An Eocene wrasse (Perciformes; Labridae) from Seymour Island

A nearly complete lower pharyngeal tooth-plate from a large (over 60 cm long) fossil wrasse (Perciformes: Labridae) was recently recovered from the middle to late Eocene La Meseta Formation on Seymour Island, Antarctic Peninsula. This find increases the number of teleosts from the Eocene of Antarcti...

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Bibliographic Details
Published in:Antarctic Science
Main Author: Long, Douglas J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Antarctic
Southern Ocean
Antarctic Peninsula
Seymour
Seymour Island
Antarc*
Antarctic Science
Antarctica
Online Access:http://dx.doi.org/10.1017/s095410209200035x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410209200035X
Description
Summary:A nearly complete lower pharyngeal tooth-plate from a large (over 60 cm long) fossil wrasse (Perciformes: Labridae) was recently recovered from the middle to late Eocene La Meseta Formation on Seymour Island, Antarctic Peninsula. This find increases the number of teleosts from the Eocene of Antarctica to five taxa, and further illustrates the diversity of the ichthyofauna in the Eocene Weddellian Sea prior to wide-scale climatic change in the Southern Ocean. The fossil wrasse represents the first occurrence of this family in Antarctica, and is one of the oldest fossils of this family from the Southern Hemisphere. Wrasses are not found in Antarctic waters today, and probably became extinct during the Oligocene due to a combination of climatic change, loss of shallow-water habitat, and changes in the trophic structure of the Wedell Sea.

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