Abstract: The Xingfuzhilu Formation is widely distributed in the southern part of the Greater Khingan Mountains. This formation may be divided into three lithologic members. The lower member, 173—342m thick, is represented by mottled conglomerate, which overlies disconformably the Upper Permian Linxi Formation; the middle member, 520 m thick, consists of purplish red graywacke and siltstone; the upper member, over 260m thick, is marked by fine clastic rocks, which is unconformably overlain by the Upper Jurassic. The upper member contains abundant animal and plant fossils. Of these the bivalves comprise the common elements of the Palaenodonta-Palaeomutela assemblage. In the past, it was considered that they only occurred in the Late Permian, but in recent years they have been found in the CIS to range into the Early Triassic. Cornia and Diaplaxa of conchostracans are Early Triassic and Triassic common elements respectively. The genera such as Neoclamites, Eguisetites, Cladophlebis and Pozozamites in the fossil flora are all Early Mesozoic common elements; while their accompanying genera such as Pecopteris, Noeggerthiosis and Paracalamites were considered previously to be restricted in the Late Paleozoic, but they are now found in Lower Triassic strata of the CIS. To sum up, the biotas in the formation show the distinctive features of mixture of Late Permian-Early Triassic elements. But from the correlation of regional stiatigraphic sequences, there are notable differences between this formation and the Late Permian strata in respect to lithology and structural deformation.It seems to be appropriate to assign its age to Early Triassic.