Marked fluctuations in Late‐glacial climate are correlated with significant changes in river behaviour and floodplain environment across much of northwest Europe. Evidence from a new site in the Kennet Valley provides a rare comprehensive picture of varying fluvial regime and local vegetation during this interval. Chronological control for the site is provided by biostratigraphical and morphostratigraphical correlations with other sites in the region, and by radiocarbon dating of carefully selected material. Preservation of the sedimentary sequence was facilitated by its occurrence within a large depression in the underlying bedrock. The origin of this depression is uncertain, perhaps reflecting subsidence or scour. Following the Last Glacial Maximum, a nival regime braided river dominated by floods deposited sandy gravels under stadial conditions. A large channel infilled by fine sediments during the latter part of the Windermere Interstadial indicates a fall in flow competence at a time of increased floodplain vegetation, most notably the appearance of tree birch. Variations in sediments and vegetation suggest fluctuations in the floodplain environment, reflecting complex vegetation dynamics and possibly climate forcing. During the Loch Lomond/Younger Dryas Stadial, a nival, braided regime was re‐established, accompanied by the disappearance of tree birch.
-3 -likely to diverge from this. Consequently, it is essential to understand catchment controls, particularly the relative significance of surface and subsurface hydrology.
A comparative palynological study of 25 taxa of the genus Orobanche L. belonging to section Trionychon Wallr. and section Orobanche L. was carried out. A clear difference between the pollen grains of section Trionychon and section Orobanche was observed. The grains of section Trionychon are typically tricolpate, radially symmetrical, more or less oblate spheroidal, with a microreticulate, or scabrate‐perforate sculpture. Section Orobanche on the other hand, had spheroidal, more or less inaperturate pollen grains, although some were tricolpate, but without any clear symmetry. The basic surface sculpture of the pollen in section Orobanche was scabrate to rugulate‐perforate. Palynoiogicaliy, six groups can be recognized amongst the species of the genus Orobanche, lor which a key is provided.
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