The fluorogenic model substrates, methylumbelliferyl [MUF]-beta-D-gluc
oside, MUF-phosphate and MUF-sulphate, were used to investigate the ac
tivities of beta-glucosidase, phosphatase and sulphatase, respectively
, in Welsh peatland soils. The method was used to investigate depth de
pendent variations in enzyme activity in a riparian wetland, and flush
channel wetland. The highest activities were found at depths of less
than 10 cm, thus confirming other studies which suggest this upper dep
th to be the site of greatest microbial activity. The most serious lim
itation to the technique was found to be the (fluorescence) quenching
effects of the phenolic materials that dominate peatland dissolved org
anic carbon. The problem necessitates the adoption of a time consuming
quench correction procedure with every sample. Fluorogenic substrates
have led to a greater understanding of the role of enzymes in other a
quatic systems. It seems likely that they will prove of equal value in
elucidating their role in nutrient cycling and the biogeochemistry of
peatlands.