Articles | Volume 22, issue 20
https://doi.org/10.5194/bg-22-5943-2025
https://doi.org/10.5194/bg-22-5943-2025
Research article
 | 
23 Oct 2025
Research article |  | 23 Oct 2025

Nitrogen dynamics and nitrate stable isotopes indicate nitrogen loss in the Bay of Bengal

Gesa Schulz, Kirstin Dähnke, Tina Sanders, Jan Penopp, Hermann W. Bange, Rena Czeschel, and Birgit Gaye

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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-2025-1660', Anonymous Referee #1, 25 May 2025
    • AC1: 'Reply on RC1', Gesa Schulz, 02 Jul 2025
  • RC2: 'Comment on egusphere-2025-1660', Anonymous Referee #2, 13 Jun 2025
    • AC2: 'Reply on RC2', Gesa Schulz, 02 Jul 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (03 Jul 2025) by Tina Treude
AR by Gesa Schulz on behalf of the Authors (11 Jul 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (11 Jul 2025) by Tina Treude
AR by Gesa Schulz on behalf of the Authors (11 Jul 2025)  Author's response   Manuscript 
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Short summary
Oxygen-minimum zones (OMZs) are low-oxygen ocean areas that deplete nitrogen, a key marine nutrient. Understanding nitrogen cycling in OMZs is crucial for the global nitrogen cycle. This study examined nitrogen cycling in the OMZ of the Bay of Bengal and the East Equatorial Indian Ocean, revealing limited mixing between both regions. Surface phytoplankton consumes nitrate, while deeper nitrification recycles nitrogen. In the BoB’s OMZ (100–300 m), nitrogen loss likely occurs via anammox.
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