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(Received for publication, December 29, 1995, and in revised form, July 19, 1996)
From the Department of Pathology and Laboratory Medicine,
University of Kansas Medical Center,
Kansas City, Kansas 66160-7410
Accumulating evidence indicates that
calcification by isolated mammalian matrix vesicles (MVs) can be
initiated by ATP. Since ATP can be hydrolyzed by either a specific
ATPase or by nonspecific alkaline phosphatase (ALP), it remains to be
established whether ATPase or ALP mediates ATP-initiated Ca and
Pi deposition. To support the hypothesis that specific
ATPase is responsible for ATP-initiated calcification by MVs isolated
from mammalian cartilage and bone, the effects of ATP analogs, ALP
substrates, and specific inhibitors on ATP hydrolysis and ATP-initiated
calcification were compared between intact MVs and monoclonal antibody
affinity-purified MV ALP. ATP analogs such as ADP and AMP exerted
marked inhibitory effects on both [ The sequence of steps that lead to the initiation of calcification
in skeletal tissues has yet to be elucidated. Since alkaline
phosphatase (ALP)1 was proposed by Robison
(1) in 1923 as an initiator of calcification in skeletal tissues,
several potential initiators, including type I collagen (2),
proteoglycans (3), osteocalcin (4), and phosphoproteins (2), have
subsequently been suggested. However, none of these putative agents are
firmly established, and indeed many prevent in vitro
calcification (4, 5, 6). Although matrix vesicles (MVs) have been
implicated as the sites of calcification initiation, evidenced through
morphological, biochemical, and pathological studies (for review, see
Ref. 7), the detailed mechanisms of initiation of calcification by MVs
have yet to be defined (for review, see Ref. 8). Despite numerous
studies that showed that ATP can initiate calcification mediated by
mammalian MVs (9, 10, 11), it is not known whether a specific ATPase or ALP
is responsible for ATP-dependent calcification, because
both enzymes can hydrolyze ATP.
To support the hypothesis that specific ATPase rather than ALP plays a
role in ATP-initiated calcification by MVs isolated from mammalian
cartilage or bone, the effects of ATP analogs, ALP substrates, and
specific inhibitors on ATP hydrolysis and ATP-initiated calcification
were compared between intact MVs and monoclonal antibody
affinity-purified MV ALP. The results of the experimentation support
the hypothesis that specific ATPase plays a role in ATP-initiated
calcification by MVs.
Matrix Vesicle Preparation
The extracellular MV fraction was
prepared from pooled epiphyseal cartilage slices of 35 rachitic rats by
the method of Hsu (12). A rachitic growth plate was used as a source of
MVs, because it is precalcified and readily calcifiable in the presence
of exogenous Pi (13, 14). Thus, it can be used as an ideal
model for studying the initiation of calcification by MVs without
complication from proliferation of preexisting mineral. Epiphyseal
growth plates were removed aseptically, minced into 3-5-mm pieces, and
then digested in a solution (10 ml/g of tissue) containing 1,000 units/ml crude collagenase (type I; Sigma), 0.12 M NaCl, 0.01 M KCl, 1,000 units/ml penicillin,
1 mg/ml streptomycin, and 0.02 M Tes buffer, pH 7.45. The
digestion was carried out at 37 °C for 3 h. The digest was
centrifuged at 30,000 × g for 10 min, and the
resulting precipitate of cells and cell debris was discarded. The
supernatant was spun at 300,000 × g for 20 min, and
the resulting MV-enriched precipitates were then resuspended in 10 mM EGTA and 10 mM Tris-buffered saline (TBS),
pH 7.6. The mixture was incubated overnight at 4 °C to maximize the
removal of the endogenous mineral contaminant. The mixture was then
centrifuged at 300,000 × g for 20 min, and the
precipitate was washed twice by resuspension and centrifugation in the
presence of 10 mM TBS, pH 7.6. This final MV precipitate
was resuspended in a small volume of TBS to provide a protein
concentration of 0.5-1.5 mg/ml. The above-mentioned EGTA treatment was
attempted to minimize endogenous mineral content in MVs to study the
initial rather than proliferative stage of calcification.
Pooled fetal calvaria were obtained from three
near-term pregnant rats. Calvaria were treated with crude collagenase
at various time intervals to obtain different bone cell populations, as
described by Luben et al. (15). MVs were then isolated from
the collagenase digest using the same centrifugation procedure for the
cartilage MV preparation.
Calcium and Phosphate Deposition
The term ``Ca and Pi deposition'' is used in this
article to mean the process by which Ca and Pi were
deposited either as undefined forms of calcium phosphate or as
Ca2+ and Pi that was taken up by or bound to
MVs. To measure calcium and Pi deposition, the method of
Hsu (12) was used. Unless otherwise stated, the standard reaction
medium (100 µl) consisted of 50 mM Tes, pH 7.6 (it should
be stressed here that pH must be adjusted to 7.6 at 37 °C, as pH
changes with temperature), 85 mM NaCl, 15 mM
KCl, 1 mM MgCl2, 10 mM
NaHCO3, 1.35 mM CaCl2, 1 mM ATP, 1.97 mM Pi, and MVs (5 µg
of protein/ml). It should be noted that although 0.2 mM ATP
is sufficient for calcification, the degree of calcification was much
less than that obtained with optimal 1 mM ATP. Therefore,
to study effects of various agents on calcification, 1 mM
ATP was used for calcification study. For Ca uptake, 45Ca
(1 × 106 cpm) was used as the radioactive tracer.
Likewise, 32Pi was used as the tracer for
Pi uptake. The reaction was incubated for 5 h at
37 °C in a water vapor-saturated incubation chamber to minimize
vaporization of the reaction mixture during incubation. At the end of
incubation, the reaction mixture was filtered through 0.1-µm pore
size Durapore membranes (Millipore Inc.). The membranes were washed
twice each with 1 ml of TBS and then transferred to vials containing
scintillation fluid for radioactivity counting. The nonspecific Ca or
phosphate binding to filter papers was calculated from radioactivity
bound to the filters under the identical conditions, except that MVs
were omitted. The nonspecific binding radioactivity was then subtracted
from the radioactivity obtained in the presence of MVs. Ca or
Pi deposition is expressed as nmol of Ca or
Pi/ml of reaction mixture/5 h, calculated as: [(cpm
retained on the filter Purification of ALP from MVs
MV ALP was purified by a monoclonal antibody affinity column as
described by Hsu et al. (16). N-terminal amino acid
sequencing, reducing polyacrylamide gel electrophoresis, and Western
blotting indicated a homogeneous pure protein.
Specific ATPase Activity
A putative specific ATPase in MVs is defined as a specific
enzyme that solely uses ATP as a substrate and specifically releases
the terminal Pi from ATP. Therefore, a subsequent release
of Determination of the Relative Strength of ATP Analogs or ALP
Substrate in Inhibiting ATP Hydrolysis
The effectiveness of an ATP analog or ALP substrate in
inhibiting ATPase is expressed as [I/S]50, which is
defined as the required molar ratio of ATP analog or ALP substrate
(I):ATP (S) to inhibit 50% of ATPase activity. The higher ratio a
phosphoester or ATP analog displays, the less it can inhibit
[ Electron Microscopy
Pellets of MVs after incubation in calcifying solution with or
without ATP for 5 h were fixed in 2.5% glutaraldehyde,
postosmicated, and embedded in situ in Epon in Beckman
Instruments polyallomer centrifuge tubes. Unstained thin sections
(approximately 500 A in thickness) were examined and photographed in a
electron microscope (model J.O.E.L.).
Other Assays
Inorganic orthophosphate was determined by the method of Martin
and Doty (17), and the protein concentration was determined by the
method of Lowry et al. (18) using bovine serum albumin as
the standard. An adenyl cyclase assay was performed according to the
procedure of Krishna et al. (19).
Previous studies demonstrated that low levels of ATP (0.2 mM) can initiate calcification by cartilage MVs, although
the released Pi from ATP did not cause the final
[Ca2+] × [HPO] ion product to exceed
the threshold for spontaneous precipitation of calcium phosphate (11,
20). To determine whether ATP-induced mineralization by MVs also occurs
in bone, we prepared MVs from fetal rat calvaria and then tested their
ability to calcify in the presence of ATP. The isolated bone vesicles
were similar to cartilage MVs in shape, size, and the ability to
deposit electron-dense particles after a 5-h incubation period with
ATP-containing calcifying medium (Fig. 1). The
heterogeneity in size (50-500 nm) and shape of the isolated MVs was
closely similar to that of MVs in situ (1-1000 nm; for
review, see Ref. 7). Therefore, a further attempt to prepare MVs with
homogeneity in size is not a physiological approach. The possibility of
cross-contamination with subcellular organelles is unlikely, since
microsomal or mitochondrial markers such as NADPH cytochrome C
reductase and succinate dehydrogenase were absent (21). The MVs were
rich in plasma membrane AMPase and ALP activities, except that adenyl
cyclase activity was undetectable compared with that of chondrocyte
plasma membranes (0.09 ± 0.08 nmol/mg protein/min). Thus, these
observations support the contention that MVs are likely derived from
plasma membranes. MVs were partially loaded with electron-dense
particles after a 5-h incubation period with ATP-containing calcifying
medium and were fully loaded after 24 h (Fig. 1, B and
C). These observations suggest that a specific ATPase is
directly involved in the mechanism of mineral initiation by MVs in
skeletal tissues.
Determining whether there is direct involvement of a specific ATPase in
MV calcification has been hampered by a lack of proof of the presence
of a specific ATPase in MVs, as ATP can be hydrolyzed either by
specific ATPase or by nonspecific ALP. Therefore, a procedure must be
developed to distinguish specific ATPase activity from nonspecific ALP
activity, thereby providing evidence that ATPase rather than ALP is
responsible for ATP-initiated calcification.
LT, a specific ALP inhibitor (22), has been used as an effective means
to demonstrate the presence of ATPase distinguished from ALP in bone
homogenates and cartilage slices (23, 24). A cytochemical study at the
electron microscopic level also suggests the presence of an
LT-resistant ATPase in MVs (25). LT was used in this study to test the
correlation between ATPase activity and ATP-initiated calcification.
Both bone MVs and cartilage vesicles were selected to assure that
specific ATPase is responsible for ATP-initiated calcification in all
skeletal tissues. LT at 1 mM inhibited >90% of
Effect of l-tetramisole on [
Effect of l-tetramisole on ATP-dependent Ca and Pi
deposition
The best approach we used to distinguish a specific ATPase from
nonspecific ALP was to determine whether ATP analogs for ATPase were
more potent than ALP substrates in inhibiting
[
Fig. 2. Relative effectiveness of various ATP analogs and phosphomonoesters in blocking ATP-initiated calcification by MVs. ATP-dependent Ca deposition was performed in the presence of various concentrations of ATP analogs or phosphomonoesters (0.1-3 mM), whereas the original ATP concentration was 1 mM. bGP, -glycerophosphate; PEA,
phosphoethanolamine.
Since the electron microscopic data show that the electron-dense
particles were closely associated with MV membranes (Fig. 1,
B and C), a density centrifugation procedure was
explored to further purify calcifiable MVs. MVs were exposed to the
ATP-containing calcifying medium for 24 h to reach the maximal
deposition of mineral by MVs. The calcified MVs were readily sedimented
at 800 × g for 10 min due to their higher mineral
density than noncalcified vesicles. The resulting sediment was then
incubated for 24 h with 10 mM EGTA and 10 mM Tris, pH 6.0, to maximize the removal of MV-associated
minerals. The EGTA-treated vesicles were then sedimented at
250,000 × g for 20 min and washed twice with TBS by
resuspension and centrifugation. The resulting MVs appear to be devoid
of minerals after the EGTA wash (Fig. 3A) and
were calcified during a 24-h incubation with ATP-containing calcifying
media (Fig. 3B). These vesicles were found to contain both
ATPase and ATP-dependent calcifying activities, which can
be inhibited by AMP but not by Fig. 3. Further purification of calcifiable MVs. MVs were exposed to ATP-containing media for 24 h to reach the full extent of calcification. The calcified MVs were readily sedimented at 800 × g for 10 min due to their high mineral density. The resulting sediment was then incubated for 24 h in the presence of 10 mM EGTA and 10 mM Tris, pH 6.0, to maximally remove MV-associated minerals. The vesicles were then sedimented at 250,000 × g for 20 min and washed twice with TBS by resuspension and centrifugation. A, electron micrograph of MVs after the EGTA wash. B, electron micrograph of the washed MVs after exposure to the ATP-calcifying medium for 24 h. Fig. 4. Effects of AMP and -glycerophosphate on
ATPase and calcifying activities of density-sedimented MVs. The
isolation of density-sedimented MVs were prepared as described in Fig.
3. The effects of 1 mM AMP or -glycerophosphate
(bGP) on Ca deposition or ATPase activities are expressed as
percentages of the control activities in the presence of 1 mM ATP without AMP or -glycerophosphate. The control
values for Ca deposition and ATPase activity are 4.8 ± 0.2 nmol/µg protein/5 h and 250 ± 30 milliunits/mg protein,
respectively. Values are expressed as the mean ± S.E.
(bars) (from three experiments).
Although vanadate has been shown to inhibit both ATPase (26) and ALP
(27), the interpretation of inhibition of MV ATPase by vanadate can be
easily obscured by the fact that part of [
To understand how MVs initiate mineralization, it is necessary to consider the origin of Ca2+ and Pi within MVs. To study the origin of these ions within MVs, it is essential to consider the biogenesis of MVs. The freeze-fracture electron microscopic observation suggests that budding from chondrocyte plasma membranes is a possible mechanism for MV biogenesis (28). If this is indeed the case, then preexisting intracellular Pi would be likely to provide an initial source of the Pi of MV. Since the cytosolic [Ca2+] is less than µM, a specific pump system would be necessary to accumulate Ca2+ from surrounding tissue fluids into the vesicles. Ca2+ ATPase could fulfill this role, provided that MVs are an inside-out version of plasma membranes, because the plasma membrane Ca ATPase provides most outwardly directed Ca2+ translocation. Although available evidence indicates that plasma membrane-derived MVs are not everted during their biogenesis, it must be stressed that all ion pumps are potentially reversible, and Ca2+ tends to flow from an energized compartment to the lower energy side of a membrane, as in the case of isolated plasma membrane vesicles (29, 30). The net flow of Ca2+ is in favor of accumulation despite the possibility of an equal distribution of inside-out and right side-out versions of membrane vesicles. If ATP is provided by hypertrophic chondrocytes, MVs in situ may allow Ca accumulation by the same mechanism as that adapted by isolated liver or kidney plasma membrane vesicles. The most recent data with phosphatidylinositol-specific phospholipase C (31) indicate that MVs are right side-out versions of plasma membranes. This contention has also been supported by the observations that the solubilization of MV membranes by detergents did not further enhance ATPase, ALP, or AMPase (data not shown). To test whether Ca uptake is a prerequisite step before calcification can take place, we tested a batch of inhibitors for Ca uptake and ATPase. We were unable to observe the inhibitory effect of various ATPase-dependent Ca uptake inhibitors, including oligomycin, ouabain, thapsigargin, and vanadate, on calcification. However, we found that cetyltrimethyl bromide, which is a cationic detergent, inhibited both ATPase and calcification. Despite this observation, we feel that the correlation may be coincidental. Thus, it seems that the observed inhibitory effect of ATP analogs provides a more reliable test to see whether a specific ATPase different from other types of ATPase is responsible for ATP-initiated Ca and Pi deposition. Whether ATPase-driven Ca uptake is required for calcification remains to be established. Although ATP-initiated Ca uptake may serve a role in the mechanism of
MV-initiated calcification, sufficient ATP must be provided by
chondrocytes or other cells to the vicinity of MVs. The extracellular
ATP concentration has yet to be determined in the cartilage matrix,
probably due to the instability and trace amounts of ATP. However, it
has been shown that various types of cells are capable of exporting ATP
(for review, see Ref. 32). A continuous supply of ATP to the vicinity
of MVs from chondrocytes could be facilitated by chondrocyte
hypertrophy prior to calcification. It has been shown that the
hypertrophic zone of cartilage before calcification contains more ATP
than the reserve zone (33). The ability of cultured chondrocytes to
export ATP has been recently reported (34). Several reports also have
implicated the role of ATP in calcification: 1) blood ATP levels are
reduced in rachitic rats (35, 36); and 2) ATP promotes mineral
deposition by chondrocyte culture (34, 37) and cartilage slices (38,
39). In particular, the appearance of hydroxyapatite formed in the
presence of ATP was more similar to bone mineral than that obtained
with * This work was supported in part by National Institutes of Health Grant DE05262. The costs of publication of this article were defrayed in part by the payment of page charges. The article must therefore be hereby marked ``advertisement'' in accordance with 18 U.S.C. Section 1734 solely to indicate this fact.
To whom correspondence should be addressed: Dept. of Pathology and
Laboratory Medicine, University of Kansas Medical Center, 3901 Rainbow
Blvd., Kansas City, KS 66160-7410. Tel.: 913-588-5395; Fax:
913-588-7073.
1 The abbreviations used are: ALP, alkaline phosphatase; MV, matrix vesicle; TBS, Tris-buffered saline; LT, l-tetramisole; Tes, N-tris(hydroxymethyl)methyl-2-aminoethanesulfonic acid. The technical assistance of L. Davis and P. Moylan is greatly appreciated.
©1996 by The American Society for Biochemistry and Molecular Biology, Inc. This article has been cited by other articles:
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