“…As examples, high free-Fe/Al and low Ca/Al have been reported for dust outbreaks from Sahel, whereas high Ca/Al were measured for Saharan dust outbreaks (Chester et al, 1971, Chester et al, 1993; Chiapello et al, 1997; Moreno et al, 2006, among others), and high Ca/Al was used as a tracer of Western China deserts in PMx from Beijing, while lower ratios pointed to a Northern China desert origin (Yuan et al, 2008). Other tracers of source regions for dust are stable isotopes and radionuclides (Papastefanou et al, 2001; Aba et al, 2018; Goudie and Middleton, 2006, and references therein; among others) (see also section on compositional patterns of dust).…”