Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia
Precisely quantifying the current climate-related sea level change requires accurate knowledge of long-term geological processes known as Glacial Isostatic Adjustments (GIA). Although the major postglacial melting phase is likely to have ended ~6–4 ka BP (before present), GIA is still significantly...
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ftnioz:oai:imis.nioz.nl:241834 2023-05-15T16:41:08+02:00 Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia Rashid, R. Eisenhauer, A. Stocchi, P. Liebetrau, V. Fietzke, J. Rüggeberg, A. Dullo, W.-C. 2014 application/pdf https://www.vliz.be/imisdocs/publications/53/265053.pdf en eng info:eu-repo/semantics/altIdentifier/wos/000340362500032 info:eu-repo/semantics/altIdentifier/doi/oi.org/10.1002/2014GC005272 https://www.vliz.be/imisdocs/publications/53/265053.pdf info:eu-repo/semantics/openAccess %3Ci%3EGeochem.+Geophys.+Geosyst.+15%286%29%3C%2Fi%3E%3A+2601-2615.+%3Ca+href%3D%22http%3A%2F%2Fdx.doi.org%2F10.1002%2F2014GC005272%22+target%3D%22_blank%22%3Ehttp%3A%2F%2Fdx.doi.org%2F10.1002%2F2014GC005272%3C%2Fa%3E info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2014 ftnioz https://doi.org/10.1002/2014GC005272 2022-05-01T14:00:09Z Precisely quantifying the current climate-related sea level change requires accurate knowledge of long-term geological processes known as Glacial Isostatic Adjustments (GIA). Although the major postglacial melting phase is likely to have ended ~6–4 ka BP (before present), GIA is still significantly affecting the present-day vertical position of the mean sea surface and the sea bottom. Here we present empirical rsl (relative sea level) data based on U/Th dated fossil corals from reef platforms of the Society Islands, French Polynesia, together with the corresponding GIA-modeling. Fossil coral data constrain the timing and amplitude of rsl variations after the Holocene sea level maximum (HSLM). Upon correction for isostatic island subsidence, we find that local rsl was at least ~1.5?±?0.4 m higher than present at ~5.4 ka. Later, minor amplitude variations occurred until ~2 ka, when the rsl started dropping to its present position with a rate of ~0.4 mm/yr. The data match with predicted rsl curves based on global ice-sheet chronologies confirming the role of GIA-induced ocean siphoning effect throughout the mid to late Holocene. A long lasting Late Holocene highstand superimposed with second-order amplitudinal fluctuations as seen from our data suggest that the theoretical predicted timing of rsl change can still be refined pending future calibration Article in Journal/Newspaper Ice Sheet NIOZ Repository (Royal Netherlands Institute for Sea Research) Pacific Geochemistry, Geophysics, Geosystems 15 6 2601 2615 |
institution |
Open Polar |
collection |
NIOZ Repository (Royal Netherlands Institute for Sea Research) |
op_collection_id |
ftnioz |
language |
English |
description |
Precisely quantifying the current climate-related sea level change requires accurate knowledge of long-term geological processes known as Glacial Isostatic Adjustments (GIA). Although the major postglacial melting phase is likely to have ended ~6–4 ka BP (before present), GIA is still significantly affecting the present-day vertical position of the mean sea surface and the sea bottom. Here we present empirical rsl (relative sea level) data based on U/Th dated fossil corals from reef platforms of the Society Islands, French Polynesia, together with the corresponding GIA-modeling. Fossil coral data constrain the timing and amplitude of rsl variations after the Holocene sea level maximum (HSLM). Upon correction for isostatic island subsidence, we find that local rsl was at least ~1.5?±?0.4 m higher than present at ~5.4 ka. Later, minor amplitude variations occurred until ~2 ka, when the rsl started dropping to its present position with a rate of ~0.4 mm/yr. The data match with predicted rsl curves based on global ice-sheet chronologies confirming the role of GIA-induced ocean siphoning effect throughout the mid to late Holocene. A long lasting Late Holocene highstand superimposed with second-order amplitudinal fluctuations as seen from our data suggest that the theoretical predicted timing of rsl change can still be refined pending future calibration |
format |
Article in Journal/Newspaper |
author |
Rashid, R. Eisenhauer, A. Stocchi, P. Liebetrau, V. Fietzke, J. Rüggeberg, A. Dullo, W.-C. |
spellingShingle |
Rashid, R. Eisenhauer, A. Stocchi, P. Liebetrau, V. Fietzke, J. Rüggeberg, A. Dullo, W.-C. Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia |
author_facet |
Rashid, R. Eisenhauer, A. Stocchi, P. Liebetrau, V. Fietzke, J. Rüggeberg, A. Dullo, W.-C. |
author_sort |
Rashid, R. |
title |
Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia |
title_short |
Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia |
title_full |
Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia |
title_fullStr |
Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia |
title_full_unstemmed |
Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia |
title_sort |
constraining mid to late holocene relative sea level change in the southern equatorial pacific ocean relative to the society islands, french polynesia |
publishDate |
2014 |
url |
https://www.vliz.be/imisdocs/publications/53/265053.pdf |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
%3Ci%3EGeochem.+Geophys.+Geosyst.+15%286%29%3C%2Fi%3E%3A+2601-2615.+%3Ca+href%3D%22http%3A%2F%2Fdx.doi.org%2F10.1002%2F2014GC005272%22+target%3D%22_blank%22%3Ehttp%3A%2F%2Fdx.doi.org%2F10.1002%2F2014GC005272%3C%2Fa%3E |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/000340362500032 info:eu-repo/semantics/altIdentifier/doi/oi.org/10.1002/2014GC005272 https://www.vliz.be/imisdocs/publications/53/265053.pdf |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1002/2014GC005272 |
container_title |
Geochemistry, Geophysics, Geosystems |
container_volume |
15 |
container_issue |
6 |
container_start_page |
2601 |
op_container_end_page |
2615 |
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1766031564693569536 |