Biomarker 13: Praeglobotruncana stephani FDO: Difference between revisions

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Created page with " Found in the Herring Formation of the Southern, Central and southern pat of the Northern North Sea (earliest Mid-Turonian, ''lata''/''Mytiloides'' zonal boundary interval). ..."
 
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Found in the Herring Formation of the Southern, Central and southern pat of the Northern North Sea (earliest Mid-Turonian, ''lata''/''Mytiloides'' zonal boundary interval). Planktonic species become common, e.g. ''Praeglobotruncana stephani, P. gibba, Dicarinella hagni'' and ''D. imbricata'' together with the benthonic species ''Lingulogavelinella globosa'' (Burnhill & Ramsey, 1981; King ''et al''., 1989; Crittenden, ''et al''., 1991).
Found in the Herring Formation of the Southern, Central and southern pat of the Northern North Sea (earliest Mid-Turonian, ''lata''/''Mytiloides'' zonal boundary interval). Planktonic species become common, e.g. ''Praeglobotruncana stephani, P. gibba, Dicarinella hagni'' and ''D. imbricata'' together with the benthonic species ''Lingulogavelinella globosa'' (Burnhill & Ramsey, 1981; King ''et al''., 1989; Crittenden, ''et al''., 1991).


'''Correlation''': This biomarker can be placed at the top of BGS foraminiferal Biozone 9 or in the basal part of Biozone 10 (Wilkinson, 2000).
'''Correlation''': This biomarker can be placed at the top of BGS foraminiferal Biozone 9 or in the basal part of Biozone 10 (Wilkinson, 2000).


[[category:Foraminiferal zonation | 013]]
[[Category:Offshore foraminiferal biomarkers in the Chalk Group | 013]]

Latest revision as of 10:57, 1 October 2013

Found in the Herring Formation of the Southern, Central and southern pat of the Northern North Sea (earliest Mid-Turonian, lata/Mytiloides zonal boundary interval). Planktonic species become common, e.g. Praeglobotruncana stephani, P. gibba, Dicarinella hagni and D. imbricata together with the benthonic species Lingulogavelinella globosa (Burnhill & Ramsey, 1981; King et al., 1989; Crittenden, et al., 1991).

Correlation: This biomarker can be placed at the top of BGS foraminiferal Biozone 9 or in the basal part of Biozone 10 (Wilkinson, 2000).

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