Temperature-dependent soil CH4 fluxes and their drivers across a forest–wetland ecotone in degrading permafrost, Northeast China

Xingfeng Dong , Chao Liu , Miao Li , Xiaodong Wu , Haoran Man , Zhichao Zheng , Huiren Jiang , Dongyu Yang , Biao Li , Ye Ma , Guangying Zhao , Shuying Zang

Journal of Forestry Research ›› 2026, Vol. 37 ›› Issue (1) : 170

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Journal of Forestry Research ›› 2026, Vol. 37 ›› Issue (1) :170 DOI: 10.1007/s11676-026-02100-4
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Temperature-dependent soil CH4 fluxes and their drivers across a forest–wetland ecotone in degrading permafrost, Northeast China
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Abstract

Methane (CH4) fluxes in permafrost regions are commonly represented as monotonic functions of temperature, despite pronounced seasonal hydrological variability and habitat heterogeneity. Here, using two years of in situ high-frequency measurements, we examined whether CH4 fluxes exhibit trajectory-dependent temperature responses across a forest–wetland ecotone in a degrading permafrost landscape, and how hydrological and microbial processes modulated. We found that: (1) Wetland patches consistently acted as CH4 sources, with an average flux of 5.14 nmol m−2 s−1, whereas forests exhibited seasonal source–sink shifts and a much lower mean flux of 0.08 nmol m−2 s−1. Importantly, phase-stratified segmented regressions revealed distinct, nonlinear temperature thresholds and hysteresis in wetlands, with contrasting CH4–temperature relationships during warming and cooling phases, while forests showed weaker trajectory dependence. (2) Across habitats and seasons, soil methanogenic communities varied more strongly than methanotrophic communities and explained a larger (35%) of CH4 flux variability than methanotrophic attributes (21%) and soil properties (24%). (3) Soil moisture and inorganic nitrogen emerged as key factors linking hydrological conditions, microbial communities, and CH4 dynamics. These findings demonstrate that CH4 fluxes in permafrost ecotones are governed by the interaction of phase-dependent temperature responses, hydrological constraints, and microbial processes. Incorporating warming–cooling asymmetry and hydrological–microbial coupling may improve the prediction of CH4 dynamics in heterogeneous permafrost landscapes undergoing thaw.

Keywords

CH4 flux / Permafrost / Forest–wetland ecotone / Temperature response / CH4-cycling microorganisms

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Xingfeng Dong, Chao Liu, Miao Li, Xiaodong Wu, Haoran Man, Zhichao Zheng, Huiren Jiang, Dongyu Yang, Biao Li, Ye Ma, Guangying Zhao, Shuying Zang. Temperature-dependent soil CH4 fluxes and their drivers across a forest–wetland ecotone in degrading permafrost, Northeast China. Journal of Forestry Research, 2026, 37 (1) : 170 DOI:10.1007/s11676-026-02100-4

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References

[1]

Bao T, Xu XY, Jia GS, Jia GS, Zhu XR, Riley SD, Yang YH. Climate-carbon feedback tradeoff between Arctic and alpine permafrost under warming. Sci Adv, 2025

[2]

Bridgham SD, Cadillo-Quiroz H, Keller JK, Zhuang QL. Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales. Glob Change Biol, 2013, 19(5): 1325-1346

[3]

Carlsen ECL, Wei J, Lejzerowicz F, Trier-Kjær S, Westermann S, Hessen DO, Dörsch P, Eiler A. Redox determines greenhouse gas production kinetics and metabolic traits in water-saturated thawing permafrost peat. ISME Commun, 2025

[4]

Chang T, Yi YH, Jiang HR, Li RX, Lu P, Liu L, Wang LX, Zhao L, Zwieback S, Zhao JY. Unraveling the non-linear relationship between seasonal deformation and permafrost active layer thickness. Npj Clim Atmos Sci, 2024, 7(1 ArticleID: 308

[5]

Chen ML, Chang L, Zhang JM, Guo FC, Vymazal J, He Q. Global nitrogen input on wetland ecosystem: the driving mechanism of soil labile carbon and nitrogen on greenhouse gas emissions. Environ Sci Ecotechnol, 2020, 4 ArticleID: 100063

[6]

Chen SY, Gu YZ, Liu EY, Wu MH, Cheng XL, Yang PZ, Bahadur A, Bai RQ, Chen JW, Zhang MY, Wu JH, Feng Q. Freeze-thaw strength increases microbial stability to enhance diversity-soil multifunctionality relationship. Commun Earth Environ, 2024, 5(1): 578

[7]

Comer-Warner SA, Romeijn P, Gooddy DC, Ullah S, Kettridge N, Marchant B, Hannah DM, Krause S. Thermal sensitivity of CO2 and CH4 emissions varies with streambed sediment properties. Nat Commun, 2018, 9(1): 2803

[8]

Dong XF, Liu C, Li M, Ma DL, Chen Q, Zang SY. Variations in active layer soil hydrothermal dynamics of typical wetlands in permafrost region in the Great Hing’an Mountains, northeast China. Ecol Indic, 2021, 129 ArticleID: 107880

[9]

Dong XF, Liu C, Wu XD, Man HR, Wu XW, Ma DL, Li M, Zang SY. Linking soil organic carbon mineralization with soil variables and bacterial communities in a permafrost-affected tussock wetland during laboratory incubation. CATENA, 2023, 221 ArticleID: 106783

[10]

Dong XF, Liu C, Li M, Wu XD, Zheng ZC, Wu XW, Zang SY. Higher CH4 production in permafrost while oxidation prevails in the active layer: insights from a forest-wetland ecotone in Northeast China. Adv Clim Change Res, 2025, 16: 273-283

[11]

Ernakovich JG, Barbato RA, Rich VI, Schädel C, Hewitt RE, Doherty SJ, Whalen ED, Abbott BW, Barta J, Biasi C, Chabot C, Hultman J, Knoblauch C, Lau-Vetter MCY, Leewis MC, Liebner S, Mackelprang R, Onstott TC, Richter A, Schütte UME, Siljanen HMP, Taş N, Timling I, Vishnivetskaya TA, Waldrop MP, Winkel M. Microbiome assembly in thawing permafrost and its feedbacks to climate. Glob Change Biol, 2022, 28(17): 5007-5026

[12]

Fan LC, Dippold MA, Thiel V, Ge TD, Wu JS, Kuzyakov Y, Dorodnikov M. Temperature sensitivity of anaerobic methane oxidation versus methanogenesis in paddy soil: implications for the CH4 balance under global warming. Glob Change Biol, 2022, 28(2): 654-664

[13]

Hao YF, Mao JF, Bachmann CM, Hoffman FM, Koren G, Chen HS, Tian HQ, Liu JG, Tao J, Tang JY, Li LC, Liu LB, Apple M, Shi MJ, Jin MZ, Zhu Q, Kannenberg S, Shi XY, Zhang X, Wang YP, Fang YL, Dai YJ. Soil moisture controls over carbon sequestration and greenhouse gas emissions: a review. Npj Clim Atmos Sci, 2025, 8(1 ArticleID: 16

[14]

Huang LY, Qin SQ, Kou D, Ciais P, Xu XF, Peñuelas J, Xi Y, Yang GB, Song YT, Yao ST, Chang JF, Yang YH. Spatiotemporal patterns of methane fluxes across alpine permafrost region on the Tibetan Plateau. Nat Commun, 2025, 16(1 ArticleID: 7474

[15]

Jin HJ, Wu QB, Romanovsky VE. Degrading permafrost and its impacts. Adv Clim Change Res, 2021, 12(1): 1-5

[16]

Lawrence DM, Koven CD, Swenson SC, Riley WJ, Slater AG. Permafrost thaw and resulting soil moisture changes regulate projected high-latitude CO2 and CH4 emissions. Environ Res Lett, 2015, 10(9 ArticleID: 094011

[17]

Liu C, Dong XF, Wu XD, Ma DL, Wu YF, Man HR, Li M, Zang SY. Response of carbon emissions and the bacterial community to freeze–thaw cycles in a permafrost-affected forest–wetland ecotone in Northeast China. Microorganisms, 2022, 10(10 ArticleID: 1950

[18]

Liu AW, Yin WP, Ma DL, Wang X, Kan SP. Vertical distribution patterns and potential activities of methanogenic and methanotrophic communities in permafrost peatlands of Greater Khingan Mountains. Ecol Indic, 2025, 175 ArticleID: 113539

[19]

Lu BQ, Song LQ, Zang SY, Wang HX. Warming promotes soil CO2 and CH4 emissions but decreasing moisture inhibits CH4 emissions in the permafrost peatland of the Great Xing’an Mountains. Sci Total Environ, 2022, 829 ArticleID: 154725

[20]

McCalley CK, Woodcroft BJ, Hodgkins SB, Wehr RA, Kim EH, Mondav R, Crill PM, Chanton JP, Rich VI, Tyson GW, Saleska SR. Methane dynamics regulated by microbial community response to permafrost thaw. Nature, 2014, 514(7523): 478-481

[21]

Miner KR, Turetsky MR, Malina E, Bartsch A, Tamminen J, McGuire AD, Fix A, Sweeney C, Elder CD, Miller CE. Permafrost carbon emissions in a changing Arctic. Nat Rev Earth Environ, 2022, 3(1): 55-67

[22]

Mu M, Mu CC, Liu HB, Lei PS, Ge YQ, Zhou ZS, Peng XQ, Ma T. Thermokarst lake drainage halves the temperature sensitivity of CH4 release on the Qinghai-Tibet Plateau. Nat Commun, 2025, 16(1): 1992

[23]

Nazaries L, Murrell JC, Millard P, Baggs L, Singh BK. Methane, microbes and models: fundamental understanding of the soil methane cycle for future predictions. Environ Microbiol, 2013, 15(9): 2395-2417

[24]

Niu SL, Luo YQ, Fei SF, Montagnani L, Bohrer G, Janssens IA, Gielen B, Rambal S, Moors E, Matteucci G. Seasonal hysteresis of net ecosystem exchange in response to temperature change: patterns and causes. Glob Change Biol, 2011, 17(10): 3102-3114

[25]

Olefeldt D, Turetsky MR, Crill PM, McGuire AD. Environmental and physical controls on northern terrestrial methane emissions across permafrost zones. Glob Change Biol, 2013, 19(2): 589-603

[26]

Peltoniemi K, Laiho R, Juottonen H, Bodrossy L, Kell DA, Minkkinen K, Mäkiranta P, Mehtätalo L, Penttilä T, Siljanen HMP, Tuittila ES, Tuomivirta T, Fritze H. Responses of methanogenic and methanotrophic communities to warming in varying moisture regimes of two boreal fens. Soil Biol Biochem, 2016, 97: 144-156

[27]

Ran YH, Cheng GD, Dong YH, Hjort J, Lovecraft AL, Kang SC, Tan MB, Li X. Permafrost degradation increases risk and large future costs of infrastructure on the Third Pole. Commun Earth Environ, 2022, 3(1): 238

[28]

Singleton CM, McCalley CK, Woodcroft BJ, Boyd JA, Evans PN, Hodgkins SB, Chanton JP, Frolking S, Crill PM, Saleska SR, Rich VI, Tyson GW. Methanotrophy across a natural permafrost thaw environment. ISME J, 2018, 12(10): 2544-2558

[29]

Song YY, Feng HH, Luo SY, Qi J, Wang XW, Mei WK, Chen N, Feng YS, Song CC. Vertical profiles of soil CO2 and CH4 emissions and their driving mechanisms in different types of permafrost peatlands. J Hydrol, 2026, 665 ArticleID: 134754

[30]

Song YY, Wang XW, Feng HH, Luo SY, Qi J, Ren JS, Feng YS, Mei WK, Fu FC, Zhao YT, Song CC. Soil CO2-fixation by cbbL-harboring microorganisms in different types of permafrost peatlands. Appl Soil Ecol, 2026, 217 ArticleID: 106639

[31]

Sturtevant CS, Oechel WC. Spatial variation in landscape-level CO2 and CH4 fluxes from arctic coastal tundra: influence from vegetation, wetness, and the thaw lake cycle. Glob Change Biol, 2013, 19(9): 2853-2866

[32]

Szylit A, Christaki U, Barret M, Cabrol L, Gandois L, Sejourne A, Bouchard F, Ollivier S, Jardillier L. Spatial heterogeneity in methane biogeochemistry and prokaryotic community structure in sub-Arctic waterbodies in northern Canada. Environ Microbiol, 2025, 27(12 ArticleID: e70210

[33]

Virkkala AM, Niittynen P, Kemppinen J, Marushchak ME, Voigt C, Hensgens G, Kerttula J, Happonen K, Tyystjärvi V, Biasi C, Hultman J, Rinne J, Luoto M. High-resolution spatial patterns and drivers of terrestrial ecosystem carbon dioxide, methane, and nitrous oxide fluxes in the tundra. Biogeosciences, 2024, 21(2): 335-355

[34]

Wang JF, Wu QB, Yuan ZQ, Kang H. Soil respiration of alpine meadow is controlled by freeze–thaw processes of active layer in the permafrost region of the Qinghai-Tibet Plateau. Cryosphere, 2020, 14(9): 2835-2848

[35]

Wang YB, Liu X, Lv MX, Zhang ZY, et al.. Mechanisms and influencing factors of hydrothermal processes in active layer soils on the Qinghai-Tibet Plateau under freeze–thaw action. CATENA, 2023, 220 ArticleID: 106694

[36]

Wang HT, Lindemann E, Liebmann P, Varsadiya M, Svenning MM, Waqas M, Petters S, Richter A, Guggenberger G, Barta J, Urich T. Methane-cycling microbiomes in soils of the pan-Arctic and their response to permafrost degradation. Commun Earth Environ, 2025, 6(1): 748

[37]

Wang PY, Wang JS, Wang S, D’Imperio L, Elberling B, Ambus P, Zhang Z, Ito A, Li Y, Pan JX, Song L, Liu N, Zhang RY, Chen WN, Niu SL. Soil moisture threshold of methane uptake in alpine grassland ecosystems. Glob Change Biol, 2025, 31(2 ArticleID: e70062

[38]

Wang YT, Wei YN, Wang GS, Ruan Y, Li L, Liu X, Yang YF, Shen QR, Ling N. Hump-shaped relationship between microbial carbon use-efficiency and soil organic carbon in alpine grasslands. Adv Sci, 2025, 13(8 ArticleID: e13917

[39]

Yang SZ, Liebner S, Winkel M, Alawi M, Horn F, Dörfer C, Ollivier J, He JS, Jin HJ, Kühn P, Schloter M, Scholten T, Wagner D. In-depth analysis of core methanogenic communities from high elevation permafrost-affected wetlands. Soil Biol Biochem, 2017, 111: 66-77

[40]

Yang SZ, Wen X, Wu TH, Wu XD, Wang XM, Jin XY, Li XY, Yang X, Yang L, Wang HW. Carbon-cycling microorganisms in permafrost and their responses to a warming climate: a review. Permafrost Periglac, 2024, 35(2): 218-231

[41]

Yuan MM, Zhang J, Xue K, Wu LY, Deng Y, Deng J, Hale L, Zhou XS, He ZL, Yang YF, Nostrand JV, Schuur EAG, Konstantinidis KT, Penton CR, Cole JR, Tiedje JM, Luo YQ, Zhou JZ. Microbial functional diversity covaries with permafrost thaw-induced environmental heterogeneity in tundra soil. Global Change Biol, 2018, 24(1): 297-307

[42]

Zhang Q, Phillips RP, Manzoni S, Scott RL, Oishi AC, Finzi A, Daly E, Vargas R, Novick KA. Changes in photosynthesis and soil moisture drive the seasonal soil respiration-temperature hysteresis relationship. Agr Forest Meteorol, 2018, 259: 184-195

[43]

Zhang QW, Yang GB, Song YT, Kou D, Wang GQ, Zhang DY, Qin SQ, Mao C, Feng XH, Yang YH. Magnitude and drivers of potential methane oxidation and production across the Tibetan alpine permafrost region. Environ Sci Technol, 2019, 53(24): 14243-14252

[44]

Zhang ZQ, Wu QB, Hou MT, Tai BW, An YK. Permafrost change in Northeast China in the 1950s–2010s. Adv Clim Change Res, 2021, 12(1): 18-28

[45]

Zhang YM, Naafs BDA, Huang XY, Song QW, Xue JT, Wang RC, Zhao ML, Evershed RP, Pancost RD, Xie SC. Variations in wetland hydrology drive rapid changes in the microbial community, carbon metabolic activity, and greenhouse gas fluxes. Geochim Cosmochim Acta, 2022, 317: 269-285

[46]

Zhao Y, Zheng C, Gelfan A, Watanabe K, Liu HJ, Wright S, Wu XL, Quinton W, Wang Y, Yi SH, Zhang YY, Shi YJ, Jiao WT. Frozen soil hydrological processes and their effects: a review and synthesis. Rev Geophys, 2026, 64(1 ArticleID: e2024RG000839

[47]

Zhu MY, Song YY, Feng YS, Li MT, Feng HH, Luo SY, Tan WW, Chen N, Zhao GY, Song CC. Soil hydrolases and microbial biomass regulate wetland CO2 emissions under warming and water level reduction. Appl Soil Ecol, 2025, 215 ArticleID: 106387

[48]

Zuo YJ, Song YY, Jiang L, Li Y, Wang YS, Chen N, Jiang P, Zheng SJ, Song CC, Xu XF, Yuan FH, Sun L. Long-term carbon release of peatland soil after permafrost thaw in northmost China. CATENA, 2025, 261 ArticleID: 109551

Funding

National Natural Science Foundation of China(42501119)

China Postdoctoral Science Foundation(2025M770323)

Natural Science Foundation of Heilongjiang Province(PL2024D006)

Heilongjiang Provincial Postdoctoral Science Foundation(LBH-Z24205)

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