Articles | Volume 6, issue 2
SOIL, 6, 435–451, 2020
SOIL, 6, 435–451, 2020

Original research article 29 Sep 2020

Original research article | 29 Sep 2020

Land-use perturbations in ley grassland decouple the degradation of ancient soil organic matter from the storage of newly derived carbon inputs

Marco Panettieri 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 (31 May 2020) by Boris Jansen
AR by Anna Wenzel on behalf of the Authors (15 Jun 2020)  Author's response
ED: Referee Nomination & Report Request started (26 Jun 2020) by Boris Jansen
RR by Anonymous Referee #1 (02 Jul 2020)
ED: Publish subject to minor revisions (review by editor) (27 Jul 2020) by Boris Jansen
AR by Abad Chabbi on behalf of the Authors (03 Aug 2020)  Author's response    Manuscript
ED: Publish as is (05 Aug 2020) by Boris Jansen
ED: Publish as is (05 Aug 2020) by Jorge Mataix-Solera(Executive Editor)
Short summary
In the context of global change, soil has been identified as a potential C sink, depending on land-use strategies. This work is devoted to identifying the processes affecting labile soil C pools resulting from changes in land use. We show that the land-use change in ley grassland provoked a decoupling of the storage and degradation processes after the grassland phase. Overall, the study enables us to develop a sufficient understanding of fine-scale C dynamics to refine soil C prediction models.