Abstract
The floodplain deposits of the upper Thames and its tributaries commonly comprise 0.5–1 m of clay alluvium overlying, with a sharp boundary, a variable thickness of sandy limestone gravel. Samples of wood (probably alder root) from the top of the gravel in a temporary exposure (SP 360084) in the floodplain of the river Windrush, south of Witney, Oxfordshire, gave a radiocarbon date of 2,660±85 yr BP (I-9337); these roots had been truncated at the gravel/clay interface. Here we consider the sequence of events and the possible causes of this change to clay deposition; we conclude that the latter resulted chiefly from a rapid increase in local forest clearance and in the amount of ploughed land, after 2,660 yr BP.
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Hazelden, J., Jarvis, M. Age and significance of alluvium in the Windrush valley, Oxfordshire. Nature 282, 291–292 (1979). https://doi.org/10.1038/282291a0
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DOI: https://doi.org/10.1038/282291a0
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