4.7 Article

Nitrogen isotopes in the soil-to-tree continuum - Tree rings express the soil biogeochemistry of boreal forests exposed to moderate airborne emissions

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 780, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.146581

关键词

Reactive N; pH; Ectomycorrhizal fungi; Soil microbiome; N transformation; Airborne pollutants

资金

  1. Geological Survey of Canada Environmental Geoscience Program
  2. Canadian Forest Service Genomics R&D initiative and cumulative effects Program at NRCan
  3. Environment & Climate Change Canada (Air Quality Division)

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This study analyzed tree ring nitrogen isotopic ratios of thirteen white spruce trees in two regions exposed to moderate anthropogenic nitrogen emissions. The results showed that tree-ring nitrogen isotopic ratios reflect specific soil nitrogen conditions and assimilation modes by trees.
Anthropogenic N emissions represent a potential threat for forest ecosystems, and environmental indicators that provide insight into the changing forest N cycle are needed. Tree ring N isotopic ratios (delta N-15) appear as a contentious choice for this role as the exact mechanisms behind tree-ring delta N-15 changes seldom benefit from a scrutiny of the soil-to-tree N continuum. This study integrates the results from the analysis of soil chemistry, soil microbiome genomics, and delta N-15 values of soil N compounds, roots, ectomycorrhizal (EcM) fungi and recent tree rings of thirteen white spruce trees sampled in five stands, from two regions exposed to moderate anthropogenic N emissions (3.9 to 8.1 kg/ha/y) with distinctive delta N-15 signals. Our results reveal that airborne anthropogenic N with distinct delta N-15 signals may directly modify the NO3- delta N-15 values in surface soils, but not the ones of NH4+ , the preferred N form of the studied trees. Hence, the tree-ring delta N-15 values reflect specific soil N conditions and assimilation modes by trees. Along with a wide tree-ring delta N-15 range, we report differences in: soil nutrient content and N transformation rates; delta N-15 values of NH4+ , total dissolved N (TDN) and EcM mantle enveloping the root tips; and bacterial and fungal community structures. We combine EcM mantle and root delta N-15 values with fungal identification to infer that hydrophobic EcM fungi transfer N from the dissolved organic N (DON) pool to roots under acidic conditions, and hydrophilic EcM fungi transfer various N forms to roots, which also assimilate N directly under less acidic conditions. Despite the complexities of & nbsp;soil biogeochemical properties and processes identified in the studied sites, in the end, the tree-ring delta N-15 averages inversely correlate with soil pH and anthropogenic N inputs, confirming white spruce tree-ring delta N-15 values as a suitable indicator for environmental research on forest N cycling. Crown Copyright (C) 2021 Published by Elsevier B.V.

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