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• W2012039374 abstract "In 1924 a Pleistocene deposit containing remains of spruce (Picea) and fruits of an arctic buttercup (Ranunculus hyperboreus) was discovered in a sewer trench in the grounds of Bembridge School, Isle of Wight (southern England). This deposit has been reinvestigated by means of two boreholes which show that the organic deposits rest directly on Bembridge Marls (Lower Oligocene) and are overlain by 3 m of head which is devoid of fossils. A new lithostratigraphical unit, the Steyne Wood Clay, is proposed for the organic deposit which lies between 38–40 m O.D. The contained fossils (pollen, plant macrofossils, diatoms, Mollusca, Ostracoda and Foraminifera) are described and demonstrate that this unit was deposited in an estuarine environment. The pollen spectra suggest that this occurred during the post-temperate zone of a Middle Pleistocene interglacial. The Steyne Wood Clay thus represents the highest fossiliferous intertidal deposit of Middle Pleistocene age yet described from the British Isles. Its relationship with the Slindon-Goodwood Raised Beach and other related deposits which lie at a similar elevation is discussed." @default.
• W2012039374 created "2016-06-24" @default.
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• W2012039374 date "1983-01-01" @default.
• W2012039374 modified "2023-09-25" @default.
• W2012039374 title "Evidence of a high Middle Pleistocene sea-level from estuarine deposits at Bembridge, Isle of Wight, England" @default.
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• W2012039374 doi "https://doi.org/10.1016/s0016-7878(83)80041-8" @default.
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