N. Arispe et al., SIMILARITY IN CALCIUM-CHANNEL ACTIVITY OF ANNEXIN-V AND MATRIX VESICLES IN PLANAR LIPID BILAYERS, Biophysical journal, 71(4), 1996, pp. 1764-1775
Matrix vesicles (MVs), structures that accumulate Ca2+ during the init
iation of mineral formation in growing bone, are rich in annexin V. Wh
en MVs are fused with planar phospholipid bilayers, a multiconductance
Ca2+ channel is formed, with activity essentially identical to that o
bserved when annexin V is delivered to the bilayer with phosphatidylse
rine liposomes. Ca2+ currents through this channel, from either MV or
annexin V liposomes, are blocked by Zn2+, as is Ca2+ uptake by MV incu
bated in synthetic cartilage lymph. Blockage by Zn2+ was most effectiv
e when applied to the side containing the MV or liposomes. ATP and GTP
differentially modulated the activity of this channel: ATP increased
the amplitude of the current and the number of conductance states; GTP
dramatically reduced the number of events and conductance states, lea
ding to well-defined Ca2+ channel activity from either MV or the annex
in V liposomes. In the distinctive effects of ATP, GTP, and Zn2+ on th
e Ca2+ channel activity observed in both the MV and the liposome syste
ms, the common factor was the presence of annexin V. From this we conc
lude that Ca2+ entry into MV results from the presence of annexin V in
these membrane-enclosed structures.