Biomarker 14: Rotalipora cushmani FDO: Difference between revisions

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Created page with " Found in the Hidra Formation (Late Cenomania, ''geslinianum'' Zone)of the Southern and Central North Sea Basin. Planktonic species such as ''Hedbergella brittonensis'' and '..."
 
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Found in the Hidra Formation (Late Cenomania, ''geslinianum'' Zone)of the Southern and Central North Sea Basin. Planktonic species such as ''Hedbergella brittonensis'' and ''H. delrioensis'' are abundant and ''Rotalipora greenhornensis'' is occasionally present.  Benthonic ''Stensioeina pokornyi'' may also occur in the Central North Sea.  See Burnhill & Ramsay (1981), King ''et al''. (1989) and Crittenden ''et al''. (1991).
Found in the Hidra Formation (Late Cenomania, ''geslinianum'' Zone)of the Southern and Central North Sea Basin. Planktonic species such as ''Hedbergella brittonensis'' and ''H. delrioensis'' are abundant and ''Rotalipora greenhornensis'' is occasionally present.  Benthonic ''Stensioeina pokornyi'' may also occur in the Central North Sea.  See Burnhill & Ramsay (1981), King ''et al''. (1989) and Crittenden ''et al''. (1991).


'''Correlation''': This biomarker can be placed at the top of BGS foraminiferal Biozone 7 (Wilkinson, 2000).
'''Correlation''': This biomarker can be placed at the top of BGS foraminiferal Biozone 7 (Wilkinson, 2000).


[[category:Foraminiferal zonation | 014]]
[[Category:Offshore foraminiferal biomarkers in the Chalk Group | 014]]

Latest revision as of 11:57, 1 October 2013

Found in the Hidra Formation (Late Cenomania, geslinianum Zone)of the Southern and Central North Sea Basin. Planktonic species such as Hedbergella brittonensis and H. delrioensis are abundant and Rotalipora greenhornensis is occasionally present. Benthonic Stensioeina pokornyi may also occur in the Central North Sea. See Burnhill & Ramsay (1981), King et al. (1989) and Crittenden et al. (1991).

Correlation: This biomarker can be placed at the top of BGS foraminiferal Biozone 7 (Wilkinson, 2000).

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