“…Therefore, the Induan is now equivalent to the late Griesbachian and Dienerian, while the early Griesbachian is roughly of Permian age (Baud 2001;Baud and Beauchamp 2001). The base of the Dienerian substage is marked by the appearance of abundant meekoceratids, gyronitids and proptychitids, a globally recognizable event (e.g., Tozer 1974;Shevyrev 2001;Brühwiler et al 2008;Ware et al 2011b). …”