Temperature, pressure and cholesterol effects on bilayer fluidity; a comparison of pyrene excimer/monomer ratios with the steady-state fluorescence polarization of diphenylhexatriene in liposomes and microsomes.

Pyrene excimer/monomer (E/M) ratios have been compared with the steady-state fluorescence polarization (P) of diphenylhexatriene (DPH) in multilamellar liposomes of dilaurylphosphatidylcholine and rat liver microsomes. The purpose was to use the well-understood properties of DPH to reveal the nature of bilayer fluidity which pyrene manifests as an E/M ratio. Reducing the temperature (from 37 degrees C to 8 degrees C), increasing the hydrostatic pressure (from 0.1 to 70 MPa), and, in liposomes, cholesterol enrichment (up to 0.30 mole fraction) separately decreased the E/M ratios and increased P. The pyrene membrane/buffer partition coefficient was affected by temperature but not by pressure, and in the case of cholesterol enrichment, it was assumed to be unaffected. Plots of P as a function of the E/M ratio showed the two to be closely correlated (r = 0.99 in liposomes and 0.96 in microsomes), independent of the treatment used to reduce fluidity. The apparent activation volume and enthalpy for excimer formation was calculated and compared with published data. Pyrene E/M ratios probably reflect the intermolecular volume (fluidity) of the outer region of the bilayer, which is reduced by a decrease in temperature and an increase in pressure and cholesterol. DPH reports the bilayer interior, which is similarly ordered by the experimental treatments. The regional distinction between the two probes, however, accounts for the divergence of E/M ratios and P, which has been reported in membranes enriched with fluidizing fatty acids.

Homeoviscous adaptation under pressure: the pressure dependence of membrane order in brain myelin membranes of deep-sea fish.

Steady-state and time-resolved anistropy of 1,6-diphenyl-1,3,5-hexatriene (DPH) fluorescence have been used to compare the hydrocarbon order of brain myelin membranes from a shallow water (plaice) and two deep-sea fish species (Coryphenoides rupestris and Coryphenoides armatus). At atmospheric pressure the deep sea fish displayed lower steady-state anisotropies than shallow water species although the pressure dependence of anisotropy was similar in all species. Time-resolved measurements allowed the separate determination of the rate of probe motion from the amplitude of that motion. Anisotropy decays were analysed in terms of two correlation times and a constant (r infinity). The r infinity and mean value of P2 order parameter for all species increased with pressure, the graphs for deep-sea species being translated to higher pressures relative to shallow-water species. The resulting pressure coefficients for C. armatus was distinctly less than for the two shallower species. These time-resolved studies show that the interspecific differences provide for similar order parameters in all three species when corrected to their respective habitat conditions of pressure and temperature. This indicates that myelin order is highly conserved despite the profound ordering effects of high hydrostatic pressure.