Late skeletal development at the articulation between upper pharyngeal jaws and neurocranial base in the fish, Astatotilapia elegans, with the participation of a chondroid form of bone

This paper presents light-microscopical details of the late development of skeletal tissues at the joint between upper pharyngeal jaws (UPJs) and neurocranial base (parasphenoid and basioccipital bones) in the acellular-boned teleost Astatotilapia elegans. On each of the supporting elements, a bone tissue (AB) is deposited that is anomalous because of its retention of cells within the matrix. Later, this layer is gradually replaced by the anomalous large-celled chondroid kind of bone (CB). Both AB and CB probably grow by apposition from the overlying fibrous layer. Osteoblastlike cells secrete osteoid, which soon calcifies and traps the cells. As in young cellular membrane bone, cells in the AB have a wide, elongate shape and lie amidst sparse, calcified, bonelike matrix but lack a canalicular system. Later generations of enclosed cells have a more vesicular shape, with at least some cells remaining alive in the calcified matrix. Appositional growth of the chondroid bone at its articular side is matched from a certain stage onward by erosion at its basal side. On the upper pharyngeal jaws this resorption is clearly related to the development of new teeth. Although in older stages and adults the chondroid tissue resembles a secondary cartilage, the term chondroid bone (CB) was preferred because of (1) the continuing formation by osteoblastlike cells; (2) the staining affinities of its matrix with that of bone; and (3) its formation both on cartilage bone (the infrapharyngobranchials III-IV and basioccipital bone) and on membrane bone (the parasphenoid bone).     

Content and Distribution of Noncollagenous Matrix Proteins in Bone and Cementum: Relationship to Speed of Formation and Collagen Packing Density

The organic matrix of collagen-based calcified tissues consists of a supporting collagen meshwork and various noncollagenous matrix proteins (NCPs). Together, they contribute to determining the structure and biomechanical properties of the tissue. Their respective organization and interrelation can advantageously be examined by immunocytochemistry, an approach which allows correlation of composition with structure. The aim of this article is to review postembedding immuno- and lectin-gold-labeling data on the characterization of the noncollagenous compartment in rat and human bone and cementum, and on its relationship to collagen. The two major NCPs, bone sialoprotein and osteopontin, generally codistribute and accumulate in cement lines and in the spaces among the mineralized collagen fibrils. However, there are variations in their distribution and density of labeling throughout the tissue. Indeed, bone and cementum can form in environments that are either poor or enriched in NCPs. The amount of NCPs generally correlates with bone and cementum types and with speed of formation of the tissue and packing density of collagen fibrils. Taken together, the data suggest that production of both collagenous and noncollagenous constituents can be "modulated" during formation of collagen-based calcified tissues. It is concluded that, in addition to structural and compositional parameters, tissue dynamics must be taken into consideration in order to understand the significance of the apparent accumulation of NCPs at some sites and to determine the mechanisms of normal and pathological calcified tissue formation.     

Osteoblasts develop from isolated fetal mouse chondrocytes when co-cultured in high density with brain tissue

Summary Chondrocytes from the hypertrophic and proliferative zones of 16-day-old fetal murine metatarsal bones were enzymatically dissociated and cultured in a high-density type of culture, exposed to the gas phase. We ascertained that no cells of the perichondrium were included in the cell suspension. Control cultures formed a solid cartilaginous mass, of which all the chondrocytes were alkaline phosphatase positive and the matrix started to calcify after 4 days. After 6 days, nearly the entire matrix was calcified. When co-cultured with pieces of cerebral tissue, some chondrocytes had transdifferentiated into osteoblasts after 4 days. They had started to form osteoid. After 6 and 11 days part of the cartilage had been replaced by bone, especially in the periphery of the cultures, but also in areas in the center. The bone matrix was partly calcified. Osteoblasts and bone matrix were identified as such electron microscopically. The nature of the bone matrix was also confirmed by immunohistochemical demonstration of collagen type I and osteocalcin. These results show that enzymatically isolated chondrocytes are able to become osteoblasts when properly stimulated. This supports the concept of chondrocytes being responsible for (part of) the endochondral bone formation in the marrow cavity of long bones.     

Bone formation in organ cultures of bone marrow

Summary Bone formation in organ cultures of intact marrow fragments from mouse is described. Marrow explants were cultured on the top surface of a millipore filter at a gas-liquid interface. Observations with both light- and electron microscopes demonstrated the formation of a well-organised trabecular matrix lined with osteoblast-like cells. The tissue and cells were positive for alkaline-phosphatase activity. Large amounts of thick, well-banded collagen fibrils and matrix vesicles typical of those found in bone were present. The tissue became mineralised in the presence of 10 mM Na--glycerophosphate; in its absence a similar trabecular matrix developed but mineralisation did not take place.     

An ultrastructural study of macrophage-mediated resorption of calcified tissue

Summary Ultrastructural observations on macrophage-mediated resorption of calcified tissue of killed fetal long bones are described and correlated with increased ⁴⁵Ca release into the medium. Macrophages disrupt calcified tissue extracellularly and appear to engulf large fragments of mineralized matrix. Ruffled borders, which are common features of osteoclasts at sites of resorption of bone, do not develop in macrophages. However, clear zones are seen in macrophages as well as osteoclasts. These findings provide additional evidence for non-osteoclast-mediated resorption of calcified tissue.This study was supported by Grant DE-04443 from USPHS     

Ovotransferrin and ovotransferrin receptor expression during chondrogenesis and endochondral bone formation in developing chick embryo

Ovotransferrin expression during chick embryo tibia development has been investigated in vivo by immunocytochemistry and in situ hybridization. Ovotransferrin was first observed in the 7 day cartilaginous rudiment. At later stages, the factor was localized in the articular zone of the bone epiphysis and in the bone diaphysis where it was concentrated in hypertrophic cartilage, in zones of cartilage erosion and in the osteoid at the chondro-bone junction. When the localization of the ovotransferrin receptors was investigated, it was observed that chondrocytes at all stages of differentiation express a low level of the oviduct (tissue) specific receptor. Interestingly, high levels of the receptor were detectable in the 13-d old tibia in the diaphysis collar of stacked-osteoprogenitor cells and in the layer of derived osteoblasts. High levels of oviduct receptor were also observed in the primordia of the menisci. Metabolic labeling of proteins secreted by cultured chondrocytes and osteoblasts and Northern blot analysis of RNA extracted from the same cells confirmed and completed the above information. Ovotransferrin was expressed by in vitro differentiating chondrocytes in the early phase of the culture and, at least when culture conditions allowed extracellular matrix assembly, also by hypertrophic chondrocytes and derived osteoblast-like cells. Osteoblasts directly obtained from bone chips produced ovotransferrin only at the time of culture mineralization. By Western blot analysis, oviduct receptor proteins were detected at a very low level in extract from differentiating and hypertrophic chondrocytes and at a higher level in extract from hypertrophic chondrocytes undergoing differentiation to osteoblast-like cells and from mineralizing osteoblasts. Based on these results, the existence of autocrine and paracrine loops involving ovotransferrin and its receptor during chondrogenesis and endochondral bone formation is discussed.     

The biomaterial influences the ossification after sinus floor elevation using tissue-engineered bone grafts

Sinus floor elevation is the standard procedure that allows dental implant insertion in the atrophic posterior maxilla. Instead of autogenous bone, tissue-engineered bone grafts can be used, but clear comparative clinical studies also assessing the influence of the biomaterial are missing. In six patients, tissue-engineered bone grafts were used in eight sinus floor elevations. After culturing osteoblast-like cells from biopsies of the maxilla, they were seeded on scaffolds made either from demineralised bovine bone matrix (DBBM) or from solvent-dehydrated mineralised bone (SDBB), and grafted. In all patients primary wound healing was without complications, except for one patient in the SDBB group. After 12 months, implant insertion was possible only in the SDBB group; in the DBBM group, fibrous connective tissue was found in an attempt of implant insertion. After 5 months, implant placement was performed in one patient of each group. However, the two implants inserted in the DBBM group were lost after 6 weeks. Histology of the bone cores in the DBBM group at 5 months showed lamellar bone and osteoid, and at 12 months showed fibrous connective tissue. Inflammation and some resorption of the scaffold was found 5 months after SDBB grafting, and after 12 months cancellous bone formation encapsulating SDBB remnants were observed. These preliminary data suggest that the preparation method of the bovine bone matrix, in particular the mineral content, and therefore the mechanical stability may have some influence on the generation of new bone.     

Ultrastructure of mineralized nodules formed in rat bone marrow stromal cell culture in vitro.

Rat bone marrow stromal cells were cultured in vitro. At days 14-15 of culture, dense clusters of polygonal cells were formed, and they mineralized 2-3 days later. The cells resembling osteoblasts or young osteocytes were histologically observed to be embedded in mineralized or unmineralized extracellular matrices of the nodules. Next, these mineralized nodules were electron-microscopically examined. The osteoblastic cells associated with the nodules had a well-developed rough endoplasmic reticulum, an evident Golgi apparatus and some mitochondria as their intracellular organellae. Some lysosomes and microfilaments were also visible in the cytoplasms. Moreover, some cells protruded cell processes toward the neighboring cells through the extracellular matrix. The extracellular matrix consisted of numerous collagen fibrils which were striated with 60-70 nm axial periodicity and which was similar to bone tissue collagen. A large number of matrix vesicles were scattered among the collagen fibrils in the unmineralized area of the nodules. In contrast, in the mineralized area, numerous matrix vesicles at different stages of maturation and many calcified spherules were observed. That is the mineralization in this culture system was considered to be initiated in association with the matrix vesicles and to progress along the collagen fibrils. From these findings, it was confirmed by the present study that the mineralized nodules formed in this bone marrow stromal cell culture were ultrastructurally similar to bone and that the mineralization also proceeded by going through the normal calcification process. This culture system is considered to be available to study osteogenic differentiation and calcification mechanisms.     

A tracer study with systemically and locally administered dinitrophenylated osteopontin.

Osteopontin (OPN), a major non-collagenous matrix protein of bone, is also found in tissue fluids and in the circulation. It is still not clear whether circulating OPN contributes to bone formation. To elucidate this question, rat OPN was tagged with dinitrophenol groups and administered to rats either intravenously or by infusion with an osmotic minipump through a "surgical window" in the bone of the hemimandible. Dinitrophenylated rat albumin (ALB) was used as a control. The presence and distribution of tagged proteins were revealed by immunogold labeling on sections of tibia and alveolar bone. Tagged molecules of OPN were found in mineralization foci, surfaces and interfaces, and matrix accumulations among calcified collagen fibrils. Even though dinitrophenylated ALB was administered at several-fold higher concentrations, it did not accumulate in these sites. These results show that circulating OPN can be incorporated into specific compartments of forming bone and suggest that such molecules may play a more important role than previously suspected.     

Transformation of fetal secondary cartilage into embryonic bone in organ cultures of human mandibular condyles

Mandibular condyles of human fetuses, 14–21 weeks in utero, were kept in an organ culture system for up to 60 days. After 6 days in culture, the cartilage of the mandibular condyle appeared to have maintained its inherent structural characteristics, including all its various layers: chondroprogenitor, chondroblastic, and hypertrophic. After 12 days in culture, no chondroblasts could be seen; instead, the entire cartilage was occupied by hypertrophic chondrocytes. At the same time, the mesenchymal cells in the vicinity of the chondroprogenitor zone differentiated into osteoblast-like cells that produced type I collagen. The progenitor cells were still actively incorporating ³H-thymidine. The newly formed osteoid-like tissue lacked both metachromatic reactivity and a response to antibodies against chondroitin sulfate. Instead, the tissue reacted positively for osteocalcin (bone gla-protein). The process of new bone formation further progressed and, by the 20th day in culture, the new bone reacted positively for type I collagen, osteonectin, and to a lesser extent for chondroitin sulfate. The osteoid also underwent mineralization as revealed by both the von Kossa stain and vital staining with tetracycline. The above feature appeared even more intense in 40-day-old cultures. After 60 days, the newly formed bone contained osteoblasts and osteocytes, whereas the extracellular matrix revealed a high degree of matrix polarization. The results of the present study recapitulate findings reported for organ cultures of mice mandibular condyles. However, the in vitro process of de novo bone formation in human specimens requires a 6-fold longer culture time than that needed for mice condyles.     

Extracellular alkaline phosphatase activity in mineralizing matrices of cartilage and bone: ultrastructural localization using a cerium-based method.

The ultrastructural localization of alkaline phosphatase (A1P) activity has been demonstrated in epiphyseal growth cartilage and metaphyseal bone of rats. Epiphyso-metaphyseal specimens were decalcified with EDTA and treated with MgCl2 to regenerate the enzymatic activity before incubation in a medium containing beta-glycerophosphate, MgCl2 and CeCl3. A1P activity was present on the outer surface of the plasmamembrane of maturing and hypertrophic chondrocytes and of osteoblasts. Moreover, the reaction product was present in chondrocyte lacunae, in matrix vesicles, and in cartilage matrix, as well as among uncalcified collagen fibrils of osteoid tissue in bone. The intensity of reaction was the lowest, or completely lacking, where the degree of matrix calcification was the highest. These results suggest that alkaline phosphatase is transported from the cells into the cartilage and bone matrix by its association with matrix vesicles and plasmamembrane components, and that its activity in cartilage and bone matrix is inhibited as it is incorporated in the mineral substance.     

Extracellular alkaline phosphatase activity in mineralizing matrices of cartilage and bone: ultrastructural localization using a cerium-based method

Summary The ultrastructural localization of alkaline phosphatase (AlP) activity has been demonstrated in epiphyseal growth cartilage and metaphyseal bone of rats. Epiphyso-metaphyseal specimens were decalcified with EDTA and treated with MgCl₂ to regenerate the enzymatic activity before incubation in a medium containing beta-glycerophosphate, MgCl₂ and CeCl₃. AlP activity was present on the outer surface of the plasmamembrane of maturing and hypertrophic chondrocytes and of osteoblasts. Moreover, the reaction product was present in chondrocyte lacunae, in matrix vesicles, and in cartilage matrix, as well as among uncalcified collagen fibrils of osteoid tissue in bone. The intensity of reaction was the lowest, or completely lacking, where the degree of matrix calcification was the highest. These results suggest that alkaline phosphatase is transported from the cells into the cartilage and bone matrix by its association with matrix vesicles and plasmamembrane components, and that its activity in cartilage and bone matrix is inhibited as it is incorporated in the mineral substance.     

Leukaemia inhibitory factor (lif) is expressed in hypertrophic chondrocytes and vascular sprouts during osteogenesis

Avascular cartilage is replaced by highly vascularized bone tissue during endochondral ossification, a process involving capillary invasion of calcified hypertrophic cartilage in association with apoptosis of hypertrophic chondrocytes, degradation of cartilage matrix and deposition of bone matrix. All of these events are closely controlled, especially by cytokines and growth factors. Leukaemia inhibitory factor (LIF), a member of the gp130 cytokine family, is involved in osteoarticular tissue metabolism and might participate in osteogenesis. Immunohistochemical staining showed that LIF is expressed in hypertrophic chondrocytes and vascular sprouts of cartilage and bone during rat and human osteogenesis. LIF is also present in osteoblasts but not in osteoclasts. Observations in a rat endochondral ossification model were confirmed by studies of human cartilage biopsies from foetuses with osteogenesis imperfecta. LIF was never detected in adult articular chondrocytes and bone-marrow mesenchymal cells. These results and other data in the literature suggest that LIF is involved in the delicate balance between the rate of formation of calcified cartilage and its vascularization for bone development.     

In vitro differentiation and calcification in a new clonal osteogenic cell line derived from newborn mouse calvaria

We investigated the capacity of a clonal osteogenic cell line MC3T3-E1, established from newborn mouse calvaria and selected on the basis of high alkaline phosphatase (ALP) activity in the confluent state, to differentiate into osteoblasts and mineralize in vitro. The cells in the growing state showed a fibroblastic morphology and grew to form multiple layers. On day 21, clusters of cells exhibiting typical osteoblastic morphology were found in osmiophilic nodular regions. Such nodules increased in number and size with incubation time and became easily identifiable with the naked eye by day 40-50. In the central part of well-developed nodules, osteocytes were embedded in heavily mineralized bone matrix. Osteoblasts were arranged at the periphery of the bone spicules and were surrounded by lysosome-rich cells and a fibroblastic cell layer. Numerous matrix vesicles were scattered around the osteoblasts and young osteocytes. Matrix vesicles and plasma membranes of osteoblasts, young osteocytes, and lysosome-rich cells showed strong reaction to cytochemical stainings for ALP activity and calcium ions. Minerals were initially localized in the matrix vesicles and then deposited on well-banded collagen fibrils. Deposited minerals consisted exclusively of calcium and phosphorus, and some of the crystals had matured into hydroxyapatite crystals. These results indicate that MC3T3-E1 cells have the capacity to differentiate into osteoblasts and osteocytes and to form calcified bone tissue in vitro.     

Three-dimensional visualization analysis of in vitro cultured bone fabricated by rat marrow mesenchymal stem cells

Marrow mesenchymal stem cells are well known for their differentiation into bone-forming osteoblasts and in vitro mineralized tissue formation. However, process details, including tissue structure and cellular environments, remain unclear. The present study demonstrates three-dimensional visualization of tissue fabricated by culturing MSCs in the presence of calcein, a fluorescent marker for bone mineralization. The 3D visualization was performed by computer-assisted confocal laser scanning microscopy and revealed that the in vitro tissue consisted of layers of a mineralized matrix with round cells in the matrix lacunae, an unmineralized matrix (osteoid), and osteoblastic cells on the osteoid surface. The findings show that the mineralization by cultured MSCs is an in vitro counterpart of in vivo bone formation and indicate that the novel technique of visualization without tissue fixation could be useful for continuous monitoring of tissue organization in an ongoing culture.     

Demonstration of the capacity of nacre to induce bone formation by human osteoblasts maintained in vitro.

Nacre implanted in vivo in bone is osteogenic suggesting that it may possess factor(s) which stimulate bone formation. The present study was undertaken to test the hypothesis that nacre can induce mineralization by human osteoblasts in vitro. Nacre chips were placed on a layer of first passage human osteoblasts. None of the chemical inducers generally required to obtain bone formation in vitro was added to the cultures. Osteoblasts proliferated and were clearly attracted by nacre chips to which they attached. Induction of mineralization appeared preferentially in bundles of osteoblasts surrounding the nacre chips. Three-dimensional nodules were formed by a dense osteoid matrix with cuboidal osteoblasts at the periphery and osteocytic-like cells in the center. These nodules contained foci with features of mineralized structures and bone-like structures, both radiodense to X-ray. Active osteoblasts (e.m.) with abundant rough endoplasmic reticulum, extrusion of collagen fibrils and budding of vesicles were observed. Matrix vesicles induced mineral deposition. Extracellular collagen fibrils appeared cross-banded and electrodense indicating mineralization. These results demonstrate that a complete sequence of bone formation is reproduced when human osteoblasts are cultured in the presence of nacre. This model provides a new approach to study the steps of osteoblastic differentiation and the mechanisms of induction of mineralization.     

Ultrastructural study of the long-term development of two experimental cutaneous calcinoses (topical calciphylaxis and topical calcergy) in the rat

Summary Skin calcification induced by topical calciphylaxis was provoked by a subcutaneous injection of iron chloride in rats previously sensitized by dihydrotachysterol. A cutaneous topical calcergy was induced by an injection of potassium permanganate. An electron-microscopical study of the long-term evolution of both these models of calcification was made. After the initial stages, mineralization of the connective tissue continued by a secondary nucleation process without matrix vesicles. The mineral composed of needle-like structures, apatite in nature, was mainly deposited between and around collagen fibrils, and showed various arrangements in calcified plaques. Intrafibrillar calcification was rarely observed and appeared only in the later stages. The extension of calcified deposits then stopped. Finally, there was a fragmentation of the mineralized area which was progressively surrounded by uncalcified collagen fibrils. A demineralization process, caused by cells such as macrophages and multinucleated giant cells, rather than a resorption of the calcified deposits, was noted. It is important to emphasize that, in both models of ectopic calcification, an evolution toward ectopic ossification was never observed, which is perhaps due to the absence of extensive resorption mechanisms.     

Immunoelectron microscopic studies of glycosaminoglycans in the metaphyseal bone trabeculae of growing rats

Summary The types and distribution of glycosaminoglycans (GAGs) were studied immunocytochemically in osteoid, mineralized bone matrix, and cartilage matrix of growing rat metaphyseal bone after aldehyde fixation and EDTA demineralization, using four monoclonal antibodies (mAbs 1-B-5, 2-B-6, 3-B-3 and 5-D-4). These mAbs specifically recognize epitopes in non-sulphated chondroitin (C0-S); chondroitin 4-sulphate (C4-S) and dermatan sulphate (DS); chondroitin 6-sulphate (C6-S) and C0-S; and keratan sulphate (KS) respectively. In osteoid, all mAbs except 1-B-5 weakly stained matrix material on and between collagen fibrils, and moderately stained organic material corresponding to bone nodules, which are known sites of mineralization. However, the staining of osteoid abruptly decreased at the mineralization front; weak staining was confined mostly to the organic material of bone nodules in mineralized bone matrix, with very weak or no staining of the rest of the bone matrix. This staining progressively decreased toward the mineralized cartilage matrix and became negative. The mineralized cartilage matrix and lamina limitans reacted strongly with all mAbs except 5-D-4. These results indicate that osteoid contains sulphated proteoglycans containing C4-S and/or DS, C6-S and KS, and subsequent bone matrix mineralization appears to require accumulation of these macromolecules within bone nodules and eventual loss of these substances for complete mineralization, whereas proteoglycans containing C0-S, C4-S and/or DS, and C6-S, still exist in mineralized cartilage matrix and lamina limitants.     

Changes in glycosaminoglycan binding to collagen during desmoid mineralization as revealed by different electron-microscopic staining techniques.

Mineralization at collagen fibrils is regulated by glycosaminoglycans (GAG). Alterations in proteoglycan composition during mineralization as well as inhibition of mineralization by GAGs are well documented. Collagen-GAG interactions during desmoid osteogenesis in fetal rat calvariae were investigated ultrastructurally by means of different fixation techniques. Mineralization was restricted to the collagen of the osteoid at the ectocranial side. Beyond the osteoid, one layer containing degenerated cells was found, followed by sheets of healthy osteoblasts with nonmineralized collagen fibrils. These fibrils were ordered in bundles, but were irregularly arranged in the mineralized osteoid. After fixation in glutaraldehyde-ruthenium red (GA-RR), small RR-positive granules were periodically attached to the fibrils of the nonmineralized collagen. These granules were absent at collagen in the mineralized osteoid. Periodically bound granules (periodicity of 62 nm) could clearly be demonstrated along collagen fibrils by pretreatment with the positively charged protamine sulfate and subsequent fixation in GA-RR in the nonmineralized collagen. In the mineralized osteoid, however, these granules were present, but periodic binding was missing. Heparin pretreatment followed by fixation in GA-RR revealed periodically bound fine strands between collagen fibrils running parallel in the nonmineralized collagen; these threads were absent in the mineralizing osteoid. Restriction of mineralization to osteoid at the mineralization border may be reflected by the observed changes in GAG binding to collagen fibrils within the osteoid of developing fetal calvariae in contrast to binding to collagen in nonmineralized areas.     

Osteoid resorption by mononuclear cells in vitro

Summary For the first time, mononuclear cell-mediated ingestion of osteoid in cultures of long bones of fetal rats is described and characterized. The mononuclear cells, located at sites of osteoid deposition, ingest collagen fibrils and clumps of mineral crystals which are segregated within cytoplasmic vacuoles or multivesicular bodies. The ingestion of osteoid continues in cultures treated with agents that normally inhibit osteoclastic bone resorption. Morphologically, the osteoid-containing cells are characterized by a moderate number of mitochondria and short-stranded rough endoplasmic reticulum, a modest Golgi apparatus and variable numbers of vesicles, vacuoles, and multivesicular bodies. The morphologic appearance of the mononuclear cell is consistent with that of a macrophage.This study was supported by NIH Grants DE-04443 and AM-16858