Articles | Volume 13, issue 6
https://doi.org/10.5194/cp-13-711-2017
https://doi.org/10.5194/cp-13-711-2017
Research article
 | 
19 Jun 2017
Research article |  | 19 Jun 2017

Extreme flood event reconstruction spanning the last century in the El Bibane Lagoon (southeastern Tunisia): a multi-proxy approach

Aida Affouri, Laurent Dezileau, and Nejib Kallel

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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: Reconsider after major revisions (21 Sep 2016) by Nathalie Combourieu Nebout
AR by Aida Affouri on behalf of the Authors (20 Oct 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (24 Oct 2016) by Nathalie Combourieu Nebout
RR by Bassetti Maria Angela (02 Nov 2016)
RR by Anonymous Referee #5 (27 Nov 2016)
RR by Anonymous Referee #6 (27 Nov 2016)
ED: Reconsider after major revisions (02 Dec 2016) by Nathalie Combourieu Nebout
AR by Aida Affouri on behalf of the Authors (12 Jan 2017)  Author's response   Manuscript 
ED: Reconsider after major revisions (06 Feb 2017) by Nathalie Combourieu Nebout
AR by Aida Affouri on behalf of the Authors (20 Mar 2017)  Author's response 
ED: Reconsider after major revisions (31 Mar 2017) by Nathalie Combourieu Nebout
AR by Aida Affouri on behalf of the Authors (27 Apr 2017)  Author's response   Manuscript 
ED: Publish as is (03 May 2017) by Nathalie Combourieu Nebout
AR by Aida Affouri on behalf of the Authors (07 May 2017)  Manuscript 
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Short summary
The past flood activity was investigated using a sedimentological and geochemical analysis of surfaces sediments from a southeastern Tunisian catchment in order to trace the origin of sediments deposit in the El Bibane Lagoon. Aeolian, fluvial and marine source. This multi-proxy analysis on the BL12-10 core shows that finer material, a high content of clay and silt, and a high content of the elemental ratios Fe / Ca and Ti / Ca characterise the sedimentological signature of palaeo-flood levels.