Cycling Dynamics of NH4+ and Amino Acid Nitrogen in Soils of a Deciduous Boreal Forest Ecosystem

McFarland JW, Ruess RW, Kielland K, Doyle AP. 2002. Cycling Dynamics of NH4+ and Amino Acid Nitrogen in Soils of a Deciduous Boreal Forest Ecosystem. Ecosystems. 5(8):775-788

Conventional studies of nitrogen (N) cycling in forest ecosystems have focused on inorganic N uptake as the primary source of N for plant metabolism. More recently, however, alternative sources of N for plant nutrition, such as free amino acids, have gained attention, particularly in nutrient-limited systems. Using a multiple stable isotope design, that allowed us to simultaneously assess root uptake of ammonium and glycine, we compared the cycling dynamics of NH4 + and amino acid N within the soils of several interior Alaskan floodplain balsam poplar stands. Our design included multiple sampling periods extending from 45 min to 14 days, which permitted us to study interpool transfers of our carbon (C) and N isotopes over time. Microbial biomass N was the largest sink of both 15 N-ammonium and glycine. Percent recovery of 15 N for this pool was an order of magnitude larger than fine-root 15 N uptake for most sampling periods. Although recovery of 15 N in fine-root biomass was small, amino acid N and NH4 + were assimilated at approximately the same rate irrespective of sampling period, and total recovery was still increasing 2 weeks after application. Recovery of 15 N in bulk soil samples did not vary significantly over time for either treatment. However, bulk soil 13 C declined steadily during the experiment, measuring less than 30% recovery of added label after 14 days. We suspect that the majority of 13 C lost from our soils was respired. Soil microorganisms strongly outcompeted plants in the short term for both NH4 + and amino acid N. However, amino acid N appears to cycle through soil N pools at approximately the same rate as inorganic N forms. The similarity in uptake patterns for inorganic and organic N suggests that these stands are meeting part of their N requirements directly from amino acids.

Type
Journal Article
Authors
McFarland, Jack; Ruess, Robert; Kielland, Knut; Doyle, Allen
Units
ARCN , BELA , CAKR , GAAR , KOVA , NOAT
Keywords
amino acid, Ammonium, annual grassland, Arctic, Arctic plants, balsam poplar, C-13 and N-15, ectomycorrhizal plants, Floodplain, glycine, inorganic-nitrogen, microbial biomass N, organic nitrogen, organic nitrogen uptake, pinus-contorta, plant-microbe competition, Tanana River floodplain, temperate forest

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