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

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

doi:https://doi.org/10.5194/bg-13-2493-2016

Articles | Volume 13, issue 8

https://doi.org/10.5194/bg-13-2493-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/bg-13-2493-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 13, issue 8

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

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Final revised paper (published on 28 Apr 2016)
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Preprint (discussion started on 11 Dec 2015)
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Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC C8499: 'minor revisions recomendeed', Anonymous Referee #1, 15 Dec 2015
RC C8931: 'P stocks and P bio-availability in Siberian soils', Anonymous Referee #3, 08 Jan 2016
AC C10142: 'Author comments', Félix Brédoire, 11 Mar 2016

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

AR by Félix Brédoire on behalf of the Authors (15 Apr 2016)

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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.