“…The above ideas are confirmed by the association of the Andean and Serra do Mar orogenies -marked by newly formed montane habitats, numerous natural barriers to gene flow, and highly dynamic climates and landscapes during the Plio-Pleistocene (Gentry, 1982;Berry, 1989;Vasconcelos et al, 1992;van der Hammen, 1995;Gregory-Wodzicki, 2000;Grazziotin et al, 2006;Garzione et al, 2008;Antonelli and Sanmartin, 2011) -with several highly diverse plant groups that are widely distributed within each region (e.g., Calceolaria, Centropogon-Burmeistera, Epidendrum, Espeletia, Fuchsia, Lepanthes, and Pleurothallis in the Andes; and Asteraceae [Lychnophora], Bromeliaceae-Bromelioideae, Eriocaulaceae [Leiothrix, Paepalanthus], Gentianaceae, Lentibulariaceae, Myrtaceae, and Velloziaceae in the Serra do Mar) (Gentry, 1982;Peixoto and Gentry, 1990;Luteyn, 2002;Young et al, 2002;Knox et al, 2008;Alves and Kolbek, 2009 [Scherson et al, 2008]). Many of these and other plant and animal clades from the Andes have origins around or after the uplift of the northern cordilleras ca.…”