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.
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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Latest update: 22 Nov 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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