Chalk Biozone 8 - Florentinia deanei: Difference between revisions
Created page with " '''Age:''' Early Coniacian to Mid Coniacian. '''Macrofaunal correlation:''' The ''M. cortestudinarium'' Zone. '''Definition:''' The interval between the LAD of ''Stepho..." |
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'''Age:''' Early Coniacian to Mid Coniacian. | '''Age:''' Early Coniacian to Mid Coniacian. | ||
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'''Lithostratigraphical correlation''': The upper Lewes Nodular Chalk Formation (Southern Province), the Burnham Chalk Formation (Northern Province) and the Mackerel Formation (North Sea). | '''Lithostratigraphical correlation''': The upper Lewes Nodular Chalk Formation (Southern Province), the Burnham Chalk Formation (Northern Province) and the Mackerel Formation (North Sea). | ||
[[Category:Palynological_zonation | ]] | [[Category:Palynological_zonation | 008]] | ||
Latest revision as of 11:08, 30 September 2013
Age: Early Coniacian to Mid Coniacian.
Macrofaunal correlation: The M. cortestudinarium Zone.
Definition: The interval between the LAD of Stephodinium coronatum to the LAD of Florentinia deanei.
Comments: Stephodinium coronatum has a well established range top close to the base of the M. cortestudinarium Zone (Foucher, 1979; Costa & Davey, 1992). The top of this biozone is also delineated by the LADs of Florentinia tenera and Psaligonyaulax deflandrei (see Foucher, 1979; Costa & Davey, 1992; Foucher & Monteil, 1998). The FAD of Florentinia tenera subdivides this biozone (Foucher & Monteil, 1998).
Lithostratigraphical correlation: The upper Lewes Nodular Chalk Formation (Southern Province), the Burnham Chalk Formation (Northern Province) and the Mackerel Formation (North Sea).