Griffith & Brydone (1911); Brydone (1912) - Marsupites Zone: Difference between revisions
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'''Biostratigraphical correlation''': Equates with the ''M. testudinarius'' Zone and part of the ''U. anglicus'' Zone of current usage (Young & Lake, 1988). | |||
'''Lithostratigraphical correlation''': Equates with an interval in the lower part of the Newhaven Chalk of southern England. | |||
'''Age''': Santonian & basal Campanian | |||
Age: Santonian & basal Campanian | |||
[[Category:Comparison of historical biozonal schemes and nomenclatures with the currently accepted standard biozonal scheme for the UK Chalk Group | 029]] | [[Category:Comparison of historical biozonal schemes and nomenclatures with the currently accepted standard biozonal scheme for the UK Chalk Group | 029]] | ||
Latest revision as of 15:04, 30 September 2013
Biostratigraphical correlation: Equates with the M. testudinarius Zone and part of the U. anglicus Zone of current usage (Young & Lake, 1988).
Lithostratigraphical correlation: Equates with an interval in the lower part of the Newhaven Chalk of southern England.
Age: Santonian & basal Campanian