Chalk Biozone 16 - Alterbidinium acutulum: Difference between revisions

From MediaWiki
Jump to navigation Jump to search
Newer edit →
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 " '''Age.''': Early Maastrichtian. '''Macrofaunal correlation''': Lower ''B. occidentalis'' Zone. '''Definition:''' The interval between the LAD of ''Neoeurysphaeridium gla..."
 
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:
'''Age.''': Early Maastrichtian.
'''Age.''': Early Maastrichtian.


Revision as of 11:18, 30 September 2013

Age.: Early Maastrichtian.

Macrofaunal correlation: Lower B. occidentalis Zone.

Definition: The interval between the LAD of Neoeurysphaeridium glabrum to the LAD of Alterbidinium acutulum.

Comments: The LAD of Alterbidinium acutulum lies within the B. occidentalis Zone (Wilson, 1974; Schiøler & Wilson, 1993).

Lithostratigraphical correlation: The Little Marl Point Chalk and the Beacon Hill Grey Chalk members (East Anglia) and the Mackerel Formation (North Sea).

Retrieved from "http://earthwise-staging.bgs.ac.uk/index.php?title=Chalk_Biozone_16_-_Alterbidinium_acutulum&oldid=1575"