Twelve pollen assemblage zones are identified in a 229 m deep borehole
(BH 81/34) from the Devil's Hole area in the central North Sea (Briti
sh sector). The sediment from this borehole is Early to Late Pleistoce
ne in age and the observation of massulae from Azolla filiculoides in
sediment with reversed polarity indicates an age younger than the Oldu
vai geomagnetic event for the entire sequence. The Early Pleistocene s
ediments were at least partly deposited in the vicinity of a river out
let and can be correlated either with the Eburonian or the Menapian co
ld stage and with the Bavel interglacial and the Linge glacial within
the Bavelian stage in the Dutch stratigraphy. The Middle Pleistocene s
equence contains an interval rich in Abies, Picea and Pinus, probably
deposited during the end of either Cromerian Complex interglacial IV (
Noordbergum) or possibly the Holsteinian. The uppermost 80 m of the co
re contains high frequencies of pre-quaternary and deteriorated palyno
morphs indicating extensive glacial or glaciofluvially reworked sedime
nt. (C) 1998 Elsevier Science Ltd. All rights reserved.