“…Cooling of the climate and tectonic movements during the early Oligocene led to the fragmentation of the boreotropical belt, and the migration of paratropical elements southward to tropical refuges, such as southwest China, Southeast Asia, Central America, and Mexico (Morley, 2003;Zachos et al, 2001). Whereas a boreotropical migration pattern has been identified in many angiosperm groups (e.g., Fabaceae: Lavin et al, 2001; Malpighiaceae: Davis et al, 2002;Sapotaceae: Smedmark and Anderberg, 2007; Rubiaceae: Antonelli et al, 2009;Annonaceae: Erkens et al, 2009), only a few fern studies invoked boreotropical connections as an explanation for intercontinental disjunctions (e.g., Nephrolepis Schott, Hennequin et al, 2010; Asplenium L., Schneider et al, 2004a; Diplazium Sw., Wei et al, 2015). Therefore, the boreotropical hypothesis should be carefully tested when reconstructing biogeographical scenario in ferns.…”