“…Regional patterns of plant diversity in MTCs may be explained both by phylogenetic analysis, in relation to historic environmental change, and by ecological analysis, in relation to environmental factors influencing contemporary species coexistence (Linder, 1991). Explosive Quaternary species radiations occurred in all MTCs, in response to drought, fire, and other stressors associated with aridification, while low extinction rates or radiations of older lineages were associated with refugia from these climatic extremes or refugia from cooling and glaciation during ice ages (Ackerly, 2009; Cowling & Lombard, 2002; Keeley & Swift, 1995; Kraft, Baldwin, & Ackerly, 2010; Raven & Axelrod, 1978; Rundel et al., 2016; Stebbins & Major, 1965). Contemporary patterns of plant diversity in MTCs have been shown to be positively correlated with environmental heterogeneity in soils, topography, precipitation, and temperature (Casazza, Zappa, Mariotti, Médail, & Minuto, 2008; Harrison, Viers, & Quinn, 2008; Linder, 1991; Richerson & Lum, 1980).…”