Ultrastructural organic-inorganic relationships in calcified tissues: cartilage and bone vs. enamel

Biomineralization of bone: a fresh view of the roles of non-collagenous proteins

The impact of genetics has dramatically affected our understanding of the functions of non-collagenous proteins. Specifically, mutations and knockouts have defined their cellular spectrum of actions. However, the biochemical mechanisms mediated by non-collagenous proteins in biomineralization remain elusive. It is likely that this understanding will require more focused functional testing at the protein, cell, and tissue level. Although initially viewed as rather redundant and static acidic calcium binding proteins, it is now clear that non-collagenous proteins in mineralizing tissues represent diverse entities capable of forming multiple protein-protein interactions which act in positive and negative ways to regulate the process of bone mineralization. Several new examples from the author's laboratory are provided which illustrate this theme including an apparent activating effect of hydroxyapatite crystals on metalloproteinases. This review emphasizes the view that secreted non-collagenous proteins in mineralizing bone actively participate in the mineralization process and ultimately control where and how much mineral crystal is deposited, as well as determining the quality and biomechanical properties of the mineralized matrix produced.

Calcospherulites isolated from the mineralization front of bone induce the mineralization of type I collagen

Previous work has suggested that "calcospherulites" actively participate in the mineralization of developing and healing bone. This study sought to directly test this hypothesis by developing a method to isolate calcospherulites and analyzing their capacity to seed mineralization of fibrillar collagen. The periosteal surface of juvenile rat tibial diaphysis was enriched in spherulites of approximately 0.5-mum diameter exhibiting a Ca/P ratio of 1.3. Their identity as calcospherulites was confirmed by their uptake of calcein at the tibial mineralization front 24 h following in vivo injection. Periosteum was dissected and unmineralized osteoid removed by collagenase in order to expose calcospherulites. Calcein-labeled calcospherulites were then released from the mineralization front by dispase digestion and isolated via fluorescence flow sorting. X-ray diffraction analysis revealed they contained apatite crystals (c-axis length of 17.5+/-0.2 nm), though their Ca/P ratio of 1.3 is lower than that of hydroxyapatite. Much of their non-mineral phosphorous content was removed by ice-cold ethanol, elevating their Ca/P ratio to 1.6, suggesting the presence of phospholipids. Western blot analyses showed the presence of bone matrix proteins and type I collagen in these preparations. Incubating isolated calcospherulites in collagen hydrogels demonstrated that they could seed a mineralization reaction on type I collagen fibers in vitro. Ultrastructural analyses revealed crystals on the collagen fibers that were distributed rather uniformly along the fiber lengths. Furthermore, crystals were observed at distances well away from the observed calcospherulites. Our results directly support an active role for calcospherulites in inducing the mineralization of type I collagen fibers at the mineralization front of bone.

Bone Acidic Glycoprotein-75 Delineates the Extracellular Sites of Future Bone Sialoprotein Accumulation and Apatite Nucleation in Osteoblastic Cultures

Addition of an organophosphate source to UMR osteoblastic cultures activates a mineralization program in which BSP localizes to extracellular matrix sites where hydroxyapatite crystals are subsequently nucleated. This study identifies for the first time novel extracellular spherical structures, termed biomineralization foci (BMF), containing bone acidic glycoprotein-75 (BAG-75), bone sialoprotein (BSP), and alkaline phosphatase that are the exclusive sites of initial nucleation of hydroxyapatite crystals in the UMR model. Importantly, in the absence of added phosphate, UMR cultures after reaching confluency contain two size populations of morphologically identifiable BMF precursors enriched in BAG-75 (15-25 and 150-250 microm in diameter). The shape and size of the smaller population are similar to structures assembled in vitro through self-association of purified BAG-75 protein. After organophosphate addition, BSP accumulates within these BAG-75-containing BMF precursors, with hydroxyapatite crystal nucleation occurring subsequently. In summary, BAG-75 is the earliest detectable biomarker that accurately predicts the extracellular sites of de novo biomineralization in UMR cultures. We hypothesize that BAG-75 may perform a key structural role in the assembly of BMF precursors and the recruitment of other proteins such as alkaline phosphatase and BSP. Furthermore, we propose a hypothetical mechanism in which BAG-75 and BSP function actively in nucleation of apatite within BMF.

Extracellular Bone Acidic Glycoprotein-75 Defines Condensed Mesenchyme Regions to be Mineralized and Localizes with Bone Sialoprotein during Intramembranous Bone Formation

Bone acidic glycoprotein-75 is expressed very early during in vivo models of intramembranous bone formation, highly enriched in condensing osteogenic mesenchyme after marrow ablation and the osteoprogenitor layer of tibial periosteum. Bone sialoprotein accumulates within bone acidic glycoprotein-75-enriched matrix areas at a later stage in both models. Decalcification of initial sites of mineralization consistently revealed focal immunostaining for bone acidic glycoprotein-75 underneath these sites suggesting that mineralization occurs within bone acidic glycoprotein-75-enriched matrix areas. Ultrastructural immunolocalization of bone acidic glycoprotein-75 does not support a direct association with banded collagen fibrils, but rather suggests it is a component of a separate, amorphous scaffold occupying interfibrillar spaces. Double immunogold labeling demonstrated that a sizeable proportion of bone sialoprotein particles were located within a 50-nm radius of bone acidic glycoprotein-75. These results define bone acidic glycoprotein-75 as the earliest bone-restricted, extracellular marker of osteogenic mesenchyme. Based on this early bone-restricted expression pattern and a previously documented propensity of bone acidic glycoprotein-75 to form supramolecular complexes through self-association, bone acidic glycoprotein-75 may serve a key structural role in setting boundary limits of condensing osteogenic mesenchyme.

Effect of deproteination on bone mineral morphology: implications for biomaterials and aging

Bone mineral morphology is altered by processing and this is rarely considered when preparing bone as a bioimplant material. To examine the degree of transformation, a commercial, coarsely particulate bone mineral biomaterial produced by prolonged deproteination, defatting, dehydration, and heating (donor material) was compared with similar particles of human bone (recipient material) prepared optimally by low-temperature milling. The two powders were freeze-substituted and embedded without thawing in Lowicryl K4M before sectioning for transmission electron microscopy (TEM) (other aliquots were processed by traditional TEM methods). To maximize resolution, electron micrographs were image-enhanced by digitization and printed as negatives using a Polaroid Sprint Scan 45. In addition to their morphology, the particles were examined for antigenicity (specific by reference to fluorescein isothiocyanate [FITC]-conjugated fibronectin, and nonspecific by reference to general FITC-conjugated immunoglobulins). Results showed that the optimally prepared human bone fragments stained discretely for fibronectin with negligible background autofluorescence. In contrast, the bioimplant fragments stained extensively with this and any other FITC-conjugated antibody and, unlike fresh bone, it also autofluoresced a uniform yellow. This difference was also expressed structurally and, although the bioimplant mineral consisted of rhomboidal plates up to 200 nm across and 10 nm thick, the optimally prepared bone mineral was composed of numerous clusters of 5-nm-wide sinuous calcified filaments of variable density and indeterminate length (which became straight needles 50 nm long and 5 nm thick following traditional chemical TEM fixation/staining). It was concluded that the inorganic phase of bone is both morphologically and immunologically transmutable and that, in biomaterials, the transformation is apparently so great that a broad indigenous antigenicity is unmasked, increasing the likelihood of resorption or rejection. This marked change may also provide preliminary insight into a more modest natural aging phenomenon with the localized lateral fusion of calcified filaments into less flexible, more immunologically reactive fenestrated plates.

Osteopontin: an interfacial extracellular matrix protein in mineralized tissues

Among the noncollagenous matrix proteins found in mineralized tissues (MTs), colloidal-gold immunocytochemistry has demonstrated that the ultrastructural distribution of osteopontin (OPN) is unique in that this protein preferentially accumulates at MT interfaces. In bone, OPN is present as a major component of cell- and matrix-matrix interfacial structures termed laminae limitantes and cement lines, respectively. Here, we review the implications of this distinct, interfacial tissue distribution as it relates to the properties and functional motifs of OPN (e.g. RGD, polyAsp, phosphorylation) in different MTs, and more specifically, how it pertains to current theory on the cellular and extracellular matrix (ECM) events associated with bone remodeling. The production of OPN as one of the earliest, and latest, secretory activities of the osteoblast lineage is discussed, together with a consideration of the role of OPN in cement lines and laminae limitantes in bone and in other normal, pathological and healing MTs such as teeth, kidney stones, bone wound healing and implant osseointegration. Further to its ability to influence cell dynamics, calcification and possibly tissue cohesion in MTs, it is proposed that OPN in cement lines may also promote adhesion between apposing substrata. With regard to this latter function, it is suggested that the molecular interactions within, and biomechanical properties of, such an OPN-rich interfacial zone may be important in minimizing strain-induced fatigue damage and microcrack propagation in bone and across other MT interfaces.