' M M .\ H ^-m cuspidatum Hoflm. vvas collected from a ren-iote site in N. Wales, and a polluted site in the S. Pennines. When added to artificial rainwater solutitin, HSO., was oxidized to SO," . The rate at which this oxidation Occurred was modified differentially by the mosses from the two sites.S. cuspidatum from the S. Pennines promoted a rapid oxidation rate and disappearance of HSO,, w as complete "1 6 h. S. cuspidatum from N. Wales, on the other hand, achieved a very slow oxidation rate and HSO., persisted 'n solution for more than 24 h. Prolonged exposure to HSO^ in the Welsh n-iaterial caused damage to, and 'eventual death of, this material hut not of the S. Pennine moss.The rates of I ISO., oxidation promoted by the mosses from the two sites appear to be related to thê concentration of the transition metal ions, l'e(lll), Mn(ii), and CU(H), present on the cell-wall cation-exchange sites. These metals, particularly Fe, present on the surface of the S. Pennine n-iaterial catalysed a rapid chemical oxidation of HSO,, to SO,-^ . The increased lev-els of transition n-ietals associated with the S. Pennine t-i-ioss Originate in the peat as a legacy of past pollution events at this site. Levels of Fe were approximately 100 times greater than those for Mn or Cu and 5-10 tin-ies higher on the S. Pennine moss than on that from N. Wales. Removal of these metal ions (using EDTA) from the surface of the S. Pennine material removed the HSO., oxidizing ability of the moss, leading eventually to cell death.The ability to withstand high levels of HSO., was conferred upon the Welsh moss by supplying I'\'(iii) in sttificial rainwater solution under laboratory conditions. Transplanting Sphagnum fron-i the Welsh to the S. "ennine site gav-e rise to a similar response. Nomet-iclature of mosses follows Smith (1978).