Abstract

The organic matter accumulation potential of a restored bog was estimated over 2 years as a balance be- tween losses to decomposition and inputs through above- ground net primary productivity (AGNPP) in five micro- habitats of increasing complexity (relating to the moss car- pet thickness and the number of vegetation functional groups). Decomposition and accumulation rates variations were hypothesized to lead to higher organic matter accumu- lation potential in the more complex micro-habitats. In general, for a given litter type, the mass losses and decom- position rates were rather homogeneous between micro- habitats, but, they were correlated to the cover of particular species: Eriophorum vaginatum with slower decomposition rates, and Ledum groendlandicum or Kalmia angustifolia with higher rates. Therefore, the abundance of some peatland species, rather than the habitat complexity itself, was a driver of decomposition rates. While the Sphagnum AGNPP did not compensate for decomposition losses, the organic matter accumulation potential was tipped towards a sink (positive) by the contribution of vascular species to the AGNPP. The organic matter accumulation potentials are much improved by the presence of Sphagnum, but from a restoration perspective, promoting the growth of vascular peatland species might also be a key to achieving a positive balance of organic matter accumulation.

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