Pollen analyses of the cromer forest bed series in east anglia with an appendix on the non-marine mollusca
The deposits which have been analyzed lie on the coast between West Runton and Corton. No single pollen diagram shows the complete vegetational history of the period during which the Cromer Forest Bed Series was laid down, but, when considered together, the diagrams show evidence of a sequence which has been divided tentatively into three zones. The first of these (zone a) shows a predominance of Betula and then Pirns ; pollen of other trees is either absent or insignificant, and the non-arboreal pollen values are very high in the early part of the zone. Alnus is strongly represented throughout zone b, which shows the rise and subsequent decline of mixed-oak forest trees and a similar but later change in Picea . The mixed-oak forest trees disappear in zone c, Alnus and Picea decrease and probably disappear and Betula and Pinus return to dominance. It is possible that these three zones represent a sequence in time; if so, the changes reflect a climatic change from cool or cold conditions through a warm period to increasing cold. The pollen zones could not be related satisfactorily to the divisions of the Cromer Forest Bed Series which were established by Clement Reid. The vegetational zones of the Cromer Forest Bed Series are compared with those of other deposits which are believed to be of the same age or to belong to subsequent interglacials. It appears that the Cromerian diagrams have a number of features in common which may be used to distinguish them from diagrams referred to deposits of other interglacials. The non-marine molluscs found in the Cromer Forest Bed Series at West Runton are listed by Mr B. W. Sparks, who considers that they indicate the formation of that part of the deposit in a marsh cut by sluggish drainage channels.