Biomedical subjects

M J Glimcher

Publications and source records attributed to M J Glimcher.

At least 73 records · Page 4Linked to original sources

PubMed1991

Resolution-enhanced Fourier transform infrared spectroscopy study of the environment of phosphate ion in the early deposits of a solid phase of calcium phosphate in bone and enamel and their evolution with age: 2. Investigations in the nu3PO4 domain.

Resolution-enhanced Fourier Transform Infrared (FTIR) spectra of early mineral deposits in enamel and bone show bands at 1020, 1100, 1110, 1125, and 1145 cm-1 in the nu3PO4 domain which do not belong to well crystallized stoichiometric hydroxyapatite. Bands at 1020 and 1100 cm-1 have been shown to occur in nonstoichiometric apatites containing HPO4(2-) ions and the weak band at 1145 cm-1 has been assigned to HPO4(2-) ions. Though the bands at 1110 and 1125 cm-1 have not been found in any well crystallized apatite, they are present in newly precipitated apatite. These latter bands disappear progressively during maturation in biological as well as synthetic samples, and partial dissolution of synthetic apatites shows that they belong to species that exhibit an inhomogeneous distribution in the mineral, and that are the first to be solubilized. Comparison of the FTIR spectra of biological apatites with those of synthetic, nonapatitic-containing phosphate minerals shows that the presence of these bands does not arise from nonapatitic, well-defined phases; they are due to the local environment of phosphate ions which may possibly be loosely related or perhaps unrelated to the phosphate groups present in the well-crystallized nonapatitic calcium phosphates. Resolution-enhanced FTIR affords a very precise characterization of the mineral phases which may be very useful in characterizing pathological deposits of Ca-P mineral phases.

Animals↗

PubMed1991

Fourier transform infrared spectroscopic study of the carbonate ions in bone mineral during aging.

The environment of CO3(2-) ions in the bone mineral of chickens of different ages and in bone fractions of different density have been investigated by resolution-enhanced Fourier Transform Infrared (FTIR) Spectroscopy. Three carbonate bands appear in the upsilon 2 CO3 domain at 878, 871, and 866 cm-1, which may be assigned to three different locations of the ion in the mineral: in monovalent anionic sites of the apatitic structure (878 cm-1), in trivalent anionic sites (871 cm-1), and in unstable location (866 cm-1) probably in perturbed regions of the crystals. The distribution of the carbonate ions among these locations was estimated by comparing the intensities of the corresponding FTIR spectral bands. The intensity ratio of the 878 and 871 cm-1 bands remains remarkably constant in whole bone as well as in the fractions obtained by density centrifugation. On the contrary, the intensity ratio of the 866 cm-1 to the 871 cm-1 band was found to vary directly and decreased with the age of the animal. In bone of the same age, the relative content of the unstable carbonate ion was found to be highest in the most abundant density centrifugation fraction. A resolution factor of the CO3(2-) band (CO3 RF) was calculated from the FTIR spectra which was shown to be very sensitive to the degree of crystallinity of the mineral. The crystallinity was found to improve rapidly with the age of the animal. The CO3 RF in the bone samples obtained by density centrifugation from bone of the same animal was found to be essentially constant.(ABSTRACT TRUNCATED AT 250 WORDS)

Aging↗

PubMed1991

A resolution-enhanced Fourier transform infrared spectroscopic study of the environment of the CO3(2-) ion in the mineral phase of enamel during its formation and maturation.

A resolution-enhanced Fourier Transform Infrared (FTIR) Spectroscopic study of the CO3(2-) ion in pig enamel of increasing age and maturity has demonstrated the existence of four different, main carbonate locations. The major CO3(2-) site arises as a result of the substitution of CO3(2-) ions in the positions occupied by PO4(3-) ions in the apatitic lattice. In addition, two minor locations have been identified in positions in which the CO3(2-) ions substitute for OH- ions. The fourth carbonate group appears to be in an unstable location. Its concentration has been found to decrease with aging and maturation, during which there is a progressive increase in the amount of mineral deposited in the enamel. The distribution of the carbonate ions in the different apatitic sites varies randomly during the formation of the mineral phase in enamel and during its maturation. Although these changes have been shown to be related to changes in the composition of the mineral phase, a comparison of the parameters assessing the degree of crystallinity of the mineral phase from upsilon 2CO3(2-) and upsilon 4PO4(3-) infrared absorption data reveals a significant discrepancy related to the nonhomogeneous partition of the CO3(2-) ion in the mineral phase. After maximum mineralization is reached, the composition of the mature mineral phase is decidedly different than that of the initial mineral deposited; the changes affect principally the concentrations of Ca2+, OH-, and HPO4(2-) ions, but not the CO3(2-) ions.

Aging↗

PubMed1991

Immunohistochemical localization of a approximately 66 kD glycosylated phosphoprotein during development of the embryonic chick tibia.

Localization of a approximately 66 kD glycosylated phosphoprotein during morphogenesis of the embryonic chick tibia has been accomplished using immunohistochemistry. Although initial expression of the tibial osteoblast phenotype is detected as early as stage 28.5, with the deposition of osteoid matrix beginning at stage 30, little or no immunoreactivity against the approximately 66 kD glycosylated phosphoprotein is observed in pre-osteoblasts, osteoblasts, osteocytes, or in the uncalcified osteoid matrix during the early events of tibia development. Immunoreactivity was first observed at stage 32 when mineralization of the osteoid matrix is initiated. At this and all later stages, the phosphoprotein is located almost exclusively in the extracellular matrix at the mineralization front with essentially no detectable staining in the adjacent unmineralized osteoid matrix. Similarly, no cellular staining is observed when even the lightly mineralized extracellular matrix is strongly immunoreactive. Only scant immunostaining is present over the heavily mineralized regions, although demineralization of these areas with EDTA exposes a low intensity, punctate staining pattern. Additionally, cryosections of developing calvaria stained with this antiserum only display reactivity in regions of bone matrix undergoing mineralization. These localization studies support the hypothesis that this phosphoprotein is intimately associated with the process of bone matrix mineralization in the developing chick long bone.

Animals↗

PubMed1990

Comparison of two phosphoproteins in chicken bone and their similarities to the mammalian bone proteins, osteopontin and bone sialoprotein II.

Two phosphorylated proteins of approximately 66 kDa and approximately 60 kDa mass with different DEAE-Sephacel elution patterns were isolated from chicken bone and were shown to be genetically distinct by both biochemical and immunological analysis. A tryptic peptide from the 60 kDa protein was identified that was similar to a sequence of the rat bone sialoprotein II. Both proteins showed RGD inhibited cell-attachment with the MG-63 osteosarcoma cell, and the approximately 66 kDa phosphoprotein appeared to promote cell adhesion better than human vitronectin. The two phosphoproteins appear to share functional and biochemical characteristics and to be homologous to the mammalian bone phosphoproteins, osteopontin and bone sialoprotein II.

Amino Acid Sequence↗

PubMed1990

Tooth 'enamelins' identified mainly as serum proteins. Major 'enamelin' is albumin.

The major enamelin protein component present in EDTA or EDTA/guanidine hydrochloride extracts of developing bovine enamel has a molecular mass of about 67 kDa; it has an amino acid composition similar to that of bovine serum albumin and reacts with polyclonal and monoclonal antibodies to albumin. Two-dimensional separation of the components in the enamelin extract by isoelectric focusing and SDS/PAGE reveal that the major approximately 67-kDa component and almost all of the minor Coomassie-staining protein components of approximately 67 kDa, as well as many of the other minor components with different molecular masses, also react with polyclonal and monoclonal antialbumin. The approximately 67-kDa band eluted after SDS/PAGE, as well as the major approximately 67-kDa spots eluted after two-dimensional separation, were found to have N-terminal amino acid sequences identical to that of bovine serum albumin. Albumin accounted for at least 70-80% of the total protein content of the enamelin extract and was essentially the only protein in the approximately 67-kDa component. The serum proteins alpha-2 HS glycoprotein, gamma-globulin and fetuin, and the proline-rich salivary protein termed P-B were also identified in the enamelin extract. The serum proteins and the salivary protein account for greater than 95% of the proteins in the enamelin extracts. Of the remaining very small amounts of non-serum or salivary protein isolated from the enamelin extracts, three minor components were isolated which had N-terminal amino acid sequences which were not similar to any known protein in the protein sequence data base and could therefore conceivably be true 'enamelins' synthesized by ameloblasts. One additional protein had the first five N-terminal amino acids and residue 8 of amelogenin, residues 6 and 7 being different from those of amelogenin. Two other very minor protein components had amino acid compositions distinct from the amelogenins and the serum proteins, but were N-terminally blocked on attempted sequencing. None of the components in the neutral soluble low-ionic-strength extract or in the 4 M guanidine hydrochloride extract, both of which consist principally of amelogenins, immunoreacted with anti-albumin or with any of the antibodies to other serum proteins and fetuin, despite the fact that the amelogenin extracts also contain non-amelogenin proteins. On the basis of the data presented, studies employing antibodies to the so-called enamelin proteins and hypotheses as to their molecular conformation, their roles as evolutionary markers, or their positive role in mineralization should be reconsidered and reviewed.

Amelogenesis↗

PubMed1990

Post-translational processing of chicken bone phosphoproteins. Identification of the bone phosphoproteins of embryonic tibia.

In order to understand the mechanism of the post-translational processing of bone phosphoproteins in embryonic bone, periosteal bone strips isolated from 12-day-embryonic-chick tibiae were cultured and the bone proteins labelled with Na2H32PO4. Of the total radiolabelled proteins recovered from the medium and bone extracts in the absence of SDS ('medium', 'EDTA extract' and 'EDTA/guanidinium chloride extract'), nearly 80% of the radioactivity was found in the EDTA extract. The three major radiolabelled phosphoproteins in the EDTA extract of apparent Mr 68,000, 63,000 and 58,000 reacted with polyclonal as well as monoclonal antibodies raised against '32-kDa' and '150-kDa' bone phosphoproteins which were derived from 14-week-old chicken. Therefore these phosphorylated embryonic proteins are identified as chicken bone phosphoproteins. Judging from their common N-terminal sequences, differences in the patterns obtained by labelling them with several radioisotopes, and slightly different amino acid compositions, these components seem to have been derived from the same original protein by sequential proteolytic cleavage and other processing such as glycosylation and phosphorylation.

Amino Acid Sequence↗

PubMed1990

Post-translational processing of chicken bone phosphoproteins. Identification of bone (phospho)protein kinase.

We have detected a protein kinase which phosphorylates bone phosphoproteins (BPPs) in the detergent extract of the membranous fractions in the periosteal bone strips of 12-day-embryonic-chick tibia. This enzyme, tentatively named BPP kinase, has a catalytic subunit of Mr approximately 39,000, utilizes GTP as well as ATP as a phospho-group donor, is inhibited by 2,3-bisphosphoglycerate and heparin, and is therefore similar to casein kinase II. The enzyme can phosphorylate dephosphorylated proteins such as casein, phosvitin and chicken BPPs, but the last-named are preferred substrates. The in vitro-phosphorylation-assay products of this enzyme in the extract were indistinguishable on an SDS/polyacrylamide gel from the major [32P]phosphoproteins metabolically labelled in the embryonic-chick bone tissue. The regulatory mechanisms of the phosphorylation process of BPPs by BPP kinase as well as the potential role of this enzyme in mineralization are discussed.

2,3-Diphosphoglycerate↗

PubMed1990

Conformational transitions in phosvitin with pH variation. Vibrational circular dichroism study.

The vibrational circular dichroism (VCD) spectra of metal-free phosvitin are presented as a function of pH and analyzed both qualitatively and by using a factor analysis approach referenced to a protein data set. The qualitative pattern of both the IR and VCD changes is consistent with a coil-to-sheet transition occurring as pH is progressively decreased to values lower than 3. A similar transition was seen in commercial preparation of phosvitin which still contained metal ions, but there the transition was more gradual and occurred at somewhat different pH values. Such a gradual change is also evident in the solution phase absorption band profile but is made clearer using Fourier deconvolution. Based on VCD results, the low pH transition appears to occur with two distinct manifestations of the beta-sheet form. However, at the lowest pH values the sample may precipitate. These two forms are not distinguishable with Fourier transform infrared alone and may be due to a twist of the beta-sheet form or to aggregation.

Circular Dichroism↗

PubMed1990

Identification and characterization of the major chicken bone phosphoprotein. Analysis of its synthesis by cultured embryonic chick osteoblasts.

The major phosphoprotein synthesized by cultured chicken embryo osteoblasts had a molecular mass of approximately 66 kDa. The 32P label on the protein was cleaved by acid phosphatase treatment and O-[32P]phosphoserine and O-[32P]phosphothreonine could be identified after partial acid hydrolysis. The phosphoprotein contributed approximately 2.0% of the total protein synthesized by osteoblasts and was shown to be secreted, as shown by its presence in the culture media. Glycosylation was demonstrated by the fact that it could be labelled with [3H]galactosamine. The major approximately 66-kDa phosphoprotein was resolved by isoelectric focusing into three major variants with pI values ranging over 3.7 - 3.9; all three forms appear to be the result of variation in the extent of protein phosphorylation. An identical approximately 66-kDa phosphoprotein could be extracted from chicken bones which had both the same range of pI values and an identical elution position following DEAE-Sephacel chromatography. Analysis of the protein isolated from bone demonstrated the presence of sialic acid and, while amino-terminal sequence analysis and internal tryptic fragment sequence analysis of about 25% of the protein revealed little similarity to the rat phosphoprotein osteopontin, a conserved nine-residue sequence spanning the Arg-Gly-Asp cell-binding site of the rat protein osteopontin, was identified in the approximately 66-kDa chicken protein. Peptide mapping with Staphylococcus aureus V8 protease of the in vivo protein compared to the in vitro synthesized protein demonstrated identical peptide fingerprints. The two proteins also had comparable amino acid compositions. Several smaller-molecular-mass phosphoproteins ranging in size over about 55 - 29 kDa were also observed in the HCl extracts of bone. Peptide mapping of these species demonstrated that the approximately 66-kDa, approximately 55-kDa, and approximately 45-kDa species had a common core of peptide fragments. Pulse/chase experiments in culture revealed no evidence for a defined pathway of intracellular proteolysis associated with the approximately 66-kDa species since this phosphoprotein remained the prevalent species after a 24-h chase. Because of the predominant association of all the smaller-molecular-mass forms with the cell layer and an absence of a quantitative conversion to any of the smaller forms over a 24-h chase, these results suggested that the lower-molecular-mass species were not the result of proteolytic processing during synthesis or secretion, but rather represent proteolysis of the approximately 66-kDa component in the extracellular matrix.(ABSTRACT TRUNCATED AT 400 WORDS)

Amino Acid Sequence↗

PubMed1990

Developmental appearance and ultrastructural immunolocalization of a major 66 kDa phosphoprotein in embryonic and post-natal chicken bone.

Biochemical analyses and immunocytochemistry were used to examine the developmental appearance of a major approximately 66 kDa bone phosphoprotein (66 kDa BPP) in the mid-diaphyseal region of embryonic and post-natal chicken tibiae in vivo. Total protein and O-phosphoserine (Ser-P) and O-phosphothreonine (Thr-P) content of 8-, 12-, and 18-day embryonic, and 4-wk post-natal chicken tibiae were determined by amino acid analysis. Similar bone samples were carried through a wide variety of tissue-processing regimes including different protocols for fixation, decalcification, dehydration, and embedding prior to electron microscopy. For immunocytochemistry, tissue sections were incubated with a polyclonal antibody raised in rabbits against 66 kDa BPP, and the antigen was revealed by the high-resolution protein A-gold technique. Amino acid analysis, Western blotting, and immunocytochemistry all showed the presence and increasing concentration of bone phosphoprotein with advancing developmental age. Immunogold labeling was observed over osteoblasts and mineral deposits throughout the bone with the most intense reaction occurring at the mineralization front in embryonic tibiae. Electron probe X-ray microanalysis confirmed the association of 66 kDa BPP with mineral. The levels of phosphoprotein in the tissue were directly correlated with increasing degrees of mineralization. These observations are consistent with previous proposals suggesting that phosphoproteins may play a significant role in the calcification of bone matrix.

Aging↗

PubMed1990

Expression and ultrastructural immunolocalization of a major 66 kDa phosphoprotein synthesized by chicken osteoblasts during mineralization in vitro.

Embryonic chicken osteoblasts cultured over a 30 day period were used as a model system for studying the expression of bone phosphoproteins during cellular differentiation and the possible role of these proteins in extracellular matrix mineralization. Accumulation of total phosphoprotein in the cultures, as determined by O-phosphoserine (Ser-P) and O-phosphothreonine (Thr-P) amino acid analysis, revealed a greater than 10-fold increase over the 30 day period. Total phosphoprotein synthesis, as assessed by (32P)-, (3H)-Ser-P, and (14C)-Thr-P protein labeling, showed the highest levels concurrent with initial mineral deposition within the matrix. The major phosphoprotein present in chicken bones and synthesized by the cultured osteoblasts had a molecular weight of approximately 66 kDa. This 66 kDa bone phosphoprotein (66 kDa BPP) was purified to homogeneity and was used for antibody production. Application of this antibody in Western blot analysis revealed that 66 kDa BPP was present only in protein extracts of mineralizing cultured osteoblasts and was absent in cultures of non-mineralizing chondrocytes, myoblasts, and tendon fibroblasts. The 66 kDa BPP in vitro accumulated continuously in the extracellular matrix in a manner that paralleled both phosphoprotein synthesis and total phospho-amino acid production. A comparison of the results obtained in vitro to those from developing embryonic tibiae in vivo demonstrated a similar qualitative and temporal expression of phosphoprotein and a continual accumulation of 66 kDa BPP in the matrix with advancing mineralization and developmental age. Ultrastructural immunocytochemistry using the 66 kDa BPP antibody and the protein A-gold technique revealed specific immunolabeling over electron-dense regions of mineralization in the cultures that appeared identical to the distribution of labeling observed in vivo (McKee et al.: Connect. Tissue Res., 21:21-29, 1989; Anat. Rec., 228:77-92, 1990). These results demonstrate that this major 66 kDa BPP was expressed concurrently with other differentiated osteoblast functions and suggests that it may play a role in the initiation or regulation of mineralization.

Animals↗

PubMed1990

Resolution-enhanced Fourier transform infrared spectroscopy study of the environment of phosphate ions in the early deposits of a solid phase of calcium-phosphate in bone and enamel, and their evolution with age. I: Investigations in the upsilon 4 PO4 domain.

In order to investigate the possible existence in biological and poorly crystalline synthetic apatites of local atomic organizations different from that of apatite, resolution-enhanced, Fourier transform infrared spectroscopy studies were carried out on chicken bone, pig enamel, and poorly crystalline synthetic apatites containing carbonate and HPO4(2-) groups. The spectra obtained were compared to those of synthetic well crystallized apatites (stoichiometric hydroxyapatite, HPO4(2-)-containing apatite, type B carbonate apatite) and nonapatitic calcium phosphates which have been suggested as precursors of the apatitic phase [octacalcium phosphate (OCP), brushite, and beta tricalcium phosphate and whitlockite]. The spectra of bone and enamel, as well as poorly crystalline, synthetic apatite in the upsilon 4 PO4 domain, exhibit, in addition to the three apatitic bands, three absorption bands that were shown to be independent of the organic matrix. Two low-wave number bands at 520-530 and 540-550 cm-1 are assigned to HPO4(2-). Reference to known calcium phosphates shows that bands in this domain also exist in HPO4(2-)-containing apatite, brushite, and OCP. However, the lack of specific absorption bands prevents a clear identification of these HPO4(2-) environments. The third absorption band (610-615 cm-1) is not related to HPO4(2-) or OH- ions. It appears to be due to a labile PO4(3-) environment which could not be identified with any phosphate environment existing in our reference samples, and thus seems specific of poorly crystalline apatites. Correlation of the variations in band intensities show that 610-615 cm-1 band is related to an absorption band at 560 cm-1 superimposed on an apatite band. All the nonapatitic phosphate environments were shown to decrease during aging of enamel, bone, and synthetic apatites. Moreover, EDTA etching show that the labile PO4(3-) environment exhibited a heterogeneous distribution in the insoluble precipitate.

Aging↗

PubMed1990

The possible role of collagen fibrils and collagen-phosphoprotein complexes in the calcification of bone in vitro and in vivo.

Samples of decalcified chicken bone containing varying concentrations of phosphoproteins from bone or egg yolk (phosvitin) were used in vitro as heterogenous nucleators for the induction induction of Ca-P apatite crystals from operationally metastable solutions of Ca and P in vitro. The lag time between exposure of the collagen-phosphoprotein complexes to a metastable solution of Ca and P and the time nucleation of crystals occurred decreased as the concentration of Ser(P) and Thr(P) increased. Enzymatic cleavage of the phosphate groups by wheat germ acid phosphatase reversed this effect, indicating that the phosphate groups per se are necessary, but may not be sufficient for the facilitation of the nucleation of Ca-P crystals by collagen complexed to phosphoprotein.

Animals↗

PubMed1989

Mechanism of calcification: role of collagen fibrils and collagen-phosphoprotein complexes in vitro and in vivo.

Samples of decalcified chicken bone together with varying concentrations of phosphoproteins from bone or egg yolk (phosvitin) were used in vitro as heterogenous nucleators for the induction of Ca-P apatite crystals. The lag time between exposure of the collagen-phosphoprotein complexes and the time nucleation of crystals occurred decreased as the concentration of Ser(P) and Thr(P) increased. Enzymatic cleavage of the phosphate groups by wheat germ and phosphatase reversed this effort, indicating that the phosphate group per se principally facilitated the nucleation of Ca-P crystals by the phosphoprotein complex and collagen.

Animals↗

PubMed1989

Tooth enamel protein, amelogenin, has a probable beta-spiral internal channel, Gln112-Leu138, within a single polypeptide chain: preliminary molecular mechanics and dynamics studies.

Molecular dynamics simulation, with backbone constraints for 20 ps of equilibration and simulation, of a repeating polypeptide segment, Gln-Pro-His-Gln-Pro-Leu-Gln-Pro-His-Gln-Pro-Leu-Gln-Pro-Met-(Gln-Pro-Leu )4, constituting residues 112-138 of bovine amelolgenin, a 19.35 kD hydrophobic protein, are discussed. It is generally believed that the above polypeptide segment is important for the interaction of amelogenin with Ca++ ions, which occurs in the early phases of enamel mineralization. An energetically stable structure of the above polypeptide with recurrent beta-turns is observed and contains a pore of approximately 1 A radius along the helical that can accommodate an unhydrated Ca++ ion. The length of the polypeptide possesses correct dimensions to span a bilayer. The proposed structure is unique among known polypeptide and protein structures.

Amelogenin↗

PubMed1989

The carbonate environment in bone mineral: a resolution-enhanced Fourier Transform Infrared Spectroscopy Study.

The environment of carbonate ions in bones of different species (rat, rabbit, chicken, cow, human) was investigated by Fourier Transform Infrared Spectroscopy (FTIR) associated with a self-deconvolution technique. The carbonate bands in the v2 CO3(2-) domain show three components which were identified by using synthetic standards and different properties of the apatitic structure (ionic affinity for crystallographic locations, ionic exchange). The major component at 871 cm-1 is due to carbonate ions located in PO4(3-) sites (type B carbonate). A band at 878 cm-1 was exclusively assigned to carbonate ions substituting for OH-ions in the apatitic structure (type A carbonate). A band at 866 cm-1 not previously observed was shown to correspond to a labile carbonate environment. The intensity ratio of type A to type B carbonate appears remarkably constant in all bone samples. The 866 cm-1 carbonate band varies in its relative intensity in different species.

Animals↗

PubMed1989

Soluble glycosylated phosphoproteins of cementum.

Ethylenediaminetetraacetate and hydrochloric acid (EDTA) (HCl) extracts of cementum were fractionated by molecular sieving, ion exchange chromotography, and reverse phase high precision liquid chromatography (HPLC). Nine fractions were isolated, all of which contained serine phosphate, threonine phosphate, and high concentrations of aspartic acid (asp) and glutamic acid (glu). Five of the fractions obtained by repeated HPLC consisted of a single band by SDS-PAGE; the others contained at least one other minor component. All of the protein bands stained with both Rhodamine B and alcian blue, the latter consistent with analytical determinations that demonstrated that the phosphoprotein component contained a significant amount of carbohydrate, including neuraminic acid.

Animals↗