Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1187-2020
https://doi.org/10.5194/cp-16-1187-2020
Research article
 | 
10 Jul 2020
Research article |  | 10 Jul 2020

Late Holocene (0–6 ka) sea-level changes in the Makassar Strait, Indonesia

Maren Bender, Thomas Mann, Paolo Stocchi, Dominik Kneer, Tilo Schöne, Julia Illigner, Jamaluddin Jompa, and Alessio Rovere

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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 (26 Sep 2019) by Pierre Francus
AR by Maren Bender on behalf of the Authors (04 Jan 2020)  Author's response
ED: Referee Nomination & Report Request started (15 Jan 2020) by Pierre Francus
RR by Anonymous Referee #3 (01 Feb 2020)
RR by Anonymous Referee #4 (22 Feb 2020)
RR by Anonymous Referee #2 (24 Feb 2020)
ED: Publish subject to minor revisions (review by editor) (03 Mar 2020) by Pierre Francus
AR by Maren Bender on behalf of the Authors (13 Mar 2020)  Author's response
ED: Publish subject to minor revisions (review by editor) (26 Mar 2020) by Pierre Francus
AR by Maren Bender on behalf of the Authors (04 Apr 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (08 Apr 2020) by Pierre Francus

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Maren Bender on behalf of the Authors (19 May 2020)   Author's adjustment   Manuscript
EA: Adjustments approved (02 Jun 2020) by Pierre Francus
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Short summary
This paper presents 24 new sea-level index points in the Spermonde Archipelago, Indonesia, and the reconstruction of the local Holocene relative sea-level history in combination with glacial isostasic adjustment models. We further show the importance of surveying the height of living coral microatolls as modern analogs to the fossil ones. Other interesting aspects are the potential subsidence of one of the densely populated islands, and we present eight samples that are dated to the Common Era.