Changes in the gene expression of collagens, fibronectin, integrin and proteoglycans during matrix-induced bone morphogenesis

Subcutaneous implantation of demineralized bone matrix in rat results in the local cartilage and bone development. This in vivo model of bone formation was used to examine the expression patterns of cartilage and bone specific extracellular matrix genes. The steady state levels of mRNA in implants for cartilage specific type II collagen, type IX collagen, proteoglycan link protein and cartilage proteoglycan core protein (aggrecan) were increased during chondrogenesis and cartilage hypertrophy. Fibronectin mRNA levels were high during mesenchymal cell migration, attachment and chondrogenesis. Integrin (beta 1 chain) mRNA was expressed throughout the endochondral bone development. Type I collagen mRNA levels in implants increased as early as day 3, reached its peak during osteogenesis. These gene markers will be useful in the study of the mechanism of action of bone morphogenetic proteins present in the demineralized bone matrix.     

Ultrastructural localization and biochemical characterization of vitronectin in developing rat bone

This study has used light and electron microscope immunohistochemical and biochemical methods to localize and characterize vitronectin in early bone formation of developing rat mandible with rabbit antimurine vitronectin IgG. Developing jaws of foetuses were collected at embryonic day 15 (day 15) to day 18 from pregnant Wistar rats. After aldehyde fixation, specimens with and without osmium post-fixation were dehydrated and embedded in paraffin, Spurr's resin or LR gold resin for morphological and immunohistochemical examinations. At the light microscope level, in day 15 samples, positive vitronectin immunostaining was observed in small elongated areas of intercellular matrix and osteoblasts. Concomitant with initiation of matrix mineralization at day 16, vitronectin staining was similarly observed in small elongated areas containing intercellular matrix and osteoblasts but not clearly detected in fully mineralized bone matrix. The same staining profile was observed at days 17 and 18. At the ultrastructural level, immunogold particles were clearly detected over unmineralized matrix and cisterns of the rough-surfaced endoplasmic reticulum and the Golgi apparatus of osteoblasts as well as over demineralized bone matrix at day 16--18. In order to assess the presence of vitronectin in the mineral phase, mineral-binding bone proteins were extracted from fresh day 18 specimens using a three-step technique: 4 m guanidine HCl (G1 extract), aqueous EDTA without guanidine HCl (E extract), followed by guanidine HCl. Subsequent Western blot analysis of sodium dodecyl sulphate (SDS)--polyacrylamide gel electrophoresis revealed that the antibodies produced only a single band at an Mr of approximately 73 000 in both G1 and E extracts, indicating the presence of vitronectin in the mineralized bone matrix. These results indicate that, at the onset of bone formation, osteoblasts synthesize and release vitronectin, which is subsequently incorporated into the bone matrix and becomes a specific component of bone tissues. The observation of vitronectin in these critical stages of bone formation suggests that it may be involved in the regulation of bone formation. © 1998 Chapman & Hall     

Comparison of bone inductive proteins of rat and porcine bone matrix

Subcutaneous implantation of demineralized bone matrix in allogenic rats induces a sequence of events resulting in de novo formation of cartilage, bone and bone marrow. In the present study endochondral bone formation by demineralized porcine matrix was studied and compared with the rat bone matrix. Endochondral bone formation was induced by 4M guanidine hydrochloride fraction IV (less than 50,000 daltons) of Sepharose CL-6B gel filtration but not by whole extract or by demineralized porcine bone matrix. Sephacryl S-200 gel filtration of the osteoinductive proteins of fraction IV showed the Porcine osteoinductive factor to be associated with protein fraction III (less than 20,000 daltons) whereas the rat with fraction II (between 20,000 and 30,000 daltons) of the chromatographic profile indicating an apparent difference in molecular weight of the osteoinductive factors between these two species.     

Extracellular matrix proteins involved in bone induction are vitamin D dependent

Subcutaneous implantation of demineralized diaphyseal bone matrix into allogeneic rats results in local formation of cartilage and bone. However, implantation of demineralized bone matrix obtained from rachitic rats did not induce bone. Rachitic bone matrix was therefore dissociatively extracted with 4 M guanidine HCl and then reconstituted with an inactive collagenous residue of control as carrier. Such reconstituted materials also lacked bone inductive potential. On the other hand, reconstitution of guanidine HCl extracts of control bone matrix with inactive vitamin D deficient matrix did result in bone induction. Partial purification (fractions containing proteins (less than 50,000 daltons) of the guanidine HCl extract from rachitic rats on Sepharose CL-6B followed by reconstitution with inactive collagenous residues resulted in a weak (25% of control) inductive response. These observations imply that bone inductive proteins are vitamin D dependent and are reduced in matrix obtained from rachitic rats.     

Dissociative extraction and partial purification of osteogenin, a bone inductive protein, from rat tooth matrix by heparin affinity chromatography

Implantation of demineralized tooth matrix in subcutaneous sites results in new bone formation locally. The osteoinductive activity of the tooth matrix was dissociatively extracted in 4.0 M guanidine hydrochloride and the residue was devoid of biologic activity. The bone inductive protein, osteogenin, was partially purified by heparin affinity chromatography. The heparin binding fraction initiated the bone differentiation cascade when implanted with guanidine extracted, inactive bone or tooth matrices. These results imply a cooperative interaction between the soluble osteogenin and collagenous substratum in bone induction.     

Distribution of bone inductive proteins in mineralized and demineralized extracellular matrix

Implantation of demineralized extracellular bone matrix results in new bone formation locally. Although the precise molecular mechanisms are not known, the reconstitution of matrix proteins less than 50,000 daltons with collagenous residue results in bone induction. The aim of the present investigation was to ascertain the distribution of the bone inductive protein(s) in various compartments of the tissue. A sequential extraction of mineralized bone matrix was employed: (1) 4 M guanidine HCl to extract proteins that are cell associated and not masked by mineral; (2) 0.5 M EDTA to dissolve the mineral phase; (3) 4 M guanidine HCl to reextract the collagenous matrix-associated proteins under dissociative conditions; (4) 4 M guanidine HCl containing 0.5 M EDTA to release any other residual proteins. This sequential method revealed that about 25% of total biological activity of bone induction is associated with first guanidine extraction, about 15% with the mineral phase and the rest of the activity is tightly associated with the collagenous matrix.     

Induction of heterotopic and orthotopic cartilage and bone formation in mice

Heterotopic cartilage, bone and bone-marrow formation was achieved in mice by transplantation of a variety of xenogeneic established cell lines, by the transitional epithelium or by implants of demineralized bone matrix. The pattern and the sequence of events were always the same, regardless of the inducer used; viz., hyaline cartilage appeared 6-7 days after implantation, and endochondral bone formation followed. However, in cases of allogeneic implants of transitional epithelium into species other than the mouse, an intramembranous osteogenesis was the main mode of bone formation. When the yield of induced bone was high enough, a true myelopoiesis developed after three weeks. Heterotopically-induced bones had a relatively short life-span. Periosteal membranes of bones at the sites of sarcomes induced by M-MSV responded with rapid and extensive proliferation, with subsequent bone and, sometimes, hyaline cartilage deposition. This phenomenon was observed in long and cranial bones. However, bone induced heterotopically by demineralized bone matrix did not respond in such a way to the presence of M-MSV-induced sarcoma, suggesting that the connective tissue-encapsulated heterotopic bone was not a functioning periosteum. M-MSV-induced sarcoma also stimulates proliferation of elastic cartilage.     

Biosynthesis and fate of proteoglycans in cartilage and bone during development and mineralization

Subcutaneous implantation of demineralized bone matrix in rats induces migration of host cells into the site and results in the sequential development of cartilage and bone. The biosynthesis and metabolic fate of proteoglycans in the plaques at the bone matrix implantation site were investigated by [35S]sulfate labeling in vivo. 35S-Labeled proteoglycans were extracted with 4 M guanidine HCl and purified by DEAE-Sephacel chromatography. Analysis of proteoglycans on Sepharose CL-2B chromatography showed two major peaks at Kd = 0.28 and 0.68 (peaks I and II, respectively). Peak I proteoglycan has a high buoyant density and contains chondroitin sulfate chains of average Mr = 20,000. Peak II proteoglycan has a lower average buoyant density and contains dermatan sulfate chains of average Mr = 33,000. Throughout the endochondral bone development sequence, peak II proteoglycan predominates. Peak I was low on Day 3, became prominent on Day 7 (approximately 30% of the total radioactivity), and declined after Day 9. The calculated half-lives of peak I and II proteoglycans labeled on Day 7 were about 1.8 and 2.8 days, respectively. After the initiation of osteogenesis, a species of mineral-associated proteoglycan was extracted with a 4 M guanidine HCl solvent containing 0.5 M EDTA. This proteoglycan has a small hydrodynamic size (Kd = 0.38 on Sepharose CL-6B chromatography) and shows a long half-life, about 6 days.     

Persistence of cartilage proteoglycan and link protein during matrix-induced endochondral bone development: An immunofluorescent study

Monospecific antibodies to cartilage proteoglycan monomer and link protein were employed with immunofluorescence microscopy to determine the tissue distribution of these constituents during matrix-induced endochondral bone development. Subcutaneous implantation of demineralized diaphyseal bone matrix resulted in new endochondral bone formation. On Day 3, the implant consisted of mesenchymal tissue which did not contain any demonstrable cartilage-related proteoglycan or link protein. With the onset of early chondrogenesis on Day 5, cartilage proteoglycan monomer and link protein were first localized together in the cartilage matrix, particularly around chondrocytes in territorial sites. Progressively more staining around cells was observed at Days 7 and 9. On Day 9, when mineralization was first observed, there was no evidence of a net loss of these molecules prior to mineralization of the cartilage matrix. On Day 11 and thereafter, bone formation was observed by appositional growth on calcified cartilage spicules. Whereas the osteoblasts and bone matrix were devoid of any staining for cartilage proteoglycan and link components, the residual, partly mineralized cartilage spicules still reacted with antibodies to cartilage proteoglycan monomer and link protein in territorial sites, but in reduced amounts, indicating a loss of these molecules associated with a loss of hypertrophic chondrocytes. Since mineral prevented the access of Fab' antibody subunits, demineralization after fixation was routinely employed. The results reveal that cartilage proteoglycan monomer and link protein are present around chondrocytes in hyaline cartilage during the early stages of endochondral bone formation and that there is no net loss of these molecules prior to mineralization of this cartilage matrix as was previously thought.     

The isolation and partial characterization of a rat incisor dentin matrix polypeptide with in vitro chondrogenic activity

In vivo implants of demineralized dentin matrix into muscle induce the formation of bone within the muscle. As with bone matrix implants, the bone induction appears to follow a chondrogenic pathway. Outgrowth cells from explants of neonatal rat muscle respond to bone matrix, in vitro, by expressing a heightened synthesis of sulfated proteoglycans and type II collagen, phenotypic of cartilage. The in vitro cell culture system has been used as an assay to monitor the isolation of the factor responsible for expression of this phenotypic transformation. Soluble proteins extracted from rat incisor dentin matrix during demineralization with EDTA, and not precipitable with 1.0 M CaCl2, were active in the in vitro system. The active extract was fractionated by Sephacryl S-100 chromatography in 6 M guanidine HCl, isoelectric focusing in Immobilines, and by reverse phase high performance liquid chromatography. All fractions were assayed for activity at every stage. The final active fraction from the reverse phase chromatography on a Zorbax Poly-F column was purified to homogeneity, and yielded a single spot on two-dimensional gel electrophoresis. The component, RP-4, had pI 5.4-5.5, and an apparent Mr 6,000-10,000, based on globular protein standards. Maximal activity with respect to both sulfate incorporation into proteoglycan and production of type II collagen was in the 1.0-10 ng/ml range. The RP-4 had a unique amino-terminal amino sequence and was rich in Gly, Pro, Glx, and Ala residues. It was different from transforming growth factor-beta and the bone morphogenetic protein family of proteins in these essential features.     

Inhibition of induced endochondral bone development in caffeine-treated rats

We have addressed questions raised by the observation in fetal rats of delayed ossification induced by caffeine at maternal doses above 80 mg/kg body weight per day. The effect of caffeine on endochondral bone development and mineralization has been studied in an experimental model system of bone formation which involves implantation of demineralized bone particles (DBP) in subcutaneous pockets of young growing rats. Caffeine's effects on cellular events associated with endochondral ossification were examined directly by quantitating cellular mRNA levels of chondrocyte and osteoblast growth and differentiation markers in DBP implants from caffeine-treated rats harvested at specific stages of development (day 7 through day 15). Oral caffeine administration to rats implanted with DBP resulted in a dose dependent inhibition of the formation of cartilage tissue in the implants. Histologic examination of the implants revealed a decrease in the number of cells which were transformed to chondrocytes compared to control implants. Those cartilaginous areas that did form, however, proceeded through the normal sequelae of calcified cartilage and bone formation. At the 100 mg/kg dose, cellular levels of mRNA for histone, collagen type II, and TGFβ were all reduced by greater than 40% of control implants consistent with the histological findings. Alkaline phosphatase activity in the implants and mRNA levels for proteins reflecting the hypertrophic chondrocyte and bone phenotype, collagen type I and osteocalcin were markedly decreased compared to controls. Lower doses of 50 and 12.5 mg/kg caffeine also resulted in decreased cellular proliferation and transformation to cartilage histologically and reflected by significant inhibition of type II collagen mRNA levels (day 7). The effects of caffeine on gene expression observed in vivo during the period of bone formation (day 11 to day 15) in the DBP model were similar to the inhibited expression of H4, alkaline phosphatase, osteocalcin, and osteopontin found in fetal rat calvarial derived osteoblast cultures following 24 hour exposure of the cultures to 0.4 mM caffeine. Thus the observed delayed mineralization in the fetal skeleton associated with caffeine appears to be related to an inhibition of endochondral bone formation at the early stages of proliferation of undifferentiated mesenchymal cells to cartilage specific cells as well as at later stages of bone formation.     

Importance of geometry of the extracellular matrix in endochondral bone differentiation

Subcutaneous implantation of coarse powders (74-420 micron) of demineralized diaphyseal bone matrix resulted in the local differentiation of endochondral bone. However, implantation of matrix with particle size of 44-74 micron (Fine matrix) did not induce bone. We have recently reported that the dissociative extraction of coarse matrix with 4 M guanidine HCl resulted in a complete loss of the ability of matrix to induce endochondral bone; the total loss of biological activity could be restored by reconstitution of extracted soluble components with inactive residue. To determine the possible biochemical potential of fine matrix to induce bone, the matrix was extracted in 4 M guanidine HCl and the extract was reconstituted with biologically inactive 4 M guanidine HCl-treated coarse bone matrix residue. There was a complete restoration of the biological activity by the extract of fine matrix upon reconstitution with extracted coarse matrix. Polyacrylamide gel electrophoresis of the extract of fine matrix revealed similar protein profiles as seen for the extract of coarse matrix. Gel filtration of the 4 M guanidine HCl extract of fine powder on Sepharose CL-6B and the subsequent reconstitution of various column fractions with inactive coarse residue showed that fractions with proteins of 20,000-50,000 mol wt induced new bone formation. These observations demonstrate that although fine bone matrix contains, osteoinductive proteins, matrix geometry (size) is a critical factor in triggering the biochemical cascade of endochondral bone differentiation. Mixing of coarse matrix with Fine results in partial response and it was confined to areas in contact with coarse particles. The results imply a role for geometry of extracellular bone matrix in anchorage-dependent proliferation and differentiation of cells.     

An Ion-exchange Bone Demineralization Method for Improved Time,Expense, and Tissue Preservation

Here, we describe an ethylenediaminetetraacetic acid (EDTA)-based bone demineralization procedure that uses cation-exchange resin and dialysis tubing. This method does not require solution changes or special equipment, is faster than EDTA alone, is cost-effective, and is environmentally friendly. Like other EDTA-based methods, this procedure yields superior tissue preservation than formic acid demineralization. Greater protein antigenicity using EDTA as opposed to formic acid has been described, but we also find significant improvements in carbohydrate-based histological staining. Histological staining using this method reveals cartilage layers that are not distinguishable with formic acid demineralization. Carbohydrate preservation is relevant to many applications of bone demineralization, including the assessment of osteoarthritis from bone biopsies and the use of demineralized bone powder for tissue culture and surgical implants. The improvements in time, expense, and tissue quality indicate this method is a practical and often superior alternative to formic acid demineralization:     

Localization of transforming growth factor beta receptor II interacting protein-1 in bone and teeth: implications in matrix mineralization

Transforming growth factor beta receptor II (TGFβR-II) interacting protein 1 (TRIP-1) is a WD-40 protein that binds to the cytoplasmic domain of the TGF-β type II receptor in a kinase-dependent manner. To investigate the role of TRIP-1 in mineralized tissues, we examined its pattern of expression in cartilage, bone, and teeth and analyzed the relationship between TRIP-1 overexpression and mineralized matrix formation. Results demonstrate that TRIP-1 was predominantly expressed by osteoblasts, odontoblasts, and chondrocytes in these tissues. Interestingly, TRIP-1 was also localized in the extracellular matrix of bone and at the mineralization front in dentin, suggesting that TRIP-1 is secreted by nonclassical secretory mechanisms, as it is devoid of a signal peptide. In vitro nucleation studies demonstrate a role for TRIP-1 in nucleating calcium phosphate polymorphs. Overexpression of TRIP-1 favored osteoblast differentiation of undifferentiated mesenchymal cells with an increase in mineralized matrix formation. These data indicate an unexpected role for TRIP-1 during development of bone, teeth, and cartilage.     

Isolation and characterization of insulin-like growth factor-II from human bone

Human bone was sequentially extracted with 4 M guanidine hydrochloride to remove nonmineralized tissue components, 0.5 M EDTA to dissolve the mineral phase, 4 M guanidine hydrochloride to remove matrix associated proteins and finally a combination of 4 M guanidine hydrochloride and 0.5 M EDTA to remove residual proteins. The extracts were examined for the presence of factors that were able to stimulate the incorporation of [3H] thymidine into DNA and [14C] leucine into protein in a cloned rat bone cell culture system. The majority of the bioactivity was found in the first guanidine hydrochloride extract (59 +/- 12%) while the second guandine hydrochloride extract contained 27 +/- 8%. In addition to several known growth factors already reported to be present in bone (transforming growth factor-beta and insulin-like growth factor-I) insulin-like growth factor-II was identified by its chromatographic, electrophoretic and immunological properties as well as by N-terminal sequence data. The insulin-like growth factor-II levels (802 +/- 112 micrograms/kg wet weight bone) were 10 fold higher than that found for insulin-like growth factor-I (84 +/- 23 micrograms/kg wet weight).     

Immunohistochemical localization of bone sialoprotein in foetal porcine bone tissues: comparisons with secreted phosphoprotein 1 (SPP-1, osteopontin) and SPARC (osteonectin)

Summary Bone sialoprotein (BSP) is a prominent component of bone tissues that is expressed by differentiated osteoblastic cells. Affinity-purified antibodies to BSP were prepared and used in combination with biotin-conjugated peroxidase-labeled second antibodies to demonstrate the distribution of this protein in sections of demineralized foetal porcine tibia and calvarial bone. Staining for BSP was observed in the matrix of mineralized bone and also in the mineralized cartilage and associated cells of the epiphysis, but was not observed in the hypertrophic zone nor in any of the soft tissues including the periosteum. In comparison, SPP-1 (osteopontin) and SPARC (osteonectin), which are also major proteins in porcine bone, were observed in the cartilage as well as in the mineralized bone matrix, In addition, SPARC was also present in soft connective tissues. Although SPP-1 distribution was more restricted than SPARC, hypertrophic chondrocytes, periosteal cells and some stromal cells in the bone marrow spaces were stained in addition to osteoblastic cells. The variations in the distribution and cellular expression of BSP, SPARC and SPP-1 in bone and mineralizing cartilage indicate these proteins perform different functions in the formation and remodelling of mineralized connective tissues.     

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 ornithine decarboxylase activity during matrix-induced cartilage, bone and bone marrow differentiation.

Subcutaneous transplantation of coarse powders of demineralized rat diaphyseal bone matrix into allogeneic recipients results in new bone formation. The changes in ornithine decarboxylase activity during such bone matrix-induced sequential differentiation of cartilage, bone and bone marrow were investigated. There was a peak in ornithine decarboxylase activity on day 3 corresponding to the appearance of fibroblasts in close contiguity to the bone matrix. This was followed by another peak of enzyme activity on day 8 which was correlated with the onset of proliferation of presumptive osteoblasts and vascular endothelial cells. The peak of ornithine decarboxylase activity on day 3 appears to be a demineralized bone matrix-specific event. Induction of ornithine decarboxylase activity represents one of the early responses to implanted bone matrix.     

Evidence that failure of osteoid bone matrix resorption is caused by perturbation of osteoclast polarization

Osteoclasts resorb bone by a complex dynamic process that initially involves attachment, polarization and enzyme secretion, followed by their detachment and migration to new sites. In this study, we postulated that mineralized and osteoid bone matrix signal osteoclasts differently, resulting in the resorption of mineralized bone matrix only. We, therefore, compared the cytoplasmic distribution of cytoskeletal proteins F-actin and vinculin using confocal laser-scanning microscopy in osteoclasts cultured on mineralized and demineralized bone slices and correlated the observations with their functional activity. Our results have demonstrated significant differences in F-actin and vinculin staining patterns between osteoclasts cultured on mineralized bone matrix and those on demineralized bone matrix. In addition, the structural variations were accompanied by significant differences in bone resorbing activity between osteoclasts grown on mineralized bone matrix and those on demineralized bone matrix after 24 h of culture -- resorption only occurring in mineralized bone but not in demineralized bone. These results indicated that failure of osteoid bone resorption is caused by perturbation of osteoclast polarization. © 1998 Chapman & Hall