Articles | Volume 19, issue 1
https://doi.org/10.5194/os-19-1-2023
https://doi.org/10.5194/os-19-1-2023
Research article
 | 
11 Jan 2023
Research article |  | 11 Jan 2023

Dimethyl sulfide cycling in the sea surface microlayer in the southwestern Pacific – Part 1: Enrichment potential determined using a novel sampler

Alexia D. Saint-Macary, Andrew Marriner, Theresa Barthelmeß, Stacy Deppeler, Karl Safi, Rafael Costa Santana, Mike Harvey, and Cliff S. Law

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-499', Anonymous Referee #1, 22 Jul 2022
  • RC2: 'Comment on egusphere-2022-499', Anonymous Referee #2, 29 Jul 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Alexia Saint-Macary on behalf of the Authors (25 Aug 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (01 Sep 2022) by Mario Hoppema
RR by Anonymous Referee #2 (06 Oct 2022)
ED: Reconsider after major revisions (17 Oct 2022) by Mario Hoppema
AR by Alexia Saint-Macary on behalf of the Authors (21 Oct 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Oct 2022) by Mario Hoppema
RR by Anonymous Referee #2 (24 Oct 2022)
ED: Publish subject to technical corrections (18 Nov 2022) by Mario Hoppema
AR by Alexia Saint-Macary on behalf of the Authors (23 Nov 2022)  Manuscript 
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Short summary
The uppermost oceanic layer was sampled to determine what can explain a potential dimethyl sulfide (DMS) enrichment in this environment. A novel sampling method was used, and the results showed that DMS was not as enriched as expected. Our results showed that the phytoplanktonic composition influenced the DMS concentration, confirming results from another study in this oceanic region. However, additional factors are required to observe a DMS enrichment in the uppermost oceanic layer.