“…East African freshwater systems possess a diverse teleost fauna shaped by a complex geological history, including large-scale tectonic movements, volcanic activity, and significant uplifting (Danley et al, 2012;Sturmbauer, Baric, Salzburger, Rüber, & Verheyen, 2001;Verheyen, Salzburger, Snoeks, & Meyer, 2003). The East African Rift (EAR) Valley, which was formed by tectonic uplift, is the major geological structure that has forged the general hydrographical network in Africa (Giddelo, Arndt, & Volckaert, 2002;Pinton, Agnèse, Paugy, & Otero, 2013) and created various freshwater habitats. For instance, major continental river systems were particularly impacted by the regional uplift, including the Nile, Congo, and Zambezi Rivers (Baker & Wohlenberg, 1971;Roberts et al, 2012).…”