PERSISTENCE OF COMPLEXED ACIDIC PHOSPHOLIPIDS IN RAPIDLY MINERALIZINGTISSUES IS DUE TO AFFINITY FOR MINERAL AND RESISTANCE TO HYDROLYTIC ATTACK - IN-VITRO DATA
Al. Boskey et al., PERSISTENCE OF COMPLEXED ACIDIC PHOSPHOLIPIDS IN RAPIDLY MINERALIZINGTISSUES IS DUE TO AFFINITY FOR MINERAL AND RESISTANCE TO HYDROLYTIC ATTACK - IN-VITRO DATA, Calcified tissue international, 58(1), 1996, pp. 45-51
Acidic phospholipids, complexed with calcium and inorganic phosphate,
are components of extracellular matrix vesicles. Both the complexed ac
idic phospholipids and matrix vesicles have previously been shown to s
erve 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 A(2). Calcium-phosphatidylserine-phosphate complex (
CPLX-PS) synthesized with C-14-labeled phosphatidylserine (PS) was use
d to measure CPLX-PS affinity for HA using a Langmuir adsorption isoth
erm model. The affinity was shown to be higher and more specific than
that of PS itself (K = 8.66 ml/mu mol; N, the number of binding sites
= 20.4 mu mol/m(2) as compared with previously reported values for PS
of K = 3.33 ml/mu mol, and N = 4.87 mu mol/m(2)). Incorporated into sy
nthetic liposomes and incubated in a calcium phosphate solution in whi
ch mineralization is induced by an ionophore, CPLX-PS showed behavior
distinct from free PS. As previously reported, PS in these liposomes t
otally blocked HA formation. On the other hand, CPLX-PS in similar con
centrations had a varied response, having no effect, slightly inhibiti
ng, or actually promoting HA formation. CPLX-PS was also shown to be a
poorer substrate for phos pholipase A(2) than PS, with Km = 4.63 mM f
or CPLX-PS and Km = 0.27 mM for PS; and V-max = 0.029 ml/minute for CP
LX-PS and V-max = 0.066 ml/minute for PS. These data explain how compl
exed acidic phospholipids may persist in the growth plate and facilita
te initial mineral deposition.