Coryphaenoides biobtusus, Lin & Brzobohatý & Nolf & Girone, 2017

Lin, Chien-Hsiang, Brzobohatý, Rostislav, Nolf, Dirk & Girone, Angela, 2017, Tortonian teleost otoliths from northern Italy: taxonomic synthesis and stratigraphic significance, European Journal of Taxonomy 322, pp. 1-44 : 5-10

publication ID

https://doi.org/10.5852/ejt.2017.322

DOI

https://doi.org/10.5281/zenodo.3848339

persistent identifier

https://treatment.plazi.org/id/61599612-9462-CE3F-7A05-A73CFCDE9181

treatment provided by

Carolina (2020-05-15 17:07:41, last updated 2024-11-26 04:58:04)

scientific name

Coryphaenoides biobtusus
status

sp. nov.

Coryphaenoides biobtusus sp. nov.

urn:lsid:zoobank.org:act:58E20EDF-1778-4704-924E-886C4028B5A1

Fig. 8 View Fig E–F

Diagnosis

This species is characterised by nearly rectangular and thickset otoliths. The anterior rim of the otoliths is blunt, which makes the highest part of the otolith at the anterior portion. The dorsal rim undulates, with the middle part being concave, while both the anterior and posterior parts are higher and angular. The posterior rim is rounded, smaller than the anterior one. The sulcus is filled with two large elongate collicula.

Etymology

The species epithet is derived from the Latin ‘ biobtusus , a, um ’, which means obtuse (or blunt) on both sides, alluding to the blunt anterior and posterior rims of the otoliths.

Type material examined

Holotype

ITALY: a left otolith ( IRSNB P 9684 , Fig. 8 E View Fig ).

Paratype

ITALY: 1 specimen ( IRSNB P 9685, Fig. 8F View Fig ).

Type locality and horizon

ITALY: Tortonian Clay at Alba, Tanaro River (massive clays, 5 m upstream of reference sandstone ledge).

Dimensions of the holotype

Length = 4.95 mm, height = 3.05 mm, thickness = 1.35 mm.

Description

The otoliths are very thick. The inner face is slightly convex; the outer face is markedly convex in all directions, but with the strongest convexity in the antero-posterior direction ( Fig. 8E View Fig 1 View Fig ). The anterior rim of the otolith is oblique, bears a blunt rostrum, and slightly protrudes in its ventral part; the posterior rim is blunt and shorter than the anterior one. The ventral rim is smooth, curving gently upwards in its posterior portion. The sulcus is pince-nez-shaped (pince-nez is a kind of glasses without ear branches that are worn by pinching the nose), rather shallow, and with unclear ends at both the anterior and the posterior ends. The cristae are well-marked. The collicula are large, highly elevated, nearly rectangular in shape, and lie symmetrical to the junction between ostium and cauda. The dorsal area is narrower than the ventral one. A deep ventral furrow running along the ventral rim is especially evident in the paratype.

Remarks

These two well-preserved otoliths represent adult specimens of this species, which allow a reasonable assignment to the genus Coryphaenoides Gunnerus, 1765 . In some Recent species, for example in C. armatus (Hector, 1875) (see Nolf 2013: pl. 92), the general outline of the otolith and the sulcus configuration are comparable to that of this fossil species.

Anfossi G. & Mosna S. 1971. Alcuni otoliti del Miocene medio-superiore Tortonese. Atti dell'Istituto geologico della Universita di Pavia 21: 138 - 147.

Bassoli G. G. 1906. Otoliti fossili terziari dell'Emilia. Rivista Italiana di Paleontologia 12: 36 - 61.

Brzobohaty R. & Schultz O. 1978. Die Fischfauna des Badeniens. In: Papp A., Cicha I., Senes J. & Steininger F. (eds) M 4 Badenien (Moravien, Wielicien, Kosovien), Chronostratigraphie und Neostratotypen. Miozan der zentralen Paratethys 6: 441 - 465.

Brzobohaty R. & Nolf D. 2000. Diaphus otoliths from the European Neogene (Myctophidae, Teleostei). Bulletin de l'Institut royal des Sciences naturelles de Belgique, Sciences de la Terre 70: 185 - 206.

Girone A., Nolf D. & Cavallo O. 2010. Fish otoliths from the pre-evaporitic (Early Messinian) sediments of northern Italy: their stratigraphic and palaeobiogeographic significance. Facies 56: 399 - 432. https: // doi. org / 10.1007 / s 10347 - 010 - 0212 - 6

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. & Cappetta H. 1980. Les otolithes de teleosteens du Miocene de Montpeyroux (Herault, France). Palaeovertebrata 10 (1): 1 - 28.

Nolf D. & Steurbaut E. 1983. Revision des otolithes de teleosteens du Tortonien stratotypique et de Montegibbio (Miocene Superieur d'Italie septentrionale). Mededelingen van de Werkgroep voor Tertiaire en Kwartaire Geologie 20: 143 - 197.

Nolf D. & Cappetta H. 1989. Otolithes de poissons pliocenes du Sud-Est de la France. Bulletin de l'Institut royal des Sciences naturelles de Belgique, Sciences de la Terre 58: 209 - 271.

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.

Nolf D. 2013. The Diversity of Fish Otoliths, Past and Present. Royal Belgian Institute of Natural Sciences, Brussels.

Robba E. 1970. Otoliti del Tortoniano-tipo (Piemonte). Rivista Italiana di Paleontologia 76: 89 - 172.

Steurbaut E. 1979. Les otolithes de teleosteens des Marnes de Saubrigues (Miocene d'Aquitaine meridionale, France). Palaeontographica A 166 (1 - 3): 50 - 91.

Steurbaut E. 1983. Les otolithes de teleosteens de la Formation de Tanaro (Langhien inferieur du Piemont, Italie septentrionale). Geologica et Paleontologica 17: 255 - 263.

Gallery Image

Fig. 8. Tortonian fish otoliths from northern Italy. A. Coelorinchus caelorhincus (Risso, 1810), Montegibbio (IRSNB P 9772). B. Coryphaenoides contortus (Bassoli, 1906), Sant’Alosio (IRSNB P 9773). C–D. “Merluccius” rattazzii sp. nov., Sant’Alosio (IRSNB P 9686 (holotype)–P 9687). E–F. Coryphaenoides biobtusus sp. nov., Alba, Tanaro (5 m) (IRSNB P 9684 (holotype)–P 9685). G–H. Nezumia aff. sclerorhynchus (Valenciennes, 1838), Alba, Tanaro (5 m) (IRSNB P 9774–P 9775). I–J. Moridae indet., Sant’Agata Fossili (IRSNB P 9776–P 9777). K. Nezumia ornata (Bassoli, 1906), Montegibbio (IRSNB P 9778). L–M. Coelorinchus robustus (Robba, 1970); L. Stazzano, M. Sant’Alosio (IRSNB P 9779–P 9780). N. Gadiculus labiatus (Schubert, 1905), Torrente Stirone (IRSNB P 9781). O–P. Melanonus paralyconus Schwarzhans, 1986, Mondovi, Madonna della Neve (IRSNB P 9782– P 9783). Q–R. Melanonus triangulus (Robba, 1970), Costa Vescovato (IRSNB P 9784–P 9785). S. Gadiculus argenteus Guichenot, 1850, Torrente Stirone (IRSNB P 9786). 1 = ventral view; 2 = inner view. Scale bars = 1 mm.

Gallery Image

Fig. 1. Map showing the sampling sites.

IRSNB

Institut Royal des Sciences Naturelles de Belgique

Kingdom

Animalia

Phylum

Chordata

Class

Actinopterygii

Order

Gadiformes

Family

Macrouridae

SubFamily

Macrourinae

Genus

Coryphaenoides