摘要
Recent excavation in the Wusha area, Xingyi, Guizhou Province, reveals new discoveries of the Triassic Xingyi Biota: 1) the fossiliferous strata can be subdivided into three reptile beds. The Lower Reptile Bed is composed of layers 26~35 and is 1.41 m in thickness, characterized by the abundance of Keichousaurus. The Middle Bed consists of layers 36~44 and is 2.11 m thick, containing both sauropterygians and ichthyosaurs. The Upper Reptile Bed includes the layers 45~53, and its the thickness is 1.88 m. The characteristic taxa in this bed are well-preserved ichthyosaurs, thalattosaurs and crinoids; and 2) the occurrence of sauropterygians in the Lower Bed, including Nothosaurus, Lariosaurus and Keichousaurus, shows a close affinity with the western Tethys, while the occurrence of complete Qianichthyosaurus, Guizhouichthyosaurus and thalattosaurs in the Upper Bed indicates a close relationship with the Guanling Biota.