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Abstract
Plant and microbial use of nitrogen (N) can be simultaneously mutualistic and competitive, particularly in ecosystems dominated by mycorrhizal fungi. Our goal was to quantify plant uptake of organic and inorganic N across a broad latitudinal gradient of forest ecosystems that varied with respect to overstory taxon, edaphic characteristics, and dominant mycorrhizal association. Using
l3C and
l5N, we observed in situ the cycling dynamics of NH
4+ and glycine through various soil pools and fine roots over 14 days. Recovery of
l5N as soil N varied with respect to N form, forest type, and sampling period; however, there were similarities in the cycling dynamics of glycine and NH
4+ among all forest types. Microbial immobilization of
l5N was immediately apparent for both treatments and represented the largest sink (~25%) for
l5N among extractable soil N pools during the first 24 h. In contrast, fine roots were a relatively small sink (
Citation
McFarland, Jack W.; Ruess, Roger W.; Kielland, Knut; Pregitzer, Kurt; Hendrick, Ronald; Allen, Michael. 2010. Cross-ecosystem comparisons of in situ plant uptake of amino acid-N and NH
4+. Ecosystems. 13: 177-193.