Griffith & Brydone (1911); Brydone (1912) - E. depressula Subzone

From Earthwise
Revision as of 14:07, 30 September 2013 by Dbk (talk | contribs)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
Jump to navigation Jump to search

Biostratigraphical correlation: Equates to an interval from within the U. anglicus Zone to a little above the Subzone of abundant O. pilula of current usage (Young & Lake, 1988).

Lithostratigraphical correlation: Equates with the middle part of the Newhaven Chalk Formation of southern England.

Age: Campanian