Results/Conclusions: The results showed that the maximum plant species richness occurs in the south of Yunnan province, while the minimum plant species richness is found on Qinghai-Tibetan Plateau. Plant species richness is significantly correlated with almost all factors examined. The annual mean precipitation is the most significant factor, and other significant factors are monthly mean temperature of January, minimum temperature, sunshine ratio, annual mean temperature, annual mean relative humidity, latitude, annual potential evapotranspiration, frost-free period etc. The pattern of species richness of seed plant in mainland of China is a result of a comprehensive effect of multi-factors, among which the annual precipitation is the most important. This differs from the energy-hypothesis that species richness is most strongly correlated with annual evapotranspiration. Energy-hypothesis is applicable to the interpretations of biogeographical patterns of richness for trees and vascular plants in North America, and is applicable to that of trees in Great Britain and Ireland. China is much more continental compared with North America and British Isles. Therefore, it is easy to understand that water-conditions in habitats are more significant for plant growth in China, especially in the west of China. The family and genus richness of seed plants have the similar patterns to that of species richness in China.