The foliar stable carbon isotope compositions (δ 13 C) of nine dominant species in seven sites, Yangling, Yongshou, Tongchuan, Fuxian, Ansai, Mizhi, and Shenmu, standing from the south to the north in the Loess Plateau of China were studied. The results showed that foliar δ 13 C values ranged from -22.61 to -30.73 ‰ with an average of -27.23 ‰ in 141 C 3 plant samples collected from the Loess Plateau. Foliar δ 13 C values varied significantly (p<0.001) among the nine C 3 species, which were Pinus tabulaeformis Carr., Robinia pseudoacacia L., Zizyphus jujuba Mill. var. spinosus Hu., Rubus parvifolius L., Hippophae rhamnoides L., Caragana korshinskii Kom., Lespedeza davurica (Laxm.) Schindl., Artemisia sacrorum Ledeb. var. incana Mattf., and Agropyron cristatum Gaertn. Comparatively, R. pseudoacacia, H. rhamnoides, and C. korshinskii had much higher δ 13 C values than the other six species, while A. sacrorum had the lowest δ 13 C value. There was no significant difference in foliar δ 13 C value among five species, P. tabulaeformis, Z. jujuba, R. parvifolius, L. davurica, and A. cristatum. Considering the life forms categorized from nine C 3 species, trees and shrubs had significantly higher δ 13 C values than herbs (p<0.001). The deciduous tree R. pseudoacacia had much higher δ 13 C value than the evergreen tree P. tabulaeformis (p<0.01). Among the four shrubs, foliar δ 13 C values in H. rhamnoides and C. korshinskii were markedly higher (p<0.01) than those in Z. jujuba and R. parvifolius. Among the three herbs, L. davurica and A. cristatum had significantly higher δ 13 C values than A. sacrorum (p<0.01). Leguminous species such as R. pseudoacacia, C. korshinskii, and L. davurica as well as a non-leguminous species with nitrogen-fixation capacity, H. rhamnoides, had higher δ 13 C values than other non-leguminous species with same life-form. The mean δ 13 C value increased by about 7 % from Yangling in the south to Shenmu in the north as climatic drought increased, and foliar δ 13 C values differed much (p<0.001) among the seven sites. For nine species in the Loess Plateau, foliar δ 13 C values were significantly and negatively (p<0.001) correlated with the mean annual precipitation, moreover, an increase of 100 mm in annual precipitation would result in a decrease of 1.2 ‰ in δ 13 C value.