Abstract
A STRATIGRAPHICAL sequence of lower peat, fen clay, upper peat and upper silt is characteristic of the whole of the southern part of the Fenland. The corresponding sequence of post-glacial vegetation successions throughout the area and their correlation with archaeological horizons is described by H. Godwin (Phil. Trans. Boy. Soc, 230, No. 570, Feb. 1940).
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Post-Glacial Vegetation of English Fenland. Nature 145, 907 (1940). https://doi.org/10.1038/145907a0
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DOI: https://doi.org/10.1038/145907a0