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Beach ridges at Keppel Bay, central Queensland, preserve a record of sediment accumulation from the historical period back to middle Holocene times. The dataset, sourced from the Australian Ocean Data Network, includes optically stimulated luminescence (OSL) ages indicating periods of rapid progradation approximately 1500, 1000, 450 and 230 years before present. It demonstrates how these deposits provide insights into sediment accumulation processes and responses to climate variations in tropical coastal systems.
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