Griffith & Brydone (1911); Brydone (1912) - Actinocamax plenus Zone: Difference between revisions

Latest revision as of 14:59, 30 September 2013

Biostratigraphical correlation: Equates with the greater part of the M. geslinianum Zone of current usage.

Lithostratigraphical correlation: Equates with the Plenus Marls Member, at the base of the Holywell Nodular Chalk Formation in southern England.

Age: Late Cenomanian

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	'''Biostratigraphical correlation''': Equates with the greater part of the ''M. geslinianum'' Zone of current usage.		'''Biostratigraphical correlation''': Equates with the greater part of the ''M. geslinianum'' Zone of current usage.