Cretacoeus planktonic foraminifera from Exmouth Plateau, Australia

An Albian to Maestrichtian planktonic foraminiferal biozonation for the Exmouth Plateau is proposed, based on the detailed analysis of pelagic successions at Sites 761 and 762 and correlation with Site 763. Twelve zones and two subzones are recognized. The Albian and Cenomanian zones, currently only...

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Bibliographic Details
Main Author: Wonders, A A H
Format: Dataset
Language:English
Published: PANGAEA 1992
Subjects:
122-761B
122-762C
DRILL
Drilling/drill rig
Joides Resolution
Leg122
Ocean Drilling Program
ODP
South Indian Ridge
South Indian Ocean
Indian
Planktonic foraminifera
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.729231
https://doi.org/10.1594/PANGAEA.729231
Description
Summary:An Albian to Maestrichtian planktonic foraminiferal biozonation for the Exmouth Plateau is proposed, based on the detailed analysis of pelagic successions at Sites 761 and 762 and correlation with Site 763. Twelve zones and two subzones are recognized. The Albian and Cenomanian zones, currently only three, can probably be subdivided into several more. The ranges of the Tethyan index species Globotruncana ventricosa and Globotruncanita elevata are discussed and found to differ from the ones usually given in standard zonal schemes. The planktonic foraminiferal succession is interpreted as a mid-latitude one in which the Tethyan influence started suddenly in the late Albian and then fluctuated throughout the Late Cretaceous, with a long low-diversity interval during the Campanian to middle Maestrichtian.

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