“…Rock varnish is not limited to any particular climate region, or to any particular environmental setting, even though varnish is most noticeable on subaerial rocky surfaces in warm deserts—hence its older name of “desert varnish.” Rock varnish is not limited to: (i) particular textures such nanoscale layering imposed by the dominance of clay minerals (Krinsley et al, 1995); (ii) samples that have microlaminations or those that do not (Liu and Broecker, 2013; Liu et al, 2013); (iii) very slow growing varnish that forms at rates of microns per millennia (Dorn, 1998; Liu and Broecker, 2000) or faster-accumulating varnishes (Dorn and Meek, 1995; Spilde et al, 2013); (iv) varnishes that contain variations in minor or trace elements such as barium (Dorn et al, 1990), lead (Dorn, 1998; Hoar et al, 2011; Otter et al, 2020; Sims et al, 2022; Spilde et al, 2013), and others (Thiagarajan and Lee, 2004); (iv) varnishes with particular suites of organic matter (Chaddha et al, 2023; Nagy et al, 1991); or (v) varnishes with ancient organic matter than can become entombed in an under varnish (Cremaschi et al, 2014; Wang et al, 2023; Zerboni and Cremaschi, 2007).…”