It is well known that the North Sea conceals an extensive former landscape of Late Pleistocene and Holocene date that was progressively submerged as result of rising post‐glacial sea levels. Although an increasingly detailed picture is emerging of these submerged palaeolandscapes, well‐dated palaeoenvironmental reconstructions from the North Sea Basin remain few and far between. Pollen, foraminifera, ostracod, plant macrofossi...