Articles | Volume 15, issue 1
https://doi.org/10.5194/bg-15-13-2018
https://doi.org/10.5194/bg-15-13-2018
Research article
 | 
03 Jan 2018
Research article |  | 03 Jan 2018

Organic matter dynamics along a salinity gradient in Siberian steppe soils

Norbert Bischoff, Robert Mikutta, Olga Shibistova, Reiner Dohrmann, Daniel Herdtle, Lukas Gerhard, Franziska Fritzsche, Alexander Puzanov, Marina Silanteva, Anna Grebennikova, and Georg Guggenberger

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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: Reconsider after major revisions (14 Jun 2017) by Jens-Arne Subke
AR by Norbert Bischoff on behalf of the Authors (20 Aug 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (21 Aug 2017) by Jens-Arne Subke
RR by Anonymous Referee #1 (18 Sep 2017)
ED: Publish subject to minor revisions (Editor review) (02 Oct 2017) by Jens-Arne Subke
AR by Norbert Bischoff on behalf of the Authors (15 Oct 2017)  Author's response   Manuscript 
ED: Publish subject to technical corrections (25 Oct 2017) by Jens-Arne Subke
AR by Norbert Bischoff on behalf of the Authors (31 Oct 2017)  Manuscript 
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Short summary
This study suggests that soil moisture significantly affects soil organic matter dynamics along a salinity gradient in semiarid steppe soils. The covarying moisture gradient along the salinity gradient serves as an explanatory factor for (i) the increasing soil organic carbon (OC) stocks with increasing salinity, (ii) the constant proportion and stability of particulate OC along the transect, and (iii) a similar fungi : bacteria ratio in the topsoils along the studied gradient.
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