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Foraminifera and palaeoenvironment of elevated Late Pleistocene sands, White Rock Point, southeastern Tasmania

Abstract

A well-preserved foraminiferal fauna similar to that living in nearby Ralphs Bay in southeastern Tasmania is documented from raised shallow-water sediment of 130-119 Ka age (Late Pleistocene; Marine Isotope Stage 5e) at about 24m above modern sea level on White Rock Point

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