Articles | Volume 23, issue 10
https://doi.org/10.5194/bg-23-3615-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-23-3615-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Thawing Siberian permafrost stabilizes organic carbon from recent plant litter inputs
Christian Knoblauch
CORRESPONDING AUTHOR
University of Hamburg, Department of Earth System Sciences, Allende Platz 2, 20146 Hamburg, Germany
University of Hamburg, Center for Earth System Research and Sustainability, 20146 Hamburg, Germany
Christian Beer
University of Hamburg, Department of Earth System Sciences, Allende Platz 2, 20146 Hamburg, Germany
University of Hamburg, Center for Earth System Research and Sustainability, 20146 Hamburg, Germany
Carolina Voigt
University of Hamburg, Department of Earth System Sciences, Allende Platz 2, 20146 Hamburg, Germany
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Permafrost Research Section, Telegrafenberg A45, 14473 Potsdam, Germany
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Lin Yu, Thomas Kleinen, Min Jung Kwon, Christian Knoblauch, and Christian Beer
EGUsphere, https://doi.org/10.5194/egusphere-2025-4648, https://doi.org/10.5194/egusphere-2025-4648, 2025
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We studied how adding biochar to soils might affect future climate. Using computer simulations, we found that while global averages of temperature and rainfall change little, extreme events respond more clearly. Heat waves and heavy rain are reduced in many regions, though drought risks rise in some dry areas. These results suggest that biochar could help moderate harmful climate extremes, especially on land, but with region-specific effects.
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Climate warming in the Arctic is causing the erosion of permafrost coasts and the transformation of permafrost lakes into lagoons. To understand how this affects greenhouse gas (GHG) emissions, we studied carbon dioxide (CO₂) and methane (CH₄) production in lagoons with varying sea connections. Younger lagoons produce more CH₄, while CO₂ increases under more marine conditions. Flooding of permafrost lowlands due to rising sea levels may lead to higher GHG emissions from Arctic coasts in future.
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During cold seasons, methane release from northern wetlands is important but often underestimated. We studied a boreal bog to understand methane emissions in spring and fall. At cold temperatures, methane release decreases due to lower production rates, but efficient methane transport through plant structures, decaying plants, and the release of methane stored in the pore water keep emissions ongoing. Understanding these seasonal processes can improve models for methane release in cold climates.
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Climate change and warming in the Arctic exceed global averages. As a result, permanently frozen soils (permafrost) which store vast quantities of carbon in the form of dead plant material (organic matter) are thawing. Our study shows that as permafrost landscapes degrade, high concentrations of organic matter are released. Partly, this organic matter is degraded rapidly upon release, while another significant fraction enters stream networks and enters the Arctic Ocean.
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Luana S. Basso, Goran Georgievski, Victor Brovkin, Christian Beer, Christian Rödenbeck, and Mathias Göckede
Biogeosciences, 23, 2815–2830, https://doi.org/10.5194/bg-23-2815-2026, https://doi.org/10.5194/bg-23-2815-2026, 2026
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Sarah Schwieger, Jan Dietrich, Mats P. Björkman, Judith M. Sarneel, Bowen Li, Joel White, Inge H. J. Althuizen, Christina Biasi, Robert G. Björk, Hanna Böhner, Brage Bremset Hansen, Michele Carbognani, Giorgio Chiari, Casper T. Christiansen, Elisabeth J. Cooper, Hans Cornelissen, Ludovica D'Imperio, Ellen Dorrepaal, Bo Elberling, Patrick Faubert, Ned Fetcher, T'ai G. W. Forte, Joseph Gaudard, Konstantin Gavazov, Zhen-Huan Guan, Jón Guðmundsson, Siri V. Haugum, Jin-Sheng He, Caitlin Hicks Pries, Mark Hovenden, Simone I. Lang, Gus Jespersen, Ingibjörg S. Jónsdóttir, Ji Young Jung, Olga Khitun, Birgitte Kortegaard Danielsen, Richard Lamprecht, Mathilde Le Moullec, Hanna Lee, Maija E. Marushchak, Anders Michelsen, Tariq Munir, Eero Myrsky, Kevin K. Newsham, Marion Nyberg, Steven F. Oberbauer, Paulo Olivas, Johan Olofsson, Hlynur Óskarsson, Thomas C. Parker, Matteo Petit Bon, Alessandro Petraglia, Emily Pickering Pedersen, Katrine Raundrup, Nynne R. Ravn, Riikka Rinnan, Heidi Rodenhizer, Ingvild Ryde, Alejandro Salazar, Niels M. Schmidt, Ted Schuur, Sofie Sjögersten, Cecilie Skov Nielsen, Sari Stark, Maria Strack, Jianwu Tang, Sylvia Toet, Anne Tolvanen, Maria Väisänen, Richard Van Logtestijn, Vigdis Vandvik, Carolina Voigt, Josefine Walz, Jeffrey M. Welker, Yuanhe Yang, Henni Ylänne, and Sybryn L. Maes
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Marius Moser, Lara Kaiser, Victor Brovkin, and Christian Beer
Biogeosciences, 23, 605–621, https://doi.org/10.5194/bg-23-605-2026, https://doi.org/10.5194/bg-23-605-2026, 2026
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Arctic warming might lead to increased carbon dioxide and methane emissions. Process-based prediction of their ratio is important for projecting the future carbon cycle. However, land surface models often assume a constant ratio. To overcome this limitation, we identify three core processes for representing methanogenesis accurately in land surface models: fermentation, acetoclastic methanogenesis, and hydrogenotrophic methanogenesis.
Kseniia Ivanova, Anna-Maria Virkkala, Victor Brovkin, Tobias Stacke, Barbara Widhalm, Annett Bartsch, Carolina Voigt, Oliver Sonnentag, and Mathias Göckede
Biogeosciences, 23, 233–262, https://doi.org/10.5194/bg-23-233-2026, https://doi.org/10.5194/bg-23-233-2026, 2026
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We measured over 13,000 methane fluxes at a site in the Canadian Arctic and linked them with drone and free satellite images. We tested four machine-learning methods and two map scales. Metre-scale maps captured small wet and dry features that strongly affect methane release, while coarser maps blurred them. Different models shifted the monthly methane estimate. This helps choose the right data and tools to map methane, design monitoring networks, and check climate models.
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EGUsphere, https://doi.org/10.5194/egusphere-2025-5771, https://doi.org/10.5194/egusphere-2025-5771, 2025
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The study examined spatial and temporal variability of taiga snowpack during spring melt using weekly measurements of height, stratigraphy, temperature, and density at four Sodankylä sites. Snow height peaked on 30 Mar. Density increased through melt, reaching ~ 500 kg/m³ by late Apr–early May. Snow structure shifted from depth hoar to melt forms, and temperatures reached 0 °C throughout. By 10 May, snow cover disappeared. Findings highlight evolving, heterogeneous melt-season snow properties.
Philipp de Vrese, Tobias Stacke, Veronika Gayler, Helena Bergstedt, Clemens von Baeckmann, Melanie Thurner, Christian Beer, and Victor Brovkin
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Lin Yu, Thomas Kleinen, Min Jung Kwon, Christian Knoblauch, and Christian Beer
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We studied how adding biochar to soils might affect future climate. Using computer simulations, we found that while global averages of temperature and rainfall change little, extreme events respond more clearly. Heat waves and heavy rain are reduced in many regions, though drought risks rise in some dry areas. These results suggest that biochar could help moderate harmful climate extremes, especially on land, but with region-specific effects.
Christian Beer
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Fauna and flora respire carbon dioxide into the atmosphere, which is a major carbon flux into the atmosphere. The underlying biochemical processes are complex, and we generalize them either assuming a first-order chemical reaction of carbon and oxygen to carbon dioxide or assuming enzymatic reactions. Here, we show that these assumptions lead to large differences in estimating the carbon–climate feedback until 2100 and the remaining carbon budget to keep warming below 2°C.
Maren Jenrich, Juliane Wolter, Susanne Liebner, Christian Knoblauch, Guido Grosse, Fiona Giebeler, Dustin Whalen, and Jens Strauss
Biogeosciences, 22, 2069–2086, https://doi.org/10.5194/bg-22-2069-2025, https://doi.org/10.5194/bg-22-2069-2025, 2025
Short summary
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Climate warming in the Arctic is causing the erosion of permafrost coasts and the transformation of permafrost lakes into lagoons. To understand how this affects greenhouse gas (GHG) emissions, we studied carbon dioxide (CO₂) and methane (CH₄) production in lagoons with varying sea connections. Younger lagoons produce more CH₄, while CO₂ increases under more marine conditions. Flooding of permafrost lowlands due to rising sea levels may lead to higher GHG emissions from Arctic coasts in future.
Katharina Jentzsch, Elisa Männistö, Maija E. Marushchak, Aino Korrensalo, Lona van Delden, Eeva-Stiina Tuittila, Christian Knoblauch, and Claire C. Treat
Biogeosciences, 21, 3761–3788, https://doi.org/10.5194/bg-21-3761-2024, https://doi.org/10.5194/bg-21-3761-2024, 2024
Short summary
Short summary
During cold seasons, methane release from northern wetlands is important but often underestimated. We studied a boreal bog to understand methane emissions in spring and fall. At cold temperatures, methane release decreases due to lower production rates, but efficient methane transport through plant structures, decaying plants, and the release of methane stored in the pore water keep emissions ongoing. Understanding these seasonal processes can improve models for methane release in cold climates.
Youssef Saadaoui, Christian Beer, Peter Mueller, Friederike Neiske, Joscha N. Becker, Annette Eschenbach, and Philipp Porada
EGUsphere, https://doi.org/10.5194/egusphere-2024-1756, https://doi.org/10.5194/egusphere-2024-1756, 2024
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Estuarine marshes are vital for capturing carbon and benefiting the climate. Our research explored how plant-microbe interactions affect carbon cycling, focusing on traits like root oxygen loss. Using a model, we found that accounting for these trait variations significantly changes carbon balance estimates. This suggests that including plant diversity in ecosystem models improves predictions about carbon dynamics in estuarine marshes, highlighting their importance in climate regulation.
Niek Jesse Speetjens, George Tanski, Victoria Martin, Julia Wagner, Andreas Richter, Gustaf Hugelius, Chris Boucher, Rachele Lodi, Christian Knoblauch, Boris P. Koch, Urban Wünsch, Hugues Lantuit, and Jorien E. Vonk
Biogeosciences, 19, 3073–3097, https://doi.org/10.5194/bg-19-3073-2022, https://doi.org/10.5194/bg-19-3073-2022, 2022
Short summary
Short summary
Climate change and warming in the Arctic exceed global averages. As a result, permanently frozen soils (permafrost) which store vast quantities of carbon in the form of dead plant material (organic matter) are thawing. Our study shows that as permafrost landscapes degrade, high concentrations of organic matter are released. Partly, this organic matter is degraded rapidly upon release, while another significant fraction enters stream networks and enters the Arctic Ocean.
Cited articles
Amundson, R. and Baisden, W. T.: Stable isotope tracers and mathematical models in soil organic matter studies, in: Methods in Ecosystem Science, edited by: Sala, O. E., Jackson, R. B., Mooney, H. A., and Howarth, R. B., Springer New York, 117–137, ISBN 978-0-387-98734-7, 2000.
Andrén, O. and Kätterer, T.: ICBM: The introductory carbon balance model for exploration of soil carbon balances, Ecol. Appl., 7, 1226–1236, https://doi.org/10.2307/2641210, 1997.
Arndt, K. A., Santos, M. J., Ustin, S., Davidson, S. J., Stow, D., Oechel, W. C., Tran, T. T. P., Graybill, B., and Zona, D.: Arctic greening associated with lengthening growing seasons in Northern Alaska, Environ. Res. Lett., 14, 125018, https://doi.org/10.1088/1748-9326/ab5e26, 2019.
Bartón, K.: MuMIn: Multi-Model Inference (R package version 1.47.5) [code], https://cran.r-project.org/web/packages/MuMIn/MuMIn.pdf (last access: 21 May 2026), 2023.
Bastviken, D., Ejlertsson, J., and Tranvik, L.: Similar bacterial growth on dissolved organic matter in anoxic and oxic lake water, Aquat. Microb. Ecol., 24, 41–49, 2001.
Beer, C., Knoblauch, C., Hoyt, A. M., Hugelius, G., Palmtag, J., Mueller, C. W., and Trumbore, S.: Vertical pattern of organic matter decomposability in cryoturbated permafrost-affected soils, Environ. Res. Lett., 17, 104023, https://doi.org/10.1088/1748-9326/ac9198, 2022.
Begill, N., Don, A., and Poeplau, C.: No detectable upper limit of mineral-associated organic carbon in temperate agricultural soils, Glob. Change Biol., 29, 4662–4669, https://doi.org/10.1111/gcb.16804, 2023.
Belshe, E. F., Schuur, E. A. G., and Bolker, B. M.: Tundra ecosystems observed to be CO2 sources due to differential amplification of the carbon cycle, Ecol. Lett., 16, 1307–1315, https://doi.org/10.1111/ele.12164, 2013.
Berner, L. T., Massey, R., Jantz, P., Forbes, B. C., Macias-Fauria, M., Myers-Smith, I., Kumpula, T., Gauthier, G., Andreu-Hayles, L., Gaglioti, B. V., Burns, P., Zetterberg, P., D'Arrigo, R., and Goetz, S. J.: Summer warming explains widespread but not uniform greening in the Arctic tundra biome, Nat. Commun., 11, 4621, https://doi.org/10.1038/s41467-020-18479-5, 2020.
Bischoff, J., Mangelsdorf, K., Gattinger, A., Schloter, M., Kurchatova, A. N., Herzschuh, U., and Wagner, D.: Response of methanogenic archaea to Late Pleistocene and Holocene climate changes in the Siberian Arctic, Global Biogeochem. Cy., 27, 305–317, https://doi.org/10.1029/2011GB004238, 2013.
Boike, J., Nitzbon, J., Anders, K., Grigoriev, M., Bolshiyanov, D., Langer, M., Lange, S., Bornemann, N., Morgenstern, A., Schreiber, P., Wille, C., Chadburn, S., Gouttevin, I., Burke, E., and Kutzbach, L.: A 16-year record (2002–2017) of permafrost, active-layer, and meteorological conditions at the Samoylov Island Arctic permafrost research site, Lena River delta, northern Siberia: an opportunity to validate remote-sensing data and land surface, snow, and permafrost models, Earth Syst. Sci. Data, 11, 261–299, https://doi.org/10.5194/essd-11-261-2019, 2019.
Bonanomi, G., Incerti, G., Giannino, F., Mingo, A., Lanzotti, V., and Mazzoleni, S.: Litter quality assessed by solid state 13C NMR spectroscopy predicts decay rate better than and ratios, Soil Biol. Biochem., 56, 40–48, https://doi.org/10.1016/j.soilbio.2012.03.003, 2013.
Breiman, L.: Random forests, Machine Learning, 45, 5–32, 2001.
Bridgham, S. D., Updegraff, K., and Pastor, J.: Carbon, nitrogen, and phosphorus mineralization in northern wetlands, Ecology, 79, 1545–1561, 1998.
Carvalhais, N., Forkel, M., Khomik, M., Bellarby, J., Jung, M., Migliavacca, M., Mu, M., Saatchi, S., Santoro, M., Thurner, M., Weber, U., Ahrens, B., Beer, C., Cescatti, A., Randerson, J. T., and Reichstein, M.: Global covariation of carbon turnover times with climate in terrestrial ecosystems, Nature, 514, 213–217, https://doi.org/10.1038/nature13731, 2014.
Cassidy, A. E., Christen, A., and Henry, G. H. R.: The effect of a permafrost disturbance on growing-season carbon-dioxide fluxes in a high Arctic tundra ecosystem, Biogeosciences, 13, 2291–2303, https://doi.org/10.5194/bg-13-2291-2016, 2016.
Cerli, C., Celi, L., Kalbitz, K., Guggenberger, G., and Kaiser, K.: Separation of light and heavy organic matter fractions in soil – Testing for proper density cut-off and dispersion level, Geoderma, 170, 403–416, https://doi.org/10.1016/j.geoderma.2011.10.009, 2012.
Cheng, X., Xing, W., and Liu, J.: Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter, Biol. Fert. Soils, 59, 777–790, https://doi.org/10.1007/s00374-023-01746-0, 2023.
Cornelissen, J. H. C., Van Bodegom, P. M., Aerts, R., Callaghan, T. V., Van Logtestijn, R. S. P., Alatalo, J., Stuart Chapin, F., Gerdol, R., Gudmundsson, J., Gwynn-Jones, D., Hartley, A. E., Hik, D. S., Hofgaard, A., Jónsdóttir, I. S., Karlsson, S., Klein, J. A., Laundre, J., Magnusson, B., Michelsen, A., Molau, U., Onipchenko, V. G., Quested, H. M., Sandvik, S. M., Schmidt, I. K., Shaver, G. R., Solheim, B., Soudzilovskaia, N. A., Stenström, A., Tolvanen, A., Totland, Ø., Wada, N., Welker, J. M., Zhao, X., and Team, M. O. L.: Global negative vegetation feedback to climate warming responses of leaf litter decomposition rates in cold biomes, Ecol. Lett., 10, 619–627, https://doi.org/10.1111/j.1461-0248.2007.01051.x, 2007.
Cotrufo, M. F., Wallenstein, M. D., Boot, C. M., Denef, K., and Paul, E.: The Microbial Efficiency-Matrix Stabilization (MEMS) framework integrates plant litter decomposition with soil organic matter stabilization: do labile plant inputs form stable soil organic matter?, Glob. Change Biol., 19, 988–995, https://doi.org/10.1111/gcb.12113, 2013.
Coward, E. K., Ohno, T., and Sparks, D. L.: Direct evidence for temporal molecular fractionation of dissolved organic matter at the iron oxyhydroxide interface, Environ. Sci. Technol., 53, 642–650, https://doi.org/10.1021/acs.est.8b04687, 2019.
Dong, H., Zeng, Q., Sheng, Y., Chen, C., Yu, G., and Kappler, A.: Coupled iron cycling and organic matter transformation across redox interfaces, Nature Reviews Earth & Environment, 4, 659-673, https://doi.org/10.1038/s43017-023-00470-5, 2023.
Drake, T. W., Wickland, K. P., Spencer, R. G. M., McKnight, D. M., and Striegl, R. G.: Ancient low–molecular-weight organic acids in permafrost fuel rapid carbon dioxide production upon thaw, P. Natl. Acad. Sci. USA, 112, 13946–13951, https://doi.org/10.1073/pnas.1511705112, 2015.
Eckhardt, T., Knoblauch, C., Kutzbach, L., Holl, D., Simpson, G., Abakumov, E., and Pfeiffer, E.-M.: Partitioning net ecosystem exchange of CO2 on the pedon scale in the Lena River Delta, Siberia, Biogeosciences, 16, 1543–1562, https://doi.org/10.5194/bg-16-1543-2019, 2019.
Elberling, B., Michelsen, A., Schädel, C., Schuur, E. A. G., Christiansen, H. H., Berg, L., Tamstorf, M. P., and Sigsgaard, C.: Long-term CO2 production following permafrost thaw, Nat. Clim. Change, 3, 890-894, https://doi.org/10.1038/nclimate1955, 2013.
Elmendorf, S. C., Henry, G. H. R., Hollister, R. D., Björk, R. G., Boulanger-Lapointe, N., Cooper, E. J., Cornelissen, J. H. C., Day, T. A., Dorrepaal, E., Elumeeva, T. G., Gill, M., Gould, W. A., Harte, J., Hik, D. S., Hofgaard, A., Johnson, D. R., Johnstone, J. F., Jónsdóttir, I. S., Jorgenson, J. C., Klanderud, K., Klein, J. A., Koh, S., Kudo, G., Lara, M., Lévesque, E., Magnússon, B., May, J. L., Mercado-Díaz, J. A., Michelsen, A., Molau, U., Myers-Smith, I. H., Oberbauer, S. F., Onipchenko, V. G., Rixen, C., Martin Schmidt, N., Shaver, G. R., Spasojevic, M. J., Þórhallsdóttir, Þ. E., Tolvanen, A., Troxler, T., Tweedie, C. E., Villareal, S., Wahren, C.-H., Walker, X., Webber, P. J., Welker, J. M., and Wipf, S.: Plot-scale evidence of tundra vegetation change and links to recent summer warming, Nat. Clim. Change, 2, 453–457, https://doi.org/10.1038/nclimate1465, 2012.
Euskirchen, E. S., McGuire, A. D., Kicklighter, D. W., Zhuang, Q., Clein, J. S., Dargaville, R. J., Dye, D. G., Kimball, J. S., McDonald, K. C., Melillo, J. M., Romanovsky, V. E., and Smith, N. V.: Importance of recent shifts in soil thermal dynamics on growing season length, productivity, and carbon sequestration in terrestrial high-latitude ecosystems, Glob. Change Biol., 12, 731–750, https://doi.org/10.1111/j.1365-2486.2006.01113.x, 2006.
Faucherre, S., Jørgensen, C. J., Blok, D., Weiss, N., Siewert, M. B., Bang-Andreasen, T., Hugelius, G., Kuhry, P., and Elberling, B.: Short and long-term controls on active layer and permafrost carbon turnover across the Arctic, J. Geophys. Res.-Biogeo., 123, 372–390, https://doi.org/10.1002/2017JG004069, 2018.
García-Palacios, P., Bradford, M. A., Benavente-Ferraces, I., de Celis, M., Delgado-Baquerizo, M., García-Gil, J. C., Gaitán, J. J., Goñi-Urtiaga, A., Mueller, C. W., Panettieri, M., Rey, A., Sáez-Sandino, T., Schuur, E. A. G., Sokol, N. W., Tedersoo, L., and Plaza, C.: Dominance of particulate organic carbon in top mineral soils in cold regions, Nat. Geosci., 17, 145–150, https://doi.org/10.1038/s41561-023-01354-5, 2024.
Gentsch, N., Mikutta, R., Shibistova, O., Wild, B., Schnecker, J., Richter, A., Urich, T., Gittel, A., Santruckova, H., Barta, J., Lashchinskiy, N., Mueller, C. W., Fuss, R., and Guggenberger, G.: Properties and bioavailability of particulate and mineral-associated organic matter in Arctic permafrost soils, Lower Kolyma Region, Russia, Eur. J. Soil Sci., 66, 722–734, https://doi.org/10.1111/ejss.12269, 2015a.
Gentsch, N., Mikutta, R., Alves, R. J. E., Barta, J., Čapek, P., Gittel, A., Hugelius, G., Kuhry, P., Lashchinskiy, N., Palmtag, J., Richter, A., Šantrůčková, H., Schnecker, J., Shibistova, O., Urich, T., Wild, B., and Guggenberger, G.: Storage and transformation of organic matter fractions in cryoturbated permafrost soils across the Siberian Arctic, Biogeosciences, 12, 4525–4542, https://doi.org/10.5194/bg-12-4525-2015, 2015b.
Gentsch, N., Wild, B., Mikutta, R., Čapek, P., Diáková, K., Schrumpf, M., Turner, S., Minnich, C., Schaarschmidt, F., Shibistova, O., Schnecker, J., Urich, T., Gittel, A., Šantrůčková, H., Bárta, J., Lashchinskiy, N., Fuß, R., Richter, A., and Guggenberger, G.: Temperature response of permafrost soil carbon is attenuated by mineral protection, Glob. Change Biol., 24, 3401–3415, https://doi.org/10.1111/gcb.14316, 2018.
Guo, Y.-X., Yu, G.-H., Hu, S., Liang, C., Kappler, A., Jorgenson, Mark T., Guo, L., and Guggenberger, G.: Deciphering the intricate control of minerals on deep soil carbon stability and persistence in Alaskan permafrost, Glob. Change Biol., 30, e17552, https://doi.org/10.1111/gcb.17552, 2024.
Haddix, M. L., Paul, E. A., and Cotrufo, M. F.: Dual, differential isotope labeling shows the preferential movement of labile plant constituents into mineral-bonded soil organic matter, Glob. Change Biol., 22, 2301–2312, https://doi.org/10.1111/gcb.13237, 2016.
Heckman, K., Hicks Pries, C. E., Lawrence, C. R., Rasmussen, C., Crow, S. E., Hoyt, A. M., von Fromm, S. F., Shi, Z., Stoner, S., McGrath, C., Beem-Miller, J., Berhe, A. A., Blankinship, J. C., Keiluweit, M., Marín-Spiotta, E., Monroe, J. G., Plante, A. F., Schimel, J., Sierra, C. A., Thompson, A., and Wagai, R.: Beyond bulk: Density fractions explain heterogeneity in global soil carbon abundance and persistence, Glob. Change Biol., 28, 1178–1196, https://doi.org/10.1111/gcb.16023, 2022.
Heikkinen, J. E. P., Elsakov, V., and Martikainen, P. J.: Carbon dioxide and methane dynamics and annual carbon balance in tundra wetland in NE Europe, Russia, Global Biogeochem. Cy., 16, 1115, https://doi.org/10.1029/2002gb001930, 2002.
Huebner, D. C., Buchwal, A., and Bret-Harte, M. S.: Retrogressive thaw slumps in the Alaskan Low Arctic may influence tundra shrub growth more strongly than climate, Ecosphere, 13, e4106, https://doi.org/10.1002/ecs2.4106, 2022.
Hugelius, G., Strauss, J., Zubrzycki, S., Harden, J. W., Schuur, E. A. G., Ping, C.-L., Schirrmeister, L., Grosse, G., Michaelson, G. J., Koven, C. D., O'Donnell, J. A., Elberling, B., Mishra, U., Camill, P., Yu, Z., Palmtag, J., and Kuhry, P.: Estimated stocks of circumpolar permafrost carbon with quantified uncertainty ranges and identified data gaps, Biogeosciences, 11, 6573–6593, https://doi.org/10.5194/bg-11-6573-2014, 2014.
Hugelius, G., Ramage, J., Burke, E., Chatterjee, A., Smallman, T. L., Aalto, T., Bastos, A., Biasi, C., Canadell, J. G., Chandra, N., Chevallier, F., Ciais, P., Chang, J., Feng, L., Jones, M. W., Kleinen, T., Kuhn, M., Lauerwald, R., Liu, J., López-Blanco, E., Luijkx, I. T., Marushchak, M. E., Natali, S. M., Niwa, Y., Olefeldt, D., Palmer, P. I., Patra, P. K., Peters, W., Potter, S., Poulter, B., Rogers, B. M., Riley, W. J., Saunois, M., Schuur, E. A. G., Thompson, R. L., Treat, C., Tsuruta, A., Turetsky, M. R., Virkkala, A. M., Voigt, C., Watts, J., Zhu, Q., and Zheng, B.: Permafrost region greenhouse gas budgets suggest a weak CO2 sink and CH4 and N2O sources, but magnitudes differ between top-down and bottom-up methods, Global Biogeochem. Cy., 38, e2023GB007969, https://doi.org/10.1029/2023GB007969, 2024.
ISO 11277:2020: Soil quality Determination of particle size distribution in mineral soil material Method by sieving and sedimentation, International Organization of Standardization, https://www.iso.org/standard/69496.html (last access: 21 May 2026), 2020.
Jagadamma, S., Steinweg, J. M., Mayes, M. A., Wang, G., and Post, W. M.: Decomposition of added and native organic carbon from physically separated fractions of diverse soils, Biol. Fert. Soils, 50, 613–621, https://doi.org/10.1007/s00374-013-0879-2, 2014.
Jia, N., Li, L., Guo, H., and Xie, M.: Important role of Fe oxides in global soil carbon stabilization and stocks, Nat. Commun., 15, 10318, https://doi.org/10.1038/s41467-024-54832-8, 2024.
Jilling, A., Grandy, A. S., Daly, A. B., Hestrin, R., Possinger, A., Abramoff, R., Annis, M., Cates, A. M., Dynarski, K., Georgiou, K., Heckman, K., Keiluweit, M., Lang, A. K., Phillips, R. P., Rocci, K., Shabtai, I. A., Sokol, N. W., and Whalen, E. D.: Evidence for the existence and ecological relevance of fast-cycling mineral-associated organic matter, Communications Earth & Environment, 6, 690, https://doi.org/10.1038/s43247-025-02681-8, 2025.
Kaiser, C., Meyer, H., Biasi, C., Rusalimova, O., Barsukov, P., and Richter, A.: Conservation of soil organic matter through cryoturbation in arctic soils in Siberia, J. Geophys. Res.-Biogeo., 112, G02017, https://doi.org/10.1029/2006JG000258, 2007.
Kang, J., Qu, C., Chen, W., Cai, P., Chen, C., and Huang, Q.: Organo–organic interactions dominantly drive soil organic carbon accrual, Glob. Change Biol., 30, e17147, https://doi.org/10.1111/gcb.17147, 2024.
Kleber, M., Sollins, P., and Sutton, R.: A conceptual model of organo-mineral interactions in soils: self-assembly of organic molecular fragments into zonal structures on mineral surfaces, Biogeochemistry, 85, 9–24, https://doi.org/10.1007/s10533-007-9103-5, 2007.
Knoblauch, C., Beer, C., Liebner, S., Grigoriev, M. N., and Pfeiffer, E.-M.: Methane production as key to the greenhouse gas budget of thawing permafrost, Nat. Clim. Change, 8, 309-312, https://doi.org/10.1038/s41558-018-0095-z, 2018.
Knoblauch, C., Beer, C., Sosnin, A., Wagner, D., and Pfeiffer, E.-M.: Predicting long-term carbon mineralization and trace gas production from thawing permafrost of Northeast Siberia, Glob. Change Biol., 19, 1160-1172, https://doi.org/10.1111/gcb.12116, 2013.
Knoblauch, C., Beer, C., Schuett, A., Sauerland, L., Liebner, S., Steinhof, A., Rethemeyer, J., Grigoriev, M. N., Faguet, A., and Pfeiffer, E.-M.: Carbon dioxide and methane release following abrupt thaw of Pleistocene permafrost deposits in Arctic Siberia, J. Geophys. Res.-Biogeo., 126, e2021JG006543, https://doi.org/10.1029/2021JG006543, 2021.
Knoblauch, C., Beer, C., and Voigt, C.: Dataset for the manuscript “Thawing Siberian permafrost stabilizes organic carbon from recent plant litter inputs” published in Biogeosciences (Copernicus Publications) 2026, Zenodo [data set], https://doi.org/10.5281/zenodo.20037052, 2026.
Köchy, M., Hiederer, R., and Freibauer, A.: Global distribution of soil organic carbon – Part 1: Masses and frequency distributions of SOC stocks for the tropics, permafrost regions, wetlands, and the world, SOIL, 1, 351–365, https://doi.org/10.5194/soil-1-351-2015, 2015.
Kögel-Knabner, I., Guggenberger, G., Kleber, M., Kandeler, E., Kalbitz, K., Scheu, S., Eusterhues, K., and Leinweber, P.: Organo-mineral associations in temperate soils: Integrating biology, mineralogy, and organic matter chemistry, J. Plant Nutr. Soil Sci., 171, 61–82, https://doi.org/10.1002/jpln.200700048, 2008.
Kuhry, P. and Vitt, D. H.: Fossil carbon/nitrogen ratios as a measure of peat decomposition, Ecology, 77, 271–275, https://doi.org/10.2307/2265676, 1996.
Kutzbach, L., Wagner, D., and Pfeiffer, E.-M.: Effect of microrelief and vegetation on methane emission from wet polygonal tundra, Lena Delta, Northern Siberia, Biogeochemistry, 69, 341–362, 2004.
LaRowe, D. E. and Van Cappellen, P.: Degradation of natural organic matter: A thermodynamic analysis, Geochim. Cosmochim. Ac., 75, 2030–2042, https://doi.org/10.1016/j.gca.2011.01.020, 2011.
Lashchinskiy, N. N., Kartoziia, A. A., and Faguet, A. N.: Permafrost degradation as a supporting factor for the biodiversity of tundra ecosystems, Contemp. Probl. Ecol., 13, 401–411, https://doi.org/10.1134/S1995425520040071, 2020.
Lewkowicz, A. G. and Way, R. G.: Extremes of summer climate trigger thousands of thermokarst landslides in a High Arctic environment, Nat. Commun., 10, 1329, https://doi.org/10.1038/s41467-019-09314-7, 2019.
Liebmann, P., Vogel, C., Kholodov, A., Bárta, J., Waqas, M., Varsadiya, M., Wang, H., Urich, T., Mansfeldt, T., Wessel-Bothe, S., Shibistova, O., and Guggenberger, G.: Perennial redox potential dynamics in Alaskan degraded and non-degraded permafrost soils, Communications Earth & Environment, 7, 120, https://doi.org/10.1038/s43247-025-03143-x, 2025.
Lim, A. G., Loiko, S. V., and Pokrovsky, O. S.: Sizable pool of labile organic carbon in peat and mineral soils of permafrost peatlands, western Siberia, Geoderma, 409, 115601, https://doi.org/10.1016/j.geoderma.2021.115601, 2022.
Lin, Y., Campbell, A. N., Bhattacharyya, A., DiDonato, N., Thompson, A. M., Tfaily, M. M., Nico, P. S., Silver, W. L., and Pett-Ridge, J.: Differential effects of redox conditions on the decomposition of litter and soil organic matter, Biogeochemistry, 154, 1–15, https://doi.org/10.1007/s10533-021-00790-y, 2021.
Louppe, G., Wehenkel, L., Sutera, A., and Geurts, P.: Understanding variable importances in forests of randomized trees, in: Advances in Neural Information Processing Systems, edited by: Burges, C. J., Bottou, L., Welling, M., Ghahramani, Z., and Weinberger, K. Q., Curran Associates, Inc., ISBN 978-1-632-66024-4, 2013.
Martens, J., Mueller, C. W., Joshi, P., Rosinger, C., Maisch, M., Kappler, A., Bonkowski, M., Schwamborn, G., Schirrmeister, L., and Rethemeyer, J.: Stabilization of mineral-associated organic carbon in Pleistocene permafrost, Nat. Commun., 14, 2120, https://doi.org/10.1038/s41467-023-37766-5, 2023.
Mikan, C. J., Schimel, J. P., and Doyle, A. P.: Temperature controls of microbial respiration in arctic tundra soils above and below freezing, Soil Biol. Biochem., 34, 1785–1795, 2002.
Monteux, S., Keuper, F., Fontaine, S., Gavazov, K., Hallin, S., Juhanson, J., Krab, E. J., Revaillot, S., Verbruggen, E., Walz, J., Weedon, J. T., and Dorrepaal, E.: Carbon and nitrogen cycling in Yedoma permafrost controlled by microbial functional limitations, Nat. Geosci., 13, 794–798, https://doi.org/10.1038/s41561-020-00662-4, 2020.
Mu, C. C., Abbott, B. W., Zhao, Q., Su, H., Wang, S. F., Wu, Q. B., Zhang, T. J., and Wu, X. D.: Permafrost collapse shifts alpine tundra to a carbon source but reduces N2O and CH4 release on the northern Qinghai-Tibetan Plateau, Geophys. Res. Lett., 44, 8945–8952, https://doi.org/10.1002/2017gl074338, 2017.
Mueller, C. W., Rethemeyer, J., Kao-Kniffin, J., Löppmann, S., Hinkel, K. M., and G. Bockheim, J.: Large amounts of labile organic carbon in permafrost soils of northern Alaska, Glob. Change Biol., 21, 2804–2817, https://doi.org/10.1111/gcb.12876, 2015.
Murphy, E. M., Zachara, J. M., and Smith, S. C.: Influence of mineral-bound humic substances on the sorption of hydrophobic organic compounds, Environ. Sci. Technol., 24, 1507–1516, https://doi.org/10.1021/es00080a009, 1990.
Natali, S. M., Schuur, E. A. G., and Rubin, R. L.: Increased plant productivity in Alaskan tundra as a result of experimental warming of soil and permafrost, J. Ecol., 100, 488–498, https://doi.org/10.1111/j.1365-2745.2011.01925.x, 2012.
Natali, S. M., Watts, J. D., Rogers, B. M., Potter, S., Ludwig, S. M., Selbmann, A.-K., Sullivan, P. F., Abbott, B. W., Arndt, K. A., Birch, L., Björkman, M. P., Bloom, A. A., Celis, G., Christensen, T. R., Christiansen, C. T., Commane, R., Cooper, E. J., Crill, P., Czimczik, C., Davydov, S., Du, J., Egan, J. E., Elberling, B., Euskirchen, E. S., Friborg, T., Genet, H., Göckede, M., Goodrich, J. P., Grogan, P., Helbig, M., Jafarov, E. E., Jastrow, J. D., Kalhori, A. A. M., Kim, Y., Kimball, J. S., Kutzbach, L., Lara, M. J., Larsen, K. S., Lee, B.-Y., Liu, Z., Loranty, M. M., Lund, M., Lupascu, M., Madani, N., Malhotra, A., Matamala, R., McFarland, J., McGuire, A. D., Michelsen, A., Minions, C., Oechel, W. C., Olefeldt, D., Parmentier, F.-J. W., Pirk, N., Poulter, B., Quinton, W., Rezanezhad, F., Risk, D., Sachs, T., Schaefer, K., Schmidt, N. M., Schuur, E. A. G., Semenchuk, P. R., Shaver, G., Sonnentag, O., Starr, G., Treat, C. C., Waldrop, M. P., Wang, Y., Welker, J., Wille, C., Xu, X., Zhang, Z., Zhuang, Q., and Zona, D.: Large loss of CO2 in winter observed across the northern permafrost region, Nat. Clim. Change, 9, 852–857, https://doi.org/10.1038/s41558-019-0592-8, 2019.
Obu, J., Westermann, S., Bartsch, A., Berdnikov, N., Christiansen, H. H., Dashtseren, A., Delaloye, R., Elberling, B., Etzelmüller, B., Kholodov, A., Khomutov, A., Kääb, A., Leibman, M. O., Lewkowicz, A. G., Panda, S. K., Romanovsky, V., Way, R. G., Westergaard-Nielsen, A., Wu, T., Yamkhin, J., and Zou, D.: Northern Hemisphere permafrost map based on TTOP modelling for 2000–2016 at 1 km2 scale, Earth-Sci. Rev., 193, 299–316, https://doi.org/10.1016/j.earscirev.2019.04.023, 2019.
Patzner, M. S., Mueller, C. W., Malusova, M., Baur, M., Nikeleit, V., Scholten, T., Hoeschen, C., Byrne, J. M., Borch, T., Kappler, A., and Bryce, C.: Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw, Nat. Commun., 11, 6329, https://doi.org/10.1038/s41467-020-20102-6, 2020.
Ping, C. L., Jastrow, J. D., Jorgenson, M. T., Michaelson, G. J., and Shur, Y. L.: Permafrost soils and carbon cycling, SOIL, 1, 147–171, https://doi.org/10.5194/soil-1-147-2015, 2015.
Possinger, A. R., Zachman, M. J., Enders, A., Levin, B. D. A., Muller, D. A., Kourkoutis, L. F., and Lehmann, J.: Organo–organic and organo–mineral interfaces in soil at the nanometer scale, Nat. Commun., 11, 6103, https://doi.org/10.1038/s41467-020-19792-9, 2020.
Prater, I., Zubrzycki, S., Buegger, F., Zoor-Füllgraff, L. C., Angst, G., Dannenmann, M., and Mueller, C. W.: From fibrous plant residues to mineral-associated organic carbon – the fate of organic matter in Arctic permafrost soils, Biogeosciences, 17, 3367–3383, https://doi.org/10.5194/bg-17-3367-2020, 2020.
Qin, S., Zhang, D., Wei, B., and Yang, Y.: Dual roles of microbes in mediating soil carbon dynamics in response to warming, Nat. Commun., 15, 6439, https://doi.org/10.1038/s41467-024-50800-4, 2024.
Qin, S., Kou, D., Mao, C., Chen, Y., Chen, L., and Yang, Y.: Temperature sensitivity of permafrost carbon release mediated by mineral and microbial properties, Sci. Adv., 7, eabe3596, https://doi.org/10.1126/sciadv.abe3596, 2021.
Rantanen, M., Karpechko, A. Y., Lipponen, A., Nordling, K., Hyvärinen, O., Ruosteenoja, K., Vihma, T., and Laaksonen, A.: The Arctic has warmed nearly four times faster than the globe since 1979, Communications Earth & Environment, 3, 168, https://doi.org/10.1038/s43247-022-00498-3, 2022.
Schädel, C., Schuur, E. A. G., Bracho, R., Elberling, B., Knoblauch, C., Lee, H., Luo, Y., Shaver, G. R., and Turetsky, M. R.: Circumpolar assessment of permafrost C quality and its vulnerability over time using long-term incubation data, Glob. Change Biol., 20, 641–652, https://doi.org/10.1111/gcb.12417, 2014.
Schädel, C., Bader, M. K. F., Schuur, E. A. G., Biasi, C., Bracho, R., Capek, P., De Baets, S., Diakova, K., Ernakovich, J., Estop-Aragones, C., Graham, D. E., Hartley, I. P., Iversen, C. M., Kane, E., Knoblauch, C., Lupascu, M., Martikainen, P. J., Natali, S. M., Norby, R. J., O'Donnell, J. A., Chowdhury, T. R., Santruckova, H., Shaver, G., Sloan, V. L., Treat, C. C., Turetsky, M. R., Waldrop, M. P., and Wickland, K. P.: Potential carbon emissions dominated by carbon dioxide from thawed permafrost soils, Nat. Clim. Change, 6, 950–953, https://doi.org/10.1038/nclimate3054, 2016.
Schmidt, M. W. I., Torn, M. S., Abiven, S., Dittmar, T., Guggenberger, G., Janssens, I. A., Kleber, M., Kögel-Knabner, I., Lehmann, J., Manning, D. A. C., Nannipieri, P., Rasse, D. P., Weiner, S., and Trumbore, S. E.: Persistence of soil organic matter as an ecosystem property, Nature, 478, 49–56, https://doi.org/10.1038/nature10386, 2011.
Schrumpf, M., Kaiser, K., Guggenberger, G., Persson, T., Kögel-Knabner, I., and Schulze, E.-D.: Storage and stability of organic carbon in soils as related to depth, occlusion within aggregates, and attachment to minerals, Biogeosciences, 10, 1675–1691, https://doi.org/10.5194/bg-10-1675-2013, 2013.
Singh, M., Sarkar, B., Sarkar, S., Churchman, J., Bolan, N., Mandal, S., Menon, M., Purakayastha, T. J., and Beerling, D. J.: Stabilization of soil organic carbon as influenced by clay mineralogy, in: Advances in Agronomy, edited by: Sparks, D. L., Academic Press, 33–84, https://doi.org/10.1016/bs.agron.2017.11.001, 2018.
Swanston, C. W., Torn, M. S., Hanson, P. J., Southon, J. R., Garten, C. T., Hanlon, E. M., and Ganio, L.: Initial characterization of processes of soil carbon stabilization using forest stand-level radiocarbon enrichment, Geoderma, 128, 52–62, https://doi.org/10.1016/j.geoderma.2004.12.015, 2005.
Torn, M. S., Kleber, M., Zavaleta, E. S., Zhu, B., Field, C. B., and Trumbore, S. E.: A dual isotope approach to isolate soil carbon pools of different turnover times, Biogeosciences, 10, 8067–8081, https://doi.org/10.5194/bg-10-8067-2013, 2013.
Tuomi, M., Thum, T., Jarvinen, H., Fronzek, S., Berg, B., Harmon, M., Trofymow, J. A., Sevanto, S., and Liski, J.: Leaf litter decomposition-Estimates of global variability based on Yasso07 model, Ecol. Model., 220, 3362–3371, https://doi.org/10.1016/j.ecolmodel.2009.05.016, 2009.
Turetsky, M. R., Abbott, B. W., Jones, M. C., Anthony, K. W., Olefeldt, D., Schuur, E. A. G., Grosse, G., Kuhry, P., Hugelius, G., Koven, C., Lawrence, D. M., Gibson, C., Sannel, A. B. K., and McGuire, A. D.: Carbon release through abrupt permafrost thaw, Nat. Geosci., 13, 138–143, https://doi.org/10.1038/s41561-019-0526-0, 2020.
van Everdingen, R. O.: Geocryological terminology, Can. J. Earth Sci., 13, 862–867, https://doi.org/10.1139/e76-089, 1976.
Virkkala, A.-M., Aalto, J., Rogers, B. M., Tagesson, T., Treat, C. C., Natali, S. M., Watts, J. D., Potter, S., Lehtonen, A., Mauritz, M., Schuur, E. A. G., Kochendorfer, J., Zona, D., Oechel, W., Kobayashi, H., Humphreys, E., Goeckede, M., Iwata, H., Lafleur, P. M., Euskirchen, E. S., Bokhorst, S., Marushchak, M., Martikainen, P. J., Elberling, B., Voigt, C., Biasi, C., Sonnentag, O., Parmentier, F.-J. W., Ueyama, M., Celis, G., St.Louis, V. L., Emmerton, C. A., Peichl, M., Chi, J., Järveoja, J., Nilsson, M. B., Oberbauer, S. F., Torn, M. S., Park, S.-J., Dolman, H., Mammarella, I., Chae, N., Poyatos, R., López-Blanco, E., Christensen, T. R., Kwon, M. J., Sachs, T., Holl, D., and Luoto, M.: Statistical upscaling of ecosystem CO2 fluxes across the terrestrial tundra and boreal domain: Regional patterns and uncertainties, Glob. Change Biol., 27, 4040–4059, https://doi.org/10.1111/gcb.15659, 2021.
Vogel, C., Mueller, C. W., Höschen, C., Buegger, F., Heister, K., Schulz, S., Schloter, M., and Kögel-Knabner, I.: Submicron structures provide preferential spots for carbon and nitrogen sequestration in soils, Nat. Commun., 5, 2947, https://doi.org/10.1038/ncomms3947, 2014.
Vonk, J. E., Mann, P. J., Davydov, S., Davydova, A., Spencer, R. G. M., Schade, J., Sobczak, W. V., Zimov, N., Zimov, S., Bulygina, E., Eglinton, T. I., and Holmes, R. M.: High biolability of ancient permafrost carbon upon thaw, Geophys. Res. Lett., 40, 2689–2693, https://doi.org/10.1002/grl.50348, 2013.
Vonk, J. E., Sanchez-Garcia, L., van Dongen, B. E., Alling, V., Kosmach, D., Charkin, A., Semiletov, I. P., Dudarev, O. V., Shakhova, N., Roos, P., Eglinton, T. I., Andersson, A., and Gustafsson, O.: Activation of old carbon by erosion of coastal and subsea permafrost in Arctic Siberia, Nature, 489, 137–140, https://doi.org/10.1038/nature11392, 2012.
Waldrop, M. P., Wickland, K. P., White III, R., Berhe, A. A., Harden, J. W., and Romanovsky, V. E.: Molecular investigations into a globally important carbon pool: permafrost-protected carbon in Alaskan soils, Glob. Change Biol., 16, 2543–2554, https://doi.org/10.1111/j.1365-2486.2009.02141.x, 2010.
Walz, J., Knoblauch, C., Böhme, L., and Pfeiffer, E.-M.: Regulation of soil organic matter decomposition in permafrost-affected Siberian tundra soils - Impact of oxygen availability, freezing and thawing, temperature, and labile organic matter, Soil Biol. Biochem., 110, 34–43, https://doi.org/10.1016/j.soilbio.2017.03.001, 2017.
Wang, X., Wang, C., Cotrufo, M. F., Sun, L., Jiang, P., Liu, Z., and Bai, E.: Elevated temperature increases the accumulation of microbial necromass nitrogen in soil via increasing microbial turnover, Glob. Change Biol., 26, 5277–5289, https://doi.org/10.1111/gcb.15206, 2020.
Wickland, K. P., Jorgenson, M. T., Koch, J. C., Kanevskiy, M., and Striegl, R. G.: Carbon dioxide and methane flux in a dynamic Arctic tundra landscape: Decadal-scale impacts of ice wedge degradation and stabilization, Geophys. Res. Lett., 47, e2020GL089894, https://doi.org/10.1029/2020GL089894, 2020.
Xu, C., Guo, L., Dou, F., and Ping, C.-L.: Potential DOC production from size-fractionated Arctic tundra soils, Cold Reg. Sci. Technol., 55, 141–150, https://doi.org/10.1016/j.coldregions.2008.08.001, 2009.
Zhang, T., Heginbottom, J. A., Barry, R. G., and Brown, J.: Further statistics on the distribution of permafrost and ground ice in the Northern Hemisphere, Polar Geogr., 24, 126–131, https://doi.org/10.1080/10889370009377692, 2000.
Short summary
Carbon release from thawing permafrost receives ample attention since it may cause rising greenhouse gas concentrations in the atmosphere. However, we demonstrate through a 9-year lasting incubation experiment that thawing permafrost stabilizes a substantial amount of fresh plant litter carbon from increasing plant productivity for decades. Although litter carbon is faster decomposed than the permafrost carbon it may contribute to the build-up of organic carbon in thawing permafrost soils.
Carbon release from thawing permafrost receives ample attention since it may cause rising...
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