Percoidei indet. 1,

Ebersole, Jun A., Cicimurri, David J. & Stringer, Gary L., 2019, Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, inclu, European Journal of Taxonomy 585, pp. 1-274: 212

publication ID

https://doi.org/10.5852/ejt.2019.585

publication LSID

lsid:zoobank.org:pub:181B6FBA-ED75-4BB4-84C4-FB512B794749

DOI

http://doi.org/10.5281/zenodo.3664474

persistent identifier

http://treatment.plazi.org/id/18174D41-FF56-FF7C-FD76-9D2C4FB20BD1

treatment provided by

Plazi

scientific name

Percoidei indet. 1
status

 

Percoidei indet. 1 

Fig. 71View Fig M–N

Material examined

UNITED STATES OF AMERICA – Alabama • 5 otoliths; GLS otolith comparative collection (4 specimens), MSC 39063View Materials  .

Description

Sulcus distinctly divided, clearly heterosulcoid. Wide ostium, much narrower cauda. Cauda is uniform in width, downturned ventrally. Ostium tends to widen ventrally.

Remarks

The five specimens exhibit features of percoids (Suborder Percoidei, Order Perciformes  ). Perciform otoliths are usually distinctly heterosulcoid, with an ostium that widens ventrally and a much narrower cauda that is usually uniform in its width and bent ventrally. Unfortunately, the specimens could not be identified to a specific perciform family.

Stratigraphic and geographic range in Alabama

All of the specimens assigned to Percoidei indet. 1 were recovered from the “upper” Lisbon Formation at site ACh-8. Bartonian, zones NP16 and NP17.