TABLE 4 in Woznikella triradiata n. gen., n. sp. - a new kannemeyeriiform dicynodont from the Late Triassic of northern Pangea and the global distribution of Triassic dicynodonts

TABLE 4. — Notable post-Permian tracks historically misidentified as belonging to ichnotaxa considered to potentially be produced by Dicynodontia. Original descriptionCountryCommentsDicynodontipus protherioides Silva, Carvalho, Fernandes, & Fergiolo, 2008 MCN-PIC.007/17-23, MCN-PIC.016/1-21, MCN-PIC.017/1-18, MCN-PIC.018/2-16Brazil (Silva et al. 2008)Tracks subsequently reinterpreted as Procolophonichnium ispp. by Klein et al. (2015) and indeterminate tetrapods footprints by Klein & Lucas (2021)“ Dicynodontipus isp.” LAR-Ic 1 and unnumbered specimens (Melchor & de Valais 2006; Melchor et al. 2006)Argentina (Melchor & de Valais 2006; Melchor et al. 2006)Melchor et al. (2006) and Melchor & de Valais (2006) noted the presence of Dicynodontipus isp. in the Santo Domingo Formation, which at the time they considered Late Triassic; however, this track-yielding surface of the Santo Domingo Formation was subsequently dated to Late Eocene (Melchor et al. 2013); thus, the tracks may rather belong to mammals (Klein & Lucas 2021)“cf. Gallegosichnus sp. ”/“cf. Dicynodontipus isp.” slab from Locality 2 (Demathieu & Wycisk 1990)Egypt (Demathieu & Wycisk 1990)Small tracks from the Turonian (Late Cretaceous) Abu Agag Formation described by Demathieu & Wycisk (1990) as cf. Gallegosichnus sp. – an ichnospecies subsequently synonymized with the ichnospecies Dicynodontopus by Melchor & de Valais (2006); possibly mammal tracks?