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Palynological investigation of dredged samples from the Great Australian Bight continental slope correlates bulk palynofloras with the Maastrichtian to earliest Paleocene Forcipites longus and Manumiella druggii zones. The data, sourced from Geoscience Australia, indicates these zones are characteristic of the upper Potoroo Formation, which is widespread in the Bight and Duntroon Basins. Environments of deposition ranged from paralic to marine, with evidence of lowland temperate rainforests on the Australian side of the rift during the Campanian-Maastrichtian.
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