全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

青藏高原及周边地区MIS3中期冰进探讨

, PP. 1055-1065

Keywords: 青藏高原,MIS3,冰进,第四纪冰川,测年

Full-Text   Cite this paper   Add to My Lib

Abstract:

随着ESR,OSL以及CRN等新技术被应用到第四纪冰川测年,青藏高原及周边山地的许多地区建立起了第四纪冰川演化的年代序列,研究人员在青藏高原南缘和东缘发现末次冰期最大规模古冰川作用出现于末次冰期的间冰阶(MIS3),而不是末次冰期晚阶段(MIS2)。对该区域内已获得的测年资料进行总结,发现在兴都库什山、喜马拉雅山、昆仑山、念青唐古拉山、唐古拉山、喀喇昆仑山、横断山、祁连山、天山、帕米尔高原以及台湾山地等(共30个点)都存在MIS3山地冰川前进的年代数据,其中,虽有部分点的数据精度和可靠性不高,但不可否认青藏高原及周边山地曾发生MIS3山地冰川前进的事实,且多数年代数据都集中于MIS3中期。通过年代学资料与古环境记录的综合分析,笔者初步得出:在季风环流控制区,MIS3(中期)冰进可能是由于该阶段中期的冷期(也可能是古里雅冰芯记录中47~43kaB.P.两次冷事件的直接作用)结合较丰富的亚洲季风降水造成;在西风环流主要控制区,如天山、帕米尔地区与西昆仑山,虽然在MIS3时由于冰盖退缩,高纬度的冷高压减弱,使得西风急流北支北撤,西风强度有所减弱,但相对LGM时大洋的温度还是较高,蒸发旺盛,因而西风环流可为上述地区带来较多的降水,配合MIS3中期的低温致使冰川前进。用多种技术方法交叉对冰川遗迹进行系统定年,是现阶段第四纪冰川研究面临的重要内容,还应注意季风与西风气候系统下冰川演化模式可能存在的异同。

References

[1]  1 Gillespie A, Molnar P.Asynchronous maximum advances of mountain and continental glacials. Reviews of Geophysics,1995, 33 (3):311~364
[2]  5 赵井东,周尚哲,崔建新等.乌鲁木齐河源冰碛物的ESR测年研究.冰川冻土,2002, 24 (6):737~743
[3]  Zhao Jingdong,Zhou Shangzhe,Cui Jianxin et al.ESR dating of glacial tills at the headwaters of the Vrümqi River in the Tianshan Mountains. Journal of Glaciology and Geocryology,2002, 24 (6):737~743
[4]  6 易朝路,焦克勤,刘克新等.冰碛物ESR测年与天山乌鲁木齐河源末次冰期系列.冰川冻土,2001, 23 (4):389~393
[5]  Yi Chaolu,Jiao Keqin,Liu Kexin et al.ESR dating on tills and the Last Glaciations at the headwaters of the Vrümqi River,Tianshan Mountains,China. Journal of Glaciology and Geocryology,2001, 23 (4):389~393
[6]  7 Zhao Jingdong, Liu Shiyin,He Yuanqing et al.Quaternary glacial chronology of the Ateaoyinake River valley,Tianshan Mountains,China. Geomorphology,2009, 103 :276~284
[7]  8 赵井东,王 杰,刘时银.天山木扎尔特河流域的冰川地貌与冰期.地理学报,2009, 64 (5):553~562
[8]  Zhao Jingdong,Wang Jie,Liu Shiyin.Glacial geomorphology and glaciations in the Muzhaerte River valley,Tianshan Mountains. Acta Geographica Sinica,2009, 64 (5):553~562
[9]  9 Abramowski U, Bergau A,Seebach D et al.Pleistocene glaciations of Central Asia: Results from \{10 Be\} surface exposure ages of erratic boulders from the Pamir(Tajikistan),and the Alay-Turkestan range(Kyrgyzstan). Quaternary Science Reviews,2006, 25 (9~10):1080~1096
[10]  10 Zech R, Abramowski U,Glaser B et al.Late Quaternary glacial and climate history of the Pamir Mountains derived from cosmogenic \{10 Be\} exposure ages. Quaternary Research,2005, 64 :212~220
[11]  11 Owen L A, Kamp U,Spencer J Q et al.Timing and style of Late Quaternary glaciation in the Eastern Hindu Kush,Chitral,Northern Pakistan: A review and revision of the glacial chronology based on new optically stimulated luminescence dating. Quaternary International,2002, 97/98 :41~55
[12]  12 Owen L A, Finkel R C,Caffee M W et al.Timing of multiple Late Quaternary glaciations in the Hunza Valley,Karakoram Mountains,Northern Pakistan: Defined by cosmogenic radionuclide dating of moraines. Geological Society of America Bulletin,2002, 114 (5):593~604
[13]  Li Jijun,Xu Shuying.Studies on the landform development and Quaternary glaciations in North Pakistan. Acta Geographica Sinica,1983, 38 (1):11~24
[14]  15 徐道明,沈永平.青藏高原的泛冰盖遗迹与冰期.冰川冻土,1995, 17 (3):213~229
[15]  Xu Daoming,Shen Yongping.On ancitent ice-sheet and ice age in the Tibetan Plateau. Journal of Glaciology and Geocryology,1995, 17 (3):213~229
[16]  16 Richards B W, Owen L A,Rhodes E J.Timing of Late Quaternary glaciations in the Himalayas of Northern Pakistan. Journal of Quaternary Science,2000, 15 :283~297
[17]  17 Owen L A, Wishart M,Bailey R M et al.Style and timing of glaciation in Lahul Himalaya,North India: A framework for reconstructing Late Quaternary paleoclimatic change in the Western Himalayas. Journal of Quaternary Science,1997, 12 :83~110
[18]  18 Ma Q H. Geomorphology and Quaternary glaciation in Naimonayi Peak region.In: Shidei T P ed. Sino Japanese Joint Science Symposium of Tibetan Plateau(Vol.02).Japan: Kyoto Press,1989.41~59
[19]  19 Finkel R C, Owen L A,Barnard P L et al.Beryllium-10 dating of Mount Everest moraines indicates a strong monsoon influence and glacial synchroneity throughout the Himalaya. Geology,2003, 31 (6):561~564
[20]  20 Zech W, Glaser B,Abramowski U et al.Reconstruction of the Late Quaternary Glaciation of the Macha Khola valley(Gorkha Himal,Nepal)using relative and absolute(\{14 C\},\{10 Be\},dendrochronology)dating techniques. Quaternary Science Reviews,2003, 22 (21~22):2253~2265
[21]  21 Owen L A, Caffee M,Bovard K et al.Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen: Ladakh Range,Northern India. Geological Society of America Bulletin,2006, 118 (3~4):383~392
[22]  29 赵井东,周尚哲,刘时银等.中国西部山岳冰川MIS 3b冰进的初步探讨.冰川冻土,2007, 29 (2):233~241
[23]  Zhao Jingdong,Zhou Shangzhe,Liu Shiyin et al.A preliminary study of the glacier advance in MIS 3b in the western regions of China. Journal of Glaciology and Geocryology,2007, 29 (2):233~241
[24]  30 Cui Zhijiu, Yang Chienfu,Liu Gengnian et al.The Quaternary glaciation of Shesan Mountain in Taiwan and glacial classification in monsoon areas. Quaternary International,2002, 97/98 :147~153
[25]  31 Spencer J Q, Owen L A.Optically stimulated luminescence dating of Late Quaternary glaciogenic sediments in the upper Hunza valley: Validating the timing of glaciation and assessing dating methods. Quaternary Science Reviews,2004, 23 :175~191
[26]  32 郑本兴,李世杰,王苏民.若尔盖盆地周围高山第四纪冰川演变历史.见: 青藏项目专家委员会编.青藏高原形成演化、环境变迁与生态系统研究——学术论文年刊(1994).北京: 科学出版社,1995.168~174
[27]  Zheng Benxing,Li Shijie,Wang Sumin.The Quaternary glacial evolution of the mountains surrounding zoige Basin.In: The Expert Committee on the Qingzang Program ed.Study on the Formation and Evolution of the Qinghai-Xizang Plateau,Environmental Change and Ecological——Annual Academic(1994).Beijing: Science Press,1995.168~174
[28]  33 Lehmkuhl F. Extent and spatial distribution of Pleistocene glaciations in Eastern Tibet. Quaternary International,1998, 45/46 :123~134
[29]  34 王靖泰.阿尼玛卿山气候地貌.冰川冻土,1988, 10 (2):161~171
[30]  Wang Jingtai.Climate geomorphology of the Anyemaqen Mountains. Journal of Glaciology and Geocryology,1988, 10 (2):161~171
[31]  35 郑本兴,王苏民.黄河源区的古冰川与古环境探讨.冰川冻土,1996, 18 (3):210~218
[32]  Zheng Benxing,Wang Sumin.A study on the paleo-glaciation and paleoenvironment in the source area of the Yellow River. Journal of Glaciology and Geocryology,1996, 18 (3):210~218
[33]  36 李吉均,郑本兴,杨锡金等编著.西藏冰川.北京: 科学出版社,1986.238~242
[34]  Li Jijun,Zheng Benxing,Yang Xijin et al.ed.Glaciers of Xizang(Tibet).Beijing: Science Press,1986.238~242
[35]  37 周尚哲,李吉均.冰期之青藏高原新研究.地学前缘,2001, 8 (1):67~75
[36]  Zhou Shangzhe,Li Jijun.A new study on Qinghai-Tibet Plateau in ice ages. Earth Science Frontiers,2001, 8 (1):67~75
[37]  38 Heinrich H. Origin and consequences of cyclic ice rafting in the north East Atlantic Ocean during the past 130000 years. Quaternary Research,1988, 29 :142~152
[38]  39 Dansgaard W, Johnsen S J,Clausen H B et al.Evidence for general instability of past climate from a 250 kyr ice core record. Nature,1993, 364 :218~220
[39]  40 Grootes P M, Stuiver M,White J W C et al.Comparison of oxygen isotopes records from the GISP2 and GRIP Greenland ice cores. Nature,1993, 366 :552~554
[40]  41 Hinnov L A, Schulz M,Yiou P. Interhemispheric space-time attributes of the Dansgaard-Oeschger oscillations between 100 and 0ka. Quaternary Science Reviews,2002, 21 :1213~1228
[41]  42 Shi Yafeng, Liu Xiaodong,Li Bingyuan et al.A very strong summer monsoon event during 30~40ka BP in the Qinghai-Xizang(Tibet)Plateau and its relation to precessional cycle. Chinese Science Bulletin,1999, 44 (20):1851~1857
[42]  43 Ganopolski A, Rahmstorf S.Rapid changes of glacial climate simulated in a coupled climate model. Nature,2001, 409 :153~158
[43]  44 Sima A, Paul A,Schulz M.The Younger Dryas——An intrinsic feature of Late Pleistocene climate change at millennial timescales. Earth and Planetary Science Letters,2004, 222 :741~750
[44]  45 Yao Tandong, Thompson L G,Shi Yafeng et al.Climate variation since the Last Interglaciation recorded in the Guliya ice core. Science in China (Series D),1997, 40 (6):662~668
[45]  46 Van Andel T H. The climate and landscape of the middle part of the Weichselian Glaciation in Europe: The Stage 3 Project. Quaternary Research,2002, 57 :2~8
[46]  47 Voelker A H L. Global distribution of centennial-scale records for Marine Isotope Stage(MIS)3: A database. Quaternary Science Reviews,2002, 21 :1185~1212
[47]  48 Arnold N S, Van Andel T H,Valen V.Extent and dynamics of the Scandinavian ice sheet during oxygen isotope stage 3(65000~25000 yr B.P.). Quaternary Research,2002, 57 :38~48
[48]  49 Yan Baoyin, Huang Weiwen,Zhang David.New evidence for human occupation of the northern Tibetan Plateau,China during the Late Pleistocene. Chinese Science Bulletin,2007, 52 (19):2675~2679
[49]  52 施雅风,贾玉连,于 革等.40~30ka BP 青藏高原及邻区高温大降水事件的特征、影响及原因探讨.湖泊科学,2002, 14 (1):1~11
[50]  Shi Yafeng,Jia Yulian,Yu Ge et al.Features,impacts and causes of the high temperature and large precipitation event in the Tibetan Plateau and its adjacent area during 40~30ka BP. Journal of Lake Sciences,2002, 14 (1):1~11
[51]  53 施雅风,于 革. 40~30kaB.P.中国暖湿气候和海侵的特征与成因探讨.第四纪研究,2003, 23 (1):1~11
[52]  Shi Yafeng,Yu Ge.Warm-humid climate and transgressions during 40~30kaB.P.and their potential mechanisms. Quaternary Sciences,2003, 23 (1):1~11
[53]  54 杨 保,施雅风.40~30kaB.P.中国西北地区暖湿气候的地质记录及成因探讨.第四纪研究,2003, 23 (1):60~68
[54]  Yang Bao,Shi Yafeng.Warm-humid climate in North West China during the period of 40~30kaB.P.:Geological records and origin. Quaternary Sciences,2003, 23 (1):60~68
[55]  55 施雅风,赵井东.40~30ka BP中国特殊暖湿气候与环境的发现与研究过程的回顾.冰川冻土,2009, 31 (1):1~10
[56]  Shi Yafeng,Zhao Jingdong.The Special warm-humid climate and environment in China during 40~30ka BP: Discovery and review. Journal of Glaciology and Geocryology,2009, 31 (1):1~10
[57]  Shi Yafeng,Huang Maohuan,Ren Binghui eds.An Introduction to the Glaciers in China Contents.Beijing: Science Press,1988.20~25
[58]  66 李吉均.中国西北地区晚更新世以来环境变迁模式.第四纪研究,1990,(3):197~204
[59]  Li Jijun.The patterns of environmental changes since Late Pleistocene in North Western China. Quaternary Sciences,1990,(3):197~204
[60]  67 Chen Fahu, Yu Zicheng,Yang Meilin et al.Holocene moisture evolution in arid Central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews,2008, 27 (3~4):351~364
[61]  68 Chen Fahu, Holmes J,Wünnemann B et al.Holocene climate variability in arid Asia: Nature and mechanisms. Quaternary International,2009 194 (1~2)
[62]  2 Phillips W M, Sloan V F,Shroder J F et al.Asynchronous glaciation at Nanga Parbat North Western Himalaya Mountains,Pakistau. Geology,2000, 28 (5):431~434
[63]  3 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. Quaternary Science Reviews,2002, 21 :147~157
[64]  4 施雅风,姚檀栋.中低纬度MIS 3b(54~44ka BP)冷期与冰川前进.冰川冻土,2002, 24 (1):1~9
[65]  Shi Yafeng,Yao Tandong.MIS 3b(54~44ka BP)cold period and glacial advance in middle and low latitudes. Journal of Glaciology and Geocryology,2002, 24 (1):1~9
[66]  13 Derbyshire E, Li Jijun,Perrott F A et al.Quaternary glacial history of the Hunza Valley,Karakoram Mountains,Pakistan.In: Miller K ed.International Karakoram Project.Cambridge: Cambridge University Press,1984.456~495
[67]  14 李吉均,徐叔鹰.巴基斯坦北部的地貌发育与第四纪冰期问题.地理学报,1983, 38 (1):11~24
[68]  22 Owen L A, Finkel R C,Ma Haizhou et al.Timing and style of Late Quaternary glaciation in North Eastern Tibet. Geological Society of America Bulletin,2003, 115 (11):1356~1364
[69]  23 Owen L A, Finkel R C,Ma Haizhou et al.Late Quaternary landscape evolution in the Kunlun Mountains and Qaidam Basin,Northern Tibet: A framework for examining the links between glaciation,lake level changes and alluvial fan formation. Quaternary International,2006, 154/155 :73~86
[70]  24 Colgan P M, Munroe J S,Zhou Shangzhe.Cosmogenic radionuclide evidence for the limited extent of last glacial maximum glaciers in the Tanggula Shan of the Central Tibetan Plateau. Quaternary Research,2006, 65 (2):336~339
[71]  25 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 by \{10 Be\} cosmogenic radionuclide surface exposure dating. Quaternary Science Reviews,2005, 24 (12~13):1391~1411
[72]  26 许刘兵,周尚哲,王 杰.沙鲁里山更新世冰川作用及西南季风波动对末次冰期冰川作用的影响.第四纪研究,2005, 25 (5):620~629
[73]  Xu Liubing,Zhou Shangzhe,Wang Jie.Pleistocene glaciations in the Shaluli Shan and the influences of southwest monsoon on the glaciations during the last glacial period. Quaternary Sciences,2005, 25 (5):620~629
[74]  27 Xu Liubing, Zhou Shangzhe.Quaternary glaciations recorded by glacial and fluvial landforms in the Shaluli Mountains,South Eastern Tibetan Plateau. Geomorphology,2009, 103 :268~275
[75]  28 赵井东,周尚哲,史正涛等.祁连山东段冷龙岭南麓白水河冰碛物ESR测年研究.兰州大学学报(自然科学版),2001, 37 (4):110~117
[76]  Zhao Jingdong,Zhou Shangzhe,Shi Zhengtao et al.ESR dating of glacial tills of Baishuihe River on the southern slope of Lenglongling in the eastern part of Qilian Mountains. Journal of Lanzhou University(Natural Sciences),2001, 37 (4):110~117
[77]  50 Shang Hong, Tong Haowen,Zhang Shuangquan et al.An early modern human from Tianyuan Cave,Zhoukoudian,China. PNAS,2007, 104 (16):6573~6578
[78]  51 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.第四纪研究,2008, 28 (1):96~102
[79]  Xia Zhengkai,Liu Decheng,Wang Youping et al.Environmental background of human activities during MIS 3 stage recorded in the Zhijidong Cave Site,Zhengzhou. Quaternary Sciences,2008, 28 (1):96~102
[80]  56 张茂恒,夏应菲,孟景闻等.下蜀黄土中记录的氧同位素3 阶段(MIS 3)特殊暖湿现象.土壤学报,2008, 45 (1):9~15
[81]  Zhang Maoheng,Xia Yingfei,Meng Jingwen et al.The especially warm and wet during MIS 3 recorded by Xiashu Loess. Acta Pedologica Sinica,2008, 45 (1):9~15
[82]  57 李世杰,张宏亮,施雅风等.青藏高原甜水海盆地MIS 3阶段湖泊沉积与环境变化.第四纪研究,2008, 28 (1):122~131
[83]  Li Shijie,Zhang Hongliang,Shi Yafeng et al.A high resolution MIS 3 environmental change record derived from lacustrine deposit of Tianshuihai Lake,Qinghai-Tibet Plateau. Quaternary Sciences,2008, 28 (1):122~131
[84]  58 李玉梅,刘东生,吴文祥等.黄土高原马兰黄土记录的MIS 3温湿气候.第四纪研究,2003, 23 (1):69~76
[85]  Li Yumei,Liu Lungsheng,Wu Wenxiang et al.Paleoenvironment in Chinese Loess Plateau during MIS 3: Evidence from Malan Loess. Quaternary Sciences,2003, 23 (1):69~76
[86]  59 Gu Zhaoyan. The carbonate isotopic composition of the loess-paleosol sequence and its implication of paleoclimatic change. Chinese Science Bulletin,1991, 36 (23):1979~1983
[87]  60 Lin B H, Liu R M,An Z S.Preliminary research on stable isotopic composition of Chinese loess.In: Liu T S ed.Loess,Environment and Global Change.Beijing: Science Press,1991.124~131
[88]  62 陈晓云,吴乃琴.黄土高原MIS 3时期蜗牛化石记录的温湿气候及其成因机制探讨.第四纪研究,2008, 28 (1):154~161
[89]  Chen Xiaoyun,Wu Naiqin.Relatively warm-humid climate recorded by mollusk species in the Chinese Loess Plateau during MIS 3 and its possible forcing mechanism. Quaternary Sciences,2008, 28 (1):154~161
[90]  63 Ding Zhongli, Sun Jimin,Yu Zhiwei et al.Chronology of environmental events over East-Asia during the past 130ka. Chinese Science Bulletin,1998, 43 (21):1761~1770
[91]  64 类延斌,张虎才,尚华明等.青藏高原年保玉则山末次冰期中期以来的湖泊演化与古冰川发育.第四纪研究,2008, 28 (1):132~139
[92]  Lei Yanbin,Zhang Hucai,Shang Huaming et al.Lake evolution and glaciation of the Nianbaoyuze Mountain in the Tibetan Plateau since the middle of the last glacial. Quaternary Sciences,2008, 28 (1):132~139
[93]  65 施雅风,黄茂桓,任炳辉编著.中国冰川概论.北京: 科学出版社,1988.20~25

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133