“…In the West Mediterranean, for example, lowering of sea levels during Pliocene and Pleistocene glacial maxima could have permitted migrations to occur across the Strait of Gibraltar (Collina-Girard, 2001;Ortiz et al, 2007), while warmer periods allowed some species to expand and others to become restricted or extinct (Taberlet et al, 1998). Most often the Strait is considered a formidable obstacle to plant expansion (e.g., Terrab et al, 2007;Cano-Maqueda et al, 2008), but there are numerous examples of species that have successfully crossed this barrier, both from the North to the South (e.g., Caujape-Castells and Jansen, 2003;Escudero et al, 2008) and from South to North (e.g., Carranza et al, 2006;Ortiz et al, 2009).…”