Coalescent methods provide opportunities to track historical fluctuations in effective population sizes (N e) from individual whole-genome sequences (Li & Durbin, 2011). Such inferences have the potential to contribute insights into species' demographic responses to past biotic pressures, such as predation and disease, and abiotic factors, particularly climatic change. Variation in species' responses to past environments will depend not only on complex interactions among biotic and abiotic processes, but also on species-specific traits such as dispersal propensity and physiological plasticity. Nevertheless, comparative studies of spatial and temporal genetic patterns have shown that co-occurring species often have congruent responses to past ecological and climatic events (e.g., Bowen et al., 2014; Moritz et al., 2009). Broader differences in population histories have been hypothesised for taxa that occupy different biomes (e.g., Antonelli