BackgroundThe facial musculature is a remarkable anatomical complex involved in vital activities of fishes, such as food capture and gill ventilation. The evolution of the facial muscles is largely unknown in most major fish lineages, such as the Actinopterygii. This megadiverse group includes all ray-finned fishes and comprises approximately half of the living vertebrate species. The Polypteriformes, Acipenseriformes, Lepisosteiformes, Amiiformes, Elopiformes, and Hiodontiformes occupy basal positions in the actinopterygian phylogeny and a comparative study of their facial musculature is crucial for understanding the cranial evolution of bony fishes (Osteichthyes) as a whole.ResultsThe facial musculature of basal actinopterygians is revised, redescribed, and analyzed under an evolutionary perspective. We identified twenty main muscle components ontogenetically and evolutionarily derived from three primordial muscles. Homologies of these components are clarified and serve as basis for the proposition of a standardized and unifying myological terminology for all ray-finned fishes. The evolutionary changes in the facial musculature are optimized on the osteichthyan tree and several new synapomorphies are identified for its largest clades, including the Actinopterygii, Neopterygii, and Teleostei. Myological data alone ambiguously support the monophyly of the Holostei. A newly identified specialization constitutes the first unequivocal morphological synapomorphy for the Elopiformes. The myological survey additionally allowed a reinterpretation of the homologies of ossifications in the upper jaw of acipenseriforms.ConclusionsThe facial musculature proved to be extremely informative for the higher-level phylogeny of bony fishes. These muscles have undergone remarkable changes during the early radiation of ray-finned fishes, with significant implications for the knowledge of the musculoskeletal evolution of both derived actinopterygians and lobe-finned fishes (Sarcopterygii).

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Trichomycterus rubbioli, herein described, is a new species from the limestone caves of the Água Clara system from theSerra do Ramalho karstic area, southwest of Bahia State, north-eastern Brazil. The new species is diagnosed by the com-bination of the following non-exclusive characters: highly reduced skin pigmentation; reduced eyes, externally visible assmall black or reddish-brown spots; long barbels, especially the nasal (86.9–127.1% of head length) and maxillary (98.1–129.3% of head length); and pectoral-fin ray count reaching I, 9. The troglobitic status is suggested by the presence oftroglomorphisms on an advanced degree, especially the reduction of skin pigmentation and the regression of the eyes, be-sides the absence of individuals in superficial drainages of the region. Population densities, recorded on two occasions,were extremely low. Trichomycterus rubbioli occurs in water bodies formed by infiltration in the rock, and, because of this, it must be considered fragile and as a priority in conservation programs of Brazilian karstic areas.

The laterosensory system is a mechanosensory modality involved in many aspects of fish biology and behavior. Laterosensory perception may be crucial for individual survival, especially in habitats where other sensory modalities are generally useless, such as the permanently aphotic subterranean environment. In the present study, we describe the laterosensory canal system of epigean and subterranean species of the genus Ituglanis (Siluriformes: Trichomycteridae). With seven independent colonizations of the subterranean environment in a limited geographical range coupled with a high diversity of epigean forms, the genus is an excellent model for the study of morphological specialization to hypogean life. The comparison between epigean and subterranean species reveals a trend toward reduction of the laterosensory canal system in the subterranean species, coupled with higher intraspecific variability and asymmetry. This trend is mirrored in other subterranean fishes and in species living in different confined spaces, like the interstitial environment. Therefore, we propose that the reduction of the laterosensory canal system should be regarded as a troglomorphic (= cave-related) character for subterranean fishes. We also comment about the patterns of the laterosensory canal system in trichomycterids and use the diversity of this system among species of Ituglanis to infer phylogenetic relationships within the genus. J. Morphol. 278:4-28, 2017. ©© 2016 Wiley Periodicals,Inc.

Trichomycterus dali, new species, is described from flooded limestone caves in Serra da Bodoquena karst area, State of Mato Grosso do Sul, Central Brazil. The new species is diagnosed by a unique character in the genus, the presence of conspicuous, ridge-like adipose folds lining dorsally throughout the body. Trichomycterus dali can be further distinguished readily from epigean congeners by the reduction of eyes and skin pigmentation (except for T. gorgona), and from remaining congeners (i.e., all hypogean plus T. gorgona) by the total loss of eyes, not visible externally (except for T. sandovali and T. spelaeus). Other diagnostic features includes very long barbels, especially the nasal (99.3-143.5% HL) and the maxillary (97.0-131.3% HL), pectoral-fin ray count reaching I,9 and a unique cranial fontanel with a conspicuous constriction on the meeting point of supraoccipital and the two frontal bones. The troglobitic status of the species is suggested by the presence of troglomorphisms on an advanced degree, especially the reduction of skin pigmentation, the total loss of eyes and the enlarged barbels. In addition, the presence of a well developed adipose fold in adults may indicate a distinctive adaptation acquired by neoteny to withstand the food scarce conditions of its hypogean habitat.
Trichomycterus dali, espécie nova, é descrita de cavernas calcárias alagadas na área cárstica da Serra da Bodoquena, estado do Mato Grosso do Sul, Brasil central. A nova espécie é diagnosticada por um caráter único no gênero, a presença de dobras adiposas conspícuas, em forma de crista, passando por toda a região dorsal do corpo. Trichomycterus dali pode ser ainda diferenciada facilmente de suas congêneres epígeas pela redução dos olhos e da pigmentação cutânea (exceto para T. gorgona), e das congêneres restantes (isto é, todas as hipógeas mais T. gorgona) pela perda total dos olhos, não visíveis externamente (exceto para T. sandovali e T. spelaeus). Outras características diagnósticas incluem barbilhões muito longos, especialmente o nasal (99,3-143,5% do comprimento da cabeça) e o maxilar (97,0-131,3% do comprimento da cabeça), contagem de raios da nadadeira peitoral atingindo I,9 e uma fontanela cranial única com uma constrição conspícua no ponto de encontro do supraoccipital e dos dois ossos frontais. O status troglóbio da espécie é sugerido pela presença de troglomorfismos em avançado grau, especialmente a redução da pigmentação cutânea, a perda total dos olhos e os barbilhões alongados. Além disso, a presença de uma dobra adiposa bem desenvolvida nos adultos pode indicar uma adaptação distintiva, adquirida por neotenia, para enfrentar as condições alimentares escassas do seu habitat hipógeo

The association between lateral‐line canals and skull bones in fishes has been the subject of several studies and raised a series of controversies, particularly with regard to the hypothesized role of lateral‐line organs (i.e. neuromasts) in osteogenesis and the consequences for hypotheses of homology of the bones associated with lateral‐line canals. Polypteridae, a group of freshwater fishes that occupies a key phylogenetic position as the most basal extant lineage of ray‐finned fishes (Actinopterygii), provides an interesting model for the study of the relationships between lateral‐line canals and skull bones. We describe the development of bones associated with lateral‐line canals in the Senegal Bichir, Polypterus senegalus, and use these data to re‐address previous hypotheses of homology of skull bones of polypterids. We demonstrate that the lateral‐line canals constitute a separate component of the dermatocranium that may interact with a membranodermal component, thereby forming compound bones in the adult. Differences in the interactions between these components determine the characteristics of the development of each independent bone in the skull of adult P. senegalus. Our results shed light on long‐standing controversies about the identity of skull bones such as the rostral, preopercle, and sphenotic in Polypteridae, and suggest the presence of an ancestral two‐component pattern of formation of bones associated with lateral‐line canals in bony fishes. These findings reveal the need to re‐address previous hypotheses of homology of bones associated with lateral‐line canals in different groups of bony fishes, especially fossil taxa.

We readdress the controversy about the valid generic name to be applied to the African Reedfish, a species from a monotypic genus that, along with the eleven valid species of Polypterus Lacepède, 1803, comprises the known extant diversity of the order Polypteriformes. The initial conflict was established due to the inadequate replacement of the name Erpetoichthys, wrongly assumed preoccupied, by Calamoichthys, combined with the desynchronization between the sequence in which Smith’s accounts with descriptions and nomenclatural acts about the Reedfish were written and submitted for publication, and the sequence in which they were actually published/distributed. The controversy seemed to be settled in the 1980s by the finding of an earlier report published in an Edinburgh’s newspaper in 1865, in which the name Erpetoichthys was used prior to all scientific accounts by Smith. However, we demonstrate that this report cannot be considered to contain a valid nomenclatural act according to the regulations of the International Code of Zoological Nomenclature. Therefore, we undertook a detailed study to reconstruct the sequence of publication of Smith’s accounts on the Reedfish, whose correct dates of publication/distribution had not been properly established yet, to settle down once and for all the dilemma about the precedence of these names. Our conclusion is that Calamoichthys Smith, 1866a is the valid generic name to be applied to the Reedfish, and Erpetoichthys Smith, 1866a, its junior synonym, represents a name published in synonymy but later made available by Smith himself. We use the nomenclatural example of the Reedfish, as well as other cases from the literature, to draw attention to the fact that, in agreement with Article 8.1.1 of the Code, zoological names are available only when there is an unequivocal intention by their authors to scientifically describe them, even if other requirements of the Code are met. When this Article is not met in a given situation, the name is considered unavailable and an available one should be set in place for the taxon, or a new name should be proposed.

A new species of Scleronema (Trichomycteridae) is described from the lowlands of three coastal river basins in the Atlantic Forest of the Santa Catarina state, Southern Brazil. Aspects of the anatomy, reproduction, diet, feeding behavior and habitat of the new species are described and discussed in comparison with related taxa. The conservation status of the new species, which currently faces several threats due to environmental impacts on its region of occurrence, is established. Based on characteristics observed in the new species, as well as in most of its congeners, the phylogenetic position and monophyly of Scleronema are discussed and traits considered synapomorphic for the subgenera Plesioscleronema and Scleronema are reviewed. The monophyly of the genus Scleronema is supported by a new synapomorphy. In addition, two new synapomorphies, one of which based on behavior, are suggested for the subgenus Scleronema, justifying the inclusion of the new species. Within the subgenus Scleronema, the new species is assigned to the S. minutum group, which currently includes the majority of species of the genus, due to the presence of synapomorphic traits related to the body shape, maxillary barbel, skin flap of the opercle, caudal and pectoral fins, as well as osteological features of the lower jaw, hyoid arch, and postcranial axial skeleton. The species herein described differs from all its congeners by a combination of characters from various morphological complexes, which are described in detail using different methodologies, including radiography, whole-specimen clearing and double-staining procedures, and tridimensional computer nanotomography (3D nano-CT).