“…The Dicynodon clade is supported by two characters (continuous character 14, shape of mandibular fenestra, and discrete state character 51, postorbital contribution to intertemporal bar relatively flat) and the Daptocephalus clade is supported by four characters (continuous characters 8, median pterygoid plate width, and 11, relative area of internal nares, and discrete state characters 92, ventral surface of median pterygoid plate smooth and flat, and 111, absence of central circular depression on occipital condyle) (refer to Supplementary Information for lists of all character states). Manuscript to be reviewed The discovery that multiple taxa of large dicynodontoids are present in the Usili Formation should not be surprising-this clade is common in the late Permian, and sympatric dicynodontoid taxa are known within more poorly-sampled, probably coeval Laurasian basins (Li et al, 2008;Kurkin, 2012;Olivier et al, 2019) in addition to the heavily sampled Karoo Basin of South Africa (Kammerer et al, 2011). What is notable about the Usili species, however, is their close similarity to (and recovery as sister-taxa of) particular Karoo species (Dicynodon lacerticeps and Daptocephalus leoniceps), to the extent that they are here considered congeneric.…”