“…Tetrapod tracks' above), such as Hyloidichnus, Dromopus, Pachypes and Dimetropus (although some are missing in certain sections) and correspond to fluvial palaeoenvironments and playa lake deposits (Gand & Durand, 2006;Mujal et al, 2016;López-Gómez et al, 2019b). Those units show a trend towards semi-arid conditions in the late Cisuralian and Guadalupian, as demonstrated by the study of palaeosols and geochemical proxies (Michel et al, 2015;compare Mujal et al, 2017a, andMujal et al, 2018;López-Gómez et al, 2021). In fact, by the middle Permian, most basins of central Pangaea have evidence of arid climates (Schneider et al, 2006;Tabor & Poulsen, 2008;De la Horra et al, 2012;Michel et al, 2015).…”