Percoidei indet. 1, Giill, 1861
publication ID |
https://doi.org/ 10.5852/ejt.2019.585 |
publication LSID |
lsid:zoobank.org:pub:181B6FBA-ED75-4BB4-84C4-FB512B794749 |
DOI |
https://doi.org/10.5281/zenodo.3664474 |
persistent identifier |
https://treatment.plazi.org/id/18174D41-FF56-FF7C-FD76-9D2C4FB20BD1 |
treatment provided by |
Plazi |
scientific name |
Percoidei indet. 1 |
status |
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Fig. 71 View Fig M–N
Material examined
UNITED STATES OF AMERICA – Alabama • 5 otoliths; GLS otolith comparative collection (4 specimens), MSC 39063 .
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.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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