“…Data from previous studies suggest that Cretaceous cooling is likely a wide‐scale event as it is apparent in many LTT data sets (Figure 9), such as in northern Malawi and Tanzania (Kasanzu et al., 2016; van der Beek et al., 1998), Zambia (Alessio et al., 2019), southern Malawi (Daszinnies et al., 2008; Eby et al., 1995), Mozambique (Bicca et al., 2019; Daszinnies et al., 2009; Emmel et al., 2011, 2014), Zimbabwe (Belton & Raab, 2010; Mackintosh, Kohn, Gleadow, & Belton, 2019), and the South African Plateau (Wildman et al., 2017). Evidence for km‐scale uplift in the Cretaceous is also recorded in various central African cratons (e.g., the Congo Craton, Alessio et al., 2019 and the Tanzanian Craton, Noble et al., 1997; Kasanzu, 2017) and may be related to isostatic rebound in response to plume induced delamination of the lithosphere (Hu et al., 2018).…”