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BG | Articles | Volume 17, issue 13
Biogeosciences, 17, 3685–3704, 2020
https://doi.org/10.5194/bg-17-3685-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Ocean deoxygenation: drivers and consequences – past, present...

Biogeosciences, 17, 3685–3704, 2020
https://doi.org/10.5194/bg-17-3685-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 15 Jul 2020

Research article | 15 Jul 2020

The control of hydrogen sulfide on benthic iron and cadmium fluxes in the oxygen minimum zone off Peru

Anna Plass et al.

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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 Feb 2020) by S. Wajih A. Naqvi
ED: Reconsider after major revisions (18 Feb 2020) by Marilaure Grégoire(Co-Editor-in-Chief)
AR by Anna Plass on behalf of the Authors (27 Feb 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (04 Mar 2020) by S. Wajih A. Naqvi
RR by Edouard Metzger (20 Mar 2020)
ED: Reconsider after major revisions (23 Mar 2020) by S. Wajih A. Naqvi
ED: Reconsider after major revisions (23 Mar 2020) by Katja Fennel(Co-Editor-in-Chief)
AR by Anna Plass on behalf of the Authors (01 Apr 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (11 Apr 2020) by S. Wajih A. Naqvi
RR by Anonymous Referee #2 (19 May 2020)
ED: Publish subject to minor revisions (review by editor) (22 May 2020) by S. Wajih A. Naqvi
ED: Publish subject to minor revisions (review by editor) (26 May 2020) by Marilaure Grégoire(Co-Editor-in-Chief)
AR by Anna Plass on behalf of the Authors (26 May 2020)  Author's response    Manuscript
ED: Publish as is (05 Jun 2020) by S. Wajih A. Naqvi
ED: Publish as is (09 Jun 2020) by Marilaure Grégoire(Co-Editor-in-Chief)
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Short summary
We compare the cycling of Fe and Cd in sulfidic sediments of the Peruvian oxygen minimum zone. Due to the contrasting solubility of their sulfide minerals, the sedimentary Fe release and Cd burial fluxes covary with spatial and temporal distributions of H2S. Depending on the solubility of their sulfide minerals, sedimentary trace metal fluxes will respond differently to ocean deoxygenation/expansion of H2S concentrations, which may change trace metal stoichiometry of upwelling water masses.
We compare the cycling of Fe and Cd in sulfidic sediments of the Peruvian oxygen minimum zone....
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