“…Soil colours have been applied to recognize soil composition and quality, and as one of basic parameters for soil classification since the beginning of the modern soil sciences (Linné, 1748). In particular soil colour may apparently reflect the origin and content of organic matter in soil (Łabaz et al, 2019;Łachacz and Załuski, 2023;Zhang and Hartemink, 2019), transformation/degradation of soil humus and humus horizons (Drewnik and Żyła, 2019;Łabaz and Kabała, 2016), mineral weathering and accumulation of iron compounds (Barajas and Ceron, 2022;Jankowski and Bednarek, 2022;Wakwoya et al, 2023), pedogenic accumulation of secondary carbonates and gypsum (Ayala-Nińo et al, 2022), illuvial accumulation of humus, iron, and clay (Durn et al, 2023;Gus-Stolarczy et al, 2023), water stagnation and redox processes (Repe and Pristovsek, 2022;Świtoniak et al, 2022), morphological transformation of soil profile (Czigány et al, 2020;Krupski et al, 2017;Mendyk et al, 2020;Świtoniak, 2014), persistence of parent materials in soil, in particular the light-coloured limestones/dolomites (Łabaz et al, 2022), lithogenic stratification of soil profile from alluvial (Jonczak et al, 2023;Kawałko et al, 2021;Loaiza-Usuga et al, 2022) or glacial (Kabala et al, 2022;Woronko et al, 2022) sedimentation, and other.…”