Fine structural and cytochemical observations of dental epithelial cells during the enameloid formation stages in red stingrays Dasyatis akajei

Histochemical and immunohistochemical examination of odontoblasts (petroblasts) in petrodentine formation of lungfish

OBJECTIVE

Petrodentine, the core of the lungfish tooth plate, is a well-mineralized tissue similar to mammalian enamel and analogous to enameloid in fish teeth. Petrodentine is formed solely by petroblasts, which are specialized odontoblasts, whereas enameloid is a composite tissue produced by both odontoblasts and dental epithelial cells. To clarify the details of petrodentine formation, petroblasts were investigated using histochemical and immunohistochemical techniques.

METHODS

Extant lungfish (Lepidosiren paradoxa) were used in this study. Tooth plates during the stage of petrodentine formation were observed by means of histochemistry and immunohistochemistry. Commercial kits were used to detect enzyme activity. Correlative sections were immunostained using antibodies against selected peptides. Routine staining such as periodic acid-Schiff (PAS) reaction to identify glycogen and Elastica van Gieson staining for the detection of elastic fibers in histological sections were performed. In addition, conventional transmission electron microscopy was used for observing the fine structure.

RESULTS

Petroblasts showed marked acid and alkaline phosphatase activities, and positive immunoreactivities against anti-nestin, anti-V-ATPase, and anti-Ca²⁺-ATPase, during the maturation stage, but in the matrix formation stage, reactions were much weaker than that of the maturation stage. During the maturation stage, petroblasts showed intense PAS reactivity, and glycogen particles were observed in petroblasts by transmission electron microscopy. Glucose transporter 1-immunoreactivity was observed in petroblasts in the matrix formation stage and the initial to mid part of the maturation stage.

CONCLUSIONS

The results in this study suggested that petroblasts have two functional stages, matrix formation and maturation, and glycogen plays an important role in the modulation of petroblasts.

Origin and evolution of the integumentary skeleton in non-tetrapod vertebrates

Most non-tetrapod vertebrates develop mineralized extra-oral elements within the integument. Known collectively as the integumentary skeleton, these elements represent the structurally diverse skin-bound contribution to the dermal skeleton. In this review we begin by summarizing what is known about the histological diversity of the four main groups of integumentary skeletal tissues: hypermineralized (capping) tissues; dentine; plywood-like tissues; and bone. For most modern taxa, the integumentary skeleton has undergone widespread reduction and modification often rendering the homology and relationships of these elements confused and uncertain. Fundamentally, however, all integumentary skeletal elements are derived (alone or in combination) from only two types of cell condensations: odontogenic and osteogenic condensations. We review the origin and diversification of the integumentary skeleton in aquatic non-tetrapods (including stem gnathostomes), focusing on tissues derived from odontogenic (hypermineralized tissues, dentines and elasmodine) and osteogenic (bone tissues) cell condensations. The novelty of our new scenario of integumentary skeletal evolution resides in the demonstration that elasmodine, the main component of elasmoid scales, is odontogenic in origin. Based on available data we propose that elasmodine is a form of lamellar dentine. Given its widespread distribution in non-tetrapod lineages we further propose that elasmodine is a very ancient tissue in vertebrates and predict that it will be found in ancestral rhombic scales and cosmoid scales.

The Origin and Evolution of Enamel Mineralization Genes

BACKGROUND/AIMS

Enamel and enameloid were identified in early jawless vertebrates, about 500 million years ago (MYA). This suggests that enamel matrix proteins (EMPs) have at least the same age. We review the current data on the origin, evolution and relationships of enamel mineralization genes.

METHODS AND RESULTS

Three EMPs are secreted by ameloblasts during enamel formation: amelogenin (AMEL), ameloblastin (AMBN) and enamelin (ENAM). Recently, two new genes, amelotin (AMTN) and odontogenic ameloblast associated (ODAM), were found to be expressed by ameloblasts during maturation, increasing the group of ameloblast-secreted proteins to five members. The evolutionary analysis of these five genes indicates that they are related: AMEL is derived from AMBN, AMTN and ODAM are sister genes, and all are derived from ENAM. Using molecular dating, we showed that AMBN/AMEL duplication occurred >600 MYA. The large sequence dataset available for mammals and reptiles was used to study AMEL evolution. In the N- and C-terminal regions, numerous residues were unchanged during >200 million years, suggesting that they are important for the proper function of the protein.

CONCLUSION

The evolutionary analysis of AMEL led to propose a dataset that will be useful to validate AMEL mutations leading to X- linked AI.

Fine structural and cytochemical mapping of enamel organ during the enameloid formation stages in gars, Lepisosteus oculatus, Actinopterygii

During cap enameloid formation in gars (Lepisosteus oculatus), the dental epithelial cells that constitute the enamel organ were observed by means of transmission electron microscopy and enzyme cytochemistry to detect the hydrolytic enzyme activities, alkaline phosphatase (ALPase), acid phosphatase (ACPase), calcium-dependent adenosine triphosphatase (Ca-ATPase) and potassium-dependent p-nitrophenylphosphatase (K-NPPase) (sodium, potassium-activated adenoshine triphosphatase (Na-K-ATPase)). The enameloid formation process in gars was divided into three stages: matrix formation, mineralisation and maturation. The enamel organ consisted of the outer dental epithelial (ODE) cells, stellate reticulum (SR), stratum intermedium (SI) and the inner dental epithelial (IDE) cells during the whole of the cap enameloid formation stages. During the matrix formation stage, many cisternae of rough endoplasmic reticulum and widely distributed Golgi apparatus, in which the procollagen granules containing cross-striations were often found, were remarkable elements in the IDE cells. During the stage of mineralisation, the IDE cells were tall columnar, and infoldings of distal plasma membrane of the IDE cells became marked. The most developed Golgi apparatus was visible at this stage, and large secretory granules containing fine granular or tubular materials were found in the distal cytoplasm that was close to the infoldings of the distal end. Many lysosomes that were ACPase positive were seen near the Golgi apparatus and in the distal cytoplasm of the IDE cells. ACPase positive granules often contained the cross-striation structure resembling procollagen, suggesting that the procollagen is degenerated in the IDE cells. During the maturation stage, the distal infoldings became unclear, and there were no large granules containing tubular materials, but many ACPase positive lysosomes were still present in the IDE cells. Non-specific ALPase was detected at the plasma membrane of the IDE cells at the mineralisation and maturation stages. K-NPPase was markedly detected at the plasma membrane of the IDE cells at the maturation stage. These results demonstrate that the IDE cells might be mainly involved in the removal of degenerated organic matrix from enameloid during the later formation stages. Strong Ca-ATPase activity was observed at the entire plasma membrane of the stratum intermedium cells, and there was slightly weak activity at the plasma membrane of the IDE cells during the mineralisation and maturation stages, implying that these cells are related to the active Ca transport to the maturing enameloid. It is likely that although the structure of the enamel organ is different, the function, especially at the mineralisation and maturation stages, is similar to other actinopterygians having well-mineralized cap enameloid.

Fine structural and cytochemical observations on the dental epithelial cells during cap enameloid formation stages in Polypterus senegalus, a bony fish (Actinopterygii)

Tooth germs during cap enameloid formation stages in Polypterus senegalus were investigated by transmission electron microscopy and enzyme histo- and cytochemistry. Enameloid formation was divided into three stages: matrix formation, mineralization, and maturation. The enamel organ consisted of the inner dental epithelial cells, stellate reticulum, and outer dental epithelial cells during cap enameloid formation stages, but no stratum intermedium was found. During the matrix formation stage, the tall inner dental epithelial cells contained well-developed Golgi apparatus, abundant cisternae of rough endoplasmic reticulum and mitochondria. Spindle-shaped vesicles containing a filamentous structure were seen in the distal cytoplasm. During mineralization and maturation stages, many ACPase positive lysosomes were present in the cytoplasm, whereas the organelles were decreased in number. The infoldings of the distal plasma membrane of the inner dental epithelial cells were visible in the mineralization stage but were not marked in the maturation stage. The activity of nonspecific ALPase, Ca-ATPase, and K-NPPase was detected at the plasma membrane of the inner dental epithelial cells during the stages of mineralization and maturation. The results of fine structure and enzyme cytochemistry suggested that the dental epithelial cells were mainly involved in the degeneration and removal of enameloid matrix and in material transportation during the enameloid mineralization and maturation stages, rather than in the enameloid matrix formation. The results also showed that the structure of the dental epithelial cells in Polypterus was different from that in teleosts and gars, but that the function of the dental epithelial cells was similar to that in teleosts possessing well-mineralized cap enameloid.

Fine structure and Ca-ATPase activity of the stratum intermedium cells during odontogenesis in gars, Lepisosteus, Actinopterygii

This is the first report on the stratum intermedium in vertebrates other than mammals. The aim of this study is to elucidate the fine structure and cytochemical features of the stratum intermedium during the stages of enameloid formation in Lepisosteus. Inner dental epithelium, stratum intermedium, stellate reticulum, and outer dental epithelium are consistently present in the tooth germs of Lepisosteus. The stratum intermedium cells are oval in shape, contain elliptical nuclei, and extend many small processes. It is implied that the structure of the enamel organ is different among actinopterygians, and that constitution of the enamel organ in Lepisosteus resembles that in higher vertebrates. Marked Ca-ATPase activity is observed at the cell membrane of the stratum intermedium cells, suggesting that the cells are involved in calcium transport during the stages of enameloid formation.

Mineralization patterns in elasmobranch fish

This article reviews current findings on the organic matrix and the mineralization patterns in elasmobranchs, including an analysis of the role of the dental epithelial cells and the odontoblasts during odontogenesis. Our electron micrographs demonstrated that tubular vesicles limited by a unit membrane occupied the bulk of the elasmobranch enameloid matrix during the stage of enameloid matrix formation. It is likely that the tubular vesicles originated from the odontoblast processes. Two types of electron-dense fibrils, with cross-striations at intervals of approximately either 17 nm or 55 nm, respectively, were detected in the enameloid matrix. These data suggest that odontoblasts were strongly involved in enameloid matrix formation and in initial enameloid mineralization. Two types of odontoblasts, dark and light cells, were recognized during the stage of dentinogenesis. The light cells contained numerous mitochondria, intermediate filaments, and microtubules that extended their processes into the dentin. The dark cells possessed a well-developed Golgi apparatus and many cisternae in the rough endoplasmic reticulum, which suggests that the dark cells are involved in the formation of dentin. The inner dental epithelial (IDE) cells exhibited a well-developed Golgi apparatus, many mitochondria, cisternae of smooth endoplasmic reticulum, vesicles, vacuoles, and granules during the mineralization and maturation stages. During the stages of mineralization and early maturation, ACPase-positive granules were visible in the IDE cells and ALPase and Ca-ATPase activities were found at the lateral and proximal cell membrane of the IDE cells, suggesting that the IDE cells are involved in the removal of enameloid organic matrix and in the process of mineralization during later stages of enameloid formation. Our data indicate that elasmobranch enameloid is distinct from teleost enameloid, based on its organic content, on the mechanisms of its mineralization, and on the role of IDE cells concerning enameloid formation.