China’s forests cover 208.3 million ha and span a wide range of climates and a large variety of forest types including tropical,temperate,and boreal forests.However the variation patterns of fine root(<2 mm in diameter biomass,production,and turnover from the south to the north are unclear.This study summarizes fine root biomass(FRB),production(FRP)and turnover rate(FRT)in Chi na’s forests as reported by 140 case studies published from 1983 to 2014.The results showed that the mean values o FRB,FRP and FRT in China’s forests were 278 gm~(-2)366 gm~(-2)a~(-1),and 1.19 a~(-1),respectively.Compared with other studies at the regional or global scales,FRB in China’s forests was lower,FRP was similar to estimates a the global scale,but FRT was much higher.FRB,FRP,and FRT in China’s forests increased with increasing mean annual precipitation(MAP),indicating that fine root vari ables were likely related to MAP,rather than mean annua temperature or latitude.This is possibly due to the smal variation in temperature but greater variation in precipitation during the growing season.These findings suggest that spatiotemporal variation in precipitation has a more profound impact on fine root dynamics in China’s forests,and this will impact carbon and nutrient cycles driven by root turnover in the future. China’s forests cover 208.3 million ha and span a wide range of climates and a large variety of forest types including tropical, temperate, and boreal forests. How the variation patterns of fine roots (<2 mm in diameter biomass, production, and turnover from the south to the north are unclear.This study summarizes fine root biomass (FRB), production (FRP) and turnover rate (FRT) in Chi na’s forests as reported by 140 case studies published from 1983 to 2014. The results showed that the mean values FRB, FRP and FRT in China’s forests were 278 gm -2 366 gm -2 a -1, and 1.19 a -1 respectively, Compared with other studies at the regional or global scales, FRB in China’s forests was lower, FRP was similar to estimates a global scale, but FRT was much higher. FRB, FRP, and FRT in China’s forests increased with increasing mean precipitation (MAP), indicating that fine root vari ables were likely related to MAP, rather than mean annua temperature or latitude. This is possibly due to the smal variation in temperature but greater variation in precipitation during temperature of the growing season. these findings suggest that spatiotemporal variation in precipitation has a more profound impact on fine root dynamics in China’s forests, and this will impact carbon and nutrient cycles driven by root turnover in the future .