A largescale of assemblage reefs is foundin Bianping Village located about 4 km to the west of Houchang Town of Ziyun County in Guizhou Province The reefs lie in the Triticites zone of Maping Formation and formed in the late stage of Late Carboniferous The reefs were divided into 6 communities from lower to upper portions Two of them are reef building communities One is Ivanovia cf manchurica,Eugonophyllum ,cyanophyceae community and another is Formit chevella community The former grew individually in various environments and formed dotreefs in parallel modeThe latter formed upper major reef by large phacelloid Formitchevella These communities represent different developing stages of the reefs and reveal biologicsuccession features of the reefs in the reefbuilding process There is a consistent and corresponding relation that controlled the growth of distribution of the reefs between the evolution of communities and the reefbuilding process Their model of growth,development and structure characterized by Formitchevella communities are very different from other reefs of Late Carboniferous in China and the world They compose rare non algae reef builder of the Late CarboniferousThe discovery of Bianping reefs increases biological types of Carboniferous communities in the worldItoffers a new example for evolution of reefbuilding biocoenose and reef growth as well its dynamic model