Eutawichthys, STRINGERI, 2018

Stringer, Gary L. & Sloan, James Carson, 2023, First Cretaceous teleostean otolith assemblage (Arkadelphia Formation, upper Maastrichtian) from Arkansas, USA, early Gadiformes, and the Western Interior Seaway, PaleoBios 40 (1994), pp. 1-39 : 18-19

publication ID

https://doi.org/ 10.5070/P940361192.

publication LSID

lsid:zoobank.org:pub:3B70D32F-9BF0-4595-AF4B-45ADEE03B204

DOI

https://doi.org/10.5281/zenodo.11474236

persistent identifier

https://treatment.plazi.org/id/2B4F878B-2573-FF8E-FC11-FA53FE30FDB9

treatment provided by

Felipe

scientific name

Eutawichthys
status

 

EUTAWICHTHYS CF. E. STRINGERI

FIG. 8F View Figure 8

Material— 48 specimens, specimen figured, DMNH 2021-09- 28 About DMNH . About DMNH

Description and Remarks— The specimens assigned to Eutawichthys stringeri are characterized by an anterior margin with a broad, dorsally shifted rostrum, a broadly rounded dorsal margin, a broadly rounded posterior margin, and a moderately deep, gently and regularly curved convex ventral margin. The inner face is slightly convex with a shallow, moderately wide sulcus divided into an ostium and cauda. The ostium is curved upwards towards the dorsal margin of the rostrum. The cauda is about the same length as the ostium and is oriented upwards. The cauda has a rounded tip that ends well before the posterior margin.

Excellent figures of the ontogeny of E. stringeri are found in Schwarzhans et al. (2018b) and readily illustrate the differences between it and other species of Eutawichthys . The distribution of E. stringeri is not nearly as widespread as E. maastrichtiensis and E. zideki . It has only been previously reported from the Woodbury Formation (early–middle Campanian) of New Jersey ( Stringer et al. 2016) and the Eutaw Formation (upper Santonian) of Alabama ( Schwarzhans et al. 2018b), where it represents the most abundant species.

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