“…The close relationships between Branco, Essequibo, and Guiana Shield taxa recovered for the Pliocene and Pleistocene can be explained by intermittent river connections between the lower portions of these drainages (as discussed in Lima, 2017); alternatively, these patterns could be related to headwater capture events between the Branco and the proto‐Berbice (a large drainage system from the central Guiana Shield that drained most of the Guyana and parts of Brazil, Venezuela, and Surinam from the Cenozoic to the Pleistocene – see Sinha, 1968; Lujan & Armbruster, 2011; Schaefer & Vale Júnior, 1997). Pleistocene and younger interactions between the Branco and Essequibo basins can be attributed to the Rupununi Portal, a flooded savanna area that allows for seasonal faunal interchange between these basins (De Souza et al, 2012, 2020; Hubert & Renno, 2006; Lovejoy & Araújo, 2000).…”