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Coarse clast ridge sequences as suitable archives for past storm events? Case study on the Houtman Abrolhos,Western Australia
Authors:Anja M Scheffers  Sander R Scheffers  Dieter H Kelletat  Peter Squire  Lindsay Collins  Yuexing Feng  Jian‐Xin Zhao  Renaud Joannes‐Boyau  Simon Matthias May  Gerhard Schellmann  Heather Freeman
Institution:1. Southern Cross GeoScience, Southern Cross University, Lismore, Australia;2. School of Earth Sciences, University of Queensland, Brisbane, Australia;3. Marine Ecology Research Center, Southern Cross University, Lismore, Australia;4. Department for Geosciences, University of Cologne, Cologne, Germany;5. Department of Applied Geology, Curtin University, Perth, Australia;6. Centre for Microscopy and Microanalysis, University of Queensland, Brisbane, Australia;7. Department of Geography, Otto Friedrich University, Bamberg, Germany
Abstract:Prehistoric storm records are relatively scarce in most parts of the world. This article presents storm records derived from coral rubble‐based geological archives of the Houtman Abrolhos Archipelago located off the west coast of Australia, where the southernmost coral reefs of the Indian Ocean are found. Winter storm swell from the circum‐Antarctic ‘Brave Westerlies’, as well as tropical cyclone waves, have left numerous ridge systems on dozens of islands of the archipelago, all composed of coral rubble from adjacent reefs. At three islands, seven ridge systems were dated by three different methods: U‐series (68 dates), radiocarbon (64 dates), electron spin resonance (7 dates); 139 radiometric dates span the last 5500 years of the Holocene. In contrast to the geomorphological interpretation, the age sequences show ‘inversions’, hiatuses and different ages for the same ridge, all pointing to complicated ridge formation processes. Time gaps, some exceeding 1000 years, are interpreted as phases of erosion and not as phases without storm activity. Copyright © 2012 John Wiley & Sons, Ltd.
Keywords:palaeotempestology  beach ridges  coastal evolution  Holocene  geomorphology
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