Localities in the interior of South Africa, such as Taung and Vaal River sites, were intensively researched after hominins were discovered (Péringuey, 1911; Dart, 1925a; Goodwin, 1928), but then neglected for the fossil-rich, dolomitic breccia sites in Gauteng Province (e.g., Cooke, 1963, 1967; Vrba, 1976; Brain, 1981, Brain and Sillen, 1988; Bamford, 1999; Pickering and Kramers, 2010; Herries and Shaw, 2011; Reynolds et al., 2011; Lee-Thorp and Sponheimer, 2013). Recently, knowledge of the interior region has increased, following excavations at Florisbad (Brink, 1988; Kuman et al., 1999; Toffolo et al., 2015), Taung, including Equus Cave (Scott, 1987; Klein et al., 1991; McKee and Tobias, 1994; Lee-Thorp and Beaumont, 1995; Johnson et al., 1997; Hopley et al., 2013; McKee, 2016), Canteen Kopje (Beaumont, 1990, 2004; McNabb and Beaumont, 2011; Smith et al., 2012; Lotter et al., 2016), Pniel (Beaumont, 1990; Kunneriath and Gaillard, 2010; Hutson, 2018), Erfkroon (Churchill et al., 2000a; Brink et al., 2015a), Bundu Farm (Kiberd, 2006; Hutson, 2018), Cornelia (Brink et al., 2012; Toffolo et al., 2019) and the Kathu Complex (Porat et al., 2010; Wilkins and Chazan, 2012; Wilkins et al., 2012; Walker et al., 2014; Lukich et al., 2019, 2020).