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Beach ridges at Keppel Bay preserve a sediment record trapping an estimated 79% of the Fitzroy River's long-term average annual bedload. Optically stimulated luminescence (OSL) ages indicate periods of rapid coastal progradation approximately 1500, 1000, 450, and 230 years before present. The dataset documents a change in sediment provenance linked to post-clearing erosion and a reduction in accumulation rates since around 1000 yr BP.
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