A Multi-Peaked Mid-Holocene Relative Sea-Level Highstand on the Sunda Shelf, Indonesia

Abstract:

Details of relative sea level (RSL) since the mid-Holocene in Southeast Asia are poorly determined. We have developed mid-Holocene RSL records at two sites on Belitung Island, Indonesia, on the Sunda Shelf, based on slabbed coral microatolls. At both sites, RSL reached its initial peak at ~6750 yr BP. RSL then fell ~70 cm, remaining at a lowstand for 60–100 years, before rising ~60 cm to a second peak at ~6550 yr BP. Evidence at both sites suggests that this was followed by at least one additional oscillation and one additional RSL peak over the following ~300 yr. On southeastern Belitung, the amplitude of the first RSL peak was more than +1.0 m above 2013 levels, the lowstand was at +0.6 m, and the second RSL peak was at +1.2 m. On northwestern Belitung, the first RSL peak, the lowstand, and the second peak were at +1.9 m, +1.2 m, and +1.7 m, respectively. The similarities in the records from the two sites, which are 80 km apart, argue that none of the oscillations are artifacts of local factors, e.g., ponding of corals. Notwithstanding these similarities, there is a uniform shift in elevations between the two sites: elevations at the NW site are consistently 0.5–0.6 m higher than contemporaneous elevations at the SE site. This difference might be explained by spatial variability in glacial isostatic adjustment (GIA), by changes over time in tidal range at one or both sites, and/or by a bias in elevations at the SE site if the modern “reference” corals were ponded. Decimetric fluctuations in RSL have also been suggested based on microatolls from southern China (Yu et al., 2009), but few other studies have the temporal and vertical resolution necessary to assess the geographic extent of such fluctuations. These RSL fluctuations across the South China Sea might be linked to oscillations in the strength of the monsoon.