Soluble rocks undergo erosion by solution when rain falls on an unprotected
rock surface. Lichens may act to protect the surface from such erosion, an
d the protected area may subsequently emerge from the surrounding lowering
surface to form an area of higher relief. Specimens of Aspicilia calcarea a
nd Diploschistes diacapsis act in this way on a gypsum surface, creating co
nical or rounded mounds up to 15 mm in height. In the case of Aspicilia, th
e lichen centre decays, re-exposing to surface solution the central area, w
hich then corrodes to create a cratered gypsum cone. The gradient of the co
ne side-slopes is a function of the relative rates of lichen radial growth
and rock surface lowering. (C) 2000 The British Lichen Society.