Articles | Volume 17, issue 6
https://doi.org/10.5194/bg-17-1507-2020
https://doi.org/10.5194/bg-17-1507-2020
Reviews and syntheses
 | 
25 Mar 2020
Reviews and syntheses |  | 25 Mar 2020

Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale

Roger D. Finlay, Shahid Mahmood, Nicholas Rosenstock, Emile B. Bolou-Bi, Stephan J. Köhler, Zaenab Fahad, Anna Rosling, Håkan Wallander, Salim Belyazid, Kevin Bishop, and Bin Lian

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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 (18 Jun 2019) by Suzanne Anderson
AR by Roger Finlay on behalf of the Authors (19 Sep 2019)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (20 Oct 2019) by Suzanne Anderson
AR by Roger Finlay on behalf of the Authors (03 Nov 2019)  Author's response    Manuscript
ED: Publish as is (16 Nov 2019) by Suzanne Anderson
AR by Roger Finlay on behalf of the Authors (17 Nov 2019)  Author's response    Manuscript
ED: Reconsider after major revisions (11 Dec 2019) by Nobuhito Ohte
AR by Roger Finlay on behalf of the Authors (12 Jan 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (17 Jan 2020) by Nobuhito Ohte
RR by Anonymous Referee #1 (21 Jan 2020)
ED: Publish subject to minor revisions (review by editor) (02 Feb 2020) by Nobuhito Ohte
AR by Roger Finlay on behalf of the Authors (16 Feb 2020)  Author's response
ED: Publish as is (20 Feb 2020) by Nobuhito Ohte
AR by Roger Finlay on behalf of the Authors (21 Feb 2020)  Author's response    Manuscript
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Short summary
Effects of biological activity on mineral weathering operate at scales ranging from short-term, microscopic interactions to global, evolutionary timescale processes. Microorganisms have had well-documented effects at large spatio-temporal scales, but to establish the quantitative significance of microscopic measurements for field-scale processes, higher-resolution studies of liquid chemistry at local weathering sites and improved upscaling to soil-scale dissolution rates are still required.
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