Articles | Volume 17, issue 13
https://doi.org/10.5194/bg-17-3367-2020
© Author(s) 2020. 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-17-3367-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
03 Jul 2020
Research article |
| 03 Jul 2020
| 03 Jul 2020
From fibrous plant residues to mineral-associated organic carbon – the fate of organic matter in Arctic permafrost soils
Soil Science, Research Department Ecology and Ecosystem Management, Technical University of Munich, 85354 Freising, Germany
Sebastian Zubrzycki
Center for Earth System Research and
Sustainability, School of Integrated Climate and Earth System Sciences, Universität Hamburg, 20146 Hamburg,
Germany
Franz Buegger
Institute of Biochemical Plant Pathology, Helmholtz Zentrum München GmbH, German Research Center for Environmental Health, 85764 Neuherberg, Germany
Lena C. Zoor-Füllgraff
Soil Science, Research Department Ecology and Ecosystem Management, Technical University of Munich, 85354 Freising, Germany
Gerrit Angst
Institute of Soil Biology and SoWa Research Infrastructure, Biology Centre, Czech Academy of Sciences, 370 05 České
Budějovice, Czech Republic
Michael Dannenmann
Institute of Meteorology and Climate Research Atmospheric Environmental Research (IMK-IFU), Karlsruhe Institute of Technology, 82467 Garmisch-Partenkirchen, Germany
Carsten W. Mueller
Soil Science, Research Department Ecology and Ecosystem Management, Technical University of Munich, 85354 Freising, Germany
Department of Geosciences and Natural
Resource Management, University of Copenhagen, Øster Voldgade 10, 1350
Copenhagen K, Denmark
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- Macrofauna amplify plant litter decomposition and stabilization in arctic soils in a warming climate V. Jílková et al. 10.1016/j.soilbio.2023.109245
- Vegetal Undercurrents—Obscured Riverine Dynamics of Plant Debris M. Schwab et al. 10.1029/2021JG006726
- Connecting soils to life in conservation planning, nutrient cycling, and planetary science R. Lybrand 10.1016/j.earscirev.2022.104247
- Hydrological Regime and Plant Functional Traits Jointly Mediate the Influence of Salix spp. on Soil Organic Carbon Stocks in a High Arctic Tundra L. Lamarque et al. 10.1007/s10021-023-00829-1
- Chronological changes in soil biogeochemical properties of the glacier foreland of Midtre Lovénbreen, Svalbard, attributed to soil-forming factors Y. Kim et al. 10.1016/j.geoderma.2022.115777
- Vertical pattern of organic matter decomposability in cryoturbated permafrost-affected soils C. Beer et al. 10.1088/1748-9326/ac9198
- Seabirds enrich Antarctic soil with trace metals in organic fractions M. Castro et al. 10.1016/j.scitotenv.2021.147271
- Natural revegetation over ∼ 160 years alters carbon and nitrogen sequestration and stabilization in soil organic matter on the Loess Plateau of China W. Yang et al. 10.1016/j.catena.2022.106647
- Dominance of particulate organic carbon in top mineral soils in cold regions P. García-Palacios et al. 10.1038/s41561-023-01354-5
- Particulate organic matter as a functional soil component for persistent soil organic carbon K. Witzgall et al. 10.1038/s41467-021-24192-8
- Unlocking complex soil systems as carbon sinks: multi-pool management as the key G. Angst et al. 10.1038/s41467-023-38700-5
- Alder-induced stimulation of soil gross nitrogen turnover in a permafrost-affected peatland of Northeast China E. Ramm et al. 10.1016/j.soilbio.2022.108757
- Soil Particulate and Mineral-Associated Organic Matter Increases in Organic Farming under Cover Cropping and Manure Addition K. Kauer et al. 10.3390/agriculture11090903
- Stabilization of mineral-associated organic carbon in Pleistocene permafrost J. Martens et al. 10.1038/s41467-023-37766-5
- Interrelationships among mountain relief, surface organic layer, soil organic carbon, and its mineral association under subarctic forest tundra V. Pichler et al. 10.1038/s41598-022-21521-9
- Microbial iron cycling during palsa hillslope collapse promotes greenhouse gas emissions before complete permafrost thaw M. Patzner et al. 10.1038/s43247-022-00407-8
- Probing the nature of soil organic matter Z. Weng et al. 10.1080/10643389.2021.1980346
- Application of Organic and Inorganic Fertilizers Affects the Growth and Biomass Semanggi (Marsilea crenata Presl.) M. Tripatmasari et al. 10.46300/91011.2021.15.19
- Microbial communities in soil macro-aggregates with less connected networks respire less across successional and geographic gradients D. Sun et al. 10.1016/j.ejsobi.2021.103378
- Lignin Preservation and Microbial Carbohydrate Metabolism in Permafrost Soils T. Dao et al. 10.1029/2020JG006181
- Global patterns of geo-ecological controls on the response of soil respiration to warming D. Haaf et al. 10.1038/s41558-021-01068-9
- Sizable pool of labile organic carbon in peat and mineral soils of permafrost peatlands, western Siberia A. Lim et al. 10.1016/j.geoderma.2021.115601
- Features of Organic Matter Transformation in the Active Layer of Permafrost in the Bureya River Basin L. Kondratyeva et al. 10.1134/S1995425523030083
- Cross-shelf processes of terrigenous organic matter drive mercury speciation on the east siberian shelf in the Arctic Ocean J. Kim et al. 10.1016/j.envpol.2023.123270
- Size, shape, and stability of organic particles formed during freeze–thaw cycles: Model experiments with tannic acid S. Dultz et al. 10.1016/j.jcis.2024.04.080
- River Organic Carbon Fluxes Modulated by Hydrodynamic Sorting of Particulate Organic Matter M. Repasch et al. 10.1029/2021GL096343
- Cryoturbation impacts iron-organic carbon associations along a permafrost soil chronosequence in northern Alaska H. Joss et al. 10.1016/j.geoderma.2022.115738
25 citations as recorded by crossref.
- Macrofauna amplify plant litter decomposition and stabilization in arctic soils in a warming climate V. Jílková et al. 10.1016/j.soilbio.2023.109245
- Vegetal Undercurrents—Obscured Riverine Dynamics of Plant Debris M. Schwab et al. 10.1029/2021JG006726
- Connecting soils to life in conservation planning, nutrient cycling, and planetary science R. Lybrand 10.1016/j.earscirev.2022.104247
- Hydrological Regime and Plant Functional Traits Jointly Mediate the Influence of Salix spp. on Soil Organic Carbon Stocks in a High Arctic Tundra L. Lamarque et al. 10.1007/s10021-023-00829-1
- Chronological changes in soil biogeochemical properties of the glacier foreland of Midtre Lovénbreen, Svalbard, attributed to soil-forming factors Y. Kim et al. 10.1016/j.geoderma.2022.115777
- Vertical pattern of organic matter decomposability in cryoturbated permafrost-affected soils C. Beer et al. 10.1088/1748-9326/ac9198
- Seabirds enrich Antarctic soil with trace metals in organic fractions M. Castro et al. 10.1016/j.scitotenv.2021.147271
- Natural revegetation over ∼ 160 years alters carbon and nitrogen sequestration and stabilization in soil organic matter on the Loess Plateau of China W. Yang et al. 10.1016/j.catena.2022.106647
- Dominance of particulate organic carbon in top mineral soils in cold regions P. García-Palacios et al. 10.1038/s41561-023-01354-5
- Particulate organic matter as a functional soil component for persistent soil organic carbon K. Witzgall et al. 10.1038/s41467-021-24192-8
- Unlocking complex soil systems as carbon sinks: multi-pool management as the key G. Angst et al. 10.1038/s41467-023-38700-5
- Alder-induced stimulation of soil gross nitrogen turnover in a permafrost-affected peatland of Northeast China E. Ramm et al. 10.1016/j.soilbio.2022.108757
- Soil Particulate and Mineral-Associated Organic Matter Increases in Organic Farming under Cover Cropping and Manure Addition K. Kauer et al. 10.3390/agriculture11090903
- Stabilization of mineral-associated organic carbon in Pleistocene permafrost J. Martens et al. 10.1038/s41467-023-37766-5
- Interrelationships among mountain relief, surface organic layer, soil organic carbon, and its mineral association under subarctic forest tundra V. Pichler et al. 10.1038/s41598-022-21521-9
- Microbial iron cycling during palsa hillslope collapse promotes greenhouse gas emissions before complete permafrost thaw M. Patzner et al. 10.1038/s43247-022-00407-8
- Probing the nature of soil organic matter Z. Weng et al. 10.1080/10643389.2021.1980346
- Application of Organic and Inorganic Fertilizers Affects the Growth and Biomass Semanggi (Marsilea crenata Presl.) M. Tripatmasari et al. 10.46300/91011.2021.15.19
- Microbial communities in soil macro-aggregates with less connected networks respire less across successional and geographic gradients D. Sun et al. 10.1016/j.ejsobi.2021.103378
- Lignin Preservation and Microbial Carbohydrate Metabolism in Permafrost Soils T. Dao et al. 10.1029/2020JG006181
- Global patterns of geo-ecological controls on the response of soil respiration to warming D. Haaf et al. 10.1038/s41558-021-01068-9
- Sizable pool of labile organic carbon in peat and mineral soils of permafrost peatlands, western Siberia A. Lim et al. 10.1016/j.geoderma.2021.115601
- Features of Organic Matter Transformation in the Active Layer of Permafrost in the Bureya River Basin L. Kondratyeva et al. 10.1134/S1995425523030083
- Cross-shelf processes of terrigenous organic matter drive mercury speciation on the east siberian shelf in the Arctic Ocean J. Kim et al. 10.1016/j.envpol.2023.123270
- Size, shape, and stability of organic particles formed during freeze–thaw cycles: Model experiments with tannic acid S. Dultz et al. 10.1016/j.jcis.2024.04.080
2 citations as recorded by crossref.
Latest update: 24 Apr 2024
Short summary
Large amounts of soil organic matter stored in permafrost-affected soils from Arctic Russia are present as undecomposed plant residues. This large fibrous organic matter might be highly vulnerable to microbial decay, while small mineral-associated organic matter can most probably attenuate carbon mineralization in a warmer future. Labile soil fractions also store large amounts of nitrogen, which might be lost during permafrost collapse while fostering the decomposition of soil organic matter.
Large amounts of soil organic matter stored in permafrost-affected soils from Arctic Russia are...
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