While previous studies revealed that matrix vesicles (MV) contain a nucleational core (NC) that converts to apatite when incubated with synthetic cartilage lymph, the initial mineral phase present in MV is not well characterized. This study explored the physicochemical nature of this Ca 2؉ and P i -rich NC. MV, isolated from growth plate cartilage, were analyzed directly by solidstate 31 P NMR, or incubated with hydrazine or NaOCl to remove organic constituents. Other samples of MV were subjected to sequential treatments with enzymes, salt solutions, and detergents to expose the NC. We examined the NC using transmission electron microscopy, energy-dispersive analysis with x-rays, and electron and x-ray diffraction, Fourier transform-infrared spectroscopy, high performance thin-layer chromatographic analysis, and SDS-polyacrylamide gel electrophoresis. We found that most of the MV proteins and lipids could be removed without destroying the NC; however, NaOCl treatment annihilated its activity. SDS-polyacrylamide gel electrophoresis showed that annexin V, a phosphatidylserine (PS)-dependent Ca 2؉ -binding protein, was the major protein in the NC; high performance thin-layer chromatographic analysis revealed that the detergents removed the majority of the polar lipids, but left significant free cholesterol and fatty acids, and small but critical amounts of PS. Transmission electron microscopy showed that the NC was composed of clusters of ϳ1.0 nm subunits, which energy-dispersive analysis with x-rays revealed contained Ca and P i with a Ca/P ratio of 1.06 ؎ 0.01. Electron diffraction, x-ray diffraction, and Fourier transform-infrared analysis all indicated that the NC was noncrystalline.

Matrix vesicles are lipid bilayer-enclosed structures that initiate extracellular mineral formation. Little attention has been given to how newly formed mineral interacts with the lipid constituents and then emerges from the lumen. To explore whether specific lipids bind to the incipient mineral and if breakdown of the membrane is involved, we analyzed changes in lipid composition and extractability during vesicle-induced calcification. Isolated matrix vesicles were incubated in synthetic cartilage lymph to induce mineral formation. At various times, samples of the lipids were taken for analysis, extracted both before and after demineralization to remove deposited mineral. Phosphatidylserine and phosphatidylinositol both rapidly disappeared from extracts made before decalcification, indicating rapid degradation. However, extracts made after demineralization revealed that phosphatidylserine had become complexed with newly forming mineral. Concomitantly, its levels actually increased, apparently by base-exchange with phosphatidylethanolamine. Though partially complexed with the mineral, phosphatidylinositol was nevertheless rapidly broken down. Sphingomyelin and phosphatidylethanolamine also underwent rapid breakdown, but phosphatidylcholine was degraded more slowly, all accompanied by a buildup of free fatty acids. The data indicate that phosphatidylserine forms complexes that accompany mineral formation, while degradation of other membrane phospholipids apparently enables egress of crystalline mineral from the vesicle lumen. Matrix vesicles (MV)1 are extracellular microstructures released by calcifying cells that initiate mineral formation in newly forming bone (1-4). MV are enclosed by a lipid bilayer membrane that is enriched in selected phospholipids, especially phosphatidylserine (PS) (5-6), a lipid with known high affinity for Ca 2ϩ (7)(8). Initially, PS is largely confined to the inner leaflet of the MV membrane (9). Previous transmission electron microscopic (TEM) studies have shown that the first mineral formed in MV is associated with the inner aspect of the membrane (10). Later, the crystals appear to emerge through the membrane and trigger formation of radial clusters of mineral centered on the remnant of the original vesicle. How the crystals penetrate the MV membrane is currently unknown. While it is possible that simple physical force mediates this process (11), there is indirect evidence that latent lipolytic enzymes become activated during Ca 2ϩ accumulation and facilitate breakdown of the membrane. To explore this latter possibility, the composition of lipids in MV was analyzed during the course of MV-mediated mineralization in vitro.Since previous work had shown that not all lipids were readily extracted from mineralizing tissues (12-13), resident MV lipids were extracted both before and after demineralization using both neutral and acidic lipid solvents. Lipid composition was analyzed qualitatively by high performance thin layer chromatography (HPTLC) and quantitatively by high performance liq...

Previous studies revealed that matrix vesicles (MV) have an acid-labile nucleationally active core (ALNAC) essential for mineral formation; current studies were aimed at characterizing and reconstituting ALNAC. SDS-PAGE and FTIR analyses revealed the presence of lipids, proteins and amorphous calcium phosphate (ACP) in ALNAC. Extraction with chloroform-methanol reduced, but did not destroy MV calcification; treatment with chloroform-methanol-HCl destroyed all activity. This acidic solvent extracted the annexins, (phosphatidylserine (PS)-dependent Ca(2+)-binding proteins), and dissociated PS-Ca(2+)-Pi complexes present in the MV. Attempts to reconstitute ALNAC, centered on the Ca(2+)-PS-Pi complex. Various pure lipids, electrolytes and proteins were combined to form a synthetic nucleationally active complex (SNAC), analyzing the rate of Ca2+ uptake. Inclusion of phosphatidylethanolamine (PE) or sphingomyelin (SM) with PS, or Mg2+ or Zn2+ with Ca2+, strongly inhibited activity; incorporation of annexin V increased SNAC activity. Thus, approaching from either deconstruction or reconstruction, it appears that ALNAC is composed of ACP complexed with PS and the annexins. Other lipids, proteins and electrolytes modulate its activity. These findings also indicate how ALNAC must be formed in vivo.

Advances in the culture of mineralizing growth plate chondrocytes provided an opportunity to study endochondral calcification under controlled conditions. Here we report that these cultures synthesize large amounts of proteins characteristically associated with mineralization: type II and X collagens, sulfated proteoglycans, alkaline phosphatase, and the bone-related proteins, osteonectin and osteopontin. Certain chondrocytes appeared to accumulate large amounts of Ca2+ and Pi during the mineralization process: laser confocal imaging revealed high levels of intracellular Ca2+ in their periphery and X-ray microanalytical mapping revealed the presence of many Ca(2+)- and Pi-rich cell surface structures ranging from filamentous processes 0.14 +/- 0.02 microns by 0.5-2.0 microns, to spherical globules 0.70 +/- 0.27 microns in diameter. Removal of organic matter with alkaline sodium hypochlorite revealed numerous deposits of globular (0.77 +/- 0.19 micron) mineral (calcospherites) in the lacunae around these cells. The size and spatial distribution of these mineral deposits closely corresponded to the Ca(2+)-rich cell surface blebs. The globular mineral progressively transformed into clusters of crystallites. Taken with earlier studies, these findings indicate that cellular uptake of Ca2+ and Pi leads to formation of complexes of amorphous calcium phosphate, membrane lipids, and proteins that are released as cell surface blebs analogous to matrix vesicles. These structures initiate development of crystalline mineral. Thus, the current findings support the concept that the peripheral intracellular accumulation of Ca2+ and Pi is directly involved in endochondral calcification.