“…Numerous studies have focused on Pleistocene and Holocene inland aeolian deposits, and associated paleosols, in non-desert unglaciated regions of the country. Examples include loess studies in the northwestern USA (Busacca, 1991;McDonald and Busacca, 1992;Busacca and McDonald, 1994;Busacca et al, 2004;Sweeney et al 2004); studies of sand and finer-grained aeolian sediment in the High Plains of the west-central USA (Muhs, 1985;Holliday, 1989Holliday, , 2001Muhs et al, 1999a;Muhs et al, 1999b;Arbogast and Muhs, 2000;Muhs and Holliday, 2001;Forman et al, 2001Forman et al, , 2008Forman et al, , 2009Rawling et al, 2003;Miao et al, 2007;Muhs et al, 2008;Halfen et al, 2010Halfen et al, , 2012, and loess studies in the eastern midcontinent (Fig. 1a) (Ruhe 1969(Ruhe , 1983Barnhisel et al, 1971;Leigh and Knox, 1994;Follmer et al, 1986;Forman et al, 1992;Follmer, 1996;Grimley et al, 1998Grimley et al, , 2003Grimley, 2000;Hall and Anderson, 2000;Muhs and Bettis, 2000;Bettis et al, 2003a,b;Karathanasis and MacNeal, 2004).…”