Nitrogen translocation in Sphagnum mosses : effects of atmospheric nitrogen deposition

•  Here, the hypothesis was tested that nitrogen (N) translocation from older to younger parts of Sphagnum decreases as N inputs from atmospheric deposition increase. •  Nitrogen translocation in Sphagnum mosses was compared in bogs with contrasting atmospheric N deposition (Adirondack - relatively...

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Veröffentlicht in:The New phytologist. - 1979. - 156(2002), 2 vom: 20. Nov., Seite 241-253
1. Verfasser: Aldous, Allison R (VerfasserIn)
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2002
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article Sphagnum mosses atmospheric N deposition bog nitrogen nitrogen-use efficiency peatlands stable isotope 15N tracer translocation
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520 |a •  Here, the hypothesis was tested that nitrogen (N) translocation from older to younger parts of Sphagnum decreases as N inputs from atmospheric deposition increase. •  Nitrogen translocation in Sphagnum mosses was compared in bogs with contrasting atmospheric N deposition (Adirondack - relatively high N deposition; Maine - relatively low) and by following the movement of a 15 NH4 15 NO3 tracer applied to plots of Sphagnum capillifolium over 2 yr. •  Annual N translocation ranged from 11% to > 80% in the lower and higher influx sites, respectively. Nitrogen translocation was an important process for the N budget of the Sphagnum mosses, contributing 0.5-11% of the annual N requirements. These results suggest that N translocation is as important as direct N retention from atmospheric deposition for the N budget of the mosses. Contrary to expectations, N translocation was greater in the high (Adirondack) than in the low (Maine) deposition sites. •  If N translocation is closely tied to water availability, the relative positions of the water tables in the sites over the course of the experiments might account for differences in N translocation among sites. The lower translocation (Maine) sites had lower water tables in the first year of the experiment and experienced a more severe drought in the second year than did the Adirondack sites 
650 4 |a Journal Article 
650 4 |a Sphagnum mosses 
650 4 |a atmospheric N deposition 
650 4 |a bog 
650 4 |a nitrogen 
650 4 |a nitrogen-use efficiency 
650 4 |a peatlands 
650 4 |a stable isotope 15N tracer 
650 4 |a translocation 
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