【英文摘要】In the field of globe change, the formation and evolution of Asia monsoon is animportant scientific forward problem to which has been paid extensive attention andstill not resolved ultimately.In recent years, Chinese scientists have made notableprogress on Asia palaeo- monsoon by studing Ocean cores and lakes, loess, ice core, andso on, and has in the front ranks of the World. Because of lacking researches oncorrsponding sediments in the southwest of China, making use of cave stalagmites tostudy the reglarity of climatic evolution from 500ka BP to 150ka BP in the Southwest ofChina is of great improtance in understanding global change and forecasting climatechange in the future. By high precision ICP-MS-U/Th or TIMS-U series dating, highresolution records of the oxygen and carbon isotopes and trace elements from cavestalagmites, the project will study the regularity of climatic change in the tenmillennial, millennial and centennial timescale from 500ka BP to 150ka BP in southwestof China, catch climatic abrupt events, and study their phase, cyclicity, amplitude,behave characters, and so on.These events will be compared with the previous records ofglobal abrupt events and reveal the history of monsoon evolution and difference on Asiamonsoon. The target of the project is to establish a standard time-scale series ofclimatic change from 500ka BP to 150ka BP in southwest of China and discuss theirresponse to the global changes and its mechanisms, and provide scientific basis for theglobal change reference and forecasting climate change in the future.