“…Most of these analyzed the uplift of the Colorado Plateau‐Sierra Madre Occidental mountain range dividing the Sonoran and Chihuahuan deserts (Gámez et al, ; Jaeger et al, ; Leaché & Mulcahy, ; Rebernig et al, ; Riddle, ; Riddle & Hafner, ) , and focused either on widely distributed species (e.g., Rebernig et al, ) or several species (e.g., Leaché & Mulcahy, ; Riddle & Hafner, ). However, other physiographic and hydrographic events occurred in the CD during the Neogene and may have favored the diversification of the biota but little is known about these events (e.g., Bryson, Jaeger, Lemos‐Espinal, & Lazcano, ; García‐Vázquez, Nieto‐Montes de Oca, Bryson, Schmidt‐Ballardo, & Pavón‐Vázquez, ; Myers et al, ). The late Neogene (i.e., Pliocene) in the CD was marked by the formation of lakes established at the bottoms of the major bolsons (Axtell, ; Morafka, ).…”