Multi-proxy approach to identify the origin of high energy coastal deposits from Laem Son National Park, Andaman Sea of Thailand

Stapana Kongsen, Sumet Phantuwongraj, Montri Choowong*, Sakonvan Chawchai, Sirawat Udomsak, Chanista Chansom, Chanakan Ketthong, Peerasit Surakiatchai, Johannes M. Miocic, Frank Preusser

*Corresponding author for this work

Research output: Contribution to journalArticleAcademicpeer-review

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Abstract

Understanding the frequency of high energy storm and tsunami events is crucial for apprehending the vulnerability of coastal communities. Identifying and dating sedimentary evidence deposited by such high energy events can assist in the planning and installation of suitable protection measurements. The Andaman Sea coast of Thailand is particularly vulnerable to such events as illustrated by the 2004 Indian Ocean Tsunami. Here, three shore-perpendicular transects and ten sediment cores along a beach ridge in the northern part of Lam Son National Park, Ranong Province, Andaman Sea coast are investigated with respect to high energy deposits. A multi-proxy analysis was conducted including stratigraphical correlations between cores, detailed description of physical characteristics, sedimentary structure, grain size, organic matter and carbonate content as well as identification of the remains of marine organisms. Optically stimulated luminescence (OSL) dating was applied for determining the age of the sediments on this beach ridge plain. The stratigraphy and sediment characteristics, in particular composition, of the sands in the study area clearly allow us to distinguish between high energy deposits and normal beach sediments. Two high energy deposits were identified and attributed to result from the 2004 Indian Ocean Tsunami as well as a past storm, which, based on OSL dating occurred more than 340 ± 20 years ago.
Original languageEnglish
Pages (from-to)82-95
Number of pages14
JournalQuaternary International
Volume625
Early online date30-Apr-2022
DOIs
Publication statusPublished - 10-Jul-2022

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