Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functions

We have investigated the benthic foraminiferal fauna from sediment event layers associated with the 2004 Indian Ocean tsunami and former storms that have been retrieved in short sediment cores from offshore environments of the Andaman Sea, off Khao Lak, western Thailand. Species composition and test...

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Main Authors: Y. Milker, M. Wilken, J. Schumann, D. Sakuna, P. Feldens, K. Schwarzer, G. Schmiedl
Format: Article
Language:English
Published: Copernicus Publications 2013-12-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/13/3113/2013/nhess-13-3113-2013.pdf
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author Y. Milker
M. Wilken
J. Schumann
D. Sakuna
P. Feldens
K. Schwarzer
G. Schmiedl
author_facet Y. Milker
M. Wilken
J. Schumann
D. Sakuna
P. Feldens
K. Schwarzer
G. Schmiedl
author_sort Y. Milker
collection DOAJ
description We have investigated the benthic foraminiferal fauna from sediment event layers associated with the 2004 Indian Ocean tsunami and former storms that have been retrieved in short sediment cores from offshore environments of the Andaman Sea, off Khao Lak, western Thailand. Species composition and test preservation of the benthic foraminiferal faunas exhibit pronounced changes across the studied sections and provide information on the depositional history of the tsunami layer, particularly on the source water depth of the displaced foraminiferal tests. In order to obtain accurate bathymetric information on sediment provenance, we have mapped the distribution of modern faunas in non-tsunamigenic surface sediments and created a calibration data set for the development of a transfer function. Our quantitative reconstructions revealed that the resuspension of sediment particles by the tsunami wave was restricted to a maximum water depth of approximately 20 m. Similar values were obtained for former storm events, thus impeding an easy distinction of different high-energy events.
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spelling doaj.art-40fe05f1029c438584cabbf3db959a352022-12-22T03:16:22ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812013-12-0113123113312810.5194/nhess-13-3113-2013Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functionsY. Milker0M. Wilken1J. Schumann2D. Sakuna3P. Feldens4K. Schwarzer5G. Schmiedl6Center of Earth System Research and Sustainability, University of Hamburg, Hamburg, GermanyCenter of Earth System Research and Sustainability, University of Hamburg, Hamburg, GermanyCenter of Earth System Research and Sustainability, University of Hamburg, Hamburg, GermanyInstitute of Geosciences, Coastal and Shelf Research, University of Kiel, Kiel, GermanyInstitute of Geosciences, Coastal and Shelf Research, University of Kiel, Kiel, GermanyInstitute of Geosciences, Coastal and Shelf Research, University of Kiel, Kiel, GermanyCenter of Earth System Research and Sustainability, University of Hamburg, Hamburg, GermanyWe have investigated the benthic foraminiferal fauna from sediment event layers associated with the 2004 Indian Ocean tsunami and former storms that have been retrieved in short sediment cores from offshore environments of the Andaman Sea, off Khao Lak, western Thailand. Species composition and test preservation of the benthic foraminiferal faunas exhibit pronounced changes across the studied sections and provide information on the depositional history of the tsunami layer, particularly on the source water depth of the displaced foraminiferal tests. In order to obtain accurate bathymetric information on sediment provenance, we have mapped the distribution of modern faunas in non-tsunamigenic surface sediments and created a calibration data set for the development of a transfer function. Our quantitative reconstructions revealed that the resuspension of sediment particles by the tsunami wave was restricted to a maximum water depth of approximately 20 m. Similar values were obtained for former storm events, thus impeding an easy distinction of different high-energy events.http://www.nat-hazards-earth-syst-sci.net/13/3113/2013/nhess-13-3113-2013.pdf
spellingShingle Y. Milker
M. Wilken
J. Schumann
D. Sakuna
P. Feldens
K. Schwarzer
G. Schmiedl
Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functions
Natural Hazards and Earth System Sciences
title Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functions
title_full Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functions
title_fullStr Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functions
title_full_unstemmed Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functions
title_short Sediment transport on the inner shelf off Khao Lak (Andaman Sea, Thailand) during the 2004 Indian Ocean tsunami and former storm events: evidence from foraminiferal transfer functions
title_sort sediment transport on the inner shelf off khao lak andaman sea thailand during the 2004 indian ocean tsunami and former storm events evidence from foraminiferal transfer functions
url http://www.nat-hazards-earth-syst-sci.net/13/3113/2013/nhess-13-3113-2013.pdf
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