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Increasing precipitation reshapes alpine plant–microbial nutrient partitioning and enhances ecosystem carbon and nitrogen retention
Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för ekologi, miljö och geovetenskap. College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, China.ORCID-id: 0000-0002-5425-137X
Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för ekologi, miljö och geovetenskap.ORCID-id: 0000-0002-0476-7335
Theoretical and Experimental Ecology Station, CNRS, Moulis, France.
Department of Earth and Environmental Sciences, The University of Manchester, Manchester, United Kingdom.
Vise andre og tillknytning
2026 (engelsk)Inngår i: Journal of Ecology, ISSN 0022-0477, E-ISSN 1365-2745, Vol. 114, nr 7, artikkel-id e70385Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]
  1. Precipitation change is an important component of the ongoing climate change and substantially influences terrestrial nutrient and carbon (C) dynamics. However, the mechanisms by which increasing precipitation affects plant–microbial nitrogen (N) assimilation and ecosystem C and N retention remain unclear.
  2. Using isotopic tracing along a manipulated precipitation gradient in a water- and nutrient-limited alpine ecosystem, we investigated how increasing precipitation alters plant nutrient strategies, plant–microbial N partitioning and ecosystem C and N retention.
  3. Increased precipitation enhanced plant and microbial N assimilation, ecosystem N retention and plant C fixation. However, these effects were not consistent across ecosystem components. Increasing precipitation progressively promoted grass-forb ratio and community-level acquisitive root traits, whereas mycorrhizal colonization was greatest at intermediate precipitation. Plant biomass C and N accumulation remained responsive across a broader portion of the precipitation gradient than did microbial N assimilation, thereby shifting plant–microbial N partitioning.
  4. Structural equation modelling indicated that the plant pathway plays a stronger role than the microbial pathway in mediating the effects of increasing precipitation on ecosystem N retention and C fixation. Our findings suggest that ecosystem responses to increasing precipitation depend on how different biotic components respond and interact.
  5. Synthesis: Increasing precipitation reshapes plant–microbial nutrient partitioning and ecosystem C and N retention in alpine ecosystems. Our findings highlight the need to account for non-linear and contrasting responses among different ecosystem components when predicting the consequences of future climate change for alpine ecosystem functioning. This work contributes to providing a basis for tracking how alpine ecosystems may reorganize under future climate change.
sted, utgiver, år, opplag, sider
John Wiley & Sons, 2026. Vol. 114, nr 7, artikkel-id e70385
Emneord [en]
ecosystem components, non-linear responses, plant–microbial interactions, precipitation change, rainfall intensification, root functional traits
HSV kategori
Identifikatorer
URN: urn:nbn:se:umu:diva-256655DOI: 10.1111/1365-2745.70385ISI: 001804726700001Scopus ID: 2-s2.0-105043009165OAI: oai:DiVA.org:umu-256655DiVA, id: diva2:2086457
Tilgjengelig fra: 2026-07-14 Laget: 2026-07-14 Sist oppdatert: 2026-07-14bibliografisk kontrollert

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