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- W1972374533 abstract "Abstract The Nepean Peninsula is a bay-mouth bar near Melbourne. It is comprised of Late Quaternary aeolianites, palaeosols and calcretes. TL dates show that most of the sands from which the aeolianites developed as mobile sand dunes were deposited during times of low sea-level towards 47 and 23 ka BP, and others during times of relatively high sea-level towards 118 ka BP. Aeolian dust mantles were laid down during brief intervals when aeolianite formation had ceased. Incipient soil formation and minor organic staining of the upper 0.3–0.5 m of the dust mantles points to a lull in dune formation and the temporary development of a widespread plant cover. The dust mantles have TL ages of 118, 57, 54, 51 and 47 ka BP, indicating that apart from the 118 ka mantle, most of the deposition was when sea-level was low and the regional climate was drier, windier, colder and under a more continental climatic regime. During times of glacially lower sea-level, the coastal climate in this region was not invariably cold, dry and windy but was punctuated by brief intervals of milder, moister and less windy conditions during which dunes and dust mantles became vegetated and soils began to form. Rapid climatic fluctuations were coeval with aeolianite deposition during times of very low sea-level." @default.
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- W1972374533 date "1994-01-01" @default.
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- W1972374533 title "Late Quaternary aeolianites, palaeosols and depositional environments on the Nepean Peninsula, Victoria, Australia" @default.
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- W1972374533 doi "https://doi.org/10.1016/0277-3791(94)90027-2" @default.
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