An intensive erosion event in the last glaciation in the west of China;

The Discovery of Sand Wedges of the Last Glaciation in the Hexi Corridor and Its Paleoclimatic Significance;

By means of the field investigation and experimental analysis in the laboratory, especially based on the absolute ages, the authors confirm the glacier evolution series of the last glaciation in Gongwangshan Mountain.

Paleo-environment of southern South China Sea since last Glacial:Evidence from planktonic foraminifera of core YSJD-86GC;

Study on the High-resolution Sequence of Vegetation Change During the Last Glacial Recorded in the Loess of Xishan Moutain of Beijing Area;

And it also suggested that the climate in the East Asian Monsoon region had rapid fluctuations in millennium to century scales in the whole last glacial.

Study on the climatic changes between the last interglacial age and the last glacial age recorded by ostracoda in eastern Qaidam Basin;

At least in the beginning of the last glacial age, the faices belts of dune sand, sandy clay and loess differentiated by the wind and aligned from north to south had already existed in the Taklimakan Desert and areas to its south.

Mineral characteristics and their environmental implication during the last ice age in Core Q43 on the outer shelf of the East China Sea;

Tracing the Changjiang River s flowing route entering the sea during the last ice age maximum;

The 14 C dating of eolian sands in sand wedges proves they formed during the Last Ice Age,with the mean annual air temperature about -5 6℃.