“…There is widespread support for a general model of alpine population history in temperate regions (Schoville & Roderick, ), from both genetic and palaeontological data (DeChaine & Martin, ; Frenzel, ; Knowles & Carstens, ; Birks, ; Galbreath et al ., ), wherein cold‐specialized species track favourable climate conditions downslope during glacial episodes and upslope during warmer interglacial periods. Across a wide variety of taxa and in alpine habitats globally, past climate change has led to rapid lineage diversification and the formation of new species (Knowles, ; Comes & Kadereit, ; Buckley & Simon, ; Schoville & Roderick, ; DeChaine et al ., ; Hedin et al ., ), exemplifying the so‐called ‘Pleistocene species pump’ (Terborgh, ; Schoville et al ., ). Speciation is not the only outcome, however, as highly dispersive species experience secondary contact during climate fluctuations, leading to admixture of divergent genomes that formed during periods of isolation (e.g.…”