Investigations of decayed sandstone colonised by a species ofTrentepohlia

The occurrence of a sub-aerial microbial community dominated by a species ofTrentepohlia, a red-orange pigmented filamentous green alga, growing on a 13th century sandstone building in the Scottish borders appears to be associated with unusual stone decay. Decay, in the form of extensive surface spalling and grain dissagregation over large areas of external stonework, are coincident with the distribution of the algal community on the north facade of the building. Comparison of S.E.M. images taken of fresh intact stone and spalled stone from decayed zones suggests that the mechanisms of decay may, in part, be a physical process which results in quartz crystals becoming separated. The investigations carried out revealed little evidence of chemical processes which may be involved in the decay. Large filaments ofTrentepohlia are clearly visible growing vertically between separate grains of stone and the amount of highly absorbent mucilage present makes the friable dry spall become soft and gelatinous on wetting. It is possible that the observed decay may have been created through the mechanical action of wet-dry cycling of mucilage and expansive stress from the growth of algal filaments.