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Liposome-mediated calcium phosphate formation in metastable solutions
Calcified Tissue International
|July 1, 1985
Summary
Anionic liposomes influence calcium phosphate precipitate formation. Intraliposomal precipitation, triggered by ionophore-induced membrane permeability, can seed external solutions, leading to enhanced mineral deposition.
Area of Science:
- Biochemistry
- Materials Science
- Biophysics
Background:
- Liposomes are crucial in drug delivery and biomimetic studies.
- Calcium phosphate precipitation is fundamental to biomineralization processes.
- Understanding liposome-mineral interactions is key to explaining biological calcification.
Purpose of the Study:
- To investigate the impact of anionic liposomes on calcium phosphate precipitate formation.
- To determine the role of intraliposomal inorganic phosphate (PI) and membrane permeability in precipitation.
- To elucidate the mechanism of mineral deposition in relation to liposome integrity.
Main Methods:
- Anionic liposomes were prepared using phosphatidylcholine, dicetyl phosphate, and cholesterol.
- Liposomes with entrapped inorganic phosphate (PI) were incubated in calcium (Ca2+) solutions.
- Ionophore X-537A was used to induce liposome membrane permeability.
- Calcium and phosphate concentrations were monitored to assess precipitate formation.
Main Results:
- Significant Ca2+ and PI losses from the external solution occurred only when liposomes containing PI became permeable to Ca2+ via ionophore addition.
- Ca2+ loss was substantially greater when coupled with PI loss, indicating a synergistic effect on precipitation.
- Intraliposomal precipitation, previously shown to reduce internal Ca2+, appeared to seed secondary precipitation in the external metastable solution.
Conclusions:
- Anionic liposomes can modulate calcium phosphate precipitation.
- Intraliposomal precipitation, facilitated by ionophore-induced permeability, can act as a nucleation site for external mineral deposits.
- This mechanism may contribute to the formation of extravesicular mineral deposits observed in matrix vesicle calcification.