In this study, based on the analyses of the sedimentary and susceptibility data of the sediments of the Liupanshan Group exposed in the Liupanshan area (central China), the authors obtained the climate records during 128.15~115.82 Ma from the terrigenous sediments. The susceptibility values are lower totally and can be classified into two segments, i. e. the lower values prior to 125 Ma and the higher values after 125 Ma. The analysis of the sedimentary environment, of the contents of magnetic minerals and the TFe in the rocks, and of their relationship with the susceptibility enhancement suggested that the susceptibility values are predominantly determined by the kinds and the contents of the magnetic minerals from the source region, which indicated that the susceptibility values can be used to interpret the climate change in this time window. The climate during 128.15~115.82 Ma was significantly arid and hot.