Articles | Volume 14, issue 20
Biogeosciences, 14, 4637–4662, 2017
Biogeosciences, 14, 4637–4662, 2017

Research article 20 Oct 2017

Research article | 20 Oct 2017

The acceleration of dissolved cobalt's ecological stoichiometry due to biological uptake, remineralization, and scavenging in the Atlantic Ocean

Mak A. Saito 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: Publish subject to minor revisions (Editor review) (08 Jun 2017) by Gerhard Herndl
AR by Mak Saito on behalf of the Authors (01 Aug 2017)  Author's response    Manuscript
ED: Publish as is (28 Aug 2017) by Gerhard Herndl

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Short summary
Cobalt has the smallest oceanic inventory of all known inorganic micronutrients, and hence is particularly vulnerable to influence by internal oceanic processes. The stoichiometry of cobalt was studied in the North Atlantic, and interpreted with regard to the context of Redfield theory with a focus on biological uptake, scavenging, and the coupling between dissolved and particulate phases. The stoichiometry of cobalt accelerated towards the surface due to increased biological activity and use.
Final-revised paper