 |
MARINE ISOTOPE STAGE 3 (MIS 3) OF SOUTH CHINA SEA |
|
Zheng Hongbo Yang Wenguang He Juan Mei Xi Chen Guocheng Xie Xin Huang Enqing Su Xiang Qiao Peijun(School of Ocean and Earth Science,Tongji University,Shanghai 200092) |
|
SINCE MIS 3 STAGE THE CORRELATION BETWEEN TRANSGRESSION AND CLIMATIC CHANGES IN THE NORTH HUANGHUA AREA,HEBEI |
|
Wang Qiang① Zhang Yufa① Yuan Guibang① Zhang Wenqing②(①Tianjin Institute of Geology and Mineral Resouces,Tianjin 300170;(②Institute of Technologic Method of Hydrogeology & Engineering Geology,Academy Geologic Sinica of China,Baoding 071051) |
|
MILLENNIAL-SCALE CLIMATE FLUCTUATIONS DURING THE LAST INTERSTADIAL RECORDED IN THE AQS3 SEGMENT OF THE AQIANG LOESS SECTION IN THE NORTH PIEDMONT OF THE KUNLUN MOUNTAINS |
|
Li Baosheng①② Wen Xiaohao① Zhang David Dian③ Li Sen④ Dong Guangrong⑤Du Shuhuan① Ou Xianjiao① Qiu Shifan① Wang Guiyong④ Li Zhiwen① Niu Dongfeng①(①Department of Geography,South China Normal University,Guangzhou 510631; ②State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi'an 710061; ③Department of Geography & Geology,The University of Hong Kong,Hong Kong,China; ④Department of Geography,Foshan University,Foshan 528000; ⑤Institute of Cold and Arid Regions Environmental and Engineering,Chinese Academy of Sciences,Lanzhou 730000) |
|
ENVIRONMENTAL EVOLUTION IN LOP NUR SINCE LATE PLEISTOCENE AND ITS RESPONSE TO THE GLOBAL CHANGES |
|
Wang Fubao① Ma Chunmei① Xia Xuncheng② Cao Qiongying① Zhu Qing①(①School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093; ②Xinjiang Insititute of Ecology and Geography Chinese Academy of Sciences,rümqi 830011) |
|
RELATIVELY WARM-HUMID CLIMATE RECORDED BY MOLLUSK SPECIES IN THE CHINESE LOESS PLATEAU DURING MIS 3 AND ITS POSSIBLE FORCING MECHANISM |
|
Chen Xiaoyun Wu Naiqin(Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029) |
|
SPATIAL CHANGES OF CHEMICAL WEATHERING RECORDED BY LOESS DEPOSITS IN THE CHINESE LOESS PLATEAU DURING THE PAST 130000 YEARS |
|
Gao Ling①② Ding Zhongli①(①Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;②Graduate University of Chinese Academy of Sciences,Beijing 100049) |
|
SUB-DANSGAARD-OESCHGER EVENTS OF EAST ASIAN MONSOON AND THEIR GLOBAL SIGNIFICANCE |
|
Liu Dianbing① Wang Yongjin① Chen Shitao① Cheng Hai② R.L.Edwards②(①College of Geography Science,Nanjing Normal University,Nanjing 210097; ②Department of Geology and Geophysics,University of Minnesota,Minneapolis MN 55455 USA) |
|
INTENSITY AND TIMING OF D-O EVENTS OF EAST ASIAN MONSOON DURING THE LATE EPISODE OF MIS 3 |
|
Zhao Kan① Kong Xinggong① Cheng Hai② Wang Yongjin①(①College of Geography Science,Nanjing Normal University,Nanjing 210097;②Department of Geology and Geophysics,University of Minnesota,Minneapolis MN 55455 USA) |
|
CHRONOSTRATIGRAPHY AND STRATIGRAPHIC DIVISION OF RED SOIL IN SOUTHERN CHINA |
|
Yuan Baoyin① Xia Zhengkai② Li Baosheng③ Qiao Yansong④ Gu Zhaoyan①Zhang Jiafu② Xu Bing① Huang Weiwen⑤ Zeng Rongshu①(①Institute of Geology and Geophisics,Chinese Academy of Sciences,Beijing 100029;②Laboratory for Earth Surface Processes,Department of Geography,Peking University,Beijing 100871;③Geography College,South China Normal University,Guangzhou 510631;④Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081; ⑤Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of Scinces,Beijing 100044) |
|
FOSSIL FAUNA IN THE LATE STAGE OF LATE PLEISTOCENE IN THE HETAO BASIN,INNER MONGOLIA |
|
Nie Zongsheng① Li Hong② Ma Baoqi①(①The Institue of Crustal Dynamics,China Seismological Bureau,Beijing 100085;②The Museum of Inner Mongolia Autonomous Region,Hohhot 010020) |
|
ENVIRONMENTAL ISOTOPES AND GEOCHEMICAL STUDY FOR GROUNDWATER CONNECTIVITY IN THE AREA OF TAILRACE CHANNEL OF THE PUMPED STORAGE POWER PLANT,WENDENG,SHANDONG PROVINCE,CHINA |
|
Yuan Renmao①② Ma Fengshan② Qin Siqing② Deng Qinghai②(①Institute of Geology,China Earthquake Administration,Beijing 100029;②Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029) |
|
COMPARISON OF LIPID COMPOSITIONS BETWEEN PLANT LEAVES AND OVERLYING SOIL IN HESHANG CAVE,QINGJIANG,HUBEI PROVINCE AND ITS SIGNIFICANCE |
|
Cui Jingwei①② Huang Junhua①② Pu Yang①② Huang Xianyu①② Xie Shucheng①②(①State Key Laboratory of Geological Process and Mineral Resources,China University of Geosciences,Wuhan 430074;②Key Laboratory of Biogeology and Environmental Geology of Ministry of Education,China University of Geosciences,Wuhan 430074) |
|
ENVIRONMENTAL BACKGROUND OF HUMAN ACTIVITIES DURINGMIS 3 STAGE RECORDED IN THE ZHIJIDONG CAVE SITE,ZHENGZHOU |
|
Xia Zhengkai① Liu Decheng① Wang Youping② Qu Tongli②①College of Environmental Science,Peking University,Beijing 100871;②School of Archaeology and Museology,Beijing 100871) |
|
OSTRACOD ASSEMBLAGES AND THEIR PALEOENVIRONMENTAL SIGNIFICANCE FROM SHELL BAR SECTION OF PALEOLAKE QARHAN,QAIDAM BASIN |
|
Zhang Hucai① Wang Qiang② Peng Jinlan③ Chen Guangjie④(①State Key Laboratory of Lake Science and Environment,Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences,Nanjing 210008;②Tianjin Institute of Geology & Mineral Resources,Tianjin 300170; ③Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing 210008;④Department of Biology,McGill University,1205 Docteur Penfield,Montreal,Quebec H3A 1B1,Canada) |
|
POLLEN RECORD REFLECTS CLIMATE CHANGES IN EASTERN QAIDAM BASIN DURING 36～18kaB.P. |
|
Wan Hewen①③ Tang Lingyu② Zhang Hucai③ Li Chunhai③ Pang Youzhi③(①College of Life Sciences,Anhui University,Hefe 230039; ②Nanjing Institute of Geology and Paleontology,Chinese Academy of Sciences,Nanjing 210008;③State Key Laboratory of Lake Science and Environment,Institute of Geography and Limnology Sciences,Chinese Academy of Sciences,Nanjing 210008) |
|
A HIGH RESOLUTION MIS 3 ENVIRONMENTAL CHANGE RECORD DERIVED FROM LACUSTRINE DEPOSIT OF TIANSHUIHAI LAKE,QINGHAI-TIBET PLATEAU |
|
Li Shijie① Zhang Hongliang①② Shi Yafeng① Zhu Zhaoyu③(①State Key Laboratory of Lake Environment,Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences,Nanjing 210008; ②Graduate University of Chinese Academy of Sciences,Beijing 100049; ③Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640) |
|
PRELIMINARY STUDY OF PREHISTORIC HUMAN MIGRATION BASED ON Sr ISOTOPE ANALYSIS FROM JIAHU RELICS |
|
Yin Ruochun① Zhang Juzhong① Yang Xiaoyong②(①Department of Scientific History and Archaeometry,University of Science and Technology of China,Hefei 230026; ②Key Laboratory of Crust-Mantle Materials and Environments,School of Earth and Space Sciences,University of Science and Technology of China,Chinese Academy of Sciences,Hefei 230026) |
|
LAKE EVOLUTION AND GLACIATION OF THE NIANBAOYUZE MOUNTAIN IN THE TIBETAN PLATEAU SINCE THE MIDDLE OF THE LAST GLACIAL |
|
Lei Yanbin①② Zhang Hucai① Shang Huaming③Yang Lunqing①② Lei Guoliang④ Zhang Wenxiang④(①State Key Laboratory of Lake Science and Environment,Nanjing Institute of Geography and Limnology,Chinese Academic Sciences,Nanjing 210008;②Graduate School of Chinese Academic Sciences,Beijing 100049;③Institute of rümqi Desert Meteorology,Chinese Meteorological Bureau,rümqi 830002;④College of Natural Resource and Environment,Lanzhou University,Lanzhou 730000) |
|
MULTI-PURPOSE REGIONAL GEOCHEMICAL SURVEY AND SOIL CARBON RESERVES PROBLEM:EXAMPLES OF JIANGSU,HENAN,SICHUAN,JILIN PROVINCES AND INNER MONGOLIA |
|
Xi Xiaohuan① Zhang Jianxin② Liao Qilin③ Chen Deyou④ Bai Rongjie⑤ Huang Zengfang⑥(①China Geological Survey,Beijiang 100011;②Henan Geology Institute,Changsha 410007;③Jiangsu Institute of Geological Survey,Nanjing 210018;④Sichuan Institute of Geological Survey,Chengdu 610081;⑤Jilin Institute of Geological Survey,Changchun 130061;⑥Inner Mongolia Institute of Geological Survey,Hohhot 010020) |
|
DISTRIBUTIONS OF PHOSPHORUS IN EUM-ORTHIC ANTHROSOLS AND ITS PEDOGENIC IMPLICATION |
|
Pan Jihua①② Zhang Ganlin①(①State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,Chinese Academy of Sciences,Nanjing 210008;②Graduate Uniersity of Chinese Academy of Science,Beijing 100049) |
