Biological soil crusts (BSCs) are special complexes composed of lower plant, microorganism (bacteria, fungi) and surface soil fine particles bonded by their exuding mucilaginous material, which are widespread in the semi-arid regions all over the world. In many literatures, BSCs are known as ecosystem restoration engineer, it not only makes great contribution to nutrient fixation (Carbon, nitrogen and phosphorus) and soil enzyme activity, but also plays vital roles in seed germination and seedling survival by regulating hydrological process of soil surface (precipitation infiltration, surface runoff, evaporation and other processes), which include autotrophic and heterotrophic organisms. The autotrophic organisms mainly consist of algae, lichen and moss, and heterotrophic organisms are composed of bacteria, microscopic fungi, etc. The classification of BSCs can be divided into three categories: algae, lichen and moss crust based on the dominant species and succession direction of BSCs. The formation, development and structure of BSCs are affected by human activities and climate disturbances, but little attention have devoted to the monitoring and management of BSCs. In this study, the simple ratio index (SRI) and normalized difference vegetation index (NDVI) were summarized to monitor the morphology of BSCs. Furthermore, the effect of BSCs succession and its ecological function on arid and semi-arid ecosystems under different utilization ways and intensity were also discussed, which laid a foundation for a further understanding of the surface process of arid and semi-arid areas and promoting the restoration of degraded ecosystem.