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Influence of Ca2+ and Mg2+ on the thermotropic behaviour and permeability properties of liposomes prepared from dimyristoyl phosphatidylglycerol and mixtures of dimyristoyl phosphatidylglycerol and dimyristoyl phosphatidylcholine.
Authors:P W Van Dijck  P H Ververgaert  A J Verkleij  L L Van Deenen  J De Gier
Abstract:Calorimetric experiments showed a marked effect of Ca2+ and Mg2+ on the thermotropic behaviour of dimyristoyl phosphatidylglycerol. 2. Concentrations of Ca2+ and Mg2+ lower than 1 ion to 2 molecules of phosphatidylglycerol produced a shift of the phase transition to higher temperatures and an increase in the enthalpy change which is consistent with a closer packing of the lipid molecules in the liposomes. 3. Above the 1:2 ratio, freeze-fracture electron microscopy demonstrated typical "crystal" structures both in the presence of Ca2+ and Mg2+. In the presence of Mg2+ a metastable behaviour was noticed in the calorimetric experiments. 4. A Ca2+- and Mg2+-induced shift in the transition temperature and an increase in the enthalpy change was also observed in a 1:1 mixture of dimyristoyl phosphatidylglycerol and dimyristoyl phosphatidylcholine. However, these mixed samples remained liposomal in structure at any concentration of the divalent ions. 5. Liposomes prepared from a 1:1 mixture of dimyristoyl phosphatidylglycerol and dimyristoyl phosphatidylcholine in the absence of divalent cations are permeable in the range 10-50 degrees C. Bilayers of mixtures neutralized by Ca2+ or Mg2+ were demonstrated to be completely impermeable to K+, except in the vicinity of the phase transition. 6. The leak of ions from liposomes of a 1:1 mixture of dimyristoyl phosphatidylglycerol and dimyristoyl phosphatidylcholine in the vicinity of the phase transition temperature was considerably less in the presence of Ca2+ than in the presence of Mg2+. 7. It is concluded that there is a correlation between the calorimetric data and the permeability properties of dimyristoyl phosphatidylglycerol-containing bilayers with respect to the influence of Ca2+ and Mg2+.
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