Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland

Carbon (C) fluxes in semiarid grasslands subject to precipitation variability play a critical role in the terrestrial C cycle. However, how ecosystem C fluxes respond to variability in precipitation (both decreases and increases precipitation along a gradient) remains unclear. In this study, we cond...

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Main Authors: Hua Chai, Jianying Ma, Jinwei Zhang, Junqin Li, Bo Meng, Chengliang Wang, Duofeng Pan, Jie Li, Wei Sun, Xuhui Zhou
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-02-01
Series:Frontiers in Plant Science
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Online Access:https://www.frontiersin.org/articles/10.3389/fpls.2025.1519879/full
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author Hua Chai
Hua Chai
Jianying Ma
Jinwei Zhang
Junqin Li
Bo Meng
Chengliang Wang
Duofeng Pan
Jie Li
Wei Sun
Xuhui Zhou
author_facet Hua Chai
Hua Chai
Jianying Ma
Jinwei Zhang
Junqin Li
Bo Meng
Chengliang Wang
Duofeng Pan
Jie Li
Wei Sun
Xuhui Zhou
author_sort Hua Chai
collection DOAJ
description Carbon (C) fluxes in semiarid grasslands subject to precipitation variability play a critical role in the terrestrial C cycle. However, how ecosystem C fluxes respond to variability in precipitation (both decreases and increases precipitation along a gradient) remains unclear. In this study, we conducted a three-year field experiment in a semiarid grassland, with six precipitation treatments (precipitation decreased by 70%, 50%, and 30% [P–70%, P–50%, and P–30%], natural precipitation [P+0%], and precipitation increased by 30% and 50% [P+30% and P+50%]) to examine how variations in precipitation influence ecosystem C fluxes, specifically focusing on gross ecosystem productivity (GEP), ecosystem respiration (ER), and net ecosystem CO2 exchange (NEE). We found that both decreased and increased precipitation significantly altered the GEP (from –26% to 14%), but only decreased precipitation significantly reduced the ER and NEE (from 1% to 31%), relative to their values during natural precipitation. This suggests that ecosystem C fluxes are more sensitive to decreased precipitation, and respond nonlinearly to the precipitation gradient. Furthermore, structural equation modeling indicated that the soil water content was the primary controlling factor driving changes in ecosystem C fluxes. Our research underscores the nonlinear response of ecosystem C fluxes to changes in precipitation within semiarid ecosystems, particularly their sensitivity to extreme drought. Considering this nonlinear response, it is crucial to improve dynamic models of the C cycle and predict ecosystem responses to precipitation variability.
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spelling doaj-art-c8f946f22c9048bc9412be0150ecebf12025-02-06T12:08:44ZengFrontiers Media S.A.Frontiers in Plant Science1664-462X2025-02-011610.3389/fpls.2025.15198791519879Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grasslandHua Chai0Hua Chai1Jianying Ma2Jinwei Zhang3Junqin Li4Bo Meng5Chengliang Wang6Duofeng Pan7Jie Li8Wei Sun9Xuhui Zhou10Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, School of Ecology, Northeast Forestry University, Harbin, ChinaInstitute of Grassland Science, Key Laboratory of Vegetation Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, ChinaKey Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, Ministry of Education, School of Geographical Sciences, Northeast Normal University, Changchun, ChinaDepartment of Grassland Science, College of Animal Science and Technology, Northeast Agricultural University, Harbin, ChinaInstitute of Grassland Science, Key Laboratory of Vegetation Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, ChinaInstitute of Grassland Science, Key Laboratory of Vegetation Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, ChinaInstitute of Grassland Science, Key Laboratory of Vegetation Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, ChinaInstitute of Forage and Grassland Sciences, Heilongjiang Academy of Agricultural Sciences, Harbin, Heilongjiang, ChinaKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, School of Ecology, Northeast Forestry University, Harbin, ChinaInstitute of Grassland Science, Key Laboratory of Vegetation Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, ChinaKey Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, School of Ecology, Northeast Forestry University, Harbin, ChinaCarbon (C) fluxes in semiarid grasslands subject to precipitation variability play a critical role in the terrestrial C cycle. However, how ecosystem C fluxes respond to variability in precipitation (both decreases and increases precipitation along a gradient) remains unclear. In this study, we conducted a three-year field experiment in a semiarid grassland, with six precipitation treatments (precipitation decreased by 70%, 50%, and 30% [P–70%, P–50%, and P–30%], natural precipitation [P+0%], and precipitation increased by 30% and 50% [P+30% and P+50%]) to examine how variations in precipitation influence ecosystem C fluxes, specifically focusing on gross ecosystem productivity (GEP), ecosystem respiration (ER), and net ecosystem CO2 exchange (NEE). We found that both decreased and increased precipitation significantly altered the GEP (from –26% to 14%), but only decreased precipitation significantly reduced the ER and NEE (from 1% to 31%), relative to their values during natural precipitation. This suggests that ecosystem C fluxes are more sensitive to decreased precipitation, and respond nonlinearly to the precipitation gradient. Furthermore, structural equation modeling indicated that the soil water content was the primary controlling factor driving changes in ecosystem C fluxes. Our research underscores the nonlinear response of ecosystem C fluxes to changes in precipitation within semiarid ecosystems, particularly their sensitivity to extreme drought. Considering this nonlinear response, it is crucial to improve dynamic models of the C cycle and predict ecosystem responses to precipitation variability.https://www.frontiersin.org/articles/10.3389/fpls.2025.1519879/fullecosystem carbon fluxesaltered precipitationnonlinear responsesprecipitation gradientsemiarid grasslands
spellingShingle Hua Chai
Hua Chai
Jianying Ma
Jinwei Zhang
Junqin Li
Bo Meng
Chengliang Wang
Duofeng Pan
Jie Li
Wei Sun
Xuhui Zhou
Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland
Frontiers in Plant Science
ecosystem carbon fluxes
altered precipitation
nonlinear responses
precipitation gradient
semiarid grasslands
title Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland
title_full Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland
title_fullStr Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland
title_full_unstemmed Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland
title_short Nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland
title_sort nonlinear responses of ecosystem carbon fluxes to precipitation change in a semiarid grassland
topic ecosystem carbon fluxes
altered precipitation
nonlinear responses
precipitation gradient
semiarid grasslands
url https://www.frontiersin.org/articles/10.3389/fpls.2025.1519879/full
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