Community‐specific impacts of exotic earthworm invasions on soil carbon dynamics in a sandy temperate forest

• Published in: Ecology (Durham) 2013, Vol.94 (12), p.2827-2837
• Main Authors: Crumsey, Jasmine M, James M. Le Moine, Yvan Capowiez, Mitchell M. Goodsitt, Sandra C Larson, George W. Kling, Knute J. Nadelhoffer
• Format: Article
• Language: English
• Subjects: A horizons; Acer rubrum; Aporrectodea caliginosa; burrows; carbon; carbon dioxide; carbon sequestration; carbon sinks; dissolved organic carbon; earthworms; Eisenia fetida; Fagus grandifolia; forest soils; Lumbricus terrestris; nitrogen; Pinus strobus; plant litter; Populus grandidentata; Quercus rubra; soil profiles; temperate forests
• ISSN: 0012-9658; 1939-9170

Exotic earthworm introductions can alter above‐ and belowground properties of temperate forests, but the net impacts on forest soil carbon (C) dynamics are poorly understood. We used a mesocosm experiment to examine the impacts of earthworm species belonging to three different ecological groups (Lumbricus terrestris [anecic], Aporrectodea trapezoides [endogeic], and Eisenia fetida [epigeic]) on C distributions and storage in reconstructed soil profiles from a sandy temperate forest soil by measuring CO₂ and dissolved organic carbon (DOC) losses, litter C incorporation into soil, and soil C storage with monospecific and species combinations as treatments. Soil CO₂ loss was 30% greater from the Endogeic × Epigeic treatment than from controls (no earthworms) over the first 45 days; CO₂ losses from monospecific treatments did not differ from controls. DOC losses were three orders of magnitude lower than CO₂ losses, and were similar across earthworm community treatments. Communities with the anecic species accelerated litter C mass loss by 31–39% with differential mass loss of litter types (Acer rubrum > Populus grandidentata > Fagus grandifolia > Quercus rubra ≥ Pinus strobus) indicative of leaf litter preference. Burrow system volume, continuity, and size distribution differed across earthworm treatments but did not affect cumulative CO₂ or DOC losses. However, burrow system structure controlled vertical C redistribution by mediating the contributions of leaf litter to A‐horizon C and N pools, as indicated by strong correlations between (1) subsurface vertical burrows made by anecic species, and accelerated leaf litter mass losses (with the exception of P. strobus); and (2) dense burrow networks in the A‐horizon and the C and N properties of these pools. Final soil C storage was slightly lower in earthworm treatments, indicating that increased leaf litter C inputs into soil were more than offset by losses as CO₂ and DOC across earthworm community treatments.