“…Signatures of fragmentation in Pleistocene forest refugia were then investigated at the intraspecific genetic scale (Hardy et al., ). Using microsatellite and plastid markers, recurrent spatial genetic discontinuities were detected in several tree species, especially among Upper Guinea in West Africa, Lower Guinea in western Central Africa and Congolia in Eastern Central Africa (White, ), but also within these domains (North‐South and/or East‐West subdivisions in Lower Guinea) (Blatrix et al., ; Dauby et al., ; Demenou, Doucet, & Hardy, ; Demenou, Piñeiro, & Hardy, ; Hardy et al., ; Heuertz, Duminil, Dauby, Savolainen, & Hardy, ; Piñeiro, Dauby, Kaymak, & Hardy, ). These patterns provided support for the role of refugia during Pleistocene climate oscillations, as suggested for the Cameroon volcanic line (CVL, Figure b) hosting endemic species and genetic lineages (Dauby et al., ; Maley, ).…”