Relative sea-level stability and the radiocarbon marine reservoir correction at Natuna Island, Indonesia, since 6400 yr BP

被引:15
作者
Wan, Jeannette Xiu Wen [1 ,2 ,3 ,6 ]
Meltzner, Aron J. [1 ,2 ]
Switzer, Adam D. [1 ,2 ]
Lin, Ke [1 ]
Wang, Xianfeng [1 ,2 ]
Bradley, Sarah L. [4 ]
Natawidjaja, Danny H. [5 ]
Suwargadi, Bambang W. [5 ]
Horton, Benjamin P. [1 ,2 ]
机构
[1] Nanyang Technol Univ, Earth Observ Singapore, 50 Nanyang Ave, Singapore 639798, Singapore
[2] Nanyang Technol Univ, Asian Sch Environm, 50 Nanyang Ave, Singapore 639798, Singapore
[3] Nanyang Technol Univ, CN Yang Scholars Programme, 50 Nanyang Ave, Singapore 639798, Singapore
[4] Univ Sheffield, Dept Geog, Winter St, Sheffield S3 7ND, S Yorkshire, England
[5] Indonesian Inst Sci LIPI, Res Ctr Geotechnol, Kompleks LIPI,Gedung 70,Jalan Sangkuriang, Bandung 40135, Indonesia
[6] McGill Univ, Dept Earth & Planetary Sci, 3450 Univ St, Montreal, PQ H3A 0E8, Canada
基金
新加坡国家研究基金会; 欧洲研究理事会;
关键词
Holocene Relative Sea Level; Sunda Shelf; Coral Microatoll; Radiocarbon Marine Reservoir Correction; AGE CALIBRATION CURVES; MC-ICP-MS; LATE PLEISTOCENE; SOUTHEAST COAST; HIGH-PRECISION; INDIAN-OCEAN; DELTA-R; HOLOCENE; C-14; CORALS;
D O I
10.1016/j.margeo.2020.106342
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A high-precision relative sea level (RSL) record over the past 6400 years, reconstructed from fossil coral microatoll colonies, is reported for Natuna Island, Indonesia. The timing of 11 fossil microatolls from four sites on Natuna Island is constrained by replicate C-14 and Th-230 dates. We investigate the local marine reservoir correction (Delta R) using the replicate dates. The two sets of dates become aligned if a Marine20 Delta R of - 143 +/- 176 yr, 1 sigma (Marinel 3 Delta R of 15 +/- 63 yr) is assigned to the C-14 dates. The distribution of microatoll ages and elevations indicates that RSL was relatively stable from 6400 to 1400 yr BP at 0.2-0.7 +/- 0.4 m (2 sigma) higher than present, before a fall to current levels. A comparison with the predictions of a suite of glacial isostatic adjustment (GIA) models for Southeast Asia suggests refinements are needed in ice-history models to fully capture our RSL data. These new constraints on past RSL of the Sunda Shelf contribute to further calibration of GIA models in the tropics, where RSL data are presently insufficient.
引用
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页数:20
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