“…The continental rifting of the Peninsula away from mainland Mexico and the volcanic upwelling of Guadalupe Island are the most ancient (>5 million years ago, MYA) and resulted in ecological speciation, island endemism and disjunctions in mainland‐peninsular and peninsular‐island sister species distributions (Aleixandre, Hernandez Montoya, & Mila, ; Grismer, ; León De La Luz, Rebman, & Oberbauer, ; Riddle et al., ; Rosas‐Escobar, Gernandt, Pinero, & Garcillan, ). More recently (1–3 MYA) and more locally, complex physical interactions between the land and the sea, such as the inundation of the Isthmus of La Paz and the formation of the temporal mid‐peninsular seaway, resulted in a north‐south genetic discontinuity within the peninsula and the generation of regions of high local endemism (Dolby et al., ; León‐De la Luz & Breceda, ; McCauley, Cortés‐Palomec, & Oyama, ; Riddle et al., ). This complex interplay was followed by progressive aridification of the Baja Peninsula and adjacent areas after the Last Glacial Maximum (LGM) (Hafner & Riddle, ; Lindell et al., ; Riddle et al., ).…”