Articles | Volume 15, issue 11
Research article
08 Jun 2018
Research article |  | 08 Jun 2018

A new look at the multi-G model for organic carbon degradation in surface marine sediments for coupled benthic–pelagic simulations of the global ocean

Konstantin Stolpovsky, Andrew W. Dale, and Klaus Wallmann


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 (16 Feb 2018) by Caroline P. Slomp
AR by Konstantin Stolpovsky on behalf of the Authors (29 Mar 2018)  Author's response    Manuscript
ED: Publish as is (11 Apr 2018) by Caroline P. Slomp

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Konstantin Stolpovsky on behalf of the Authors (31 May 2018)   Author's adjustment  
EA: Adjustments approved (01 Jun 2018) by Caroline P. Slomp
Short summary
The paper describes a new way to parameterize G-type models in marine sediments using data about reactivity of organic carbon sinking to the seafloor.
Final-revised paper