Trachycorystes menezesi, Britski & Akama, 2011

Britski, Heraldo A. & Akama, Alberto, 2011, New species of Trachycorystes Bleeker, with comments on other species of the genus (Ostariophysi: Siluriformes: Auchenipteridae), Neotropical Ichthyology 9 (2), pp. 273-279: 274-278

publication ID 10.1590/S1679-62252011000200004

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scientific name

Trachycorystes menezesi

new species

Trachycorystes menezesi   , new species

Fig. 1 View Fig

Holotype. MZUSP 104671, 185.7 mm SL, igarapé do Aeroporto , right bank tributary of rio Aripuanã, Aripuanã, Mato Grosso State, Brazil, 9 Nov 1976, Equipe Ictiologia INPA.  

Paratypes. Brazil, Mato Grosso State, Município de Aripuanã : MZUSP 37601 View Materials , 62 View Materials , 32.7 View Materials   - 160.0 mm SL, 1 c&s, same data as holotype. INPA 35313 View Materials , 5 View Materials   , 71.2-155.2 mm SL, same data as holotype. ANSP 191672 View Materials , 5 View Materials   , 53.5-124.4 mm SL, same data as holotype. MZUSP 63287 View Materials   4, 179.1- 199.2 mm SL, igarapé Genipapo, right bank tributary of rio Aripuanã, 70 km above Dardanelos and Andorinhas falls , 14 Nov 1976, Equipe Ictiologia INPA. MZUSP  

104672, 3, 151.6-189.3, rio Aripuanã, 2 km above Dardanelos and Andorinhas falls, near Cachoeira dos Patos, 13 Oct 2005, Francisco Machado.

Diagnosis. Trachycorystes menezesi   can be distinguished from its sole congener T. trachycorystes   by having: jaws equal in length (vs. lower jaw longer, prognathous in T. trachycorystes   ); skull roof covered by thick integument concealing bony sculptures (vs. skull roof covered by thin integument, bony sculptures visible); inner mental barbel thin and very short, not reaching base of outer mental barbel (vs. inner mental barbel thicker, extending to or beyond base of outer mental barbel); dorsal-fin spine serrated only along posterior margin (vs. dorsal-fin spine serrated only along anterior margin); caudal fin weakly forked (vs. emarginate); gas bladder simple, without diverticula (vs. gas bladder with three posterior diverticula, one medial and paired posterolateral).

Description. Morphometrics presented in Table 1. Body short, stout, approximately round in cross section in front of dorsalfin origin, compressed at caudal peduncle. Head about as wide as long, depressed anteriorly; interorbital region slightly convex in frontal view. Dorsal profile strongly convex from upper lip to second nostril; straight, ascending gradually from that point to dorsal-fin origin; shallowly convex from dorsal fin to adipose fin; shallowly concave from adipose fin to caudal fin. Ventral profile convex from lower lip to anal fin, belly more or less protruded depending on stomach repletion; straight, gradually ascending along anal-fin base and concave between anal and caudal fins.

Integument on skull roof relatively thick, concealing bony sculptures. Facial and opercular bones also covered with somewhat thick integument. Posterior cleithral process long, reaching two thirds of pectoral-spine length, dorsal margin partially covered by integument, surface longitudinally striated, ventral portions covered by very thin integument.

Jaws equal, lower jaw not protruding. Mouth terminal, wide, posterior angle aligned with vertical through anterior margin of eye. Premaxillary tooth patch rounded laterally, without posteriorly projected angle. Dentary tooth patch laterally with angle projected posteriorly. Viliform teeth distributed in about eight series in each premaxillary and dentary patch. Branchiostegal membranes broadly attached to isthmus. Gill opening reduced, not extending ventrally to base of pectoral-fin spine. Gill arches covered by somewhat thick integument, without gill-rakers. Eye lateral; moderately inclined anteromedially and covered by integument (orbital margin not free). Anterior nostril tubular; posterior nostril with a small medial flap. Fontanel elliptical, elongated longitudinally, situated between dorsal margins of orbits.

Barbels slightly flattened dorsoventrally. Maxillary barbel short, extending to pectoral-fin spine or slightly beyond its base, not surpassing pectoral-fin base. Basal portion of maxillary barbel sheltered in deep groove bellow eye that becomes gradually shallower toward opercular area. Outer mental barbel short, extending half the distance from its base to pectoral-fin base. Inner mental barbel very thin and short, not reaching base of outer mental barbel.

Lateral line pores extending along sides to caudal-fin base and conspicuous due to accompanying white (despigmented) points; about eight vertical columns of white points along body; columns extending to near dorsal profile, shorter ventrally.

Dorsal fin roughly triangular, its origin at vertical through tip of posterior cleithral process. Dorsal-fin rays I+6. Dorsalfin spine shorter than first two or three branched rays.Anterior margin of dorsal spine smooth or rough, not serrated; posterior margin with 5 to 24 retrorse serrations (number increasing with size of specimen). Adipose fin short, teardrop shaped with posterior base at vertical through base of last anal-fin ray. Pectoral fin roughly triangular, its origin just posterior to gill opening. Pectoral-fin rays I+7. Ossified portion of pectoral spine same length or shorter than first branched rays. Tip of spine with minute unossified segmented portion; spine finely striated above and below and with well developed serrations along entire anterior and posterior margins; anterior margin with 20-31 conical antrorse serrations; posterior margin with 13-26 retrorse serrations enlarged distally; postero-lateral border of each serration with two or three minute spines. Posterior margin of depressed pectoral fin distant from pelvicfin origin. Pelvic fin roughly ovoid. Pelvic-fin base posterior to vertical through posterior insertion of dorsal fin. Pelvic-fin rays i+8. Pelvic-fin posterior margin rounded, reaching analfin origin.Anal-fin base long, distal margin straight to shallowly convex.Anal-fin rays iii,16 (4*), iii,17 (10), iii,18 (7) or iii,19 (2), first branched anal-fin ray about three times as long as last one. Caudal fin bilobed, weakly forked; upper lobe slightly longer than lower. Principal caudal-fin rays i+7+8+i; procurrent caudal-fin rays (counted in one c&s specimen): 18 dorsal; 20 ventral. Total vertebrae 41. Branchiostegal rays 8.

Gas bladder abbreviated cordiform (wider than long), simple (without diverticula) and with a well-developed internal T-shaped septum ( Fig. 2a View Fig ).

Coloration in alcohol. Head and body grayish-brown to dark brown, darker dorsally, becoming grayish-yellow or white on ventral surface; sometimes with dark irregular blotches of melanophores, giving to whole the aspect of dirty color. Dorsal, pectoral, pelvic, anal and caudal fins grayish-brown to dark brown or black, sometimes with light basal portion and darker distal portion (two portions more or less conspicuously separated); adipose fin brown with yellowish or whitish margin.

Sexual dimorphism. In males of Trachycorystes menezesi   the deferent canal runs in front of the anal-fin first unbranched rays; urogenital aperture positioned at tip of first branched ray. Urogenital aperture of females opens at distal end of a very small papilla located just in front of anal-fin origin. No modifications observed in the maxillary barbel and in the dorsal-fin spine of males, as is usual in some genera of Auchenipteridae   as Auchenipterus   (see for example Ferraris &Vari, 1999).

Distribution. Trachycorystes menezesi   is known from the rio Aripuanã (Madeira drainage) and its tributaries above the falls of Dardanelos and Andorinhas, Mato Grosso State, Brazil ( Fig. 3 View Fig ).

Ecological notes. Specimens of Trachycorystes menezesi   were collected during the INPA expedition that took place in November 1976, during the low water period of the rio

Aripuanã and its clear water tributaries. Specimens from the rio Aripuanã were easily caught at night, using fishhooks baited with small pieces of characiform fishes and placed near the banks (2 or 3 m deep). They were also abundant in tributaries of the rio Aripuanã, such as igarapé do Aeroporto and igarapé Genipapo, clear water creeks two or three m wide and up to 0.6 m deep, with forested margins and sandy bottoms where fallen trunks, branches and vegetal detritus were abundant. Specimens were caught using deep nets and by displacing the submerged debris, the natural hiding-places of the species. Stomach and intestinal contents included mainly carapace parts of different orders of insects, as well as parts of a scorpion, a crustacean and a characiform fish; one individual had within its stomach a piece of a curimatid fish used as bait with a hook attached. In the rio Aripuanã, besides Trachycorystes menezesi   , the only other large-sized predator collected was the “traíra”, Hoplias malabaricus   , caught in large number with fishhooks. In small creeks, besides Hoplias malabaricus   , the new species was collected with a larger variety of small predators like Rhamdia quelen   , Acestrorhynchus sp.   , Crenicichla sp.   , Tatia sp.   , and Synbranchus marmoratus   . Specimens of Trachycorystes menezesi   caught at night with fishhooks or gill nets emitted a guttural sound, possibly produced by its gas bladder like many other siluriforms.

Etymology. The name menezesi   is given in honor of Naércio A. Menezes who participated in the INPA expedition of 1976, when the new species was collected for the first time, and for his major contributions to the scientific knowledge of the ichthyofauna of the Neotropics.

Remarks. According to Kullander (1995) at least ten nominal fish species are known from the upper rio Aripuanã, suggesting a high degree of endemism for this portion of the river. Noteworthy is the presence of two carnivorous species above the rio Aripuanã waterfalls, the “sapatão” or “ mandubé” ( Trachycorystes menezesi   ) and the “traíra” ( Hoplias malabaricus   ), both of which are remarkably abundant. Both species were easily captured in large numbers in the rio Aripuanã using fishhooks during the expedition. The section of the river below the falls is dominated by the much diversified Amazonian carnivorous fishes that reach the base of the falls, but are almost completely absent in the section above the falls (H. A. Britski, pers. obs.). The large number of individuals in populations of T. menezesi   (as well as of H. malabaricus   ) may be attributed to the absence of competitors above the falls of Dardanelos and Andorinhas.

Although the description of Trachycorystes menezesi   is largely based on specimens collected during the INPA 1976 expedition, specimens of the new species were again obtained in 2005 from the Aripuanã River (MZUSP 104672). Recent collections made above the falls of tributaries of the Rivers Madeira, Tapajós, and Xingu, and of the Amazon proper failed to provide specimens of the new species. These facts strengthen the assumption that the new species is limited to the upper portion of the Aripuanã River basin ( Fig. 3 View Fig ).

Kullander (1995) mentioned that Parotocinclus aripuanensis   (not P. aripuananus   as cited by Kullander 1995: 158) was collected in the rio Canumã. His statement, based on information provided by Garavello (1988) when describing that species, deserve some comments. Garavello (1988: 122) indicated the type locality of P. aripuanensis   as “Ingazeiro, 20 km upstream of Boca do Rio Canumã, Aripuanã, MT”, but gave no information about the collectors and date of collection. Since the specimen was collected during the INPA expedition to rio Aripuanã, we can now say that the type locality is correctly “igarapé Ingazeiro, tributary of the rio Canamã (not Canumã), about 20 km upstream of its mouth along the right bank of the rio Aripuanã, State of Mato Grosso, collected during INPA expedition, 17 November 1976 ”. The rio Canumã (not Canamã) empties into the Paraná dos Abacaxis or Urariá, a right branch of the rio Madeira that forms the southeastern limit of the Tupinambaranas islands. In spite of this correction, Kullander’s comments that the fish was collected in a river downstream of Dardanelos falls, prevails because the rio Canamã does in fact empty into the rio Aripuanã at 09º55’18”S 59º19’02”W, downstream of the falls.

In a recent study Birindelli et al. (2009) reviewed the gross morphology of the gas bladder of 31 genera of Doradidae   and provided a classification of the different types they found. According to that classification the gas bladder of Trachycorystes menezesi   ( Fig. 2a View Fig ) is abbreviated cordiform simple (without diverticula) with a well-developed internal Tshaped septum. On the other hand, in T. trachycorystes   the gas bladder ( Fig. 2b View Fig ) has three posterior diverticula, one single, well-developed and relatively short terminal diverticulum and a pair of posterolateral diverticula (one on either side), similar albeit longer than those found in Agamyxis albomaculatus   ( Birindelli et al., 2009: 266, fig. 4 I, J).

Trachycorystes menezesi   is similar to T. trachycorystes   in most morphometric features. The only apparent morphometric differences between the two species are related to cleithral width and mouth width. The cleithral width is smaller in T. menezesi   (25.36-28.32% of SL, mean 26.74%) than in T. trachycorystes   (27.95-34.29% of SL, mean 31.45%), and the width of mouth is again smaller in the new species (59.70- 71.91% of head length, mean 65.79%) than in T. trachycorystes   (70.25-84.90% of SL, mean 76.32%). These two proportions indicate that T. menezesi   is a more slender species.

In the holotype of Trachycorystes cratensis Miranda Ribeiro, 1937   (MNRJ 947), the sphenotic bone is almost rectangular, parallel to the frontals, and excluded from the orbital border. Those features are distinctive of the genus Trachelyopterus   , and depart from the typical subtriangular shape of the sphenotic, which is laterally expanded and forms part of the dorsal orbital rim in Trachycorystes   . Trachycorystes cratensis   is thereby allocated to the genus Trachelyopterus Valenciennes, 1840   .

We also examined the holotype of Auchenipterus trachycorystes Valenciennes, 1840   (MNHN A.9422) and present the morphometric data for the stuffed and dry mounted specimen ( Table 1), as well as a photograph ( Fig. 4 View Fig ). Valenciennes’ (in Cuvier & Valenciennes, 1840: 214) description is very incomplete, and no other data on the holotype is found in the literature subsequent to the original description. Additional data for Trachycorystes trachycorystes   taken on 10 specimens deposited at MZUSP (See list of material) are included in Table 1.

Valenciennes’ (in Cuvier & Valenciennes, 1840: 216) description of Trachycorystes trachycorystes   stated “Il vient du Cabinet de Lisbonne, et nous croyons du Brésil. [It comes from the Cabinet de Lisbonne, and we believe to be from Brazil]”. The holotype represents one of the pieces taken from the Cabinet de Lisbonne when Napoleon’s troops invaded Portugal in 1808 and collections of that museum were transferred as spoils of war to the Jardin des Plantes in Paris ( Myers, 1964). The fish was collected during an expedition conducted from 1783 to 1792 by Brazilian naturalistAlexandre Rodrigues Ferreira who explored the rivers of the Amazon and Paraguay basins, Brazil. The type locality of T. trachycorystes   can be considered the Amazon basin, Brazil, as this species is unknown from the Paraguay basin. Trachycorystes trachycorystes   (possibly the holotype specimen) was drawn by one of Ferreira’s artists and is figured in his “Viagem Filosófica” ( Ferreira, 1971: pl. 27) under the common name “cabeça-de-ferro” (iron head).

Material examined. All from Brazil. Trachycorystes trachycorystes   . MNHN A. 9422, holotype, 235 mm SL. Amazonas   : MZUSP 7381 View Materials , 2 View Materials , 133 View Materials - 108.6 mm SL, igarapé Limãozinho , Maués, 4 Dec 1967   , EPA (H. A. Britski); MZUSP 31322 View Materials , 1, 246.6 mm SL, rio Negro , just downstream of mouth of rio Daraá, 00º30’S 64º40’W, 16 Feb 1980 GoogleMaps   , M. Goulding; MZUSP 52079 View Materials , 1 View Materials , Vista Escura , Tefé, 31 Jul 1979   , Michael Goulding; MZUSP 52080 View Materials , 5 View Materials , rio Tefé , Supiã-Pucu (Xavascal), 29 Jul 1979   , M. Goulding; MZUSP 52081 View Materials , 2, 124.3 mm SL, alc., 221 mm SL, sk), rio Tefé , lago Mucura, 30 Jul 1979   , M. Goulding; MZUSP 52091 View Materials , 2 View Materials , rio Negro at mouth of rio Arirará, 28 May 1979   , Michael Goulding; MZUSP 52092 View Materials , 2 View Materials , Cachoeira do Aracu , rio Daraá (pedral), 01º40’S 64º40’W, 10 Feb 1979 GoogleMaps   , Michael Goulding; MZUSP 52093 View Materials , 2 View Materials , rio Arirará , 10º30’S 63º48’W, 8 Oct 1979 GoogleMaps   , Michael Goulding; MZUSP 59093 View Materials , 1, 220.5 mm SL, rio Negro , Ilha Mari-Mari, 31 May 1979   , M. Goulding; MZUSP 52094 View Materials , 1 View Materials , rio Negro , Cachoeira de São Gabriel , Apr-May 1980, Michael Goulding   ; MZUSP 52095 View Materials , 3 View Materials , São Pedro , upper rio Negro, at mouth of igarapé do Ibará, 23 May 1979   , Michael Goulding; MZUSP 108575 View Materials , 1, 125.4 mm SL, rio Negro , Marautá (igapó), 27 May 1979   , Michael Goulding; MZUSP 93463 View Materials , 1, 110.7 mm, rio Tiquié , comunidade Pirarara-Poço, rio Negro drainage, 00º08’40”N 69º12’41”W. 19-20 Nov 2006 GoogleMaps   , Flávio C. T. Lima et al   .; MZUSP 103386 View Materials , 1, 155.8 mm SL, igarapé Sirinau , bank of rio Cuieiras , about 25 km from its mouth, 02º42’S 60º20’W, rio Negro drainage, Manaus, 30 Jan 1977 GoogleMaps   , Alpha Helix Amazon Expedition; MZUSP 104547 View Materials , 1, 188 mm SL, sk, no data   ; MZUSP 104673 View Materials , 1, 190.7 mm SL, Fortaleza , Paraná de Urariá, 27 Feb 1972   , EPA (P. E. Vanzolini); MZUSP 104674 View Materials , 2 View Materials , 186.9 View Materials - 208.8 mm, igarapé near Moura , rio Negro drainage, 01º27’S 61º38’W GoogleMaps   , EPA (P. E. Vanzolini). Pará   : MZUSP 15690 View Materials , 1 View Materials : 142.1 mm, igapó do lago Leonardo , Reserva Biológica de Trombetas, rio Trombetas, 14 Jul 1979   , R. M. C. Castro. Trachycorystes cratensis     . MNRJ 947 View Materials , holotype, 60.6 mm SL, Grangeiro , Crato, Ceará, Antenor L. de Carvalho   .


Museu de Zoologia da Universidade de Sao Paulo


Instituto Nacional de Pesquisas da Amazonia


Museum National d'Histoire Naturelle


Tavera, Department of Geology and Geophysics


Departamento de Geologia, Universidad de Chile