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A new middle Eocene protocetid whale (Mammalia: Cetacea: Archaeoceti) and associated biota from Georgia

Published online by Cambridge University Press:  14 July 2015

Richard C. Hulbert Jr.
Affiliation:
1Department of Geology and Geography, Georgia Southern University, Statesboro 30460-8149
Richard M. Petkewich
Affiliation:
1Department of Geology and Geography, Georgia Southern University, Statesboro 30460-8149
Gale A. Bishop
Affiliation:
1Department of Geology and Geography, Georgia Southern University, Statesboro 30460-8149
David Bukry
Affiliation:
2United States Geological Survey, MS-915, 345 Middlefield Road, Menlo Park, California 94025
David P. Aleshire
Affiliation:
3Department of Biology, Georgia Southern University, Statesboro 30460-8042

Abstract

A shallow-marine fossil biota was recovered from the Blue Bluff unit (formerly part of the McBean Formation) in the Upper Coastal Plain of eastern Georgia. Biochronologically significant mollusks (e.g., Turritella nasuta, Cubitostrea sellaeformis, Pteropsella lapidosa) and calcareous nannoplankton (e.g., Chiasmolithus solitus, Reticulofenestra umbilica, Cribocentrum reticulatum) indicate a latest Lutetian-earliest Bartonian age, or about 40 to 41 Ma. Georgiacetus vogtlensis new genus and species is described from a well-preserved, partial skeleton. Georgiacetus is the oldest known whale with a true pterygoid sinus fossa in its basicranium and a pelvis that did not articulate directly with the sacral vertebrae, two features whose acquisitions were important steps toward adaptation to a fully marine existence. The posterior four cheek teeth of G. vogtlensis form a series of carnassial-like shearing blades. These teeth also bear small, blunt accessory cusps, which are regarded as being homologous with the larger, sharper accessory cusps of basilosaurid cheek teeth.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

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