Rowe (1900) - Terebratulina gracilis Zone: Difference between revisions
Jump to navigation
Jump to search
(Created page with " '''Biostratigraphical correlation''': Equates with the ''T. lata'' Zone and basal ''S. plana'' Zone of current usage. '''Lithostratigraphical correlation''': Equates with t...") |
No edit summary |
||
| Line 1: | Line 1: | ||
'''Biostratigraphical correlation''': Equates with the ''T. lata'' Zone and basal ''S. plana'' Zone of current usage. | '''Biostratigraphical correlation''': Equates with the ''T. lata'' Zone and basal ''S. plana'' Zone of current usage. | ||
Latest revision as of 13:40, 30 September 2013
Biostratigraphical correlation: Equates with the T. lata Zone and basal S. plana Zone of current usage.
Lithostratigraphical correlation: Equates with the New Pit Chalk Formation and lower part of the Lewes Nodular Chalk Formation in southern England. Rowe (1900) placed the top of this zone at the Bridgewick Marl (Wood, WH/95/31R).
Age: Turonian