“…Nevertheless, ambiguity in the interpretation of OSL ages arises from partially bleached sediments since they carry residual signals from transport and depositional cycles earlier in the history of the minerals. Recent OSL dating studies on relict proglacial and glaciofluvial/deltaic sediments have encountered problems with incomplete bleaching of the luminescence signal prior to deposition, leading to anomalously old ages in some samples, and mixtures of differentially-bleached quartz grains (Rendell et al, 1994;Rhodes and Pownall, 1994;Berger and Anderson, 2000;Rhodes, 2000;Bitinas et al, 2001;Spencer and Owen, 2004;Raukas and Stankowski, 2005;Alexanderson and Murray, 2007;Boe et al, 2007;Gemmell et al, 2007;Klasen et al, 2007;Lukas et al, 2007;Thrasher et al, 2009). Fast component OSL quartz grains and grains whose OSL derives from other components could also exist within a deposit that has been evenly bleached, creating an 'apparently' inconsistently bleached sediment (Bailey, 2000;Murray and Wintle, 2003;Singarayer and Bailey, 2003).…”