“…In these regions, the historical fragmentation and contraction of habitats and subsequent dispersal mediated by rugged relief and climate fluctuations are thought to be key factors underlying the dynamics of diversification (Mayr and Diamond, 1976;Patton and Smith, 1992;Graham et al, 2014;Antonelli, 2015;Rangel et al, 2018). While empirical evidence addressing the interplay between climate and topography has been available for some time and has provided invaluable insights into the diversification of tropical montane organisms ( Van der Hammen, 1961;Hooghiemstra and Van der Hammen, 2004;Chesser, 2000;Pérez-Emán, 2005;Bonaccorso, 2009;Weir, 2009;Gutiérrez-Pinto et al, 2012;Ramírez-Barahona and Eguiarte, 2013;Valderrama et al, 2014;Winger and Bates, 2015;Manthey et al 2017, Cadena et al, 2019, Muellner-Riehl 2019, Rahbek et al, 2019, our ability to understand these range shifts in the recent and more distant past and the genomic footprint left by them is still limited. This is because these processes have rarely been empirically investigated in a detailed explicit spatiotemporal framework.…”