“…The Gila River marks either the geographical limit or site of genetic divergence in lizards ( Crotaphytus nebrius , McGuire et al, ; Uma rufopunctatus , U. cowlesi , and U. sp ., Gottscho et al, ), snakes ( Lichanura trivirgata , Wood, Fisher, & Reeder, ), rodents ( Chaetopidus penicillatus , Jezkova et al, ) and scorpions (haplotype groups 5 and 6 of Hadrurus arizonensis , Graham et al, ). The Bill Williams river marks a similar pattern for snakes ( Chionactis annulatus and C. occipitalis , Wood et al, ), toads (haplogroups within Anaxyrus punctatus , Jaeger et al, ), lizards ( Sceloporus magister , S. “uniformis” , Leaché & Mulcahy, ; Uma spp, Gottscho et al, ), mammals (Nelson and Mexican groups of Ovis canadensis , Buchalski et al, ) and arachnids (haplotype group 3 of Aphonopelma mojave , Graham et al, ). Geomorphic studies show that the Colorado and Gila rivers experienced increased discharge and gravel transport during Pleistocene glacial periods of higher rainfall, and channel deposits were incised by erosion during the drier interglacial periods (Anders et al, ; Chadwick, Hall, & Phillips, ; Sharp, Ludwig, Chadwick, Amundson, & Glaser, ; Waters, ; Waters & Haynes, ).…”