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Sammanfattning

Nitrogen is rapidly taken up by plants and microbes, but questions remain as to which forms are preferred. Using in situ stable isotope labelling (13C and 15N), we show that co-existing plant species of alpine heath mainly take up ammonium and nitrate, passing 15N from root to shoot over time, leading to accumulated nitrogen in the shoots (over 10-fold increase compared with roots), with more complex organic nitrogen forms such as amino acids taken up to a lesser extent. Conversely, soil microbes preferred amino acids, potentially as a side-effect of satisfying their carbon requirements to build cellular structures. We show that competition for nitrogen can be alleviated by differing growth rates in plants and varying microbial preference of nitrogen forms.

Nyckelord

Amino acids; Alpine; Mass ratio hypothesis; nitrogen cycling; Soil microbes; Dual labelled 15N/13C

Publicerad i

Soil Biology and Biochemistry
2026, volym: 216, artikelnummer: 110127
Utgivare: PERGAMON-ELSEVIER SCIENCE LTD

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Markvetenskap

Publikationens identifierare

  • DOI: https://doi.org/10.1016/j.soilbio.2026.110127

Permanent länk till denna sida (URI)

https://res.slu.se/id/publ/146381