“…It is acknowledged that the present‐day Macaronesia is only the residual of a larger complex that now is submerged for a major part (Fernández‐Palacios et al, ). The emerged seamounts since the beginning of the Palaeogene (60 Myr) until the Pleistocene, now eroded and submerged, could have played two different roles: first as stepping stones, allowing the dispersion between the different archipelagos of the Macaronesia and the mainland (Chevolot, Hoarau, Rijnsdorp, Stam, & Olsen, ; Fernández‐Palacios et al, ; Van Den Broeck, Breugelmans, De Wolf, & Backeljau, ); second, allowing the allopatric differentiation and later a secondary contact between the diverged lineages (Jowers et al, ). Moreover, the possible role of Macaronesia region as refugium during Pleistocene glaciations was documented before for groups of marine invertebrates such as limpets and sponges (Sá‐Pinto, Branco, Sayanda, & Alexandrino, ; Xavier, Soest, Breeuwer, Martins, & Menken, ).…”