Gobionellus Girard, 1858

Schwarzhans, Werner W. & Aguilera, Orangel A., 2024, Otoliths of the Gobiidae from the Neogene of tropical America, Swiss Journal of Palaeontology (13) 143 (1), pp. 1-129 : 98

publication ID

https://doi.org/10.1186/s13358-023-00302-5

persistent identifier

https://treatment.plazi.org/id/492D87AA-FFCA-FF85-0236-FE506167FADF

treatment provided by

Felipe

scientific name

Gobionellus Girard, 1858
status

 

Genus Gobionellus Girard, 1858 View in CoL

Te genus Gobionellus contains seven recognized species according to Froese and Pauly (2023): three in the East Pacific, three West Atlantic, and one in the East Atlantic. Otoliths are known from Gobionellus liolepis (Meek & Hildebrand, 1928) ( Fig. 44a–b View Fig ), G. dague (Eigenmann, 1918) ( Fig. 44e View Fig ), and G. microdon (Gilbert, 1892)

( Fig. 44g View Fig ) from the East Pacific; G. oceanicus (Pallas, 1770) ( Fig. 44d View Fig ) from the West Atlantic; and G. occidentalis (Boulenger, 1909) from the East Atlantic. Otoliths are not known from the two remaining West Atlantic species, i.e., G. munizi Vergara, 1978 , endemic to Cuba, and G. stomatus Starks, 1913 , endemic to Brazil.

Te otoliths of Gobionellus are characterized by a high-bodied shape (OL:OH= 0.8–1.0) with a much-expanded postdorsal region, a commonly strongly sculptured dorsal rim, a relatively short and somewhat simplified sole-shaped sulcus (OL:SuL =1.8–2.2) with a low inclination angle (3–10°), and the ventral furrow running relatively distant from the ventral rim of the otolith and commonly opening to the anterior-ventral and posterior-ventral rims of the otolith. Te otoliths are usually thin with a concave to flat outer face. A subcaudal iugum is usually not present, except in G. microdon , where it is large and well developed.

Specimens of Gobionellus are collected in shallow estuarine, tide pool, and mangrove environments ( Pezold, 2004).

Kingdom

Animalia

Phylum

Chordata

Order

Perciformes

Family

Gobiidae

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