3):133-140.[李潇丽,张双权,魏明瑞,等.周口店田园洞MIS 3阶段古人类生存环境[J].海洋地质与第四纪地质,2009,29(3):133-140.]
[11]Wang Yongjin,Wu Jiangying,Wu Jinquan,et al.Correlation betw een high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the Last Glaciation[J].Science in China:Series D Earth Sciences,2001,44(1):14-23.[汪永进,吴江滢,吴金全,等.末次冰期南京石笋高分辨率气候记录与GRIP冰芯对比[J].中国科学:D辑地球科学,2000,30(5):533-539.]
[12]Zhang Meiliang,Lin Yushi,Feng Yumei,et al.The records of paleoclimate change from a stalagmite of Dongge cave in the preiod of 42.0 ka BP to 65.0 ka BP in Libo[J].Guangxi Sciences,2004,11(3):218-220.[张美良,林玉石,冯玉梅,等.贵州荔波42.0~65.0 ka BP气候变化的石笋记录[J].广西科学,2004,11(3):218-220.]
[13]Yao Tandong,Thompson L G,Shi Yafeng,et al.Climate variation since the Last Interglaciation recorded in the Guliya ice core[J].Science in China:Series D Earth Sciences,1997,40(6):662-668.[姚檀栋,Thompson L G,施雅风,等.古里雅冰芯中末次间冰期以来气候变化记录研究[J].中国科学:D辑地球科学,1997,27(5):447-452.]
[14]Yang Wenyu,Huang Baoqi,Xiao Jie,et al.Environmental changes of surface sea recorded in planktonic foram in ifera during M IS 3 in the w estern South China Sea[J].Quaternary Sciences,2008,28(3):437-446.[杨文瑜,黄宝琦,肖洁,等.南海西部浮游有孔虫记录的MIS 3期表层海洋环境变化[J].第四纪研究,2008,28(3):437-446.]
[15]Zheng Hongbo,Yang Wenguang,He Juan,et al.Marine isotope stage 3(M IS 3)of South China Sea[J].Quaternary Sciences,2008,28(1):69-78.[郑洪波,杨文光,贺娟,等.南海的氧同位素3期[J].第四纪研究,2008,28(1):69-78.]
[16]Du Jianghui,Huang Baoqi.Variations in upper water structure during M IS 3 from the w estern South China Sea[J].Chinese Science Bulletin,2010,55(3):301-307.
[17]Niu Yaocheng,Zhang Yiyuan,Du Jianghui,et al.Variations in paleoproductivity recorded by benthic foraminifera during M IS 3from the w estern South China Sea[J].M arine Geology and Quaternary Geology,2011,31(1):85-92.[钮耀诚,张译元,杜江辉,等.南海西部MIS 3期底栖有孔虫的生产力变化[J].海洋地质与第四纪地质,2011,31(1):85-92.]
[18]Chen Xiaoyun,Wu Naiqin.Relatively warm-humid climate recorded by mollusk species in the Chinese Loess Plateau during M IS 3 and its possible forcing mechanism[J].Quaternary Sciences,2008,28(1):154-161.[陈晓云,吴乃琴.黄土高原M IS 3时期蜗牛化石记录的温湿气候及其成因机制探讨[J].第四纪研究,2008,28(1):154-161.]
[19]Zhai Xinwei,Li Fuqiang,Wu Song,et al.Huining MIS 3 stage climate change based on the loess grain size record[J].Arid Land Geography,2013,36(5):773-780.[翟新伟,李富强,吴松.会宁剖面黄土粒度记录的MIS 3阶段气候变化研究[J].干旱区地理,2013,36(5):773-780.]
[20]Wu Jinglu,Wang Sumin,Pan Hongxi,et al.Climatic variations in the past 140 ka recorded in core RM,east Qinghai-Xizang Plateau[J].Science in China:Series D Earth Sciences,1997,40(4):443-448.[吴敬禄,王苏民,潘红玺,等.青藏高原东部RM孔140 ka以来湖泊碳酸盐同位素记录的古气候特征[J].中国科学:D辑地球科学,1997,27(3):255-259.]
[21]Wu Jinglu,Wang Sumin,Shi Yafeng,et al.Temperature estimation by oxygen-stable record over the past 200 ka in Zoige Basin[J].Science in China:Series D Earth Sciences,2000,43(6):577-586.[吴敬禄,王苏民,施雅风,等.若尔盖盆地200 ka以来氧同位素记录的古温度定量研究[J].中国科学:D辑地球科学,2000,30(1):73-80.]
[22]Li Shijie,Zhang Hongliang,Shi Yafeng,et al.A high resolution M IS 3 environmental change record derived from lacustrine deposit of Tianshuihai Lake,Qinghai-Tibet Plateau[J].Quaternary Sciences,2008,28(1):121-131.[李世杰,张宏亮,施雅风,等.青藏高原甜水海盆地MIS 3阶段湖泊与环境变化[J].第四纪研究,2008,28(1):122-131.]
[23]Yang Xiangdong,Wang Sumin,Tong Guobang,et al.The late Pleistocene pollen record in the lake sediments from ancient Heqing Lake and its significance for palaeoclimate[J].Quaternary Sciences,1998,18(4):335-342.[羊向东,王苏民,童国榜,等.云南鹤庆古湖晚更新世的孢粉记录及其古气候学意义[J].第四纪研究,1998,18(4):335-342.]
[24]Zhao Zengyou,Yuan Daoxian,Shi Shengqiang,et al.MIS3b vegetation and climate changes based on pollen and charcoal on Qianxi Plateau[J].Acta Ecologica Sinica,2012,32(15):4811-4818.[赵增友,袁道先,石胜强,等.孢粉、炭屑揭示的黔西高原MIS3b期间古植被、古气候演变[J].生态学报,2012,32(15):4811-4818.]
[25]van Andel T H.The climate and landscape of the middle part of the Weichselian Glaciation in Europe:the stage 3 project[J].Quaternary Research,2002,57(1):2-8.
[26]Zhang Zhigang,Wang Jian,Xu Xiaobin,et al.Cosmogenic isotope10Be dating for Kuzhaori moraine in Daocheng Ice Cap[J].M arine Geology and Quaternary Geology,2012,32(1):85-91.[张志刚,王建,徐孝彬,等.稻城冰帽库照日冰碛垄的宇生核素10Be年代测定[J].海洋地质与第四纪地质,2012,32(1):85-91.]
[27]Zhang Zhigang,Wang Jian,Xu Xiaobin,et al.Cosmogenic10Be and26Al chronology of the Last Glaciation of the PalaeoDaocheng Ice Cap,southeastern Qinghai-Tibetan Plateau[J].Acta Geologica Sinica,2015,89(2):575-584.
[28]Wang Jian,Zhang Zhigang,Xu Xiaobin,et al.Cosmogenic isotopes dating of Quaternary glacial activity of the Paleo-Daocheng Ice Cap,on the southeastern part of the Qinghai-Xizang Plateau[J].Quaternary Sciences,2012,32(3):394-402.[王建,张志刚,徐孝彬,等.青藏高原东南部稻城古冰帽南缘第四纪冰川活动的宇生核素年代研究[J].第四纪研究,2012,32(3):394-402.]
[29]Xu Liubing,Zhou Shangzhe,Cui Jianxin,et al.Dating of the Pleistocene glaciations around the Daocheng Ice Cap[J].Journal of Glaciology and Geocryology,2004,26(5):528-534.[许刘兵,周尚哲,崔建新,等.稻城冰帽区更新世冰川测年研究[J].冰川冻土,2004,26(5):528-534.]
[30]Xu Liubing,Zhou Shangzhe.Quaternary glaciations recorded by glacial and fluvial landforms in the Shaluli M ountains,Southeastern Tibetan Plateau[J].Gemorphology,2009,103(2):268-275.
[31]Fu Ping,Stroeven A P,Harbor J M,et al.Paleoglaciation of Shaluli Shan,Southeastern Tibetan Plateau[J].Quaternary Science Review s,2013,64(433):121-135.
[32]Zheng Benxing,Ma Qiuhua.A study on the geomorphological characteristics and glaciations in Paleo-Daocheng Ice Cap,w estern Sichuan[J].Journal of Glaciology and Geocryology,1995,17(1):23-32.[郑本兴,马秋华.川西稻城古冰帽的地貌特征与冰期探讨[J].冰川冻土,1995,17(1):23-32.]
[33]Lin Zhenyao,Wu Xiangding.A study on the path of moisture transportation in the Tibetan Plateau[J].Geographical Research,1990,9(3):33-40.[林振耀,吴祥定.青藏高原水气输送路径的探讨[J].地理研究,1999,9(3):33-40.]
[34]Gou Xiaohua,Yang Tao,Gao Linlin,et al.A 457-year reconstruction of precipitation in the southeastern Qinghai-Tibet Plateau[J].Chinese Science Bulletin,2013,58(10):1107-1114.
[35]Luo Laixing,Yang Yichou.An approach of geomorphological formation in the region of West Sichuan and North Yunnan[C]//Geographical Bulletin No.5.Beijing:Science Press,1963:1-58.[罗来兴,杨逸畴.川西滇北地貌形成的探讨[C]//地理集刊5号.北京:科学出版社,1963:1-58.]
[36]Yao Tandong,Feng Zhaodong,Li Jijun.The basic features of Daocheng ancient ice cap[C]//Studies in Qinghai-Xizang(Tibet)Plateau special issue of Hengduan M ountains scientific expedition(1).Kunming:Yunnan People's Publishing House,1983:132-139.[姚檀栋,冯兆东,李吉均.稻城古冰帽的基本特征[C]//青藏高原研究横断山考察专集(一).昆明:云南人民出版社,1983:132-139.]
[37]Li Jijun,Yao Tandong,Feng Zhaodong.The development model of the Daocheng former ice cap[C]//Studies in Qinghai-Xizang(Tibet)Plateau special issue of Hengduan Mountains scientific expedition(2).Beijing:Beijing Science and Technology Press,1986:271.[李吉均,姚檀栋,冯兆东.稻城古冰帽发育模式[C]//青藏高原研究横断山考察专集(二).北京:北京科学技术出版社,1986:271.]
[38]Li Jijun,Feng Zhaodong,Zhou Shangzhe.The vestiges of Quaternary glaciation in the Hengduan M ountains region[M]//Glacier in the Hengduan M ountains region.Beijing:Science Press,1996:157-173.[李吉均,冯兆东,周尚哲.横断山第四纪冰川作用遗迹[M]//横断山冰川.北京:科学出版社,1996:157-173.]
[39]Zhou Shangzhe,Xu Liubing,Cui Jianxin,et al.Geomorphologic evolution and environmental changes in the Shaluli M ountain region during the Quaternary[J].Chinese Science Bulletin,2005,50(1):52-57.
[40]Schfer J M,Tschudi S,Zhao Zhizhong,et al.The limited influence of glaciations in Tibet on global climate over the past170 000 yr[J].Earth and Planetary Science Letters,2002,194:287-297.
[41]Wang Jian,Raisbeck G,Xu Xiaobin,et al.In situ cosmogenic10Be dating of the Quaternary glaciations in the southern Shaluli M ountain on the Southeastern Tibetan Plateau[J].Science in China:Series D Earth Sciences,2006,49(12):1291-1298.
[42]Shi Yafeng,Yao Tandong.MIS 3b(54~44 ka BP)cold period 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.]
[43]Zhen Zhiguo,Zhong Wei,Xue Jibin,et al.Progress in the studies of climatic features in different areas of China during the M IS-3[J].Journal of Glaciology and Geocryology,2008,30(5):814-824.[甄治国,钟巍,薛积彬,等.中国不同区域M IS-3时期气候特征研究进展[J].冰川冻土,2008,30(5):814-824.]
[44]Fang Xiaomin,Lu Liangqing,Mason J A,et al.Pedogenic response to millennial summer monsoon enhancements on the Tibetan Plateau[J].Quaternary International,2003,106(2):79-88.
[45]Yao Jing,Yu Hongjun,Xu Xingyong,et al.Paleoenvironmental changes during the late Quaternary as inferred from foraminifera assemblages in the Laizhou Bay[J].Acta Oceanologica Sinica,2014,33(10):10-18.
[46]Zhao Yan,Yu Zicheng,Herzschuh U,et al.Vegetation and climate change during M arine Isotope Stage 3 in China[J].Chinses Science Bulletin,2014,59(33):4444-4455.
[47]Gillespie A,Molnar P.Asynchronous maximum advances of mountain and continental glaciers[J].Review s of Geophysics,1995,33(3):311-364.
[48]Phillips W M,Sloan V F,Shroder J F J,et al.Asynchronous glaciation at Nanga Parbat,northw estern Himalaya M ountains,Pakistan[J].Geology,2000,28(5):431-434.
[49]Owen L A,Finkel R C,Caffee M W.A note on the extent of glaciation throughout the Himalaya during the global Last Glacial M aximum[J].Quaternary Science Review s,2002,21(1):147-157.
[50]Zhao Jingdong,Zhou Shangzhe,Liu Shiyin,et al.A preliminary study of the glacier advance in M IS3b in the w estern 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.]
[51]Wang Jie.Glacial advance in the Qinghai-Xizang Plateau and peripheral mountains during the mid-M IS 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.]
[52]Finkel R C,Owen L A,Barnard P L,et al.Beryllium-10 dating of M ount Everest moraines indicates a strong monsoonal influence and glacial synchroneity throughout the Himalaya[J].Geology,2003,31:561-564.
[53]Zech W,Glaser B,Abramowski U,et al.Reconstruction of the Late Quaternary Glaciation of the M acha Khola valley(Gorkha Himal,Nepal)using relative and absolute(14C,10Be,dendrochronology)dating techniques[J].Quaternary Science Review s,2003,22(21):2253-2265.
[54]Owen L A,Caffee M W,Bovard K R,et al.Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen:Ladakh Range,northern India[J].Geological Society of America Bulletin,2006,118(3):383-392.
[55]Owen L A,Robinson R,Benn D I,et al.Quaternary glaciation of M ount Everest[J].Quaternary Science Review s,2009,28(15):1412-1433.
[56]Dortch J M,Owen L A,Caffee M W.Quaternary glaciation in the Nubra and Shyok valley confluence,northernmost Ladakh,India[J].Quaternary Research,2010,74(1):132-144.
[57]Owen L A,Yi Chaolu,Finkel R C,et al.Quaternary glaciation of Gurla M andhata(Naimon'anyi)[J].Quaternary Science Review s,2010,29(15):1817-1830.
[58]Hedrick K A,Seong Y B,Owen LA,et al.Towards defining the transition in style and timing of Quaternary glaciation betw een the monsoon-influenced Greater Himalaya and the semi-arid Transhimalaya of Northern India[J].Quaternary International,2011,236(1):21-33.
[59]Owen L A,Finkel R C,Caffee M W,et al.Timing of multiple Late Quaternary glaciations in the Hunza Valley,Karakoram M ountains,northern Pakistan:defined by cosmogenic radionuclide dating of moraines[J].Geological Society of America Bulletin,2002,114(5):593-604.
[60]Owen L A,Finkel R C,Ma Haizhou,et al.Timing and style of Late Quaternary glaciation in northeastern Tibet[J].Geological Society of America Bulletin,2003,115(11):1356-1364.
[61]Owen L A,Finkel R C,Ma Haizhou,et al.Late Quaternary landscape evolution in the Kunlun M ountains and Qaidam Basin,Northern Tibet:a framew ork for examining the links betw een glaciation,lake level changes and alluvial fan formation[J].Quaternary International,2006,154(5):73-86.
[62]Abramowski U,Bergau A,Seebach D,et al.Pleistocene glaciations of Central Asia:results from10Be surface exposure ages of erratic boulders from the Pamir(Tajikistan)and the Alay-Turkestan range(Kyrgyzstan)[J].Quaternary Science Review s,2006,25(9):1080-1096.
[63]Koppes M,Gillespie A R,Burke R M,et al.Late Quaternary glaciation in the Kyrgyz Tien Shan[J].Quaternary Science Review s,2008,27(7/8):846-866.
[64]Li Yingkui,Liu Gengnian,Chen Yixin,et al.Timing and extent of Quaternary glaciations in the Tianger Range,eastern Tian Shan,China,investigated using10Be surface exposure dating[J].Quaternary Science Reviews,2014,98:7-23.
[65]Owen L A,Finkel R C,Barnard P L,et al.Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by10Be cosmogenic radionuclide surface exposure dating[J].Quaternary Science Review s,2005,24:1391-1411.
[66]Colgan P M,Munroe J S,Zhou Shangzhe.Cosmogenic radionuclide evidence for the limited extent of Last Glacial M aximum glaciers in the Tanggula Shan of the central Tibetan Plateau[J].Quaternary Research,2006,65(2):336-339.
[67]Dong Guocheng,Yi Chaolu,Caffee M.10Be dating of boulders on moraines from the last glacial period in the Nyainqentanglha M ountains,Tibet[J].Science China:Series D Earth Sciences,2014,57(2):221-231.
[68]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 Review s,2011,30(15/16):1988-2001.
[69]Wang Jie,Kassab C,Harbor J M,et al.Cosmogenic nuclide constraints on late Quaternary glacial chronology on the Dalijia Shan,northeastern Tibetan Plateau[J].Quaternary Research,2013,79(3):439-451.
[70]Zech R,Abramowski U,Glaser B,et al.Late Quaternary glacier and climate history of the Pamir M ountains derived from cosmogenic10Be exposure ages[J].Quaternary Research,2005,64(2):212-220.
[71]Xu Liubing,Ou Xianjiao,Lai Zhongping,et al.Timing and style of Late Pleistocene glaciation in the Queer Shan,northern Hengduan M ountains in the eastern Tibetan Plateau[J].Journal Quaternary Science,2010,25(6):957-966.
[72]Wang Jie,Zhou Shangzhe,Zhao Jingdong,et al.Quaternary glacial geomorphology and glaciations of Kongur M ountain,eastern Pamir,China[J].Science in China:Series D Earth Sciences,2011,54(4):591-602.[王杰,周尚哲,赵井东,等.东帕米尔公格尔山地区第四纪冰川地貌与冰期[J].中国科学:D辑地球科学,2011,41(3):350-361.]
[73]Wang Jie,Pan Baotian,Zhang Guoliang,et al.Late Quaternary glacial chronology on the eastern slope of Gongga M ountain,eastern Tibetan Plateau,China[J].Science China:Series D Earth Sciences,2012,56(3):354-365.[王杰,潘保田,张国梁,等.贡嘎山东坡中更新世晚期以来冰川作用年代学研究[J].中国科学:D辑地球科学,2012,42(12):1889-1900.]
[74]Jiang Heli,Zhao Jingdong,Yin Xiufeng,et al.New OSL Chronology of the Last Glaciation in Kanas River Valley,Altay M ountains,China[J].Journal of Glaciology and Geocryology,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.]
[75]Zhang Wei,Liu Beibei,Li Yonghua,et al.Quaternary glacier development and environmental evolution in Qianhu M ountain,Northw estern 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.]
[76]Zhang Wei,Cui Zhijiu,Li Yonghua,et al.Quaternary glacier development and the relationship betw een the climate change and tectonic uplift in the Helan M ountain[J].Chinese Science Bulletin,2012,57(34):4491-4504.[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.]
[77]Zhang Wei,Chai Le.The preliminary study of the Quaternary glacier in middle part of the Tenasserim Chain w ith ESR dating method[J].Journal of Glaciology and Geocryology,2016,38(5):1281-1291.[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.]
[78]Chen Yixin,Li Yingkui,Wang Yueyan,et al.Late Quaternary glacial history of the Karlik Range,easternmost Tian Shan,derived from10Be surface exposure and optically stimulated luminescence datings[J].Quaternary Science Review s,2015,115:17-27.
[79]Liu Beibei,Zhang Wei,Cui Zhijiu,et al.Climate-tectonics coupling effect on Late Quaternary glaciation in the M ayaxue Shan,Gansu Province[J].Journal of Glaciology and Geocryology,2015,37(3):701-710.[刘蓓蓓,张威,崔之久,等.青藏高原东北缘玛雅雪山晚第四纪冰川发育的气候和构造耦合[J].冰川冻土,2015,37(3):701-710.]
[80]He Ze,He Yuanqing,Zhang Zhigang,et al.OSL dating of the Quaternary glacial sedimentary sequences at M t.Yulong,China[J].Journal of Glaciology and Geocryology,2016,38(6):1544-1552.[何则,何元庆,张志刚,等.玉龙雪山冰川沉积序列OSL定年[J].冰川冻土,2016,38(6):1544-1552.]
[81]Bi Weili,Yi Chaolu.Review of ESR dating technique in Quaternary glacial chronology[J].Journal of Glaciology and Geocryology,2016,38(5):1292-1299.[毕伟力,易朝路.ESR测年技术在第四纪冰川年代学中的研究综述[J].冰川冻土,2016,38(5):1292-1299.]
[82]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.]
[83]Wang Jie,Cui Hang,Harbor J M,et al.Mid-MIS3 climate inferred from reconstructing the Dalijia Shan ice cap,north-eastern Tibetan Plateau[J].Journal of Quaternary Science,2015,30(6):558-568.