Xenodermichthys senesi Nolf & Brzobohatý, 1994
publication ID |
https://doi.org/10.5852/ejt.2017.322 |
persistent identifier |
https://treatment.plazi.org/id/61599612-9468-CE38-79A2-A222FC8894BA |
treatment provided by |
Carolina (2020-05-15 17:07:41, last updated 2020-05-15 17:07:44) |
scientific name |
Xenodermichthys senesi Nolf & Brzobohatý, 1994 |
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Xenodermichthys senesi Nolf & Brzobohatý, 1994
A large specimen ( Fig. 2P) in our material is somewhat higher in its overall shape and the antero-dorsal angle is more pronounced than those of the similar-sized Chattian type specimens from the Aquitaine Basin, southwest France ( Nolf & Brzobohatý 1994: pl. 2, figs 5, 11); the smaller specimens in our material ( Fig. 2 N–O) are characterised by thick otoliths and a convex outer face, and are reasonably similar to the type series from Aquitaine ( Nolf & Brzobohatý 1994: pl. 2, figs 6–10). Because modern alepocephalid otoliths commonly show a great intraspecific variability (e.g., Nolf & Brzobohatý 1994: pl. 2, figs 1–4), the specimens in question are all assigned to X. senesi . The studied material, including large and small specimens, allows us to refer the otoliths figured by Lin et al. (2015: fig. 2(5), as Xenodermichthys aff. copei (Gill, 1884)) to juvenile specimens of X. senesi .
Brzobohaty R. 1994. Die Fischotolithen des Badenien von Gainfarn, Niederosterreich (Mittelmiozan, Wiener Becken). Annalen des Naturhistorischen Museums Wien 96 A: 67 - 93.
Lin C. - H., Girone A. & Nolf D. 2015. Tortonian fish otoliths from turbiditic deposits in northern Italy: taxonomic and stratigraphic significance. Geobios 48: 249 - 261. https: // doi. org / 10.1016 / j. geobios. 2015.03.003
Nolf D. & Brzobohaty R. 1994. Fish otoliths from the Late Oligocene (Eger and Kiscell Formations) in the Eger area (northeastern Hungary). Bulletin de l'Institut royal des Sciences naturelles de Belgique, Sciences de la Terre 64: 225 - 252.
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Harvard University - Arnold Arboretum |
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