“…Linking these lithic assemblages is a paucity of retouched flakes, with denticulates perhaps being the most common form (Thompson and Marean, 2008;Volman, 1980;Will et al, 2013;Wurz, 2012). Earlier MSA assemblages are currently known from many sites in the WRZ/YRZ, including Cape St Blaize, Nelson Bay Cave, Klasies River, Blombos Cave, Pinnacle Point, Die Kelders, Peers Cave, Ysterfontein, Hoedjiespunt, Elands Bay Cave, Diepkloof, Hollow Rock Shelter and Klipfonteinrand (Avery, 1997;Avery et al, 2008;Högberg and Larsson, 2011;Mackay, 2009;Marean, 2010;Marean et al, 2007;Porraz et al, 2013a;Thompson and Marean, 2008;Volman, 1980;Will et al, 2013).…”