Articles | Volume 18, issue 14
https://doi.org/10.5194/bg-18-4305-2021
https://doi.org/10.5194/bg-18-4305-2021
Research article
 | 
23 Jul 2021
Research article |  | 23 Jul 2021

Nitrogen loss processes in response to upwelling in a Peruvian coastal setting dominated by denitrification – a mesocosm approach

Kai G. Schulz, Eric P. Achterberg, Javier Arístegui, Lennart T. Bach, Isabel Baños, Tim Boxhammer, Dirk Erler, Maricarmen Igarza, Verena Kalter, Andrea Ludwig, Carolin Löscher, Jana Meyer, Judith Meyer, Fabrizio Minutolo, Elisabeth von der Esch, Bess B. Ward, and Ulf Riebesell

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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 bg-2021-6', Annie Bourbonnais, 05 Feb 2021
  • RC2: 'Comment on bg-2021-6', Anonymous Referee #2, 15 Feb 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (01 Apr 2021) by Hans-Peter Grossart
AR by Kai G. Schulz on behalf of the Authors (13 Apr 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (13 Apr 2021) by Hans-Peter Grossart
RR by Anonymous Referee #2 (23 Apr 2021)
RR by Annie Bourbonnais (27 Apr 2021)
ED: Publish subject to minor revisions (review by editor) (10 May 2021) by Hans-Peter Grossart
ED: Publish subject to minor revisions (review by editor) (18 May 2021) by Hans-Peter Grossart
AR by Kai G. Schulz on behalf of the Authors (15 Jun 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (26 Jun 2021) by Hans-Peter Grossart
AR by Kai G. Schulz on behalf of the Authors (28 Jun 2021)
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Short summary
Upwelling of nutrient-rich deep waters to the surface make eastern boundary upwelling systems hot spots of marine productivity. This leads to subsurface oxygen depletion and the transformation of bioavailable nitrogen into inert N2. Here we quantify nitrogen loss processes following a simulated deep water upwelling. Denitrification was the dominant process, and budget calculations suggest that a significant portion of nitrogen that could be exported to depth is already lost in the surface ocean.
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