Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-491-2021
https://doi.org/10.5194/cp-17-491-2021
Research article
 | 
23 Feb 2021
Research article |  | 23 Feb 2021

Atmospheric iron supply and marine productivity in the glacial North Pacific Ocean

François Burgay, Andrea Spolaor, Jacopo Gabrieli, Giulio Cozzi, Clara Turetta, Paul Vallelonga, and Carlo Barbante

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 (03 Dec 2020) by Alberto Reyes
AR by Andrea Spolaor on behalf of the Authors (03 Dec 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (15 Dec 2020) by Alberto Reyes
RR by Anonymous Referee #3 (09 Jan 2021)
ED: Publish subject to minor revisions (review by editor) (13 Jan 2021) by Alberto Reyes
AR by Andrea Spolaor on behalf of the Authors (13 Jan 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (14 Jan 2021) by Alberto Reyes
AR by Andrea Spolaor on behalf of the Authors (18 Jan 2021)  Manuscript 
Download
Short summary
We present the first Fe record from the NEEM ice core, which provides insight into past atmospheric Fe deposition in the Arctic. Considering the biological relevance of Fe, we questioned if the increased eolian Fe supply during glacial periods could explain the marine productivity variability in the Fe-limited subarctic Pacific Ocean. We found no overwhelming evidence that eolian Fe fertilization triggered any phytoplankton blooms, likely because other factors play a more relevant role.