Early larval ontogeny of the Permo-Carboniferous temnospondyl Sclerocephalus

The early larval development of the temnospondyl Sclerocephalus sp. is analyzed, based on 38 specimens from the Lower Rotliegend (Permo-Carboniferous boundary) of the Saar-Nahe Basin (south-west Germany). The study focuses on the smallest larval specimens, which exemplify changes in both proportions and ossification patterns. In comparison with dissorophoid larvae, the skull ossifies more fully and at a much faster rate; the smallest specimens already have completely formed circumorbital bones that are sutured throughout. Sculpturing undergoes two marked changes, first from uniformly pitted to pits of variable size and regional differentiation, and finally to the origin of ridges. The palate of small larvae differs from that of larger specimens in patterns of dentition, having more teeth including a denticle field on the cultriform process. The mandible of small larvae is described for the first time, being narrower than in adults and having three dentigerous coronoid elements. The smallest specimens have poorly ossified neural arches, lack vertebral centra, and have faintly ossified humeri, femora, and very poorly developed distal elements. The posterior ribs, metapodia, and phalanges appeared after the dermal elements of the pectoral girdle, whereas the scapulocoracoid and ischium are absent throughout the larval period. Early growth and differentiation of the limbs and the ilium illustrates the developmental patterning of the appendages, which proceeded from proximal to distal. Dermal squamation is uniform in small stages, consisting of round or oval osteoderms with pronounced growth rings; in large larvae, they start to differentiate in certain body regions.     

Ontogeny of the Early Carboniferous acanthodian <Emphasis Type="Italic">Acanthodes lopatini</Emphasis> Rohon

The sequence of ossification of skeletal elements in the growth series of the acanthodian Acanthodes lopatini Rohon from the Lower Tournaisian of the Minusa Trough (Siberia) is described. Four formal ontogenetic stages are recognized. It is shown that even 20?30-mm-long juveniles have well-developed fin spines, scapulocoracoids, mandibular bones, branchiostegal rays, and incipient gill rakers. At this stage, scales cover the posterior part of the body and the orbits are marked by dark “eye stains” of uncertain nature. Further ontogenetic changes are connected with the development of sclerotic ring elements, sensory line system, squamation of the head region and fin webs, perichondral ossifications of the Meckel’s, quadrate, and palatine cartilages, and, finally, mineralization of the hyoid and gill arches. Ontogenetic features of A. lopatini are compared with those in other members of the genus and other acanthodiforms. Some developmental features shared by A. lopatini and Lodeacanthus gaujicus Upeniece suggest that acanthodids could have evolved from mesacanthids.     

Study of the pectoral girdle and fins of the Late Carboniferous sibyrhynchid iniopterygians (Vertebrata,Chondrichthyes, Iniopterygia) from Kansas and Oklahoma (USA) by means of microtomography,with comments on iniopterygian relationships

The latest works on iniopterygians question their monophyly when considering only the neurocranium of the two families (Sibyrhynchidae and Iniopterygidae), which have different conditions of preservation. Some of the synapomorphies of the Iniopterygia concern the pectoral girdle and fins. However, the anatomy of these different elements is still poorly known in this taxon. Here we describe in details three dimensionally preserved cartilages of the pectoral girdle and fins of the sibyrhynchid Iniopera sp. These structures have been extracted virtually from phosphatised nodules thanks to conventional and synchrotron microtomography, using absorption and phase contrast based techniques in the later case. The pectoral girdle of Iniopera sp. consists of three elements, which are, from dorsal to ventral, a paired suprascapular cartilage, a pair of robust scapulocoracoids and an unpaired intercoracoid cartilage. The scapular part of the scapulocoracoids is extremely reduced and the suprascapular cartilages link the scapulcoracoids to the rear of the neurocranium. These characters may be iniopterygian synapomorphies. Iniopterygians, stem and crown-holocephalans share a basipterygium that articulates with the pectoral girdle and bears an enlarged first pectoral fin radial. Posteriorly, the basipterygium articulates with either a well-defined metapterygium (in crown-holocephalans) or a metapterygial axis (in stem-holocephalans).     

Some osteological features ofVarasichthys ariasi Arratia (Pisces,Teleostei) from the Late Jurassic of Chile

Bones of the head and pectoral girdle are studied in additional specimens ofVarasichthys ariasi. The parietal and supraoccipital are similar to those ofLeptolepis and other primitive teleosts. The suborbital is the smallest known in teleosts; it differs from that of other teleosts and holosteans in not contacting the dermopterotic or pterotic, the supratemporal or infraorbital 3. The pattern of the parietals and the supraoccipital, the presence of a suborbital, extension of the infraorbital sensory canal onto the antorbital, and the presence of two postsupracleithra and six postcleithra are primitive features within teleosts. Two postsupracleithra and six broad postcleithra with crenulated posterior border form an unique series within teleosts.     

Larval development of Argentine hake Merluccius hubbsi

The ontogeny of the developmental stages of the hake Merluccius hubbsi is described. Fish larvae and post-transitional juveniles were collected in the Nor-Patagonian area from 1989 to 2004. The opening of the mouth and the pigmentation of the eyes are coincident with yolk resorption, finishing the yolk-sac stage. This species presents pigmentation on the head, trunk and tail typical of gadiform larvae. Pectoral fin development is completed during the transformation stage. The post-transitional juvenile stage begins when the fin-ray complements are complete and squamation begins. The fins become fully formed in the following sequence: pelvic fins, first dorsal fin, second dorsal and anal fins together, caudal fin and pectoral fins. The caudal complex is totally developed in larvae of 22·0–23·0 mm standard lengths ( L _S) and all vertebral elements are first observed in larvae of 8·5 mm L _S. The rate of development of M. hubbsi observed in this study could be faster than the rates reported for other species of Merluccius by different authors.     

Galeus longirostris,a new species of the sawtail catshark from Japan

Galeus longirostris sp. nov. is described based on 46 specimens taken off the southern part of Japan. It is distinguished from all known species ofGaleus in having a considerably longer snout. This species is morphologically close toG. nipponensis, which commonly occurs off the southern part of Japan, but differs in having longer preoral length than the mouth width, a bluntly rounded snout, larger pectoral fins, a shorter interspace between anal and lower caudal fins, and a greater number of monospondylous vertebrae.     

Early ontogeny of two bothid species,Psettina iijimae andLaeops kitaharae

From specimens collected in the western North Pacific, the early ontogeny ofPsettina iijimae andLaeops kitaharae is described. Diagnostic characters of the genera throughout larval stages are also provided. It is suggested that these species are distributed on continental shelf or at the edge, and that they spawn between July and September.     

On the spines of the Stethacanthidae (Chondrichthyes), with a description of a new genus from the Mississippian Bear Gulch limestone

Several specimens of an elasmobranch from the upper Mississippian Bear Gulch limestone of Montana are described. The first dorsal spine and fin closely resemble Stethacanthus erectus and to a lesser extent Stethacanthus altonensis. The new genus and species Orestiacanthus fergusi is proposed for the specimens, and it is suggested that recent attempts to synonymize the species of Stethacanthus on the basis of spines are unjustified. The specimens also share the enlarged cranial denticles, general form of the palatoquadrate, cladodont teeth and pectoral fin with S. altonensis. They differ from S. altonensis in proportions of jaws, numbers of tooth families, numbers of prearticular basals and axial radials, morphology of the second dorsal fin, and in the presence of generalized squamation in some specimens (but not the female). The pelvic fins differ greatly in having a prominent metapterygium.     

The morphology and post-hatching development of the skull of Bolitoglossa nicefori (Caudata: Plethodontidae): developmental implications of recapitulation and repatterning

The cranial morphology of the direct-developing salamander Bolitoglossa nicefori and its post-hatching development are described and compared with that of other urodeles. Four stages of cranial development are defined on the basis of conspicuous events that occur during post-hatching ontogeny. The adult skull morphology of B. nicefori is similar to that of other plethodontids; however, some regions show interspecific variation. The post-hatching ontogeny of the skull and the stage of ossification observed in the hatchlings of B. nicefori show two important ontogenetic features: (1) a mosaic of early larval, metamorphic and post-metamorphic skull features in hatchlings, and (2) absence of characteristic larval elements in skull and hyoid apparatus. The distinctive stage of ossification in the hatchlings of B. nicefori could be caused by heterochronic changes in the ossification sequence, compared to the ontogeny of metamorphic salamanders. The possible heterochronic changes and the absence of larval traits are perhaps due to ontogenetic repatterning, yet without an obvious impact on the adult skull morphology (absence of morphological novelties). This might indicate a compartmentalized development. Further studies should be performed in order to establish the possible occurrence of recapitulatory patterns or ontogenetic repatterning in the skull morphogenesis of B. nicefori during its embryonic development.     

Systematic observations on tropical Asian medakas or ricefishes of the genusOryzias, with descriptions of four new species

The so-calledOryzias melastigma (McClelland, 1839), reported from India, Bangladesh, Myanmar, and Malaysia by numerous authors beginning with Day (1877), is based mainly or entirely onAplocheilus panchax (Hamilton, 1822). India and Bangladesh have two species ofOryzias, both large. The deeper-bodied of these two species is reported for the first time asO. dancena (Hamilton, 1822). The other is identified asO. carnaticus (Jerdon, 1849). Myanmar has one large species,O. dancena, and one tiny species,O. uwai new species.Oryzias minutillus Smith, 1945 andO. uwai differ from all otherOryzias in having 4/5 instead of 5/6 principal caudal fin rays.Oryzias uwai differs fromO. minutillus in being more conspicuously pigmented and having large, 6-rayed pelvic fins often extending to anal fin origin instead of much smaller and shorter 5-rayed pelvic fins. In Thailand (including its part of the Mekong basin) three species are known: a large estuarine species tentatively identified asO. javanicus (Bleeker, 1854) and two tiny inland species,O. mekongensis Magtoon & Uwa, 1986, andO. minutillus. Oryzias minutillus from many localities are more or less melanoproctic, i.e. have a darkly pigmented genital or vent area not seen in other species. The Mekong basin in Laos has two large species,O. latipes (Temminck & Schlegel, 1846) andO. pectoralis new species, distinguished by a prominent black blotch on the pectoral fin base, both recently collected in the Nam Theun watershed in central Laos; and two tiny species,O. mekongensis andO. minutillus. Only one species ofOryzias is known from the Mekong delta in Vietnam, the small moderately deep-bodiedO. haugiangensis new species, with 19–22 anal and 9–10 pectoral fin rays. The Indonesian island of Java has one large species,O. javanicus (Bleeker, 1852) with 21–25 anal and 11 pectoral fin rays, and one small species,O. hubbsi new species, with only 17–21 anal and 9 pectoral fin rays.     

A new cottid species, Icelus sekii (Perciformes: Cottoidei), from Hokkaido, Japan

A new cottid species, Icelus sekii, is described on the basis of six specimens collected from off Rausu and Urakawa, Hokkaido Island, Japan. This species is distinguished from its congeners by the following combination of characters: supraocular and parietal spines absent; nuchal spine obscure; uppermost preopercular spine unbranched; no scales between dorsal scale row and lateral line scale row, and no scales below lateral line scale row; supraocular, parietal, and nuchal cirri present; five dark brown saddles dorsolaterally; anal fin rays 13; pectoral fin rays 15; vertebrae 12 + 24–25 = 36–37. Icelus sekii can be mature at the smallest size among the species of Icelus. As a secondary sexual character, the male holotype has unique ensiform flaps on the distal tips of the first dorsal fin.     

Comparative squamation of the lateral line canal pores in sharks

The current study collected the first quantitative data on lateral line pore squamation patterns in sharks and assessed whether divergent squamation patterns are similar to experimental models that cause reduction in boundary layer turbulence. In addition, the hypothesis that divergent orientation angles are exclusively found in fast‐swimming shark species was tested. The posterior lateral line and supraorbital lateral line pore squamation of the fast‐swimming pelagic shortfin mako shark Isurus oxyrinchus and the slow‐swimming epi‐benthic spiny dogfish shark Squalus acanthias was examined. Pore scale morphology and pore coverage were qualitatively analysed and compared. In addition, pore squamation orientation patterns were quantified for four regions along the posterior lateral line and compared for both species. Isurus oxyrinchus possessed consistent pore scale coverage among sampled regions and had a divergent squamation pattern with multiple scale rows directed dorsally and ventrally away from the anterior margin of the pore with an average divergent angle of 13° for the first row of scales. Squalus acanthias possessed variable amounts of scale coverage among the sampled regions and had a divergent squamation pattern with multiple scale rows directed ventrally away from the anterior margin of the pore with an average angle of 19° for the first row of scales. Overall, the squamation pattern measured in I. oxyrinchus fell within the parameters used in the fluid flow analysis, which suggests that this pattern may reduce boundary layer turbulence and affect lateral line sensitivity. The exclusively ventral oriented scale pattern seen in S. acanthias possessed a high degree of divergence but the pattern did not match that of the fluid flow models. Given current knowledge, it is unclear how this would affect boundary layer flow. By studying the relationship between squamation patterns and the lateral line, new insights are provided into sensory biology that warrant future investigation due to the implications for the ecology, morphology and sensory evolution of sharks.     

Description of transformation larvae and a juvenile of the dextral flounder,poecilopsetta praelonga (pleuronectidae, poecilopsettinae) from the northwestern waters of australia

Three late metamorphic transformation larvae ofPoecilopsetta praelonga (68.0–82.3 mm SL) and a juvenile (92.7 mm SL) captured from the waters off northwestern Australia (400–460 m deep) are described. The transformation larvae ofP. praelonga are distinguishable from the congeners of the same stage in having relatively low body depth (2.20–2.44 in SL), relatively large maxilla extending to anterior one-third of lower eye, and seven and six distinct spots along the dorsal and ventral margins of ocular side body, respectively. In the smallest specimen, the intestine was expanded posteriorly beyond the posterior wall of visceral cavity, but not in the larger specimens. The pectoral fin rays and the spines of scales were supposed to begin to be formed by about 80 mm SL. Ontogenetic changes which include decreasing ratios of upper jaw length to head length. and increasing ratios of depth of body muscle to body depth, were observed, based on a comparison of transformation larvae, a juvenile and adults.     

Osteological development of the lophiid anglerfish,lophius gastrophysus

The osteological development of the head skeleton and dorsal, pectoral, and anal fin supports, are described from cleared and stained specimens ofLophius gastrophysus larvae, ranging from 4.6 to 21.8 mm NL; the results are compared with those of juvenile (79.8 mm SL) and adult (398 mm SL) specimens. Tiny conical teeth are present on the premaxillary, dentary, palatine and vomer since early stage. The first three dorsal fin spines are initially positioned on the midline of body posterior to the supraoccipital, but they migrate forward with growth and become cephalic in juveniles. The forward movement of the dorsal spines is produced by the forward extension of the cartilaginous basal inside the subepidermal space. During the planktonic larval stage the pectoral fins are on the sides of body as in ordinary fishes, but they move ventrad and become leg-like in bottom living juveniles and adults. Ossification of the caudal complex ofL. gastrophysus larvae proceeds very slowly and only the 21.8 mm NL larva has an almost completely ossified caudal complex. Eight principal caudal rays are loosely attached on the posterior edge of the hypurals and no procurrent rays are present. Larvae have well developed parhypurapophysis at the mid-portion of the urostyle which transforms into keel-like structure in juveniles and adults.     

Postembryonic ontogeny of the spadefoot toad,Scaphiopus intermontanus (Anura: Pelobatidae): Skeletal morphology

Postembryonic skeletal ontogeny of the pelobatid frog Scaphiopus intermontanus is described based on a developmental series of cleared-and-stained, whole-mount specimens. The focus is on laboratory-reared individuals fed a herbivorous diet as larvae. Although there is variation in the timing of ossification of individual skeletal elements relative to developmental stages based on external morphological criteria, the sequence of skeletal development generally is conservative. Compared with its close relative, S. bombifrons, ossifications that occur during prometamorphosis tend to be slightly delayed in S. intermontanus; however, cranial bones that ossify during late metamorphic climax in S. intermontanus are delayed until postmetamorphosis in S. bombifrons. The differences in timing between the two species are consistent, however, with differences observed between two developmental series of S. intermontanus raised at two different temperatures. Noteworthy features of skeletal development in S. intermontanus include: 1) presence of palatine ossifications that form from independent centers of ossification and soon fuse with the postnarial portion of the vomers to form the compound vomeropalatine bones; 2) compound sphenethmoid that may arise from four or more endochondral centers of ossification and one dorsal, dermal center of ossification; and 3) presence of transverse processes and vestigal prezygapophyses on the first postsacral vertebra. The morphology of the larval orbitohyoideus and interhyoideus muscles is compared. The record of skeletal ontogeny and muscle morphology presented herein for the herbivorous larval morph can serve as a baseline for comparisons with the ontogeny of the carnivorous larval morph of Scaphiopus. J. Morphol. 238:179–244, 1998. © 1998 Wiley-Liss, Inc.     

Ontogenetic causes and mechanisms for formation of differences in number of fish scales

Fish squamation is developed in late ontogeny. Therefore, the conditions of development significantly affect its characteristics (number of scales). This study is aimed at considering the influence of external and internal factors on variation of the number of scales in fish. Acceleration of development results in decrease of the number of scales, while it increases with retardation. Experiments on regulation of thyroid status of fish showed that the certain mechanism of alteration of the number of scales is related with heterochrony, such as a shift of the timing of squamation. Accelerated development is caused by early scale development at smaller body length, while retarded development is characterized with later scale development and at greater body length. Data considering heterochrony as the possible reason for differences in the number of scales in related fish species are represented. Moreover, alterations of the distance between scales (morphogenetic count) can serve as another alteration mechanism of the number of scales in fish (especially phyletically distant species).