Eutawichthys

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

publication ID

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

publication LSID

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

persistent identifier

https://treatment.plazi.org/id/2B4F878B-2573-FF89-FF4B-FC2DFBF9FE0D

treatment provided by

Felipe

scientific name

Eutawichthys
status

 

EUTAWICHTHYS SCHWARZHANS, HUDDLESTON, AND TAKEU-

CHI, 2018b

EUTAWICHTHYS MAASTRICHTIENSIS ( NOLF AND STRINGER, 1996)

FIG. 8D View Figure 8

Material— 21 specimens, specimen figured, DMNH 2021-09- 26 View Materials . View Materials

Description and Remarks— Eutawichthys maastrichtiensis has a nearly circular to slightly oval outline (sensu Smale et al. 1995). The dorsal margin is irregular, while the ventral margin can have crenulations that are often obliterated by erosion. The thin sagitta is only slightly convex with a distinctive, long sulcus (heterosulcoid type) that is wide and continuously curved. The cauda curves diagnostically dorsally in its posterior section. There is a depressed area that is fairly distinct above the center of the sulcus.

Eutawichthys maastrichtiensis was designated as an apogonid for many years, and there are certainly resemblances to the apogonids. Its designation as a berycid is discussed at length in Stringer et al. (2016) and is more congruent with molecular studies such as Betancur-R. et al. (2013) that indicate a much later divergence for the apogonids (around 45 Ma). The fossil-based genus Eutawichthys was erected by Schwarzhans et al. (2018b). Eutawichthys maastrichtiensis is known from several Cretaceous formations including the Severn Formation of Maryland ( Huddleston and Savoie 1983), the Woodbury Formation of New Jersey ( Stringer et al. 2016), the Eutaw Formation of Alabama ( Schwarzhans et al. 2018a), the Tar Heel Formation of North Carolina (Stringer et al. 2018), the Coon Creek Formation of Tennessee ( Stringer 2016b), the Ripley Formation of Mississippi (Stringer et al. 2020), and the Kemp Clay of Texas ( Schwarzhans and Stringer 2020a).

CHI

University of Illinois

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