Abstract: Fossils of the coral Cyathocarinia tuberculata Soshkina have been recently collected from lime-stone sandwicked in volcanic rocks north of Ewirgol in the North Tianshan,Xinjiang.The volcanic rocks were formerly ascribed to the Upper Carboniferous Qiergusitao Formation.These fossils are of Early Permi-an age,which indicates that a part of the Qiergusitao Formation should be Early Permian in age.More-over,fossils of the other coral Grootia ivanovi Dubrolyubova have been collected from limestone gravels in pyroclastic rocks assigned formerly to the Upper Carboniferous Qiergusitao Formation along the Toutun River in the North Tianshan,Xinjiang.The age of the fossils is Late Carboniferous ,equivalent to the Dalan Stage(i.e.Moscovian Stage)and the age of the strata containing the fossil should be later than the Late Carboniferous Dalan Stage.According to the regional correlation,it may be inferred that a part of the strata mentioned above is also of Early Permian age.The discovery of the above-mentioned Early Per-mian coral fossils in the vicinity of Ewirgol indicates that the upper part of the Qiergusitao Formation is assigned to the Lower Permian in the North Tianshan,Xinjiang,and the Carboniferous strong extension event may have continued to the Early Permian.This discovery has important significance for the recon-struction of the Late Paleozoic tectonic framework and further study of the tectonic evolution and back-ground of minerogenesis in the North Tianshan,Xinjiang.