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The Poukawa Basin on the eastern North Island of New Zealand was cored to a maximum depth of 234 m during investigations from 1976 to 1984, and again in 1997 as part of the New Zealand contribution to Pole Equator Pole Transect 2. The nonmarine sediments recovered were fossiliferous Quaternary silts and sands with some peat and marl layers. The common and diverse marine fossils present (molluscan...
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