Articles | Volume 14, issue 9
https://doi.org/10.5194/bg-14-2245-2017
https://doi.org/10.5194/bg-14-2245-2017
Research article
 | 
04 May 2017
Research article |  | 04 May 2017

Low planktic foraminiferal diversity and abundance observed in a spring 2013 west–east Mediterranean Sea plankton tow transect

Miguel Mallo, Patrizia Ziveri, P. Graham Mortyn, Ralf Schiebel, and Michael Grelaud

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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: Reconsider after major revisions (17 Oct 2016) by Markus Kienast
AR by Patrizia Ziveri on behalf of the Authors (28 Nov 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 Dec 2016) by Markus Kienast
RR by Anonymous Referee #1 (09 Dec 2016)
RR by Anonymous Referee #3 (12 Dec 2016)
RR by Manuel Weinkauf (16 Dec 2016)
ED: Reconsider after major revisions (20 Dec 2016) by Markus Kienast
AR by Svenja Lange on behalf of the Authors (02 Feb 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Feb 2017) by Markus Kienast
RR by Anonymous Referee #1 (16 Feb 2017)
RR by Manuel Weinkauf (17 Feb 2017)
ED: Publish subject to minor revisions (Editor review) (21 Feb 2017) by Markus Kienast
AR by Patrizia Ziveri on behalf of the Authors (07 Mar 2017)  Author's response    Manuscript
ED: Publish as is (12 Mar 2017) by Markus Kienast
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Short summary
Single-celled living calcareous planktic foraminifera data across the Mediterranean Sea suggest that stratification of the surface water column, food availability, temperature, and seawater carbonate chemistry are the main factors controlling their distribution and mass. Increasing temperature, salinity, surface ocean stratification, and trophic conditions could be the causes of reduced abundance, diversity and species-specific changes in calcification in planktic foraminifera.
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