Constraining mid to late Holocene relative sea level change in the southern equatorial Pacific Ocean relative to the Society Islands, French Polynesia

• Published in: Geochemistry, Geophysics, Geosystems
• Main Authors: Rashid R, Eisenhauer A, Stocchi P, Liebetrau V, Fietzke J, Rüggeberg A, Dullo WC
• Other Authors: Rashid, R, Eisenhauer, A, Stocchi, P, Liebetrau, V, Fietzke, J, Rüggeberg, A, Dullo, Wc
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2014
• Subjects: Pacific; Ice Sheet
• Online Access: https://hdl.handle.net/11576/2726024; https://doi.org/10.1002/2014GC005272

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 similar to 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 similar to 1.560.4 m higher than present at similar to 5.4 ka. Later, minor amplitude variations occurred until similar to 2 ka, when the rsl started dropping to its present position with a rate of similar to 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.