Articles | Volume 13, issue 21
https://doi.org/10.5194/bg-13-6049-2016
https://doi.org/10.5194/bg-13-6049-2016
Research article
 | 
03 Nov 2016
Research article |  | 03 Nov 2016

Unveiling the Si cycle using isotopes in an iron-fertilized zone of the Southern Ocean: from mixed-layer supply to export

Ivia Closset, Damien Cardinal, Mathieu Rembauville, François Thil, and Stéphane Blain

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
ED: Reconsider after major revisions (18 Aug 2016) by Clare Woulds
AR by Ivia Closset on behalf of the Authors (28 Aug 2016)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (11 Sep 2016) by Clare Woulds
AR by Ivia Closset on behalf of the Authors (14 Sep 2016)  Author's response    Manuscript
ED: Publish as is (28 Sep 2016) by Clare Woulds
Download
Short summary
Isotopic measurements were used to investigate the seasonal evolution of the silicon (Si) biogeochemical cycle in a naturally iron-fertilized area of the Southern Ocean. When comparing data from early spring and summer periods, the relationship between Si depletion, biogenic silica production, and their isotopic composition appears decoupled in this region. Considering these results, we refined the seasonal net Si production that was mainly sustained by surface phytoplankton populations.
Altmetrics
Final-revised paper
Preprint