【英文摘要】Siberia loess is mostly distributed in the mid and north part of Eurasian loess zone, which is the transition and conjunction zone of the Eastern European loess, central Asian loess and Chinese loess. Because of the special location, It is significant difference with other loess area at the formation of loess, the development of palaeosols, the mechanism of paleocliamte and paleoenvironment and so on. Using high-resolution indicators of magnetic susceptibility, CaCO3, grain size, Carbon and oxygen isotopic and age model, we study three loess sections in Siberia, four loess sections in xinjiang province, three lake drill in the arid land and one loess section in the edge of the asian monsoon area. We preliminarily discuss the relationship of different indicators in different area, in different types of deposition. Furthermore, we discuss the process of paleoenvironment in different area. The mechanism of climatic record in Siberia is very similarity to that in the westerly area of Xinjiang. Magnetic susceptibility is not the optimum indicator for recording climate change, especially in millennial time scales. The mechanism of magnetic susceptibility is very complicated, and the grain size is an effect indictor of the climate change at this area. We primarily construct climate and environment change in different area and different depositional record, and analyze the controlling factors. For understanding current physical process,we also study the relationship between global warming and the variations of glaciers in westerly area and the edge of Asian monsoon area. Generally, the glaciers are retreated in the last 40 years. The rate of glacier retreat is varied in different mountain ranges, for example the rate of the glacier retreat in the eastern part is faster than that in the western part of Qilian Mountains.