“…During the Pleistocene when sea levels were up to 200 m lower, the Great Bahama Bank, made up of present-day Bimini, Andros, New Providence, Eleuthera, the Exumas, Long and Cat Island, was within 15 km of Cuba at its closest point, which likely resulted in the natural movement of many species between these two landmasses (Holzapfel & Harrell 1968, Pregill & Olson 1981, Carew & Mylroie 1997. Cycles of rising sea levels would have resulted in range fragmentation for many species as landmasses became smaller and more separated from one another by ocean, with some populations going extinct while others experienced divergence (Gillespie & Roderick 2002, Glor et al 2005, Oneal et al 2010. In addition to vicariance, dispersal, whether from over-water means or rafting, has also been important in moving organisms around the Caribbean, and thus promoting divergence of populations between islands (Holzapfel & Harrell 1968, Censky et al 1998, Glor et al 2005, Scharer & Epler 2007.…”