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《Earth Science Frontiers》 2003-02
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THE GEOLOGICAL TIME SCALE AND CLIMATIC EVENTS FROM STALAGMITES IN THE LATE OR RECENT QUATERNARY PERIOD IN THE LIBO AREA, GUIZHOU, SOUTHWEST CHINA

LIN Yu shi 1, ZHANG Mei liang 1, CHENG Hai 2, YUAN Dao xian 1, QIN Jia ming 1, WANG Zhao rong 3, RAN Jing cheng 4 (1.Karst Dynamics Laboratory, Institute of Karst Geology, CAGS, Guilin 541004, China; 2.Department Geology and Geophysics, Minnesota University, MN 55455,USA; 3.University of Science and Technology of China, Hefei 230023, China; 4.The Management of Maolan National Nature Reserve in Guizhou, Libo 558400, China)  
The chrono stratigraphy study of the large stalagmites in the karst area in south China shows that stalagmites are one of the main study object in the Quaternary period. The high precision estimation of the age of stalagmite is more possible than that of the other sediments in the Quaternary period. From the normal order of the parallel dating age with 68 TIMS U series samples in the Libo area of South Guizhou the geological time scale has been established since the late or recent Quaternary or since 162.3 ka B P, the boundary age of 128.5ka B P between Holocene and the late Pleistocene has been confirmed; the jump time of a series cold events which ranges from 350 year B P to 2 300 year B P, the younger Dryas and the similar Heinrich, and so on have been put forward; the trans chron of the cold and warm climate is of the region correlation significance . It has been firmly believed that the geological time scale should be established by using the data of the system dating ages of large stalagmites rather than a calculation from two or three sediment rates by using a few dating age value and the "system" dating ages of the small stalagmites in order to avoid missing some important information such as depositional break, and the natural lack bed.
【Fund】: IGCP44 8国际对比研究项目 ;; 国家自然科学基金项目( 4 0 15 2 0 0 2 )
【CateGory Index】: P642.25
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