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Biogeosciences An interactive open-access journal of the European Geosciences Union
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BG | Articles | Volume 17, issue 13
Biogeosciences, 17, 3367–3383, 2020
https://doi.org/10.5194/bg-17-3367-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 17, 3367–3383, 2020
https://doi.org/10.5194/bg-17-3367-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 03 Jul 2020

Research article | 03 Jul 2020

From fibrous plant residues to mineral-associated organic carbon – the fate of organic matter in Arctic permafrost soils

Isabel Prater et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (06 May 2020) by Yakov Kuzyakov
AR by Isabel Prater on behalf of the Authors (08 May 2020)  Author's response    Manuscript
ED: Publish as is (25 May 2020) by Yakov Kuzyakov
Publications Copernicus
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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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