Articles | Volume 12, issue 4
https://doi.org/10.5194/bg-12-1113-2015
https://doi.org/10.5194/bg-12-1113-2015
Research article
 | 
24 Feb 2015
Research article |  | 24 Feb 2015

What prevents nitrogen depletion in the oxygen minimum zone of the eastern tropical South Pacific?

B. Su, M. Pahlow, H. Wagner, and A. Oschlies

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Bei Su on behalf of the Authors (19 Dec 2014)  Manuscript 
ED: Referee Nomination & Report Request started (04 Jan 2015) by S. Wajih A. Naqvi
RR by Anonymous Referee #1 (18 Jan 2015)
ED: Publish subject to technical corrections (27 Jan 2015) by S. Wajih A. Naqvi
AR by Bei Su on behalf of the Authors (03 Feb 2015)  Author's response   Manuscript 
Download
Short summary
A box model of the eastern tropical South Pacific oxygen minimum zone suggests that anaerobic water-column remineralization rates have to be slower than aerobic remineralization in order to explain the relatively high values of observed nitrate concentrations. Lateral oxygen supply sufficient to oxidize about one-fifth of the export production is required to prevent an anoxic deep ocean. Under these circumstances, the region can be a net source of fixed nitrogen to the surrounding ocean.
Altmetrics
Final-revised paper
Preprint