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New constraints on late Holocene eustatic sea-level changes from Mahé, Seychelles

Woodroffe, S.A.; Long, A.J.; Milne, G.A.; Bryant, C.L.; Thomas, A.

New constraints on late Holocene eustatic sea-level changes from Mahé, Seychelles Thumbnail


Authors

G.A. Milne

C.L. Bryant

A. Thomas



Abstract

This study provides new estimates of globally integrated ice sheet melt during the late Holocene (since 4 ka BP) from Seychelles in the western Indian Ocean, a tectonically stable, far field location where the necessary Glacial-Isostatic Adjustment (GIA) correction is small and is relatively insensitive to predictions using different Earth viscosity profiles. We compare sea level data from Seychelles to estimates of eustasy from two GIA models, ICE-5G and EUST3, which represent end-members in the quantity of global melt during the late Holocene. We use data from a range of coastal environments including fringing reef, present day beaches, fossil plateau and mangrove deposits on the largest island of the Seychelles archipelago, Mahé to reconstruct relative sea-level changes. Our data suggest that extensive coastal deposits of carbonate-rich sands that fringe the west coast formed in the last 2 ka and the horizontal nature of their surface topography suggests RSL stability during this period. Mangrove sediments preserved behind these deposits and in river mouths date to c. 2 ka and indicate that RSL was between −2 m and present during this interval. Correcting the reconstructed sea level data using a suite of optimal GIA models based on the two ice models mentioned above and a large number (c. 350) of Earth viscosity models gives a result that is consistent with the sedimentological constraints. When uncertainties in both model results and data are considered, it is possible to rule out eustatic sea levels below c. 2 m and more than a few decimetres above present during the past two millennia. This uncertainty is dominated by error in the reconstructions rather than the model predictions. We note, however, that our estimates of eustasy are more compatible with the EUST3 model compared to the ICE-5G model during the late Holocene (2–1 ka BP). Our evidence from Seychelles shows that the timing of when eustatic sea level first rose close to present is between the predictions of the two end-member GIA models presented here (4 ka BP for ICE-5G and 1 ka BP for EUST3). Using all lines of evidence currently available from Mahé we suggest that the eustatic contribution during the last 2 ka has been less than 2 m . This conclusion is drawn from a tectonically stable, far-field region that is relatively insensitive to earth and ice model uncertainties, and implies that global eustasy has been relatively insensitive to climate fluctuations over the pre-industrial part of the last 2 ka.

Citation

Woodroffe, S., Long, A., Milne, G., Bryant, C., & Thomas, A. (2015). New constraints on late Holocene eustatic sea-level changes from Mahé, Seychelles. Quaternary Science Reviews, 115, 1-16. https://doi.org/10.1016/j.quascirev.2015.02.011

Journal Article Type Article
Acceptance Date Feb 12, 2015
Online Publication Date Mar 19, 2015
Publication Date May 1, 2015
Deposit Date May 12, 2015
Publicly Available Date Mar 19, 2016
Journal Quaternary Science Reviews
Print ISSN 0277-3791
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 115
Pages 1-16
DOI https://doi.org/10.1016/j.quascirev.2015.02.011
Keywords Eustasy, Relative sea level, Mangroves, Seychelles, Late Holocene, Glacial-isostatic adjustment.

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Copyright Statement
NOTICE: this is the author’s version of a work that was accepted for publication in Quaternary Science Reviews. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Quaternary Science Reviews, 115, 1 May 2015, 10.1016/j.quascirev.2015.02.011.







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