“…some taxa show nearly reciprocal monophyly in mtDNA over relatively short distances, probably as a consequence of isolation during the Pleistocene (e.g., barber et al 2000,2002). For many taxa, interestingly, the locations of likely vicariance due to Pleistocene sea level change are also associated with regions of persistent population genetic structure, most notably the sunda shelf (McMillan et al 1999, Deboer et al 2008, Ackiss et al 2013, torres strait (Mirams et al 2011), and Halmahera Eddy (barber et al 2006, 2011), although there is also evidence that this structure is being eroded by contemporary dispersal in some species , Liu et al 2012, Deboer et al 2014. Finally, nearly all loci and taxa that have been examined to date show signatures of Pleistocene-era population expansions onto newly submerged continental shelf habitats (e.g., chenoweth et al 1998, Lind et al 2007, crandall et al 2008a,b, 2012a, Gaither et al 2010.…”