“…The effective absence of distinct ungual impressions in the pes tracks of the AODF 904.S1 trackway distinguishes it from many sauropod tracks, such as Occitanopodus gandi (Moreau et al, 2020), Polyonyx gomesi (Santos, Moratalla & Royo-Torres, 2009), unnamed sauropod tracks from Niger (Ginsburg et al, 1966), unnamed sauropod tracks from Spain (Pascual Arribas et al, 2008;Pascual-Arribas & Hernández-Medrano, 2010), Brontopodus birdi (Farlow, Pittman & Hawthorne, 1989), Brontopodus pentadactylus (Kim & Lockley, 2012), and unnamed titanosaur tracks from the Anacleto Formation of Mendoza, Argentina (González Riga et al, 2015). Although the near absence of distinct digit impressions in the track walls is noteworthy, it is unclear whether or not this is a consequence of poor preservation, reduced pedal digits in the trackmaker, distortion caused by the movement of the pedal unguals during the step cycle, or a combination of some or all of these factors.…”