“…BP occur (Table 1). In the northeastern part of the TP, the loess accumulation in the basins is up to several meters and the paleoclimatic record of these aeolian sediments dates into the late Quaternary, but most accumulation started since the late Glacial period (Lehmkuhl, 1995(Lehmkuhl, , 1997Kaiser et al, 2007;Liu et al, 2012;Stauch et al, 2012;Yu and Lai, 2012;Liu et al, 2013;Qiang et al, 2013;Lehmkuhl et al, 2014).…”