“…Historical environmental change across tropical East Africa has been frequent since the Miocene, and the current CFEA are considered to be the remnants of a once continuous forest that has expanded and contracted for the past 40 million years (Axelrod & Raven, ; Demenocal, ; Maslin et al., ; Mumbi, Marchant, Hooghiemstra, & Wooller, ). Combined knowledge of endemism patterns and environmental change have led to the assumption that current CFEA biodiversity mainly originated from the isolation and persistence of ancient lineages in forest refugia, with local extinctions and in some cases adaptation to non‐forest habitats across the rest of the region (Azeria, Sanmartín, Ås, Carlson, & Burgess, ; Barratt et al., 2017a; Burgess et al., ). The coastal forests have thus been described as a “vanishing refuge” (Burgess et al., ), although to date forest refugial processes have not been thoroughly tested against alternative modes of diversification (Damasceno, Strangas, Carnaval, Rodrigues, & Moritz, ; Kirschel et al., ; Schneider et al., ; Zhen et al., ).…”