Abstract
The Mid-Waipara section has yielded a succession of planktonic Foraminifera which can be correlated with similar Danian, Upper Paleocene, and Lower Eocene faunas described from Europe, Trinidad, and the Gulf and Atlantic Coastal Plains of the United States (Berggren, 1962; Bolli, 1957; Loeblich and Tappan, 1957).

This publication has 0 references indexed in Scilit: