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Anthropogenic nitrogen enrichment enhances soil carbon accumulation by impacting saprotrophs rather than ectomycorrhizal fungal activity.
Journal article

Anthropogenic nitrogen enrichment enhances soil carbon accumulation by impacting saprotrophs rather than ectomycorrhizal fungal activity.

  • Maaroufi NI Institute of Plant Sciences, University of Bern, Bern, Switzerland.
  • Nordin A Department of Forest Genetics and Plant Physiology, Umeå Plant Science Center, Swedish University of Agricultural Sciences, Umeå, Sweden.
  • Palmqvist K Department of Ecology and Environmental Science, Umeå University, Umeå, Sweden.
  • Hasselquist NJ Department of Forest Ecology and Management, Swedish University of Agriculture Sciences, Umeå, Sweden.
  • Forsmark B Department of Forest Ecology and Management, Swedish University of Agriculture Sciences, Umeå, Sweden.
  • Rosenstock NP Center for Environmental and Climate Research, Lund University, Lund, Sweden.
  • Wallander H Department of Microbial Ecology, Lund University, Lund, Sweden.
  • Gundale MJ Department of Forest Ecology and Management, Swedish University of Agriculture Sciences, Umeå, Sweden.
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  • 2019-06-06
Published in:
  • Global change biology. - 2019
Gadgil effect
ITS amplicons
carbon sequestration
ecological stoichiometry
high-throughput sequencing
ingrowth mesh bags
litter decomposition
root exclosure
soil organic matter
Carbon
Mycorrhizae
Nitrogen
Soil
Soil Microbiology
Sweden
English There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in boreal forest soils. However, it is unclear how free-living saprotrophs (bacteria and fungi, SAP) and ectomycorrhizal (EM) fungi responses to N addition impact soil C dynamics. Our aim was to investigate how SAP and EM communities are impacted by N enrichment and to estimate whether these changes influence decay of litter and humus. We conducted a long-term experiment in northern Sweden, maintained since 2004, consisting of ambient, low N additions (0, 3, 6, and 12 kg N ha-1  year-1 ) simulating current N deposition rates in the boreal region, as well as a high N addition (50 kg N ha-1  year-1 ). Our data showed that long-term N enrichment impeded mass loss of litter, but not of humus, and only in response to the highest N addition treatment. Furthermore, our data showed that EM fungi reduced the mass of N and P in both substrates during the incubation period compared to when only SAP organisms were present. Low N additions had no effect on microbial community structure, while the high N addition decreased fungal and bacterial biomasses and altered EM fungi and SAP community composition. Actinomycetes were the only bacterial SAP to show increased biomass in response to the highest N addition. These results provide a mechanistic understanding of how anthropogenic N enrichment can influence soil C accumulation rates and suggest that current N deposition rates in the boreal region (≤12 kg N ha-1  year-1 ) are likely to have a minor impact on the soil microbial community and the decomposition of humus and litter.
Language
  • English
Open access status
closed
Identifiers
Persistent URL
https://folia.unifr.ch/global/documents/186657
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