Nitrogen isotope pattern in Mongolian larch stands at the southern Eurasian boreal forest boundary

Research output: Contribution to journalArticleResearchpeer review

Authors

  • Mika Hayashi
  • Maximo Larry Lopez Caceres
  • Yoshihiro Nobori
  • Byambasuren Mijidsuren
  • Jens Boy

External Research Organisations

  • Yamagata University
  • Mongolian University of Life Sciences
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Details

Original languageEnglish
Pages (from-to)608-621
Number of pages14
JournalIsotopes in Environmental and Health Studies
Volume54
Issue number6
Early online date29 Aug 2018
Publication statusPublished - 2 Nov 2018

Abstract

In the last decades a drastic increase in air temperature but a stable precipitation regime in Mongolia has led to gradual drying conditions. Thus, we evaluated the effect of spatial and climatic characteristics on the soil–plant nitrogen dynamics in three representative larch stands (Larix sibirica) with different geographical and climatic conditions using stable nitrogen isotopes. The results showed significant differences in the soil inorganic N content among sites and consequently a different isotopic composition in the plant–soil system. Litter, bark and wood had the lowest δ15N values for all sites, slightly higher δ15N values for needles, while the highest δ15N values were observed for roots and soil. These differences could be the result of the larch stands age themselves, but were in agreement with the spatial and climatic characteristics of the sites. Based on the δ15N value a higher reliance on ectomycorrhizal fungi (ECMF) was observed in the warmest and driest site, while lower dependency was shown in the cooler northern site with higher soil inorganic N content. In both sites, the rate of air temperature increase has been similar in the last decades; however, their soil–plant N dynamics showed different characteristics.

Keywords

    Boreal forest, climatic impact, isotope ecology, larch stands, Mongolia, nitrogen dynamics, nitrogen-15

ASJC Scopus subject areas

Cite this

Nitrogen isotope pattern in Mongolian larch stands at the southern Eurasian boreal forest boundary. / Hayashi, Mika; Lopez Caceres, Maximo Larry; Nobori, Yoshihiro et al.
In: Isotopes in Environmental and Health Studies, Vol. 54, No. 6, 02.11.2018, p. 608-621.

Research output: Contribution to journalArticleResearchpeer review

Hayashi M, Lopez Caceres ML, Nobori Y, Mijidsuren B, Boy J. Nitrogen isotope pattern in Mongolian larch stands at the southern Eurasian boreal forest boundary. Isotopes in Environmental and Health Studies. 2018 Nov 2;54(6):608-621. Epub 2018 Aug 29. doi: 10.1080/10256016.2018.1509073
Hayashi, Mika ; Lopez Caceres, Maximo Larry ; Nobori, Yoshihiro et al. / Nitrogen isotope pattern in Mongolian larch stands at the southern Eurasian boreal forest boundary. In: Isotopes in Environmental and Health Studies. 2018 ; Vol. 54, No. 6. pp. 608-621.
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abstract = "In the last decades a drastic increase in air temperature but a stable precipitation regime in Mongolia has led to gradual drying conditions. Thus, we evaluated the effect of spatial and climatic characteristics on the soil–plant nitrogen dynamics in three representative larch stands (Larix sibirica) with different geographical and climatic conditions using stable nitrogen isotopes. The results showed significant differences in the soil inorganic N content among sites and consequently a different isotopic composition in the plant–soil system. Litter, bark and wood had the lowest δ15N values for all sites, slightly higher δ15N values for needles, while the highest δ15N values were observed for roots and soil. These differences could be the result of the larch stands age themselves, but were in agreement with the spatial and climatic characteristics of the sites. Based on the δ15N value a higher reliance on ectomycorrhizal fungi (ECMF) was observed in the warmest and driest site, while lower dependency was shown in the cooler northern site with higher soil inorganic N content. In both sites, the rate of air temperature increase has been similar in the last decades; however, their soil–plant N dynamics showed different characteristics.",
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AU - Nobori, Yoshihiro

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AU - Boy, Jens

N1 - Funding information: We want to thank the Mongolian personnel and students from Mongolian University of Life Sciences for all the support during this research and the members of Soil Institute Laboratory at the Leibniz Universität Hannover, who supported us there during the analysis. We also want to thank Dr. G. Hill for the English correction of the paper. We want to thank the Mongolian personnel and students from Mongolian University of Life Sciences for all the support during this research and the members of Soil Institute Laboratory at the Leibniz Universit?t Hannover, who supported us there during the analysis. We also want to thank Dr. G. Hill for the English correction of the paper.

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