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Biomedical subjects

L Spevak

Publications and source records attributed to L Spevak.

12 recordsLinked to original sources
PubMed2005

Importance of phosphorylation for osteopontin regulation of biomineralization.

Previous in vitro and in vivo studies demonstrated that osteopontin (OPN) is an inhibitor of the formation and growth of hydroxyapatite (HA) and other biominerals. The present study tests the hypotheses that the interaction of OPN with HA is determined by the extent of protein phosphorylation and that this interaction regulates the mineralization process. Bone OPN as previously reported inhibited HA formation and HA-seeded growth in a gelatin-gel system. A transglutaminase-linked OPN polymer had similar effects. Recombinant, nonphosphorylated OPN and chemically dephosphorylated OPN, had no effect on HA formation or growth in this system. In contrast, highly phosphorylated milk OPN (mOPN) promoted HA formation. The mOPN stabilized the conversion of amorphous calcium phosphate (a non-crystalline constituent of milk) to HA, whereas bone OPN had a lesser effect on this conversion. Mixtures of OPN and osteocalcin known to form a complex in vitro, unexpectedly promoted HA formation. To test the hypothesis that small alterations in protein conformation caused by phosphorylation account for the differences in the observed ability of OPN to interact with HA, the conformation of bone OPN and mOPN in the presence and absence of crystalline HA was determined by attenuated total reflection (ATR) infrared (IR) spectroscopy. Both proteins exhibited a predominantly random coil structure, which was unaffected by the addition of Ca(2+). Binding to HA did not alter the secondary structure of bone OPN, but induced a small increase of beta-sheet (few percent) in mOPN. These data taken together suggest that the phosphorylation of OPN is an important factor in regulating the OPN-mediated mineralization process.

Animals↗
PubMed2003

Osteopontin facilitates bone resorption, decreasing bone mineral crystallinity and content during calcium deficiency.

Osteopontin null-mice were previously shown to have bones containing more mineral and larger mineral crystals. These bones were independently seen to be resistant to ovariectomy-induced remodeling. To separate the physicochemical effects of osteopontin, which is an in vitro inhibitor of mineral crystal formation and growth, from effects of osteopontin on in vivo bone remodeling, this study examined mature (5-month-old) osteopontin-null (Opn-/-) and wildtype (WT) mice given a calcium-deficient diet. Biochemical parameters were measured during 4 weeks of Ca deficiency, followed by 1 week of refeeding adequate Ca. Ca deficiency caused a transiently greater rise in bone resorption in WT than Opn-/- mice (P = 0.01), whereas only the Opn-/- mice tended to increase Ca absorption (P = 0.08), yet both groups showed elevated levels of parathyroid hormone (PTH) (P < 0.001). The rise in markers of bone formation due to Ca deficiency was similar in both groups during Ca deficiency. Fourier transform infrared microspectroscopy assessed mineral properties at 20 microm spatial resolution in different anatomic regions of the bone. The Ca-deficient Opn-/- animals had slightly increased mineral content as compared to the WT, and there was a significant increase in the mineral content of older (endosteal) bone, implying that osteoclast recruitment was impaired. Crystallinity in the Ca-deficient Opn-/- bones was increased relative to the Ca-deficient WT at all sites except adjacent to the periosteum (younger mineral). These data suggest that osteopontin has both a physicochemical effect (inhibiting crystal growth and crystal proliferation) and a role in osteoclast recruitment, and in its absence, extraskeletal organs maintain calcium homeostasis.

Amino Acids↗
PubMed2002

Osteopontin deficiency increases mineral content and mineral crystallinity in mouse bone.

Fourier transform infrared microspectroscopy (FTIRM) and infrared imaging (FTIRI) were used to characterize the mineral in bones of two different lines of Opn-deficient (Opn-/-) mice and their background-matched wild-type controls (Opn+/+). Sections of tibia and femur from 12-week-old and 16-week-old mice were evaluated with a spatial resolution between 10 microm (FTIRM) and 7 microm (FTIRI). FTIRI was used to examine 400 microm x 400 microm areas in cortical bone and trabecular bone and FTIRM examined selected 20 microm x 20 microm areas at sites within these anatomically defined areas. Despite the absence of an obvious phenotype in Opn-deficient mice, being undetectable by radiographic and histological methods, FTIRM analyses revealed that the relative amount of mineral in the more mature areas of the bone (central cortical bone) of Opn-knockout mice was significantly increased. Moreover, mineral maturity (mineral crystal size and perfection) throughout all anatomic regions of the Opn-deficient bone was significantly increased. The 2-dimensional, color-coded data (images) produced by FTIRI showed similar increases in mineral maturity in the Opn-/- bone, however, the crystallinity parameters were less sensitive, and significance was not achieved in all areas analyzed. Nonetheless, the findings of increased mineral content and increased crystal size/perfection in both lines of Opn-deficient mice at both ages are consistent with in vitro data indicating that Opn is a potent inhibitor of mineral formation and mineral crystal growth and proliferation, and also support a role for Opn in osteoclast recruitment and function.

Animals↗
PubMed2002

Optimal methods for processing mineralized tissues for Fourier transform infrared microspectroscopy.

Fourier transform infrared microspectroscopy (FTIRM) and infrared imaging (FTIRI) are techniques utilized in the analysis of bone mineral and matrix properties in health and disease. Since the spatial arrangement of bone tissue is conserved using FTIRM and FTIRI, quantitative data can be obtained on bone mineral (hydroxyapatite) crystalline size and composition, and on matrix structure and composition at discrete anatomic locations with a spatial resolution from approximately 7 mm (FTIRI) to 10 mm (FTIRM). To section bone for FTIRM and FTIRI, it must be preserved ("fixed") to maintain its properties, and embedded in a hard supportive material. Since most of the embedding media have components that spectrally overlap the components of mineralized tissues, it is critical to define optimal embedding and fixation protocols that have the least effect on mineral and matrix spectra. In the current study, the spectra of mouse calvaria in seven different fixatives and six different commonly used embedding media were assessed by FTIRM and FTIRI. The fixatives evaluated were absolute ethanol, 70% ethanol, glycerol, formaldehyde, EM fixative, and formalin in cacodylate or phosphate-buffered saline. The embedding media tested were Araldite, Epon, JB-4, LR White, PMMA, and Spurr. Comparisons were made to FTIR spectra obtained from unprocessed ground calvaria and to spectra of cryosections of unfixed tissue, fast-frozen in polyvinyl alcohol (5% PVA). Non-aqueous fixatives and embedding in LR White, Spurr, Araldite, and PMMA had the least effect on the spectral parameters measured (mineral to matrix ratio, mineral crystallinity, and collagen maturity) compared with cryo-sectioned calvaria and non-fixed, non-embedded calvaria in KBr pellets.

Animals↗
PubMed2001

Establishment of an osteoid preosteocyte-like cell MLO-A5 that spontaneously mineralizes in culture.

The mechanisms controlling the initiation of mineralization of bone matrix are not clear. To examine this process, we established a cell line called MLO-A5 that mineralizes in sheets, not nodules, within 3 days of culture in the presence of beta-glycerophosphate (beta-GP) and ascorbic acid and within 7 days in the absence of beta-GP and ascorbic acid. The mineral formed in both cases was shown to be bonelike apatite by Fourier transformed infrared (FTIR) spectroscopy. Mineral-to-matrix ratios (min/matrix) calculated from the FTIR data, which are related directly to ash weight, were approximately 0.4 in the absence of beta-GP and ascorbic acid and approximately 1.2 in the presence of beta-GP and ascorbic acid. By comparison, these ratios in fetal rat calvarial cells without beta-GP equal 0 and with beta-GP 1.9. This cell line and three others (MLO-A2, -D1, and -D6) were isolated from the long bones of transgenic mice expressing the large T-antigen driven by the osteocalcin promoter, the same mice from which the osteocyte-like cell line MLO-Y4 was isolated.(1) The cell lines were selected based on a dendritic or stellate morphology. MLO-A5 cells express high alkaline phosphatase, collagen type 1, parathyroid hormone/parathyroid hormone-related peptide (PTH/PTHrP) receptor, bone sialoprotein (BSP), and osteocalcin (767 ng/10(6) cells compared with <1-2.2 ng/10(6) cell for primary mouse osteoblasts and five osteoblast cell lines). The single unique feature of the MLO-A5 cells compared with the other three nonmineralizing cell lines is the high expression of messenger RNA (mRNA) for BSP. These cell lines may represent stages of osteocyte differentiation and the MLO-A5 cells represent the postosteoblast, preosteocyte responsible for triggering mineralization of osteoid.

Alkaline Phosphatase↗
PubMed2000

Dentin sialoprotein (DSP) has limited effects on in vitro apatite formation and growth.

Sialoproteins such as bone sialoprotein (BSP) and dentin sialoprotein (DSP) accumulate at the mineralization fronts in bone and dentin, respectively, suggesting they have some function in the mineralization process. BSP, a highly phosphorylated protein rich in polyglutamate repeats, is an effective nucleator of hydroxyapatite (HA) formation in vitro. The present study examines the effect of DSP, a low phosphorylated but related sialoprotein, on the formation and growth of HA. In vitro, in a gelatin gel diffusion system, DSP at low concentrations (<25 microg/ml) slightly increased the yield of HA formed at 3.5 and 5 days, while at higher concentrations (50-100 microg/ml) it slightly inhibited accumulation. Fewer mineral crystals were formed in the presence of high concentrations of DSP but they tended to aggregate (making them appear larger by electron microscopic analysis) than those formed in DSP-free gels. X-ray diffraction line broadening analysis failed to show significant changes in c-axis crystal dimensions with increasing DSP concentration. When HA-seed crystals were coated with DSP before inclusion in the gelatin gel there was a reduction in mineral accumulation relative to HA-seeds which had not been coated with DSP, but the extent of inhibition was significantly less than that seen in this system with other mineralized tissue matrix sialoproteins, such as osteopontin or BSP. The low affinity of DSP for well-characterized seed crystals and the limited effect of this protein on HA formation and growth suggest that the role of DSP in dentin is not primarily that of a mineralization regulator.

Animals↗
PubMed1997

Effects of bone CS-proteoglycans, DS-decorin, and DS-biglycan on hydroxyapatite formation in a gelatin gel.

The small leucine-rich bone proteoglycans, biglycan and decorin, can be purified by chromatography on hydroxyapatite columns, demonstrating their potential affinities for bone apatite. To determine their effects on in vitro apatite formation and growth, a mixture of the chondroitin-sulfate (CS) bone proteoglycans, or purified fractions of the dermatan sulfate (DS) containing proteoglycans, DS-decorin and DS-biglycan obtained from skin and articular cartilage, respectively, were analyzed in a gelatin gel diffusion system in which apatite formation occurs in the absence of proteins in a 3.5 day period. Low concentrations of the bone CS-proteoglycan mixture and low DS-biglycan concentrations (5-25 microg/ml) increased apatite formation relative to proteoglycan-free controls at 3.5 days. The CS-proteoglycan mixture was less effective at 50 microg/ml than at 10 microg/ml. DS-biglycan was similarly most effective at 5-25 microg/ml. At 5 days, when apatite growth and proliferation were assessed, 10 and 50 microg/ml of both CS-bone proteoglycan and DS-biglycan increased mineral yields. DS-decorin, in contrast, had no significant effect on mineral accumulation at any of these concentrations. In seeded growth experiments, 1 and 10 microg/ml CS-proteoglycan and 10 and 50 microg/ml DS-biglycan were significant effective inhibitors of mineral accretion, whereas DS-decorin showed no tendency to inhibit seeded growth. Using molar extinction coefficients to determine concentrations, the binding of DS-biglycan and DS-decorin to apatite (specific surface 54 m2/g) was determined using a Langmuir adsorption isotherm model. DS-biglycan had a greater affinity for apatite than DS-decorin (0.285 ml/micromol versus 0.0098 ml/micromol). DS-biglycan binding was more specific with fewer binding sites (3.5 micromol/m2 compared with 18. 2 micromol/m2 for DS-decorin). Data suggest that of the small proteoglycans, biglycan may play a more significant role than decorin in the regulation of mineralization.

Animals↗
PubMed1996

Persistence of complexed acidic phospholipids in rapidly mineralizing tissues is due to affinity for mineral and resistance to hydrolytic attack: in vitro data.

Acidic phospholipids, complexed with calcium and inorganic phosphate, are components of extracellular matrix vesicles. Both the complexed acidic phospholipids and matrix vesicles have previously been shown to serve as hydroxyapatite (HA) nucleators in solution and when implanted in a muscle pouch. The present study supplies evidence that complexed acidic phospholipids can persist in mineralizing tissues both because of their affinity for HA and because of their resistance to hydrolysis by phospholipase A2. Calcium-phosphatidylserine-phosphate complex (CPLX-PS) synthesized with 14C-labeled phosphatidylserine (PS) was used to measure CPLX-PS affinity for HA using a Langmuir adsorption isotherm model. The affinity was shown to be higher and more specific than that of PS itself (K = 8.66 ml/mumol; N, the number of binding sites = 20.4 mumol/m2 as compared with previously reported values for PS of K = 3.33 ml/mumol, and N = 4.87 mumol/m2). Incorporated into synthetic liposomes and incubated in a calcium phosphate solution in which mineralization is induced by an ionophore, CPLX-PS showed behavior distinct from free PS. As previously reported, PS in these liposomes totally blocked HA formation. On the other hand, CPLX-PS in similar concentrations had a varied response, having no effect, slightly inhibiting, or actually promoting HA formation. CPLX-PS was also shown to be a poorer substrate for phospholipase A2 than PS, with Km = 4.63 mM for CPLX-PS and Km = 0.27 mM for PS; and Vmax = 0.029 ml/minute for CPLX-PS and Vmax = 0.066 ml/minute for PS. These data explain how complexed acidic phospholipids may persist in the growth plate and facilitate initial mineral deposition.

Calcification, Physiologic↗