“…The late Pleistocene climates and environments of the region around Klein Kliphuis are poorly documented due to a lack of natural and cultural archives, exacerbated in places by issues with dating. The complexities of the southern African climate systems also limit the relevance of records from elsewhere in southern Africa (Tyson, 1986), though those from coastal and hinterland regions to the north (Lim et al ., 2016; Stuut et al ., 2002), south (Braun et al ., 2019a,b; Chase et al ., 2018; Esteban et al ., 2020; Faith et al ., 2018), and east of Klein Kliphuis (Mackay et al ., 2019b) tend to indicate increased humidity during glacial phases MIS 4 and MIS 2 (Engelbrecht et al ., 2019). Data from hyrax middens in the Cederberg Mountains east and south‐east of Klein Kliphuis reveal spatially complex patterns of humidity through MIS 2 and the Holocene, though these records do not extend further into the Pleistocene and thus the period of interest here (Chase et al ., 2019).…”