Articles | Volume 13, issue 4
https://doi.org/10.5194/bg-13-1269-2016
https://doi.org/10.5194/bg-13-1269-2016
Research article
 | 
01 Mar 2016
Research article |  | 01 Mar 2016

Unambiguous evidence of old soil carbon in grass biosilica particles

Paul E. Reyerson, Anne Alexandre, Araks Harutyunyan, Remi Corbineau, Hector A. Martinez De La Torre, Franz Badeck, Luigi Cattivelli, and Guaciara M. Santos

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ED: Publish subject to minor revisions (Editor review) (08 Jan 2016) by Roland Bol
AR by Guaciara Santos on behalf of the Authors (27 Jan 2016)  Author's response   Manuscript 
ED: Publish as is (08 Feb 2016) by Roland Bol
AR by Guaciara Santos on behalf of the Authors (10 Feb 2016)  Manuscript 
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Short summary
We characterize the origin of carbon (C) in phytoliths (biosilica of higher plants) by a multi-isotope approach. We show that phytoliths occlude soil organic C adsorbed through the roots, making them unsuitable for paleo-proxy studies, 14C dating or atmospheric CO2 sequestration. Our findings are in parallel with recent soil paradigm shifts showing that soil microbes access old C and therefore call for further investigations on the role of old C in root–plant interactions and biomineralization.
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