Faculty Bibliography

The localization of fibrillar type I and II collagen was investigated by immunofluorescence staining with specific antibodies in order to obtain a better understanding of tissue remodelling during the development of first rib cartilage. In childhood and early adolescence type I collagen was found to be restricted to the perichondrium of first rib cartilage, while type II collagen was localized in the matrix of hyaline cartilage. However, in advanced age type I collagen was also found in the territorial matrix of intermediate and central chondrocytes of first rib cartilage. The matrix of subperichondrial chondrocytes was negative for type I collagen. This suggests that some chondrocytes in first rib cartilage undergo a modulation to type I collagen-producing cells. The first bone formation was observed in rib cartilages of 20- to 25-year-old adults. Interestingly, the ossification began peripherally, adjacent to the innermost layer of the perichondrium where areas of fibrocartilage had developed. The newly formed bone matrix showed strong immunostaining for type I collagen. Fibrocartilage bordering peripherally on bone matrix revealed only a faint staining for type I collagen, but strong immunoreactivity to type II collagen. The interterritorial matrix of the central chondrocytes failed to react with the type II collagen antibody, in both men and women, from the end of the second decade. These observations indicate that major matrix changes occur at the same time in male and female first rib cartilages. Thus, our findings indicate that ossification in human first rib cartilage does not follow the same pattern as that observed in endochondral ossification of epiphyseal discs or sternal cartilage

The distribution of type I, II, IX, XI and X collagens in and close to areas of asbestoid (amianthoid) fibers in thyroid cartilages of various ages was investigated in this study. Asbestoid fibers were first detected in thyroid cartilage from a 3-year-old male child. Areas of asbestoid fibers functionally appear to serve as guide rails for vascularization of thyroid cartilage. Alcian blue staining in the presence of 0.3 M MgCl2 revealed a loss of glycosaminoglycans in areas of asbestoid fibers. In addition, the fibers reacted positively with antibodies against collagen types II, IX and XI, but showed no staining with antibodies to collagen types I and X. Territorial matrix of adjacent chondrocytes showed the same staining pattern. In addition to staining for type II, IX and XI collagens, asbestoid fibers showed strong immunostaining for type I collagen after puberty but not for type X collagen. However, groups of chondrocytes within areas of asbestoid fibers reacted strongly with antibodies to type X collagen, suggesting that this collagen plays an important role in matrix of highly differentiated chondrocytes. The finding that these type X collagen-positive chondrocytes also revealed immunostaining for type I collagen confirms previous studies showing that hypertrophic chondrocytes can further differentiate into cells that are characterized by the synthesis of type X and I collagens

Mineralization and osteogenesis in the human first rib cartilage were studied radiologically and by means of normal and polarized light microscopy. Onset of mineralization occurs at the end of puberty and is located directly beneath the perichondrium. Bone is formed in a typical spur-like pattern, arising medially from the upper edge of the manubrium sterni and laterally from the caudal rim of the bony part of the rib. From the middle of the second decade, large cartilage canals with several blood vessels and loose perivascular connective tissue are seen in central areas of the first costal cartilage. These parts are the last to be mineralized and ossified in old age. The type of osteogenesis cannot be classified according to common patterns. In spite of the subperichondral localization it cannot be intramembranous, because the new bone is separated from the perichondrium by a layer of mineralized cartilage. Osteogenesis cannot be called endochondral compared with the epiphyseal plate for the following reasons: there are no hypertrophied chondrocytes; an immunoreactivity for collagen type X is missing; areas where bone is formed directly on hyaline cartilage could be proved. Vascularization and onset of osteogenesis are separated in time and localization. Mineralization and osteogenesis in human first rib cartilage are physiological age-related changes, which cannot be regarded as degenerative processes. Ossification is not directly correlated with the invasion of blood vessels and cannot be classified as one of the classical concepts of intramembranous or endochondral osteogenesis

Matrix vesicles (MV) were shown to initiate mineralization in cartilage and other vertebrate tissues. However, the factors that drive this process remain to be fully elucidated. Recent studies have shown that a preformed nucleational core consisting mainly of a Ca(2+)-phosphatidylserine-Pi complex, is necessary for the accumulation of Ca2+ by MV. In addition, the collagens attached to the MV surface were shown to play an important role in stimulating Ca2+ uptake. In this study, we extend this knowledge by showing that both, the nucleational core and the collagens (types II and X), are co-requirements for rapid influx of Ca2+ into intact MV. MV to which collagen fragments were attached were released from hypertrophic chicken cartilage by trypsin and collagenase digestion (trypsin/collagenase-released MV (TCRMV), while 'collagen-free' MV were released by hyaluronidase and collagenase digestion (hyaluronidase/collagenase-released MV (HCRMV). In contrast to TCRMV which showed active uptake of Ca2+, HCRMV showed only little uptake. However, binding of native type II collagen to HCRMV stimulated uptake of Ca2+. Sucrose gradients separated TCRMV and HCRMV into three different density fractions: a low density top fraction (SI), an intermediate density middle fraction (SII), and a high density pellet fraction (SIII). The SIII fractions of TCRMV and HCRMV contained significantly higher levels of mineral ions than did the SI and SII fractions. Only the SIII fraction of TCRMV which contained a stable nucleational core and surface-attached collagens, showed active Ca2+ uptake; all other sucrose fractions of TCRMV and HCRMV showed little or no uptake. Detergent treatment to purposely rupture the membrane greatly enhanced Ca2+ uptake by the SIII fraction of HCRMV, presumably by exposing the internal nucleational core. Addition of either native type II or type X collagen to the intact SIII fraction of HCRMV stimulated Ca2+ uptake to a level similar to that of the SIII fraction of TCRMV; however, incubation of the SI and SII fractions of either TCRMV or HCRMV with type II or X collagen did not activate Ca2+ uptake. These findings indicate that both a functional nucleational core and surface-attached collagens need to be present to support active mineralization of MV

Thyroid cartilages of various ages were investigated by immunofluorescence staining for localization of the fibrillar collagen types I and II in order to understand the tissue remodeling occurring during the mineralization and ossification of thyroid cartilage. In fetal and juvenile thyroid cartilages, type I collagen was restricted to the inner and outer perichondrium, while type II collagen was localized in the matrix of hyaline cartilage. However, in advanced ages, type I collagen was also localized in the pericellular and in the interterritorial matrix of intermediate and central chondrocytes of thyroid cartilage. The matrix of peripheral chondrocytes was negative for type I collagen. This suggest that some chondrocytes in thyroid cartilage undergo a differentiation to type I collagen-producing chondrocytes. At the beginning of ossification, bone-related type I collagen was chiefly detected in the central cartilage layer, but was never deposited first from the perichondrium in the direction to the subperichondrial cartilage. This observation confirmed previous findings showing that osteogenesis mainly follows an endochondral ossification pattern. Interterritorial matrix failed to react with the type II collagen antibody in men from the beginning of the third decade, and later still in women, even after treatment with hyaluronidase. These observations indicate that major matrix changes occur faster in male than in female thyroid cartilage

In this study the distribution of type X collagen in thyroid cartilages of various ages is described. Fetal and juvenile thyroid cartilage was negative for type X collagen, but showed a strong staining reaction for type II collagen. Type X collagen and calcium deposition were first detected in thyroid cartilage of 18-to 21-year-old adults. Type X collagen was restricted to large chondrocytes near or in mineralized cartilage, confirming the notion that type X collagen precedes mineralization. From these observations it was concluded that chondrocytes in thyroid cartilage undergo differentiation steps that are similar, but much slower, compared to cells in growth plate and sternal cartilage. Some type X collagen-positive areas also showed staining for type I collagen, suggesting that there is a further differentiation of chondrocytes to cells which are characterized by the simultaneous synthesis of type X and I collagen. However, a dedifferentiation process during aging of thyroid cartilage where cells switch from synthesis of type II to type I collagen cannot be excluded

The factors that drive mineralization of matrix vesicles (MV) have proven difficult to elucidate; in the present studies, various detergent, chemical, and enzyme treatments were used to reveal the nature of the nucleational core. Incubation with detergents that permeabilized the membrane enhanced calcification of treated MV incubated in synthetic cartilage lymph. While detergents removed most of the membrane lipid, they left significant amounts of the MV annexins and nearly all of the Ca2+, Pi, and Zn2+. Extraction with 1 M NaCl removed much of the Ca2+ and Pi present in MV, markedly reducing Ca2+ accumulation; these effects could be prevented by low levels of Ca2+ and Pi in the NaCl extractant. Treatment with chymotrypsin appeared to damage proteins required for MV mineralization; further treatment with detergents to bypass the membrane reactivated MV mineralization. Treatment of MV with pH 6 citrate removed Ca2+ and Pi, destroying their ability to mineralize; subsequent treatment with detergents did not reactivate these MV. Incubation of the detergent-resistant core with o-phenanthroline complexed Zn2+ and stimulated mineralization; addition of Zn2+ to synthetic cartilage lymph blocked the ability of the core to mineralize. These studies show that once the nucleational core complex is formed, the membrane-enclosed domain is no longer essential for MV calcification. Our findings indicate that the MV core contains two main components as follows: a smaller membrane-associated complex of Ca2+, Pi, phosphatidylserine, and the annexins that nucleates crystalline mineral formation, and a larger pool of Ca2+ and Pi bound to lumenal proteins. These proteins appear to bind large amounts of mineral ions, stabilize the nucleational complex, and aid its transformation to the first crystalline phase. Once nucleated, the crystalline phase appears to feed on protein-bound mineral ions until external ions enter through the MV ion channels. Zn2+ appears to regulate gating of the ion channels and conversion of the nucleational complex to the crystalline state