Surface waters in forested watersheds in the Adirondack Mountains and northern New York State are susceptible to nitrogen (N) saturation. Atmospheric deposition of N to watersheds in this region has been measured but the extent of internal N inputs from symbiotic N fixation in alder-dominated wetlands is not known. We estimated N fixation by speckled alder in these wetlands by the N natural abundance method and by acetylene reduction using a flow-through system. Foliar N derived from fixation (%N) was estimated for five wetlands. The δN of speckled alder foliage from four of the five sites did not differ significantly (P≤0.05) from that of nodulated speckled alders grown in N-free water culture (-1.2±0.1‰). Estimates from the N natural abundance method indicated that alders at these sites derive 85-100% of their foliar N from N fixation. At one of the sites, we also measured biomass and N content and estimated that the alder foliage contained 43 kg N ha of fixed N in 1997. This estimate was based on a foliar N content of 55.4±7 kg N ha (mean±SE), 86±4%N, and an assumption that 10% of foliar N was derived from reserves in woody tissues. At this site, we further estimated via acetylene reduction that 37±10 kg N ha was fixed by speckled alders in 1998. This estimate used the theoretical 4:1 CH reduction to N fixation ratio and assumed no night-time fixation late in the season. Nitrogen inputs in wet and dry deposition at this site are approximately 8 kg N ha year. We conclude that speckled alder in wetlands of northern New York State relies heavily on N fixation to meet N demands, and symbiotic N fixation in speckled alders adds substantial amounts of N to alder-dominated wetlands in the Adirondack Mountains. These additions may be important for watershed N budgets, where alder-dominated wetlands occupy a large proportion of watershed area.
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http://dx.doi.org/10.1007/s004420000500 | DOI Listing |
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