Articles | Volume 13, issue 8
https://doi.org/10.5194/bg-13-2493-2016
https://doi.org/10.5194/bg-13-2493-2016
Research article
 | 
28 Apr 2016
Research article |  | 28 Apr 2016

What is the P value of Siberian soils? Soil phosphorus status in south-western Siberia and comparison with a global data set

Félix Brédoire, Mark R. Bakker, Laurent Augusto, Pavel A. Barsukov, Delphine Derrien, Polina Nikitich, Olga Rusalimova, Bernd Zeller, and David L. Achat

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (14 Mar 2016) by Yakov Kuzyakov
AR by Félix Brédoire on behalf of the Authors (14 Apr 2016)  Author's response    Manuscript
ED: Publish as is (15 Apr 2016) by Yakov Kuzyakov
Download
Short summary
We assessed soil phosphorus (P) status in aspen forests and grasslands in SW Siberia. Results show rather limited variation across sites. Relative to a global database, total, organic and inorganic P levels in SW Siberia were relatively high. Plant-available P levels had intermediate levels in topsoils, but large amounts of plant-available P are stored in subsurface layers down to 1 m. Overall, P resources do not seem to constrain current and future vegetation production.
Altmetrics
Final-revised paper
Preprint