“…The Sierra Madre Occidental (SMOc) in Western Mexico is a mainly volcanic province of Tertiary origin that extends from the Southwestern United States to Central Mexico through 1,200 km of length and 200 km of width (Ferrari, Pasquare, Venegas‐Salgado, & Romero‐Ríos, ; López‐González, Correa‐Ramírez, & García, ). This volcanic system has acted both as a barrier that promoted diversification of many taxa as well as an important corridor for dispersal and expansion during Pleistocene glaciations (Bryson, Murphy, Lathrop, & Lazcano, ; Rodríguez‐Banderas, Vargas‐Mendoza, Buonamici, & Vendramin, ; Ruiz, Rinehart, Hayes, & Zuñiga, ; Schönhuth et al., ; Schönhuth et al, ). It has been hypothesized that Pleistocene climatic changes could lead to contraction and expansion of pine‐oak forests in the SMOc (McDonald, ; Spellman & Klicka, ).…”