Interaction of alkaline earth cations with the negatively charged phospholipid 1,2-dimyristoyl-sn-glycero-3-phosphoglycerol: A differential scanning and isothermal titration calorimetric study

Citation
P. Garidel et A. Blume, Interaction of alkaline earth cations with the negatively charged phospholipid 1,2-dimyristoyl-sn-glycero-3-phosphoglycerol: A differential scanning and isothermal titration calorimetric study, LANGMUIR, 15(17), 1999, pp. 5526-5534
Citations number
47
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
LANGMUIR
ISSN journal
07437463 → ACNP
Volume
15
Issue
17
Year of publication
1999
Pages
5526 - 5534
Database
ISI
SICI code
0743-7463(19990817)15:17<5526:IOAECW>2.0.ZU;2-5
Abstract
The interaction of the alkaline earth cations Mg2+, Ca2+, and Sr2+ with 1,2 -dimyristoyl-sn-glycero-3-phosphoglycerol (DMPG), dispersed in 0.1 M NaCl a t pH 7, was investigated by differential scanning calorimetry (DSC) and iso thermal titration calorimetry (ITC). Both calorimetric methods revealed tha t the interaction of Mg2+,and Sr2+ With DMPG is of similar nature but diffe rent from the behavior of Ca2+. In the first heating scans of DMPG:Mg2+ and DMPG:Sr2+ complexes, transition peaks at 31-35 and 60 degrees C are observ ed. The higher transition peak disappears in consecutive heating and coolin g cycles and only the transition at 31-35 degrees C remains. The transition at lower temperature occurs from a metastable gel phase into a liquid-crys talline phase, whereas the high-temperature transition occurs from the stab le quasicrystalline lamellar phase. The thermotropic behavior of DMPC:Ca2complexes is different. The high-temperature transition from the stable sta te is centered at 80 degrees C. Cooling induces a metastable gel phase at l ow temperatures. However, this converts upon heating into the stable gel ph ase at a temperature of 40-50 degrees C, which then melts at 80 degrees C. From the ITC experiments, the binding enthalpies and the change in heat cap acity (Delta c(p),) for the binding reaction was obtained. Delta c(p), has contributions arising from hydrophobic (Delta c(p)(hydrophobic)) and/or hyd rophilic (Delta c(p)(hydrophilic)) hydration or dehydration of the bilayer. The ITC results showed that a similar hydrophobic dehydration of the metas table gel phase was induced in the presence of Mg2+ and Sr2+, whereas Ca2binding leads to a much stronger dehydration of hydrophobic regions. In the stable or metastable Liquid-crystalline phase, this dehydration effect is strongly reduced for all complexes with divalent cations. On the basis of t he DSC and ITC results, enthalpy-temperature diagrams were constructed that illustrate the enthalpies of the different metastable states and the entha lpic changes observed in the DSC and ITC experiments.