In memory of Constantine Spiro Anast.
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Biomedical subjects
Publications and source records attributed to M J Glimcher.
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alpha 2(I) chains of chicken bone collagen were isolated and purified. Analyses confirmed previous studies that the alpha 2(I) chains contained gamma-glutamyl phosphate residues. Sodium borohydride reduction of the gamma-glutamyl phosphate residues of the CaCl2 extracted and purified alpha 2(I) chains and subsequent CNBr cleavage showed that most of the gamma-glutamyl phosphate groups were located on the alpha 2CB3-5 peptides of the type I collagen molecule, suggesting a specific function for these phosphorylated residues. The reported linkage of the Ser(P) containing phosphoproteins of dentin to the alpha 2CB4 regions of collagen may indicate different biological functions for these two different, protein-bound organic phosphate residues.
Immunocytochemistry utilizing the protein A-gold technique was used to examine the ultrastructural cellular and extracellular distribution of a major phosphoprotein in chick bone. HCl-extracts of embryonic and neo-natal chick bones contain a major 66kD phosphoprotein (BPP) which was purified and used to raise polyclonal antibodies in rabbits. The mid-diaphyseal regions of 8-, 12- and 18-day embryonic chick tibiae were fixed with 1% glutaraldehyde and embedded in Epon or Lowicryl. Electron microscopy following incubation of tissue sections with the antibody and the protein A-gold complex revealed specific immunolabeling over the rER and Golgi apparatus of osteoblasts and over those areas of bone matrix containing Ca and P as determined by electron probe x-ray microanalysis. These included extracellular areas in the matrix undergoing early mineralization and electron dense patches occurring at the mineralization front and extending throughout the more mature bone regions. Biochemical analyses of bone tissue processed similarly to that used for immunocytochemistry confirmed the retention of phosphoprotein in the tissue. The spatial correlation of phosphoprotein in the extracellular matrix with Ca-P mineral deposits confirms an earlier report using 33Pi and radioautography and may indicate a role for phosphoproteins in calcification.
Decalcified samples of chicken bone containing phosphoproteins of varying concentrations were used to assess the effect of phosphoproteins and of protein-bound Ser(P) and Thr(P) in the in vitro nucleation of a Ca-P solid phase from metastable solutions of Ca and P. Phosphoproteins of bone as well as the phosphoproteins from egg yolk (phosvitin) were used. Increasing concentrations of phosphoprotein [as measured by the amount of protein bound Ser(P) and Thr(P)] in the decalcified bone particles significantly reduced the time required for nucleation to occur after exposure to metastable solutions of Ca and P (decreased operational lag times). Treatment with wheat germ acid phosphatase markedly reduced the concentration of Ser(P) and Thr(P) in the decalcified bone samples and in the decalcified bone collagen samples complexed with phosphoproteins (almost to zero). The loss of the organic phosphate groups significantly increased the operational lag time, but did not abolish nucleation of apatite crystals by the bone collagen fibrils essentially devoid of Ser(P) and Thr(P). Bone phosphoproteins were not specific; substitution of phosvitin for bone phosphoproteins as complexes with bone collagen also proved to be effective facilitators of nucleation, which was interesting since both types of phosphoproteins have certain common chemical and structural characteristics. Noncollagenous components other than phosphoproteins were present in the decalcified bone samples. However, the marked dependence of the lag time on the Ser(P) and Thr(P) concentrations and the very marked diminution in the efficacy of the nucleation phenomenon as a result of treatment with wheat germ acid phosphatase, clearly suggests that the organic phosphate residues of the phosphoproteins play a direct and significant role in the process of in vitro nucleation of a solid phase of Ca and P (apatite) by bone collagen, and by implication, possibly in in vivo mineralization as well.
When chicken embryonic progenitor cells were selected and grown in culture as previously described, by 30 days cellular differentiation could be demonstrated by expression of in vivo levels of osteocalcin, alkaline phosphatase (APase), type I collagen and phosphoproteins (PP). Ultrastructural analysis revealed that the cultures were similar morphologically to young osteoid in vivo with structural features including well-developed, orthogonally arranged collagen fibrils with 64-70 nm periodicity and electron opaque areas consisting of very poorly crystalline hydroxyapatite. Analysis of collagen synthesis versus collagen accumulation in the matrix indicated a temporal inconsistency between the time of synthesis and accumulation, suggesting that accumulation was largely controlled at the level of fibril formation. Analysis of PP accumulation demonstrated a 10-fold increase in total phosphoamino acid content over the 30 day time course. PP synthesis analyzed by [3H]-Ser(P) and [14C]-Thr(P) incorporation showed an induction similar to that seen for APase. Experiments undertaken to characterize the nature of PP synthesized by the cultures identified a unique 66 kD protein. This protein was purified from chick tibial and calvarial bone and a polyclonal antibody was raised in rabbits. Ultrastructural immunocytochemistry using this antibody and the protein A-gold technique revealed specific immunolabelling over regions of mineralizing matrix in vitro, a reaction identical to that observed for the distribution of this 66 kD PP in vivo during embryonic tibial bone development in the chicken.
High-voltage (1.0 mega-volt) electron stereomicroscopy has been used to examine the spatial relationship between the inorganic crystals and the collagen fibrils of pickerel and herring bone. Stereomicrographs of cross sections of the collagen fibrils encompassing regions of initial to full mineralization showed that the calcium phosphate crystals are located within the collagen fibrils. In all stages of mineralization, calcium-phosphate deposits were not observed associated or within membrane-bound structures. Serial cross sections of the fully mineralized collagen fibrils were three-dimensionally reconstructed using the computer graphic imaging process. Findings from this study suggest that there exist a local "bulging" along the fibrils corresponding to the 680 A periodicity in which additional mass of minerals were observed to be accommodated within the collagen fibril structure at this sites.
Resolution enhanced FT-IR spectroscopy shows that non-apatitic environments of phosphate and carbonate ions occur in bone mineral. The spectroscopic characteristics of these environments and their chemical and biological properties are reviewed. The potential effectiveness of FT-IR for the detailed study of bone mineral changes in bone disease is shown by analysis of several samples.
The major, non-amelogenin protein component (enamelin) present in EDTA or EDTA-GU HCl extracts of developing bovine enamel has a molecular weight of approximately 67 kD and an amino acid composition rich in asp, glu, ala, leuc and lys. Elution of this component from 1.5 and 3.0 mm thick strips SDS-PAGE gels and subsequent analyses show that the component selectively reacts with polyclonal antibody to bovine serum albumin. Absolute identification of this major enamelin component as serum albumin is established by an amino acid sequence of the first 40 N-Terminal amino acids which was found to be identical to bovine serum albumin. In addition to albumin, alpha-2 HS glycoprotein was also identified in the same extracts by Western blotting against a monospecific polyclonal antibody against human alpha-2 HS glycoprotein.
Secondary structural features of bovine amelogenin, a hydrophobic protein of developing enamel implicated in ename mineralization, are derived using 2D NMR spectroscopy in solution and molecular mechanics-dynamics studies. A beta-turn: beta-sheet model with some "unordered" segments was previously proposed from circular dichroism, Fourier-transform infrared and Raman spectroscopy augmented by Chou-Fasman predictive algorithm. The proposed structure contains a repetitive beta-turn segment, "beta-spiral" between Gln112 and Leu138 residues containing a (Pro, Leu, Gln) rich segment. The beta-spiral structure offers a probable site for interaction of Ca++ ions. Assignment of proton resonances using 2D COSY spectroscopy is presently in progress. Preliminary 2D NOESY spectra have revealed the presence of Tyr residues (TRAP segment) on the surface of amelogenin molecule and clusters of cross peaks reminiscent of beta-turns and sheets which are consistent with the primary structure and proposed secondary structures of amelogenin. The channel-like beta-spiral structure embedded in amelogenin provides a novel mechanism for trapping of Ca++ ions and their passage for a hydrophobic protein sparse in Ser(P) and charged amino acid residues.
Monoclonal and polyclonal antibodies were raised against 150k, 60k, 32k, and 15k phosphoprotein components of 14-week chicken bone. Hybridomas were prepared by immunizing Balb/c mice with 150k, 60k, or 32k phosphoproteins followed by fusion of their spleen cells with X63-Ag8.653 myeloma cells. Polyclonal antibodies to the 60k, 32k, and 15k phosphoprotein components were produced in immunized rabbits. Immunological cross-reactivity between antigen and antibody was examined by enzyme-linked immunosorbent assay (ELISA) and dot-blotting. There was cross-reactivity between the 150k, 32k, and 15k phosphoprotein components and between the 150k, 90k, and 60k components. The antibodies raised against 60k component do not bind 32k and 15k antigens.
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Osteocalcin, the vitamin K-dependent protein in bone containing gamma-carboxyglutamic acid, has been found to be significantly decreased in the osteomalacic bone of chicks made vitamin D deficient for 6 weeks. To evaluate whether this decrease in bone osteocalcin was due directly to the decrease or absence of vitamin D and its metabolites or to the secondary hypocalcemia and osteomalacia or other changes accompanying the deficiency of vitamin D, three experimental groups of Holtzman rats were studied. One group was made rachitic by a diet deficient in vitamin D, and the other groups were made rachitic by diets deficient in inorganic orthophosphate or calcium. The changes in bone and serum osteocalcin, serum 1,25-dihydroxyvitamin D3 [1,25-(OH)2D3], and bone mineral content were evaluated, and morphological evaluation of bone was made. In the vitamin D-deficient animals, osteomalacia was evident histologically by 7 weeks, at which time serum 1,25-(OH)2D3 was not detectable, bone osteocalcin was decreased by 50%, and serum osteocalcin was decreased by 20%. In the animals fed a diet deficient in either calcium or inorganic orthophosphate but which were not depleted of vitamin D, the osteocalcin content of osteomalcic bone was normal, and an increase in the concentration of serum osteocalcin accompanied an increase in serum 1,25-(OH)2D3. These data are consistent with the conclusion that the metabolism of osteocalcin is affected by serum 1,25-(OH)2D3 and that the diminished level of osteocalcin in the bone of vitamin D-deficient animals is the result of a direct action of the metabolites and is not secondary to a decrease in the mineralization of bone tissue.
From the physical chemical standpoint, the formation of a solid phase of Ca-P in bone represents a phase transformation, a process exemplified by the formation of ice from water. Considering the structural complexity and abundance of highly organized macromolecules in the cells and extracellular tissue spaces of mineralized tissues generally and in bone particularly, it is inconceivable that this phase transformation occurs by homogeneous nucleation, i.e., without the active participation of an organic component acting as a nucleator. This is almost surely true in biologic mineralization in general. Electron micrographs and low-angle neutron and X-ray diffraction studies clearly show that calcification of collagen fibrils occurs in an extremely intimate and highly organized fashion: initiation of crystal formation within the collagen fibrils in the hole zone region, with the long axes (c-axis) of the crystals aligned roughly parallel to the long axis of the fibril within which they are located. Crystals are initially formed in hole zone regions within individual fibrils separated by unmineralized regions. Calcification is initiated in spatially distinct nucleation sites. This indicates that such regions within a single, undirectional fibril represents independent sites for heterogeneous nucleation. Clearly, sites where mineralization is initiated in adjacent collagen fibrils are even further separated, emphasizing even more clearly that the process of progressive calcification of the collagen fibrils and therefore of the tissue is characterized principally by the presence of increasing numbers of independent nucleation sites within additional hole zone regions of the collagen fibrils. The increase in the mass of Ca-P apatite accrues principally by multiplication of more crystals, mostly by secondary nucleation from the crystals initially deposited in the hole zone region. Very little additional growth of the crystals occurs with time, the additional increase in mineral mass being principally the result of increase in the number of crystals (multiplication), not size of the crystals (crystal growth). The crystals within the collagen fibers grow in number and possibly in size to extend into the overlap zone of the collagen fibrils ("pores") so that all of the available space within the fibrils, which has possibly expanded in volume from its uncalcified level, is eventually occupied by the mineral crystals. It must be recognized that the calcification of separate tissue components and compartments (collagen, mitochondria, matrix vesicles) must be an independent physical chemical event.(ABSTRACT TRUNCATED AT 400 WORDS)
Circular dichroism and Fourier transform infrared spectroscopic studies of the major amelogenin protein of developing bovine tooth enamel in solution and in the solid state suggest a unique secondary structure containing beta-sheet and repetitive beta-turn structures. The repetitive beta-turn structure at the C-terminal end results from the unique primary structure of amelogenin.
Laser Raman spectroscopy has been employed to study the structure of the hen egg yolk protein phosvitin in H2O and D2O solutions at neutral and acidic pH (pD) and in the solid state. The Raman data indicate an unusual conformation for phosvitin in neutral aqueous solution, which is deficient in both alpha-helix and conventional beta-sheet conformations. This unusual pH 7 structure is, however, largely converted to a beta-sheet conformation in strongly acidic media (pH less than 2). beta-Sheet is also the predominant secondary structure for phosvitin in the solid state, obtained by lyophilization of the protein from aqueous solution at neutral pH. The imidazolium rings of histidyl residues remain significantly protonated near neutrality, which suggests substantial elevation of the pK for imidazolium ring ionizations of phosvitin in aqueous solution. This may result from extensive ion-pair interactions involving positively charged histidines and negatively charged phosphoserines, which are prevalent in the phosvitin sequence. The present results suggest that antiparallel beta-sheets may not be the secondary structure most characteristic of native phosvitin (physiological pH), even though beta-sheet is the predominant conformation for phosvitin in acidic solutions (pH 1.5) and in the lyophilized solid. Phosvitin appears to be the first protein for which the major component to the Raman amide I band is centered near 1685 cm-1, which is 10-40 cm-1 higher than proteins heretofore examined in aqueous solution by Raman spectroscopy.
The solid mineral phases of calcium-phosphate (Ca-P) in the long bones from embryonic chicks between the ages of 9 and 13 days have been examined by high voltage (1.0 MV) electron microscopy and electron microdiffraction. The study was undertaken to identify the chemical and crystallographic nature of the inorganic mineral phase(s) prepared under conditions which significantly reduce artifacts of specimen preparation and microscopic examination of the tissues. Electron microdiffraction patterns of solid mineral phase particles in the osteoid matrices of the subperiosteal region of tibiae were principally those of poorly crystalline hydroxyapatite. In rare instances (less than 1% of the estimated volume of the mineral phase present in the zone of early mineralization), relatively large single crystals were observed within clusters of hydroxyapatite. From calculations of both interplanar spacings and measurements of angular displacement of diffraction reflections from single crystal microdiffraction patterns, two distinct phases other than hydroxyapatite were identified: brushite and beta-tricalcium phosphate. A third phase, resembling an apatite, remains unidentified. The results suggest that very small amounts of nonapatitic phases of Ca-P exist in chicken bone tissue. No temporal relationship could be established between the nonapatitic and apatitic phases. There is at present no evidence from this study to support the concept that nonapatitic phases are precursors of a final apatitic phase in bone.
The majority of phosphoproteins in bovine bone and dentin are insoluble in EDTA and guanidine hydrochloride (Gu.HCl) at 2 degrees C. After removal of EDTA and Gu.HCl-soluble proteins at 2 degrees C, collagen alpha-chains and alpha-chain polymers were extracted from bovine bone and dentin in Gu.HCl at elevated temperatures and purified by several chromatographic techniques and SDS-PAGE. Small amounts of O-phosphoserine were found in all collagen components. In contrast, O-phosphoserine was not detected in the purified collagen components soluble in EDTA or Gu.HCl at 2 degrees C nor was hydroxyproline detected in the EDTA-soluble phosphoproteins. In contrast, although the vast majority of EDTA-insoluble collagen and phosphoprotein molecules can be readily dissociated by a variety of molecular sieving and ion-exchange chromatographic procedures, a small number are very strongly associated or covalently cross-linked. These results are consistent with the findings that both hydroxyproline and hydroxylysine are present in purified phosphoprotein components released from the EDTA-insoluble tissue by bacterial collagenase. The hydroxylysine/100 hydroxyproline ratios in the phosphoprotein-collagen complexes are much higher than those in dentin or bone collagens.
The secondary structures of two phosphoproteins from chicken bone matrix of Mr approximately 15kDa and approximately 28kDa, rich in Asx, Glx, and Ser, and containing Ser(P) and Thr(P) residues, have been investigated in solution by Circular Dichroism (CD) and Fourier Transform-Infrared Spectroscopy (FT-IR). CD spectroscopy, which yields useful information on the backbone conformation of polypeptides and proteins, suggests a predominantly beta-sheet structure for the two phosphoproteins. The FT-IR spectra of the approximately 15kDa protein, which is sensitive to secondary structure and hence provides complimentary information to CD spectroscopy, are consistent with the results obtained by CD studies.