Figure 7
From: Late Holocene relative sea-level records from coral microatolls in Singapore
Map and regional comparison of RSL data. (a) Map of the study area showing the ___location of major faults43,80 and existing studies of Late Holocene RSL in the region (locations 1–11), created using QGIS 3.32.3 (https://www.qgis.org/). 1: Natuna Island1,2; 2: Thale Noi, Thailand84; 3: Merang, Terengganu6,7; 4: Kuantan31; 5: Tioman14; 6: Singapore12,40,41; 7: Senggarang13; 8: Pasir Panjang, Malaysia13; 9: Port Dickson13; 10: Teluk Batik39; 11: Langkawi39. The boundary of the Sunda Shelf (dashed line) is based on the 200 m bathymetric contour79. Background: map of the ICE-6G_C HetML140 glacial isostatic adjustment model77,78 at 2 kyr BP, generated using GMT 5.4.5 (https://www.generic-mapping-tools.org/). (b–d) Late Holocene RSL for Siloso Point, Sentosa, Singapore, compared to data from (b) elsewhere in Singapore (site 6); (c) East Coast Malay Peninsula (ECMP) and Riau Islands (sites 1–5); and (d) West Coast Malay Peninsula (WCMP) (sites 7–11). Dashed lines: low quality data; solid fill: high quality data. The horizontal line of marine limiting data is plotted at the bottom of the RSL uncertainty and indicate that RSL could have been anywhere at or above the horizontal line, vice versa for terrestrial limiting data, whose horizontal line is plotted at the top of the RSL uncertainty and indicate RSL is at or below it. The vertical ticks in the limiting data are purely symbolic and do not represent the magnitude of RSL uncertainty. RSL: relative sea level; SLIP: sea-level index point.
