“…However, from the first step of the preliminary analysis, posterior estimates were unrealistically recent and truncated by zero. Thus, considering that all priors were interdependent, to make the models more realistic we performed two more steps of the preliminary analysis with increased specificity based on more detailed biogeographic scenarios that were built from independent records of geologic events (Supporting Information Figure ) and published population genetics data (Beadell et al, ; Opiro et al, ; Saarman et al, ). There were three major river reorganizations in the region that would have impacted tsetse distribution and connectivity: (a) Lake Victoria formed ~400 ka and reversed the direction of flow of the major river systems from west to north (Supporting Information Figure a; Williams, Adamson, Prescott, & Williams, ; Danley et al, ), (b) the outflow from Lake Victoria altered its course to connect through Kafu River to Lake Albert ~20–40 ka (Supporting Information Figure b; Bishop, ) and (c) the outflow from Lake Victoria altered its course a third time to bypass the Kafu River and to connect directly to Albert Nile through Murchison falls (Supporting Information Figure c; Talbot & Williams, ).…”