Griffith & Brydone (1911); Brydone (1912) - Offaster pilula Zone: Difference between revisions
Jump to navigation
Jump to search
No edit summary |
No edit summary |
||
| Line 1: | Line 1: | ||
'''Biostratigraphical correlation''': Equates with an interval from within the ''U. anglicus'' Zone to the top of the ''O. pilula'' Zone of current usage (Young & Lake, 1988). | '''Biostratigraphical correlation''': Equates with an interval from within the ''U. anglicus'' Zone to the top of the ''O. pilula'' Zone of current usage (Young & Lake, 1988). | ||
Latest revision as of 15:06, 30 September 2013
Biostratigraphical correlation: Equates with an interval from within the U. anglicus Zone to the top of the O. pilula Zone of current usage (Young & Lake, 1988).
Lithostratigraphical correlation: Equates with the middle to higher part of the Newhaven Chalk Formation of southern England.
| Subzones: | abundant O. pilula Subzone |
| E. depressula Subzone |
Age: Campanian