Articles | Volume 3, issue 1
SOIL, 3, 17–30, 2017
SOIL, 3, 17–30, 2017

Original research article 05 Jan 2017

Original research article | 05 Jan 2017

Timescales of carbon turnover in soils with mixed crystalline mineralogies

Lesego Khomo 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: Reconsider after major revisions (19 Aug 2016) by Karolien Denef
AR by Susan Trumbore on behalf of the Authors (20 Oct 2016)  Author's response    Manuscript
ED: Publish as is (18 Nov 2016) by Karolien Denef
ED: Publish subject to technical corrections (27 Nov 2016) by Johan Six(Executive Editor)
AR by Susan Trumbore on behalf of the Authors (09 Dec 2016)  Author's response    Manuscript
Short summary
We evaluated mineral control of organic carbon dynamics by relating the content and age of carbon stored in soils of varied mineralogical composition found in the landscapes of Kruger National Park, South Africa. Carbon associated with smectite clay minerals, which have stronger surface–organic matter interactions, averaged about a thousand years old, while most soil carbon was only decades to centuries old and was associated with iron and aluminum oxide minerals.