We will compare multi-proxies of cave stalagmite records in different space-time scales between Southern China and Western Henan Province, which is located in the south-eastern edge of the Loess Plateau in typical Central China. Based on the previous work in cave monitoring from Chongqing and Guizhou Province, we focus on monitoring Jiguan Cave areas, those areas are sensitively influenced by monsoonal climate and near to the China geographical North and South boundaries. The proxies include the modern atmospheric precipitation, cave drip water and modern cave sediments etc, and then make sure the relationship with temperature, humidity and the monsoon index etc, in study areas, Luanchuan, Henan Province. Based on the absolute high-precision MC-ICP-MS U-series dating and high-resolution oxygen and carbon isotope data of environmental record etc,we will analyse several stalagmites from study areas, the millennium-to-annual timescales records of the Asian Monsoon will be established from the Last Glacial Maximum (LGM)on precessional cycle. We focus on the time of beginning and end, and the characteristics of typical abrupt climate events (H1 and LIA, etc.) and those internal structural changes. According to the cave monitoring, the long-to-short timescales of stalagmites and other geological records,we will make a clear to the transmittable mechanism of climatic signal and climate significance for those oxygen isotopes proxies, etc. Moreover, we will analyse changes of the Asian Monsoon climate system and possible driving mechanism from the LGM, and further validate the circulation effect of stalagmite oxygen isotopes by the Chinese monsoon, and further validate the origin and transition of Chinese civilization by the climate factors.