Enchytraeid worms (Oligochaeta) enhance mineralization of carbon in organic upland soils

We investigated the functional role of enchytraeid worms (Oligochaeta) in o rganic upland soils experimentally, because that role of these animals is l ittle known. We made microcosms of intact soil cores cut from two depths, 0 -4 cm and 4-8 cm, of a Cambic Stagnohumic Gley from the Moor House National Nature Reserve (UK). Enchytraeids were added to half of the microcosms, re sulting in four treatments: litter (L), litter + enchytraeids (L + E), soil (S) and soil + enchytraeids (S + E). Triplicates of each treatment were es tablished, and all microcosms (60) were then incubated in the dark at 15 de grees C, arranged in a fully randomized design. The experiment ran over 110 days, with five destructive harvests at days 10, 25, 50, 75 and 110, when microbial measurements (soil respiration and biomass C) as well as measures of decomposition (nutrient concentration in leachates) were made. Enchytra eids almost doubled the availability of organic carbon (measured as dissolv ed organic carbon in soil leachates) in the surface (0-4 cm) microcosms onl y. There were no effects of enchytraeids on the release of inorganic N or P from either soil horizon, although the release of ammonium and phosphate w as correlated with the number of enchytraeids in the microcosms. The depth from which the soil was taken exerted a strong influence on nutrient leachi ng, with almost six times more ammonium and four times more carbon being le ached from the surface (0-4 cm) layer than from the more decomposed (4-8 cm ) horizon. There was little nitrate leaching from any of the treatments, wi th only one-quarter as much nitrate leached from the surface (0-4 cm) as fr om the subsurface (4-8 cm) horizon. Enchytraeids had no detectable effect o n microbial biomass, but they increased microbial respiration by 35% in the surface (0-4 cm) horizon. Because they enhanced microbial activity in this horizon we suggest that enchytraeids indirectly drive the processes of dec omposition and nutrient mineralization in organic upland soils.