Ultrastructural data on the scales of the dipnoan Protoptems annectens (Sarcopterygii, Osteichthyes)

The structure and the mineralization of the scales of the living dipnoan (lungfish) Protoptems annectens have been investigated by transmission electron microscopy (TEM). The thin and imbricated scales are composed of two layers: the squamulae and the basal plate. At the outer surface, the squamulae form isolated plates superficially ornamented with spines and concretions and made up of acellular bone. After demineralization, the squamulae show a heterogeneous organic matrix composed of thin randomly oriented collagen fibrils forming a loose network within which the concretions appear as electronlucent circular areas. Abundant and aggregated concretions are located within the spines. The crystallites are oriented by the collagen fibrils except in the concretions. Anchoring bundles composed of parallel collagen fibrils arise from the squamulae and connect the scales to the overlying dermis.
The basal plate, the most developed part of the scale, is made up of isopedine. Its main component consists of thick, closely packed collagen fibrils organized in a 'double twisted plywood-like structure'. Fibroblasts are present in the basal plate. Mineralization occurs only in few plies located beneath the squamulae. Mandl's corpuscles are found in front of the mineralization front. The mineral deposit is oriented by the collagen fibrils.
The scales of Protoptems annectens differ from the typical elasmoid scales of the teleosts by the peculiar structure of the squamulae, nevertheless they show enough structural characteristics to support the hypothesis that they can be considered as scales of the elasmoid grade, which have retained some plesiomorphic characteristics.     

Scale structure in the Australian lungfish,Neoceratodus forsteri (Osteichthyes: Dipnoi)

Scales of the Australian lungfish, Neoceratodus forsteri, are secreted within the dermis by a capsule of scleroblasts, and enclosed in a pouch made of collagen fibers, in contact with the epidermis over the posterior third of the scale. Each scale grows from a focus, which represents the first formed part of the scale. On the internal surface of the scale is elasmodin, made of collagen fiber bundles arranged in layers. Elasmodin, unmineralized in N. forsteri, contains cells in the living animal, and the number of layers increases as the scales grow. Squamulin, on the thin external part of the scale, is also laid down in layers, and based on a matrix of fine collagen fibrils, mineralized with a poorly crystalline biogenic calcium hydroxylapatite. Squamulin is divided into separate sections called squamulae, and contains long tubules with cells applied to the wall of the tubule. The anterior and lateral surfaces of the squamulin are ornamented with pediculae, and the posterior surface has longitudinal ridges, from which collagen fibers extend to anchor the scale within the pouch. Elasmodin and squamulin are linked by unmineralized collagen fibrils. The layers, formed at irregular intervals, are connected around the margin of the scale, effectively converting the whole scale into a flat structure resembling a pearl, with the first formed tissues deeply embedded inside the scale, and the youngest on the outer surface. Incremental lines in the hard tissue, and the number of layers in the elasmodin, do not reflect the chronological age of the fish. J. Morphol. 276:1137–1145, 2015. © 2015 Wiley Periodicals, Inc.     

Skin structure in the snout of the Australian lungfish,Neoceratodus forsteri (Osteichthyes: Dipnoi)

Many fossil lungfish have a system of mineralised tubules in the dermis of the snout, branching extensively and radiating towards the epidermis. The tubules anastomose in the superficial layer of the dermis, forming a plexus consisting of two layers of vessels, with branches that expand into pore canals and flask organs, flanked by cosmine nodules where these are present. Traces of this system are found in the Australian lungfish, Neoceratodus forsteri, consisting of branching tubules in the dermis, a double plexus below the epidermis and dermal papillae entering the epidermis without reaching the surface. In N. forsteri, the tubules, the plexus and the dermal papillae consist of thick, unmineralised connective tissue, enclosing fine blood vessels packed with lymphocytes. Tissues in the epidermis and the dermis of N. forsteri are not associated with deposits of calcium, which is below detectable limits in the skin of the snout at all stages of the life cycle. Canals of the sensory line system, with mechanoreceptors, are separate from the tubules, the plexus and the dermal papillae, as are the electroreceptors in the epidermis. The system of tubules, plexus, dermal papillae and lymphatic capillaries may function to protect the tissues of the snout from infection.     

Structural peculiarities of the tubercles in the skin of the turbot,Scophthalmus maximus (L., 1758) (Osteichthyes,Pleuronectiformes, Scophthalmidae)

The structure of the bony tubercles of the turbot, Scophthalmus maximus (L., 1758), was examined using ground sections, microradiography, SEM, and TEM. The tubercles are small, isolated, mineralized conical plates randomly distributed in the eyed side of the body. They are composed of three layers: the outer limiting layer, the external layer, and the basal plate, which make up the thin and flat elasmoid scales of Teleostei. The main difference between regular elasmoid scales and bony tubercles lies in the organization and the growth of the basal plate. Indeed, the conical shape of the tubercle is the result of a prominent thickening of the central part of the basal plate where the collagen matrix is organized in a complicated three-dimensional network. Densely packed thick collagen fibrils form superimposed plies organized in a plywood-like structure that resembles that of the elasmoid scales but it is criss-crossed by numerous vertical sheets of thin collagen fibrils. The tubercles originate from thin and flat plates located in the skin of larvae and juveniles, whose structure is that of regular-developing elasmoid scales. Thus, the tubercles of Scophthalmus maximus could be considered as modified elasmoid scales rather than bony structures. They might be the result of specific arrangements related to the general trend of reduction of the dermal skeleton in the teleostean lineage.     

Cytoskeletal organization and collagen orientation in the fish scales

Summary Immunofluorescence and electron microscopy were used to analyze the relationships between the organization of collagen fibrils in elasmoid scales, and the orientation of microtubules and actin microfilaments in the scleroblasts producing this collagenous stroma. Attention was focused on the basal plate of the scales because of the highly ordered three-dimensional arrangement of the collagen fibrils in superimposed plies forming an acellular plywood-like structure. The collagen fibrils are synthesized by the scleroblasts forming a monolayered pseudo-epithelium, the hyposquama, at the lowest surface of the scale. Fully developed scales with a low collagen deposition rate were compared with regenerating scales active in fibrillogenesis. When an ordered array of the collagen fibrils is found, the innermost collagen fibrils are coaligned with microtubules and actin microfilaments. Thus, because of this coalignment, microtubules and actin microfilaments of the hyposquamal scleroblasts are subjected to consecutive alterations during the formation of the plies of the basal plate. The sequence of events when the collagen fibrils change their direction from one ply to the other in the basal plate is deduced from immunofluorescence and phase-contrast-microscopic observations. During the formation of the orthogonal plywood-like structure in the regenerating scales, first microtubules may change their curse with a rotating angle of about 90°; then, actin microfilaments are disorganized and reorganized by interacting mechanically with the microtubules with which they are coaligned. Collagen fibrils are synthesized in a direction that is roughly perpendicular to that of the preceding ply. The unknown signals inducing the change in direction of the cytoskeleton may be transmitted throughout the hyposquama via gap junctions.This work is dedicated to the memory of Jacques Escaig     

The ultrastructure and calcification of the scales of Tilapia mossambica (Peters)

Summary The scales of Tilapia are surrounded by an envelope of scleroblasts responsible for the production of layers of collagen that constitute the bulk of the scale. The scleroblasts adjoining the lateral face of the oldest scale region gradually atrophy. New collagen layers are deposited against the inner face of the scale, the adjoining scleroblasts showing evidence of high metabolic activity. Calcification occurs by inotropic deposition of crystals alongside the fibres. There is no sharp demarcation between calcified and non-calcified scale regions, a calcification front gradually moving towards newly formed collagen layers. It is felt that fish scales should be considered as calcified derivatives of dermal collagen layers.     

Structure of the dermal scales in gymnophiona (Amphibia)

Histology and cytology of dermal scales of the gymnophionans Ichthyophis kohtaoensis and Hypogeophis rostratus reveal their structure and the nature of their mineralization. Dermal scales are small flat disks set in pockets in the transverse ridges of the skin. Each pocket contains several scales of various sizes. A ring of “hypomineralization” of varying diameter may occur on scales of a particular dermal pocket but bears no relation to the diameter of these scales. Three different layers form the scales and are seen on sections perpendicular to the surface. The cells of the basal layer lie deepest. Each of the two or three more superficial fibrous layers is composed of bundles of fibres that are oriented in parallel. The orientation varies among layers. The striation of the fiber scales has a periodicity comparable to that of the surrounding dermal fibers. Squamulae form a discontinuous layer on the scale surface and are the only mineralized part of the scale. The minerals are deposited both on the collagen fibers passing from the fibrous layers into the squamulae, and in the interfibrillar spaces. Spherical concretions, either isolated or coalescent, reaching up to 1 μm, are found on the surface of the squamulae. The dermal scales of Gymnophiona present some analogies with those of evolved bony fishes. Their characteristics could make them an original model for the study of mineralization.     

Fine Structure of the Developing Scale in the Cichlid Hemichromis bimaculatus (Pisces,Teleostei, Perciformes)

The study of the formation and structure of the early teleost scale and its associated cells has been carried out on Hemichromis bimaculatus fry using in toto staining with alizarin and transmission electron microscopy techniques. Results of the study show very rapid scale formation in Hemichromis. The papilla of the scale differentiates a little in advance of the bone scale formation. No epidermal cells are involved in the constitution of the scale pocket made up of scleroblasts. In Hemichromis, as in other teleost scales, the osseous layer is the first one to be secreted by, presumably, only the scleroblasts. Then the scleroblasts specialize in their functions. Superficial ones are involved in the formation of osseous circuli; marginal scleroblasts are responsible for growth in diameter of the scale; while deep scleroblasts allow the scales to thicken owing to the progressive addition of collagen fibrils organized in a “plywood-like” structure which constitutes the fibrillary plate of the scale. Mineralization occurs very rapidly within the osseous layer in the form of hydroxyapatite-like crystal deposits. The fibrillary plate is not yet mineralized in Hemichromis at the stages studied here, but presumably is later. Results obtained in Hemichromis are discussed against similar data available in the literature on teleost scale formation.     

Spatial Organization and Mineralization of the Basal Plate of Elasmoid Scales in Osteichthyans

In Sarcopterygii (Latimeria, Neoceratodus, Protopterus, Leptdosiren)and Amiidae (Amia) collagen fibrils of the basal plate are packedin bundles whereas they remain isolated in Teleostei. The basalplate looks like plywood, a system of superimposed layers ofparallel fibers or fibrils the directions of which rotate witha regular angle in two successive layers. The double twistedplywood is constituted of two imbricate systems, the odd andthe even, where the rotation of the fibrillar directions isright-handed in Sarcopterygii and lefthanded in Amiidae andnumerous primitive Teleostei. The orthogonal plywood, with itstwo main orthogonal fibrillar directions, characterizes theevolved Teleostei and some more primitive ones. In most teleosteanspecies, as in Amia and Protopterus, mineralization of the basalplate in elasmoid scales involves Mandl's corpuscles that mineralizewithout contact with a pre-existing calcified tissue; they growand coalesce with the neighbouring ones and fuse to the mineralizingfront. Their shape is directly influenced by the local arrangementof the collagenous fibrils. In two teleostean families (Osteoglossidaeand Mormyridae) Mandl's corpuscles are completely lacking butspreading of mineralization in the basal plate has a peculiaraspect. Whatever that may be, the various characteristic organizationsof the skeletal tissues or isopedine that constitute the basalplate of osteichthyan elasmoid scales, all are varieties ofbone tissue that have undergone more or less important specializationlinked to the general regression of dermal ossifications andto functional adaptations.     

Ultrastructural data on the melanophores associated with the cellular elasmoid scales in Leporinus friderici (Teleostei: Ostariophysi,Anastomidae): Their putative participation in scale matrix formation

Transmission electron microscopic (TEM) examination of cellular scales of Leporinus friderici reveals the presence of melanophores associated with the hyposquama, a continuous cellular layer lining the inner surface of the scale. Hyposquamal scleroblasts synthesize the collagen fibrils forming the scale matrix. Some scleroblasts lining the deep surface of the scale margin become trapped within the collagenous matrix. Neighboring melanophores become inserted within the hyposquama. They contact the scale matrix and show morphological features resembling those of the adjacent hyposquamal scleroblasts with which they are connected and, like them, they appear to be involved in the production of the collagenous scale matrix. The present ultrastructural study favors the hypothesis that melanophores in vivo are like tumorous cell lines in vitro in that they maintain a degree of plasticity allowing changes in their phenotype according to environmental conditions. The close morpho-functional links between scale scleroblasts and melanophores suggest that they could be closely related lineages derived from the same basic stem cells and support the hypothesis that scale scleroblasts as well as melanophores are neural crest derivatives. © 1996 Wiley-Liss, Inc.     

The twisted collagen network of the box-fish scutes

The present article describes the three-dimensional arrangement of collagen fibrils in dermal plates of different species of Ostraciidae. These dermal plates or 'scutes' are transformed scales, which have a polygonal shape and form a rigid tiling. They are natural composites, associating a fibrous network with a mineral deposit lying at two different levels of the scute, the 'ceiling' and the 'floor', plus a set of similarly mineralized walls joining the two levels. The three-dimensional structure of the collagen network can be compared to that of 'plywood': fibrils align parallel within superposed layers of uniform thickness, and their direction changes from layer to layer. In the dermal plate, two types of plywood have been evidenced: (1) one lying between the two mineralized plates, where the orientation of fibrils rotates continuously, and (2) one under the lower plate, with thick layers of fibrils, each showing a constant orientation, but abrupt angular changes are observed at the transition from one layer to the following one. In oblique sections, both types of plywood reveal large series of arced patterns, testifying to a twisted arrangement of collagen fibrils, analogous to the arrangement of molecules or polymers in cholesteric liquid crystals. The network is reinforced by some collagen fibrils running unidirectionally and almost normally to the lamellate structure. Moreover in the overall organization of the scute, these plywood systems form a set of nested boxes. This original architecture is compared to the arrangement of the collagenous network previously described in most fish scales and in other extracellular matrices.     

Skin and Blood Vessels of the Snout of the Australian Lungfish,Neoceratodus forsteri,and their Significance for Interpreting the Cosmine of Devonian Lungfishes

Improved structural and functional interpretations regarding the dermal skeleton of Paleozoic lungfishes (Dipnoi) can be derived from a direct comparison of Recent and fossil tissues. In particular, skin from the snout of adult Australian lungfish (Neoceratodus forsteri) contains horizontal plexuses and vertical capillary loops which resemble in structure, size and density components of the cosmine layer in such Paleozoic lungfishes as Dipterus valenciennesi and Chirodipterus australis. In addition to these dermal papillae, the skin of the snout also contains ampullary electroreceptors, goblet cells, compound mucus glands, and terminal branches and openings of the mechanoreceptive lateral line system. Pore canal systems of fossil lungfishes previously have been interpreted as housing electroreceptors or other cutaneous sense organs of the lateral line system. In contrast, we regard pore canal systems as evidence of a complex cutaneous vasculature involved in the deposition of mineralized tissues. Prevailing ideas on the structure and biological role of cosmine are reinterpreted, including the theory that electroreceptors played an important part in the origin of the dermal skeleton.     

The distribution of Tyr- and Glu-microtubules during fish scale regeneration

Cyclic rearrangements of the microtubules (Mts) occur in the hyposquamal scleroblasts which synthesize the highly ordered three-dimensional collagen network forming the basal plate of the fish scale. The distribution of Mts containing tyrosinated and detyrosinated alpha-tubulin (Tyr-Mts and Glu-Mts, respectively) was analyzed in relation to the frequency of Mt reorganization in the teleostean elasmoid scale during collagen deposition using two specific monoclonal antibodies. In the very flat hyposquamal scleroblasts of fully developed scales (with a very low synthetic activity) two microtubule populations were identified. Most contain Tyr-tubulin while Glu-tubulin is found in some "stable" Mts. In the tall prismatic scleroblasts of regenerating scales (active in collagen synthesis) only Tyr-Mts have been revealed. In late stage of regeneration, when the synthetic activity decreases and the scleroblasts flatten, an increasing centriole and Mt labeling with Glu-tubulin antibody was observed. The intimate relationship of intracellular microtubule arrangement and extracellular collagen fibril pattern reported earlier (Zylberberg et al., Cell Tissue Res. 253, 597-603 (1988], together with the results presented here, support the hypothesis that a changing Mt pattern is involved in the generation of the collagen plywood.     

Cartilage,bone, and intermandibular connective tissue in the australian lungfish,Neoceratodus forsteri (Osteichthyes: Dipnoi)

The connective tissue that links the bones of the mandible in the Australian lungfish, Neoceratodus forsteri, has been described as an intermandibular cartilage, and as such has been considered important for phylogenetic analyses among lower vertebrates. However, light and electron microscopy of developing lungfish jaws demonstrates that the intermandibular tissue, like the connective tissue that links the bones of the upper jaw, contains fibroblasts and numerous bundles of collagen fibrils, extending from the trabeculae of the bones supporting the tooth plates. It differs significantly in structure and in staining reactions from the cartilage and the bone found in this species. In common with the cladistian Polypterus and with actinopterygians and some amphibians, lungfish have no intermandibular cartilage. The connective tissue linking the mandibular bones has no phylogenetic significance for systematic grouping of lungfish, as it is present in a range of different groups among lower vertebrates. J. Morphol. 274:1085–1089, 2013. © 2013 Wiley Periodicals, Inc.     

Evidence for participation of the epidermis in the deposition of superficial layer of scales in zebrafish (Danio rerio): A SEM and TEM study

Comparative studies on scale structure and development in bony fish have led to the hypothesis that elasmoid scales in teleosts could be dental in origin. The present work was undertaken to determine whether the scales in zebrafish (Danio rerio), a species widely used in genetics and developmental biology, would be an appropriate focus for further studies devoted to the immunodetection of dental components or to the detection of the expression of genes coding for various dental proteins in fish scales. The superficial region of mature and experimentally regenerated scales and its relationships to the epidermal cover were studied in adult zebrafish using scanning (SEM) and transmission (TEM) electron microscopy. The elasmoid scales are relatively large, thin, and are located in the upper region of the dermis, close to the epidermis. In adults, the surface of the posterior region appears smooth at the SEM level and is entirely covered by the epidermis. During regeneration, the relationship of the epidermal cover to the scale surface is established within 4 days. This interface is easier to study in regenerating than in mature scales because the former are poorly mineralized. TEM revealed that: (1) the epidermis is in direct contact with the scale surface, from which it is separated only by a basement membrane-like structure, (2) there are no dermal elements at the scale surface except at the level of grooves issuing from the focus and crossing the scale surface radially, (3) the mineral crystals located in this superficial region are perpendicular to the scale surface, whereas those located deeper within the collagenous scale matrix are randomly disposed, and (4) when decalcified, the matrix of the superficial region of the scale appears devoid of collagen fibrils but contains thin electron-dense granules, some of which are arranged into layers. The continuous epidermal covering, the absence of dermal elements, as well as the fine structure of the matrix and its type of mineralization, strongly suggest that epidermal products, possibly enamel-like proteins, are deposited at the scale surface and contribute to the thickening of the upper layer in zebrafish scales. J. Morphol. 231:161–174, 1997. © 1997 Wiley-Liss, Inc.     

Development and fine structure of the bony scutes in Corydoras arcuatus (Siluriformes,callichthyidae)

The development and the structure of the bony scutes have been studied in a growth series of the armored catfish Corydoras arcuatus using light and electron microscopy. Fibroblast-like cell condensations appear in the dermis, in the posterior region of the caudal peduncle, and these will constitute the scute papillae. Collagen bundles of the preexisting dermis colonized by the papilla cells are remodeled and incorporated in the papilla to form, in addition to newly synthesized woven-fibered bony material, the initium of the scute. This process of formation differs from that described for the dermal papilla of an elasmoid scale. During growth, the osteoblasts surrounding the scute constitute the scute sac in which the scute grows. Parallel-fibered bone is deposited on both sides of the initium, and osteoblasts are incorporated within the scute matrix. The remodeling and incorporation of collagen bundles of the preexisting dermis is maintained during growth only in the deep, anterior region of the scute. The posterior region and the upper surface of the scute are close to the epidermal-dermal boundary. When growth slows down in the upper part of the scute, a characteristic, well-mineralized tissue, composed of thin vertical fibrils and granules and devoid of typical striated collagen fibrils, is deposited on the scute surface. A new term, hyaloine, is introduced for this nonosseous, highly mineralized layer constituting the upper part of the scute. Hyaloine shows thin electron-dense lines, which probably correspond to periodic growth arrests. The structure and localization of the hyaloine are compared to other well-mineralized, similar tissues found on the surface of the dermal skeleton in lower vertebrates. © 1993 Wiley-Liss, Inc.     

Convergent evolution of the lateral line system in Apogonidae (Teleostei: Percomorpha) determined from innervation

The lateral line system and its innervation were examined in two species of the family Apogonidae (Cercamia eremia [Apogoninae] and Pseudamia gelatinosa [Pseudamiinae]). Both species were characterized by numerous superficial neuromasts (SNs; total 2,717 in C. eremia; 9,650 in P. gelatinosa), including rows on the dorsal and ventral halves of the trunk, associated with one (in C. eremia) and three (in P. gelatinosa) reduced trunk canals. The pattern of SN innervation clearly demonstrated that the overall pattern of SN distribution had evolved convergently in the two species. In C. eremia, SN rows over the entire trunk were innervated by elongated branches of the dorsal longitudinal collector nerve (DLCN) anteriorly and lateral ramus posteriorly. In P. gelatinosa, the innervation pattern of the DLCN was mirrored on the ventral half of the trunk (ventral longitudinal collector nerve: VLCN). Elongated branches of the DLCN and VLCN innervated SN rows on the dorsal and ventral halves of the trunk, respectively. The reduced trunk canal(s) apparently had no direct relationship with the increase of SNs, because these branches originated deep to the lateral line scales, none innervating canal neuromast (CN) homologues on the surface of the scales. In P. gelatinosa, a CN (or an SN row: CN homologue) occurred on every other one of their small lateral line scales, while congeners (P. hayashii and P. zonata) had an SN row (CN homologue) on every one of their large lateral line scales.     

Lateral line scale types and review of their taxonomic distribution

The trunk canal of fishes is contained within a series of lateral line (LL) scales. To categorise LL scale structural types, and determine their distribution, an analysis of original data was undertaken using light and scanning electron microscopy in combination with a literature survey from over 1,000 species representative of most orders of bony fishes. Our categorisation of LL scales is based on the relationship between the tube, or ossified trunk canal segment, and associated scale. Tubular‐Scalar LL scales consist of a distinguishable tube and elasmoid scale in scale pockets. Four types occur only in species with elasmoid scales. Integrated LL scales do not develop in scale pockets, and their tube is enclosed or extended by a non‐elasmoid scale or spines. Integrated 1 and 2 LL scales co‐occur with ganoid and calcidermoid scales, and Integrated 3 LL scales occur when common scales are absent or elasmoid. Tubular LL scales are tubes only, occurring mainly in scaleless species or with calcidermoid and elasmoid scales. Non‐Tubular LL scales are composed only of a scale, co‐occurring mainly with cycloid scales. There is consistency of LL scale type in many orders, families and genera and the presence of different types within taxa can be meaningful.     

Fine structure of regenerating scales and their associated cells in the cichlid Hemichromis bimaculatus (Gill)

Summary Scale regeneration has been studied in Hemichromis bimaculatus. The removed scale, which serves as a control, is covered by its surrounding scleroblasts as can be seen with scanning electron microscopy. Subsequently, during regeneration, a population of scleroblasts arises in the empty dermal pocket as shown with transmission electron microscopy. At first, an elongated papilla of regeneration forms, probably from the differentiation of dermal fibroblasts. A scale anlage composed of the osseous layer appears in the middle of the papilla, which becomes a regenerating bag. All the surrounding large scleroblasts are involved in scale formation, although later three populations of scleroblasts specialize according to their location around the scale. Superficial scleroblasts flatten when the final thickness of the osseous layer of the scale is attained; the deep scleroblasts are responsible for the formation of the basal plate whereas marginal scleroblasts increase the diameter of the osseous layer of the scale.During scale regeneration, scleroblasts are more numerous and larger than during scale ontogenesis. In particular, deep scleroblasts form a columnar epithelium when the basal plate is laid down, a feature which is not found during scale ontogenesis. Moreover, the regenerated basal plate exhibits an orthogonal plywood arrangement that is never seen in the embryonic scale where the plywood is of the intermediate type.