Published June 4, 2024 | Version v1
Taxonomic treatment Open

Neobythites stringeri Goode & Bean 1885

  • 1. Biodiversity Research Center, Academia Sinica, 128 Academia Road, Seca 2, Nankang, Taipei 11529, Taiwan.
  • 2. Royal Belgian Institute of Natural Sciences, 29 Vautier Street, 1000 Brussels, Belgium. & Department of Earth and Environmental Sciences, KU Leuven, Celestijnenlaan 200 E, 3001 Leuven, Belgium.
  • 3. Royal Belgian Institute of Natural Sciences, 29 Vautier Street, 1000 Brussels, Belgium.

Description

Neobythitesstringeri sp. nov.

urn:lsid:zoobank.org:act: A1E1BA6B-78E3-4FCC-BAE7-35737F87131D

Fig. 8D–E

Diagnosis

OL/OH = 1.6–1.8, OsL/CaL = 2.9–4.1. Fusiform otoliths with blunt antero-dorsal bulge and pointed posterior rim.Anterior rim largely blunt. Sulcus wide, elongate, well-divided. Ostium markedly elongate; cauda oval, pointing downward.

Etymology

This species is dedicated to Gary L. Stringer (University of Louisiana at Monroe) for his major contributions to the knowledge of the fossil otoliths from the USA.

Type material examined

Holotype UNITED STATES OF AMERICA • Right otolith; Alabama, Hatchetigbee Bluff, Hatchetigbee Formation; Fig. 8E; IRSNB P 10749.

Paratypes (3 in total) UNITED STATES OF AMERICA • 3 otoliths of which one is figured: Fig. 8D; same collection data as for holotype; IRSNB P 10748.

Type locality and horizon

United States of America, Hatchetigbee Bluff (Alabama), Hatchetigbee Formation.

Dimensions of the holotype

Length = 4.36 mm; height = 2.43 mm; thickness = 1.21 mm.

Description

This species is characterized by robust and fusiform otoliths that bear a blunt antero-dorsal bulge, forming the highest and thickest part of the otoliths in the anterior portion (Fig. 8E 1). The otoliths taper in the posterior part and end with a pointed tip. The ventral rim is regularly curved. The inner face is convex; the outer face is essentially flat, becoming thinner towards the ventral and posterior rims. The sulcus occupies nearly the entire length of the inner face and is constituted by a long, horizontal ostium and a very short, downward-bent cauda. A shallow dorsal depression is observed above the central part of the crista superior. The ventral area is slightly larger than the dorsal one.

Remarks

At first glance, the otoliths of “ N.stringeri sp. nov. are very similar to those of N. longesulcatus sp. nov. (see above), but they can be distinguished by the short, strongly bent cauda and larger ventral area in the former species. “ Neobythitesstringeri is only known form the type locality.

Stratigraphic and geographic distribution

Ypresian: Hatchetigbee Formation, Alabama.

Notes

Published as part of Lin, Chien-Hsiang, Steurbaut, Etienne & Nolf, Dirk, 2024, Early Eocene fish otoliths from the eastern and southern USA, pp. 203-240 in European Journal of Taxonomy 935 on pages 223-224, DOI: 10.5852/ejt.2024.935.2557, http://zenodo.org/record/11526096

Files

Files (2.7 kB)

Name Size Download all
md5:289253214ae2d3021892423eac4fab8d
2.7 kB Download

System files (18.5 kB)

Name Size Download all
md5:e1eb77041a32a33d5c135ce4d5f7e05e
18.5 kB Download

Linked records

Additional details

Identifiers

URL
http://treatment.plazi.org/id/03971F35FFF0FFB5995A2A07FD62FD61
LSID
urn:lsid:zoobank.org:act:E7434385-3EEF-4F21-B545-519B63B9EA49

Biodiversity

Collection code
IRSNB
Material sample ID
P 10748 , P 10749
Scientific name authorship
Goode & Bean
Kingdom
Animalia
Phylum
Chordata
Order
Ophidiiformes
Family
Ophidiidae
Genus
Neobythites
Species
stringeri
Taxon rank
species
Type status
holotype , paratype
Taxonomic concept label
Neobythites stringeri Goode, 1885 sec. Lin, Steurbaut & Nolf, 2024