N. 2015. Dissimilar bacterial and fungal decomposer communities across rich to poor fen peatlands exhibit functional redundancy. Can. J. Soil Sci. 95: 219Á230. Climatic and environmental changes can lead to shifts in the dominant vegetation communities present in northern peatland ecosystems, including from Sphagnum-to vascular-dominated systems. Such shifts in vegetation result in changes to the chemical quality of carbon substrates for soil microbial decomposers, with leaves and roots deposited in the peat surface and subsurface that potentially decompose faster. This study characterized the bacterial and fungal communities present along a nutrient gradient ranging from rich to poor fen peatlands and assessed the metabolic potential of these communities to mineralize a variety of organic matter substrates of varying chemical complexity using substrate-induced respiration (SIR) assays. Distinct microbial communities existed between rich, intermediate and poor fens, but SIR in each of the three sites exhibited the same pattern of carbon mineralization, providing support for the concept of functional redundancy, at least under standardized in vitro conditions. Preferential mineralization of simple organic substrates in the rich fen and complex compounds in the poor fen was not observed. Similarly, no preference was given to ''native'' organic matter extracts derived from each fen, with microbial communities opting for the most bioavailable substrate. This study suggests that soil bacteria and fungi might be able to respond relatively rapidly to shifts in vegetation communities and subsequent changes in the quality of carbon substrate additions to peatlands associated with environmental and climatic change. Redondance fonctionnelle des populations de bacte´ries et de champignons assurant la de´composition dans les riches a`pauvres tourbie`res de carex. Can. J. Soil Sci. 95: 219Á230. Les changements climatiques et environnementaux peuvent entraıˆner une modification des peuplements dominants de plantes dans l'e´cosyste`me des tourbie`res nordiques, notamment le passage des tourbie`res domine´es par le genre Sphagnum a`celles domine´es par les plantes vasculaires. De tels changements au niveau de la ve´ge´tation modifient la qualite´du substrat carbone´que de´compose la microflore du sol en raison du de´poˆt de feuilles et de racines susceptibles de se de´composer plus vite en surface et sous la surface. L'e´tude a permis de caracte´riser les populations de bacte´ries et de cryptogames qui occupent le gradient des tourbie`res a`carex riches a`pauvres; elle a aussi e´value´la capacite´de ces populations a`mine´raliser, par voie me´tabolique, divers substrats de matie`re organique d'une complexite´chimique variable, graˆce a`des essais sur la respiration induite par le substrat (RIS). La microflore des tourbie`res riches, interme´diaires et pauvres varie, mais la RIS illustre le meˆme mode de mine´ralisation du carbone dans les trois cas, ce qui appuie l'hypothe`se d'une redondance fonctionnelle, du moins dans des co...