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Increasing precipitation reshapes alpine plant–microbial nutrient partitioning and enhances ecosystem carbon and nitrogen retention
Zhao, Qingzhou
Umeå University, Faculty of Science and Technology, Department of Ecology and Environmental Sciences. College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing, China.
ORCID iD:
0000-0002-5425-137X
Wardle, David A.
Umeå University, Faculty of Science and Technology, Department of Ecology and Environmental Sciences.
ORCID iD:
0000-0002-0476-7335
Freschet, Grégoire T.
Theoretical and Experimental Ecology Station, CNRS, Moulis, France.
Tao, Tingting
Department of Earth and Environmental Sciences, The University of Manchester, Manchester, United Kingdom.
Ma, Miaojun
State Key Laboratory of Herbage Improvement and Grassland Agro-Ecosystems, College of Ecology, Lanzhou University, Lanzhou, China.
Hu, Shuijin
College of Agro-Grassland Science, Nanjing Agricultural University, Nanjing, China.
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2026 (English)
In:
Journal of Ecology, ISSN 0022-0477, E-ISSN 1365-2745, Vol. 114, no 7, article id e70385
Article in journal (Refereed) Published
Abstract [en]
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.
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.
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.
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.
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.
Place, publisher, year, edition, pages
John Wiley & Sons, 2026. Vol. 114, no 7, article id e70385
Keywords [en]
ecosystem components, non-linear responses, plant–microbial interactions, precipitation change, rainfall intensification, root functional traits
National Category
Ecology
Identifiers
URN:
urn:nbn:se:umu:diva-256655
DOI:
10.1111/1365-2745.70385
ISI:
001804726700001
Scopus ID:
2-s2.0-105043009165
OAI: oai:DiVA.org:umu-256655
DiVA, id:
diva2:2086457
Available from:
2026-07-14
Created:
2026-07-14
Last updated:
2026-07-14
Bibliographically approved
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