The state and transition models is applied to discuss the threshold in vegetation composition from steppe to thicketization-steppe,Xilin River Basin,Inner Mongolia.From the increase of soil patchiness scale in the thicketization of steppe,it is suggested that the transition from steppe to thicketization-steppe dominated by Caragana microphylla patches could be irreversible once this threshold is passed.The thicketization of steppe is an important stage of grazing succession,which may be considered as a self-rehabilitation of a degraded ecosystem.The model on the steppe grazing succession is developed, and it is the important framework for the research into the thicketization of steppe in Xilin River Basin,Inner Mongolia.