Articles | Volume 6, issue 1
SOIL, 6, 195–213, 2020
SOIL, 6, 195–213, 2020

Original research article 15 May 2020

Original research article | 15 May 2020

Boreal-forest soil chemistry drives soil organic carbon bioreactivity along a 314-year fire chronosequence

Benjamin Andrieux et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Revision (18 Mar 2020) by Stefan Doerr
AR by Benjamin Andrieux on behalf of the Authors (27 Mar 2020)  Author's response    Manuscript
ED: Publish as is (14 Apr 2020) by Stefan Doerr
ED: Publish as is (14 Apr 2020) by Jorge Mataix-Solera(Executive Editor)
Short summary
Our study aimed to disentangle the contribution of several drivers to explaining the proportion of soil carbon that can be released to CO2 through microbial respiration. We found that boreal-forest soil chemistry is an important driver of the amount of carbon that microbes can process. Our results emphasize the need to include the effects of soil chemistry into models of carbon cycling to better anticipate the role played by boreal-forest soils in carbon-cycle–climate feedbacks.