Rowe (1900) - Terebratulina gracilis Zone: Difference between revisions

From MediaWiki
Jump to navigation Jump to search
Dbk (talk | contribs)
Image-reviewer, administrator, autoreview, Bots, Bureaucrats, commentadmin, editor, Interface administrators, reviewer, smwadministrator, smwcurator, Administrators, Upload Wizard campaign editors, widgeteditor
18,104 edits
Created page with " '''Biostratigraphical correlation''': Equates with the ''T. lata'' Zone and basal ''S. plana'' Zone of current usage. '''Lithostratigraphical correlation''': Equates with t..."
 
Dbk (talk | contribs)
Image-reviewer, administrator, autoreview, Bots, Bureaucrats, commentadmin, editor, Interface administrators, reviewer, smwadministrator, smwcurator, Administrators, Upload Wizard campaign editors, widgeteditor
18,104 edits
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 14:40, 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

Retrieved from "http://earthwise-staging.bgs.ac.uk/index.php?title=Rowe_(1900)_-_Terebratulina_gracilis_Zone&oldid=1688"