4.7 Article

The fate of nitrogen inputs in a warmer alpine treeline ecosystem: a 15N labelling study

期刊

JOURNAL OF ECOLOGY
卷 105, 期 6, 页码 1723-1737

出版社

WILEY
DOI: 10.1111/1365-2745.12780

关键词

delta C-13; N-delta 15; ammonium; climate change; glycine; plant-soil (below-ground) interactions; stable isotope; Vaccinium gaultherioides; Vaccinium myrtillus

资金

  1. Swiss National Science Foundation [315200-116861]
  2. Velux Foundation [371]
  3. WSL
  4. Swiss State Secretariat for Education, Research and Innovation

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1. Global warming may accelerate nitrogen (N) transformations in the soil, with potentially large effects in N-poor high-elevation ecosystems. To gain insight into the partitioning of inorganic and organic N inputs within the plant-soil system and how warming influences these patterns, we applied a N-15 label ((NH4Cl)-N-15 or N-15-glycine) shortly after snowmelt during the sixth year of experimental soil warming (+4 degrees C) at treeline in the Swiss Alps. 2. Seven weeks after labelling, approximately 60% of the applied label remained in the soil organic layer to 10 cm depth, whereas label recovery summed over all measured plant pools was <10% of the added label. Soil warming led to a weaker Delta N-15 signal in plants and no change in the amount of added label recovered in plants. This Delta N-15 dilution resulted from a greater N pool size of some plant species in warmed plots as well as enhanced availability of (unlabelled) N under warming. Temporal dynamics of foliar Delta N-15 in dominant dwarf shrub species suggested that these plants primarily take up N early in the season. In a subset of plots labelled with C-13-enriched glycine (U-C-13(2)-N-15-glycine), the labelled glycine was mineralized rapidly, with approximately 50% of the applied C-13 respired as CO2 during the first 99 h, suggesting that effects of warmer soils on N dynamics in this treeline system are only slightly modulated by the preferences of different plant species for inorganic and organic N forms. 3. Synthesis. Plants growing in warmer soils acquired more unlabelled, soil-derived N in the sixth year of treatment, implying a sustained increase in N mineralization and availability in alpine treeline ecosystems with higher soil temperatures predicted for the future. Wide variation in the ability of plant species and functional groups to compete for early-summer N inputs means that there is a feedback between plant community shifts and N dynamics under environmental change at the treeline.

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