Articles | Volume 12, issue 23
https://doi.org/10.5194/bg-12-6915-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/bg-12-6915-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Biodegradability of dissolved organic carbon in permafrost soils and aquatic systems: a meta-analysis
J. E. Vonk
CORRESPONDING AUTHOR
Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
Arctic Center, University of Groningen, Groningen, the Netherlands
S. E. Tank
Department of Biological Sciences, University of Alberta, Edmonton, Canada
P. J. Mann
Department of Geography, Northumbria University, Newcastle Upon Tyne, UK
R. G. M. Spencer
Department of Earth, Ocean & Atmospheric Science, Florida State University, Tallahassee, USA
C. C. Treat
Earth Systems Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, USA
R. G. Striegl
National Research Program, US Geological Survey, Boulder, Colorado, USA
B. W. Abbott
OSUR-UMR 6553 ECOBIO, Université de Rennes and Centre National de la Recherche Scientifique, Rennes, France
K. P. Wickland
National Research Program, US Geological Survey, Boulder, Colorado, USA
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Short summary
We found that dissolved organic carbon (DOC) in arctic soils and aquatic systems is increasingly degradable with increasing permafrost extent. Also, DOC seems less degradable when moving down the fluvial network in continuous permafrost regions, i.e. from streams to large rivers, suggesting that highly bioavailable DOC is lost in headwater streams. We also recommend a standardized DOC incubation protocol to facilitate future comparison on processing and transport of DOC in a changing Arctic.
We found that dissolved organic carbon (DOC) in arctic soils and aquatic systems is increasingly...
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