Abstract

"It is probable that all the planktonic foraminifera in the type Thanetian are derived. They represent re-working of Campanian deposits during the initial phase of the Thanet cycle of deposition and of Campanian and Danian deposits during the deposition of the Reculver silts, immediately prior to the filling of the Anglo-French- Belgian sedimentary basin with deltaic sediments."

You do not currently have access to this article.