“…Rock crusts may evolve into Soil crusts once enough mineral soil material has accumulated, or dust material has been trapped, for example in rock pockets/bowls (Souza-Egipsy et al, 2004). Nos crusts, in literature also called cryptogamic covers, may appear even on non-rocky solid substrates, like bark (Elbert et al, 2012), building and historical monuments (Gadd, 2007), human manuscripts or paintings (Sterflinger and Pinar, 2013), plastics (Crispim et al, 2003), or even liquid substances (mud, oil, dirty water, Höpner et al, 1994). With the help of a knife it is possible to remove the thickest humipedons from the substrate like a carpet or a stiff aggregate crust (< 3 cm), corresponding to thick Nos crusts (example in Figure 2e) or Soil crusts (Fig.…”