Effects of the early stage of decomposition on change in carbon and nitrogen isotopes in Sphagnum litter

Abstract

Isotope and elemental composition of carbon (C) and nitrogen (N) as well as its mass loss were measured for Sphagnum fuscum litter after one and two years of incubation in three different soil zones defined by the position of water table in a pristine Sphagnum-dominated peatland on the coast of western Canada. Mass losses were greater for the first year than for the second year, and the greatest loss was found in the oxic zone closest to the peatland surface. Early stage of decomposition clearly affected isotope signatures in Sphagnum litter. Litter δ¹³C values significantly decreased after the first year of incubation. The depletion of ¹³C content during the first year might be related to the loss of more isotopically enriched soluble constituents coupled with the large mass loss. Litter δ¹⁵N values significantly increased after the first year of incubation in spite of the large mass loss. Litters incubated in the oxic zone had the greatest mass loss and ¹⁵N enrichment, suggesting that the enrichment was the result of interactions with soil microbes and preferential loss of lighter N. Conversely, litters incubated in the anoxic zone had smaller mass loss and the amount of N significantly increased, suggesting that the incorporation of bacterial biomass might also contribute to the ¹⁵N enrichment. The ¹⁵N enrichment trend continued in the second year, but the change was not significant as the first year. Increases in the δ¹⁵N values with depth in the near surface Sphagnum peat core suggests that the enrichment trend of litter ¹⁵N abundance with age is likely to continue for much longer periods than observed over the two-year period of this study.