A largescale 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 dotreefs in parallel modeThe 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 reefbuilding process  There is a consistent and corresponding relation that controlled the growth of distribution of the reefs between the evolution of communities and the reefbuilding 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 CarboniferousThe discovery of Bianping reefs increases biological types of Carboniferous communities in the worldItoffers a new example for evolution of reefbuilding biocoenose and reef growth as well its dynamic model