“…Diversification of neotomines in general and Peromyscus in particular occurred during the late Miocene and the Pliocene [30]. At present, and based on recent revisions using molecular and morphometric analysis, the P. mexicanus species group is considered a monophyletic group of Pleistocene origin [31], which currently includes 12 mountain species, P. nudipes, P. tropicalis, P. mexicanus, P. gymnotis, P. zarhynchus, P. gardneri, P. salvadorensis, P. nicaraguae, P. guatemalensis, P. grandis, P. carolpattonae, and P. bakeri [17,20,[32][33][34][35], distributed at lowlands and highlands across Guatemala-Chiapas and Central America mountains.…”