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|Title:||Half-metre sea-level fluctuations on centennial timescales from mid-Holocene corals of Southeast Asia||Authors:||Meltzner, Aron Jeffrey
Switzer, Adam Douglas
Hill, David F.
Bradley, Sarah L.
Kopp, Robert E.
Hill, Emma Mary
Majewski, Jędrzej M.
Natawidjaja, Danny Hilman
Suwargadi, Bambang W.
Horton, Benjamin P.
|Keywords:||Relative sea level (RSL)
|Issue Date:||2017||Source:||Meltzner, A. J., Switzer, A. D., Horton, B. P., Ashe, E., Qiu, Q., Hill, D. F., et al. (2017). Half-metre sea-level fluctuations on centennial timescales from mid-Holocene corals of Southeast Asia. Nature Communications, 8, 14387-.||Series/Report no.:||Nature Communications||Abstract:||Sea-level rise is a global problem, yet to forecast future changes, we must understand how and why relative sea level (RSL) varied in the past, on local to global scales. In East and Southeast Asia, details of Holocene RSL are poorly understood. Here we present two independent high-resolution RSL proxy records from Belitung Island on the Sunda Shelf. These records capture spatial variations in glacial isostatic adjustment and paleotidal range, yet both reveal a RSL history between 6850 and 6500 cal years BP that includes two 0.6m fluctuations, with rates of RSL change reaching 13±4mm per year (2s). Observations along the south coast of China, although of a lower resolution, reveal fluctuations similar in amplitude and timing to those on the Sunda Shelf. The consistency of the Southeast Asian records, from sites 2,600 km apart, suggests that the records reflect regional changes in RSL that are unprecedented in modern times.||URI:||https://hdl.handle.net/10356/80768
|ISSN:||2041-1723||DOI:||10.1038/ncomms14387||Rights:||© 2017 The Author(s). This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.||Fulltext Permission:||open||Fulltext Availability:||With Fulltext|
|Appears in Collections:||EOS Journal Articles|
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