Articles | Volume 17, issue 7
Biogeosciences, 17, 1933–1953, 2020
Biogeosciences, 17, 1933–1953, 2020

Research article 09 Apr 2020

Research article | 09 Apr 2020

Benthic foraminifera as tracers of brine production in the Storfjorden “sea ice factory”

Eleonora Fossile et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (05 Feb 2020) by Hiroshi Kitazato
AR by Anna Wenzel on behalf of the Authors (17 Feb 2020)  Author's response    Manuscript
ED: Publish as is (02 Mar 2020) by Hiroshi Kitazato
AR by Eleonora Fossile on behalf of the Authors (05 Mar 2020)  Author's response    Manuscript
Short summary
This study focuses on benthic foraminiferal distribution in an Arctic fjord characterised by continuous sea ice production during winter and the consequent cascading of salty and corrosive waters (brine) to the seabed. The inner fjord is dominated by calcareous species (C). In the central deep basins, where brines are persistent, calcareous foraminifera are dissolved and agglutinated (A) dominate. The high A/C ratio is suggested as a proxy for brine persistence and sea ice production.
Final-revised paper