The Kungurian Stage is one of the three remaining stages of the Permian that is not yet defined at the base by a Global Stratotype Section and Point(GSSP).The candidate section at the Yuryuzan’River in the Urals yields few conodonts,and contains non-marine sediments near the boundary.The search for a suitable,continuous marine succession is a principal task for the Subcommission on Permian Stratigraphy.The Leonardian,with its type area in the southwest United States,and in objective stratigraphic succession directly beneath the basal Guadalupian Roadian Stage, has priority to serve as a subseries of the Lower Permian.However,distinct provincialism limits the correlation of Leonardian fossil zones with the fusuline-based Tethyan timescale.Conodonts can be correlated in many important regions on opposite sides of Pangea,yet contradictions arise when relating conodont zones with fusuline and ammonoid zones.The different taxonomic philosophies are highly suspected for the cause of the conflicts,but also there are different conodonts from the type Roadian in West Texas.Given that the Pamir and Darvaz in central Asia are difficult to access,further investigations should focus on South China,where abundant fusulines and ammonoids facilitate correlation throughout the Tethyan region,and where conodonts permit correlation with North America. The Kungurian Stage is one of the three remaining stages of the Permian that is not yet defined on the base by a Global Stratotype Section and Point (GSSP). The candidate section at the Yuryuzan ’River in the Urals yields few conodonts, and contains non -marine sediments near the boundary. The search for a suitable, continuous marine succession is a principal task for the Subcommission on Permian Stratigraphy. Leonardian, with its type area in the southwest United States, and in objective stratigraphic succession directly beneath the basal Guadalupian Roadian Stage, has priority to serve as a subseries of the Lower Permian. Yet, distinct provincialism limits the correlation of Leonardian fossil zones with the fusuline-based Tethyan timescale .Conodonts can be correlated in many important regions on the opposite sides of Pangea, yet contradictions arise when relating conodont zones with fusuline and ammonoid zones. the different taxonomic philosophies are highly suspected for the cause of the conf licts, but also there are different conodonts from the type Roadian in West Texas. Given that the Pamir and Darvaz in central Asia are difficult to access, further investigations should focus on South China, where abundant fusulines and ammoniations facilitate correlation throughout the Tethyan region, and where conodonts permit correlation with North America.