“…Two main routes connecting the northeastern AF and AM have been proposed (Andrade‐Lima, 1982; Bigarella et al., 1975; Bigarella & Andrade‐Lima, 1982). One along the coastal region of northeastern Brazil through remnants of humid and forested vegetation, known as ‘brejos de altitude’, that were probably continuous in the past (Andrade‐Lima, 1964, 1982; Bigarella & Andrade‐Lima, 1982; Castro et al., 2019), and have current persisted in montane forest fragments surrounded by an open and dry environment of the Caatinga (Andrade‐Lima, 1982; Batalha‐Filho et al., 2013; Carnaval & Bates, 2007; Lima, 2021; Santos et al., 2007; Thomé et al., 2016). Another route would have been through a corridor formed in the middle of the Caatinga during the Plio‐Pleistocene (Auler et al., 2004; Auler & Smart, 2001; Batalha‐Filho et al., 2013; Oliveira et al., 1999), or earlier during the Miocene (De Sá et al., 2019; Pellegrino et al., 2011; Prates et al., 2017; Rodrigues et al., 2014).…”