This paper reports a Lower Triassic inorganic carbon isotope profile from the North Ping-dingshan Section in Chaohu, Anhui Province, China, which was situated in a deep part of the LowerYangtze carbonate ramp. The δ(13C) excursion shows two periods from the Permian-Triassic boundaryto the lower Spathian substage, corresponding to the ecosystem undergoing evolution and recovery afterthe end-Permian mass extinction and related events. The first period starts at the δ (13 C) depletioncaused by the mass extinction and evolves with a gradual δ(13C) increase resulting from the developmentof some disaster taxa during the Induan. The strong Smithian δ(13 C) depletion in the second periodmight be formed by the collapse of the disaster ecosystem and the biotic recovery occurred with the explo-sive increase of bioproductivity in the Spathian. Thus the δ(13C) excursion in the Lower Triassic expres-ses patterns of biotic evolution and recovery during the erratic ecosystem that followed the great end-Permian mass extinction.