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The AAPG/Datapages Combined Publications Database

GCAGS Transactions

Abstract


Gulf Coast Association of Geological Societies Transactions
Vol. 22 (1972), Pages 305-313

Late Quaternary Climates Indicated by Foraminifers from the Southwestern Gulf of Mexico

Bruce R. Sidner (1), C. Wylie Poag (1)

ABSTRACT

The planktonic foraminiferal assemblages were examined in 22 deep-sea cores from the Bay of Campeche in the southwestern Gulf of Mexico. Analysis of these assemblages clearly indicates three distinct successive biofacies during the Late Pleistocene and Holocene. The biofacies are defined by variations in the relative percentages of the Globorotalia cultrata group and Turborotalia inflata. Excellent correlation can be made between these biofacies and those found in a core from the continental slope in the northern Gulf of Mexico. These biofacies are interpreted as representing climatic changes.


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