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Late Quaternary evolution of coral reefs on a cool-water carbonate margin: the Abrolhos Carbonate Platforms, southwest Australia |
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| Authors: | L B Collins Z R Zhu K -H Wyrwoll B G Hatcher P E Playford J H Chen A Eisenhauer and G J Wasserburg |
| Institution: | a School of Applied Geology, Curtin University of Technology, GPO Box U 1987, Perth, 6102, Australia b University of Western Australia, Nedlands, 6009, Australia c Department of Oceanography, Dalhousie University, Halifax, NS B3H 4J1, Canada d Geological Survey of Western Australia, East Perth, 6004, Australia e Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA |
| Abstract: | Late Quaternary coral reefs have developed on the southwestern Australian margin, which has otherwise been characterised by cool-water carbonates since the Eocene. The Houtman Abrolhos coral reefs are at the limits of existence, extending, with the assistance of the Leeuwin Current, a poleward-flowing, warm water stream, into a region dominated by more temperate communities. Coring in the Easter Group reefs, supported by high precision dating, by both U/Th TIMS and 14C methods, has shown vigorous coral growth, with reefs over 26 m thick in the Holocene and over 15 m thick in the Last Interglacial. Each of the three Abrolhos platforms consists of a central platform composed of Last Interglacial reefs, about which windward and leeward Holocene reefs developed asymmetrically. Reef, peritidal and eolian facies comprise the emergent Last Interglacial limestones which are extensively calcretized, with reef facies up to 5 m above MSL. The Last Interglacial high stand lasted for at least 10 ka from 130 to 120 ka, and possibly 15 ka, from 132 to 117 ka. Holocene reef facies are also emergent by 0.5 m, and are overlain by peritidal and storm ridge facies in an upward-shallowing sequence. Windward (10 m thick) and leeward (26 m thick) Holocene reefs in the Easter Group show contrasting lithofacies. The wave-exposed windward reefs consist of a slow-growing association of coralline algal bindstones and coral framestones, whereas fast-growing coral framestones dominate the more protected leeward reefs. The leeward reefs commenced growth 10,000 years ago and grew to the present sea level by 6500 years ago, generating Holocene constructional topography consisting of ‘blue-hole’ terrain in the leeward parts of the platforms. |
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