Plant-derived compounds stimulate the decomposition of organic matter in arctic permafrost soils

Arctic ecosystems are warming rapidly, which is expected to promote soil organic matter (SOM) decomposition. In addition to the direct warming effect, decomposition can also be indirectly stimulated via increased plant productivity and plant-soil C allocation, and this so called "priming effect...

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Bibliographic Details
Main Authors: Wild, Birgit, Gentsch, Norman, Capek, Petr, Diakova, Katerina, Alves, Ricardo J. Eloy, Barta, Jiri, Gittel, Antje, Hugelius, Gustaf, Knoltsch, Anna, Kuhry, Peter, Lashchinskiy, Nikolay, Mikutta, Robert, Palmtag, Juri, Schleper, Christa, Schnecker, Jörg, Shibistova, Olga, Takriti, Mounir, Torsvik, Vigdis L., Urich, Tim, Watzka, Margarete, Santruckova, Hana, Guggenberger, Georg, Richter, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: London : Macmillan Publishers Limited 2016
Subjects:
Soil Organic Matter
Soil Organic Carbon Mineralization
SOC
SOM
ddc:500
Arctic
Global warming
permafrost
Online Access:http://www.repo.uni-hannover.de/handle/123456789/497
https://doi.org/10.15488/473
Description
Summary:Arctic ecosystems are warming rapidly, which is expected to promote soil organic matter (SOM) decomposition. In addition to the direct warming effect, decomposition can also be indirectly stimulated via increased plant productivity and plant-soil C allocation, and this so called "priming effect" might significantly alter the ecosystem C balance. In this study, we provide first mechanistic insights into the susceptibility of SOM decomposition in arctic permafrost soils to priming. By comparing 119 soils from four locations across the Siberian Arctic that cover all horizons of active layer and upper permafrost, we found that an increased availability of plant-derived organic C particularly stimulated decomposition in subsoil horizons where most of the arctic soil carbon is located. Considering the 1,035 Pg of arctic soil carbon, such an additional stimulation of decomposition beyond the direct temperature effect can accelerate net ecosystem C losses, and amplify the positive feedback to global warming. Austrian Science Fund (FWF)/I370-B17 BMBF/03F0616A Czech Ministry of Education, Youth and Sports/MSM 7E10073 Russian Ministry of Education and Science /14.B25.31.0031 Swedish Research Council/824-2009-77357 Norwegian Research Fund (NFR)/NFR-200411

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