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《Quaternary Sciences》 2003-01
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CLIMATIC CHANGE AND LAKE-LEVEL VARIATION OF NAM CO, XIZANG SINCE THE LAST INTERGLACIAL STAGE

Zhao Xitao① Zhu Dagang② Yan Fuhua③ Wu Zhonghai② Ma Zhibang① Mai Xueshun③ (① Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029; ② Institute of Geomechanics, Chinese Academy of Geological Sciences,Beijing 100081; ③ Institute of Geology, Chinese Bureau of Seismology, Beijing 100029)  
Nam Co, located at the southeast part of the North Xizang (Tibetan) Plateau,is the biggest lake (1 920 km2) and the highest big lake (4 718 m a.s.l.) in Xizang. Leveling survey shows that there are 6 lake terraces and highstand lacustrine sediments from 48 m to 139.2 m above the lake level. Result of U-series dating of carbonate-bearing lacustrine sediments samples indicates that the highstand lacustrine sediments were deposited from 115.9±12.1 to 71.8±8.5kaB.P., the terraces of Nos.6, 5, 4, 3, 2 and 1 were formed in ca. 53.7±4.2kaB.P.?41.2±4.7~39.5± 3.0kaB.P.?36.1±2.2~35.2±3.0kaB.P.?32.3±4.4kaB.P.?28.2±2.8kaB.P.and 11.2±2.0kaB.P., respectively. Based on the data of U-series dating and sporo-pollen analysis, the paleovegetation, paleoclimate and lake-level variation of Nam Co and the adjacent regions since the Last Interglacial Stage (MIS 5) are discussed in this paper. Lake-level variation of Nam Co and the adjacent regions can be divided into the three stages: (1) The great paleo-lake of 116~37kaB.P., "Lake East Qiangtang", (2) outflow lake between 37 and 30ka B.P., the "Paleo-Nam Co" and the remnant great paleo-lake, and (3) Nam Co and North Xizang lakes since 30ka B.P. In the stage of great paleo-lake of MIS 5, a series of lakes, such as Nam Co, Siling Co and other big and moderate lakes in the southeast North Xizang Plateau were joined together into a great lake whose range might overstep the water divide between the North Xizang endorheic regions and the Nujiang River drainage. Especially in the stage of highest lake-level of late MIS 5e, the surface area of "Lake East Qiangtang" may be achieved 78,800 km2, and its drainage area, 167,000 km2.It might be joined together with the other great paleo-lakes in the central-southern and the southwestern North Xizang Plateau, formed a giant net-shaped coalescent deep lake, "Lake Qiangtang". A comparison of the climatic change and lake-level variation from Nam Co with the data of Oxygen isotopic curve from the Guliya ice core in West Kunlun Mountains and that of the ice cores of GISP2, Greenland and Vostok, Antarctic shows that the temperature in MIS 5 was higher than that of the Last interstadial (MIS 3). During the MIS 5, the great paleo-lake stage, the climate in the southeast North Xizang Plateau was mild and slightly drier than that of the present. In the two stadials of Last Glaciation, MIS 4 and MIS 2, the lake level were obviously lowering and the small-size valley glaciation occurred in the Nyaiqentanglha Mountains. During the interstadial of MIS 3,the amplitudes of the climatic and lake-level variations in the region were higher than that of the other regions of the world, especially in period of 36~35ka B.P., the temperature and moisture were slightly or much higher than that of the present, but not the Holocene Climatic Optimum. In a word, the Asian Summer Monsoons on the Xizang Plateau in the periods of MIS 5 and MIS 3 were stronger than that of the present, especially in MIS 5e.
【Fund】: 中国地质调查局“西藏纳木错第四纪环境演变调查研究”(批准号 :DKD2 0 0 10 0 6);; 1∶2 50 0 0 0当雄幅地质调查 (批准号 :DKD990 10 0 1)资助项目
【CateGory Index】: P532
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9 CHEN Jianfeng~(①②) SHI Zhenming~(①②) SHI Yubing~③(①Department of Geotechnical Engineering,Tongji University,Shanghai 200092 ) (②Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education,Tongji University,Shanghai 200092) (③Chengdu Hydroelectric Investigation & Design Institute of SPC,Chengdu 610072 );ANALYSES OF THE STABILITY AND EARTHQUAKE RESPONSE OF A BARRIER LAKE DAM[A];[C];2008
10 HUANG LinPei~(1,2*),WU NaiQin~1,GU ZhaoYan~1 & CHEN XiaoYun~1 1 Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences, Beijing 100029,China; 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China;Variability of snail growing season at the Chinese Loess Plateau during the last 75 ka[A];[C];2013
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