“…For 18 samples, the MG quartz CAM ages are significantly older (ratios >1.2) than the corresponding FG quartz OSL ages, implying that the finer grains may have been more thoroughly bleached prior to burial. This is contrary to results from previous investigations of different grain-size fractions within fluvial sediments (Kadereit et al, 2006;Unkel et al, 2007;Vandenberghe et al, 2007;Hu et al, 2010;Zhang et al, 2010a, b;Shen and Mauz, 2012) and glaciofluvial sediments (Richards et al, 2000a, b;Preusser et al, 2001Preusser et al, , 2003Alexanderson, 2007) which a C, M and F in brackets represent coarse, medium and fine sand. b Skew (c) and standard error (s c ) were calculated using the formula of Bailey and Arnold (2006).…”