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BIOPHYSICS
Membrane growth can generate a transmembrane pH gradient in fatty acid vesicles
Howard Hughes Medical Institute and Department of Molecular Biology, Massachusetts General Hospital, Boston, MA 02114
Edited by Leslie Orgel, The Salk Institute for Biological Studies, La Jolla, CA, and approved March 22, 2004 (received for review December 4, 2003)
| Abstract |
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In addition to their self-reproducing properties, a major advantage of fatty acid vesicles over phospholipid liposomes as prebiotic membranes is their chemical simplicity. Fatty acids have been found in extraterrestrial samples, such as the Murchison meteorite (9, 10), and can be synthesized under simulated prebiotic conditions (1115). However, a perceived disadvantage of pure fatty acid membranes is that they are highly permeable to protons and are therefore incapable of maintaining pH gradients. Indeed, the addition of a small amount of oleic acid to phospholipid vesicles results in the dissipation of preestablished pH gradients within several seconds (1619).
The mechanism of pH gradient decay in phospholipid vesicles doped with fatty acid is believed to involve incorporation of fatty acid into the membrane, followed by flip-flop of protonated fatty acid molecules and release of protons, thereby equilibrating the pH across the membrane (16, 20). The change of pH inside vesicles can also be used as a surrogate measurement for the change in cation concentration, in situations in which proton flux is electrically counterbalanced by cation flux (21). Cation permeability constants are quite low for model phospholipid membranes. Permeability constants for potassium through pure phosphatidylcholine membranes are typically from 1010 to 1012 cm/s, such that the equilibration of large unilamellar liposomes takes at least several hours (22). However, the flip-flop of fatty acids is much faster, with equilibration occurring within a few seconds (20, 23, 24).
Although previous work on proton and cation permeation has focused on pure phospholipid membranes or phospholipid membranes doped with a small amount of fatty acid, fatty acids themselves form negatively charged vesicles when prepared at a pH close to the pKa of the acid when incorporated into the membrane (2527). Vesicles are initially formed as an aqueous dispersion of fatty acid, with a highly polydisperse size distribution (50 nm to several microns in diameter; ref. 28), which is consistent with the thermodynamics of vesicle systems (29). These preparations can be extruded through small-pore filters to yield vesicles of a defined size (30) that are stable for at least several hours (3, 25). Under these conditions, fatty acid micelles and free molecules are present in equilibrium with vesicles at a concentration equal to the critical aggregate concentration (cac), which is similar to a phase equilibrium (1, 31).
For pure fatty acid vesicles prepared in high buffer concentrations, proton flux driven by a transmembrane pH gradient would soon lead to a significant membrane potential, halting further flux unless cations were moved in the opposite direction (21, 32). To understand the properties of pure fatty acid vesicles with respect to the maintenance and decay of pH gradients, we studied the pathway of proton flux and found that the transmembrane movement of cation-associated fatty acid appears to be the rate determining process in pH gradient decay. We also used an impermeant cation, arginine, to create pure fatty acid vesicles that can maintain a pH gradient for several hours.
The ability of fatty acid vesicles to grow by incorporating additional fatty acid is one of their most interesting dynamic properties from an origin-of-life perspective. Growth can be achieved by the addition of fatty acid micelles, prepared at high pH, to a solution of preformed vesicles buffered at the proper pH. The system is transiently out of equilibrium upon micelle addition but reequilibrates as the fatty acid is incorporated into preformed and de novo vesicles (33). The final vesicle size distribution may depend on the protocol used for micelle addition (2, 3, 28). Growth in these systems has been demonstrated by several methods, including cryotransmission electron microscopy (2), dynamic light scattering (DLS) (34, 35), field flow fractionation with inline multiangle light scattering, and fluorescence resonance energy transfer (FRET) changes in membrane-incorporated dyes (3). The FRET assay relies on the distance-dependent fluorescence of nonexchanging lipid dyes. As membrane area increases, the surface density of the dyes decreases, causing a quantitative decrease in the FRET signal. This assay has been used to specifically measure changes in the surface area of preformed membranes, and it is insensitive to the potentially confounding effects of de novo vesicle formation and the so-called "matrix effect" on vesicle diameter (28).
In fatty acid vesicles capable of maintaining a pH gradient, we found that growth resulted in the creation of a pH gradient, because protonated fatty acid molecules crossed the membrane and released protons into the interior. Our results demonstrate a simple means of capturing some of the energy released during membrane growth. Our results also put strong constraints on the composition of a protocellular system capable of maintaining and using pH gradients.
| Materials and Methods |
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Preparation of Fatty Acid Vesicles. Large unilamellar vesicles were prepared by mixing fatty acid with buffer (0.2 M bicine unless otherwise noted) to obtain the desired pH, typically between 7 and 9. To encapsulate HPTS, 0.5 mM HPTS was included in the resuspension solution. Vesicles labeled with the FRET dyes N-(7-nitrobenz-2-oxa-1,3-diazol-4-yl)-1,2-dihexadecanoyl-sn-glycero-3-phosphoethanolamine (NBD-PE) and lissamine rhodamine B 1,2-dihexadecanoyl-sn-glycero-3-phosphoethanolamine (Rh-DHPE) were prepared by mixing the dyes with fatty acid in methanol, removing the solvent by rotary evaporation, and resuspending in the desired buffer. The pH of buffer solutions was adjusted with the appropriate cation hydroxide. Final fatty acid concentration in the preparation was 80 mM. Preparations were vortexed briefly and mixed end over end overnight under argon. Vesicles were extruded for eleven passes through 100-nm pore filters by using the MiniExtruder system (Avanti Polar Lipids), unless otherwise noted. Vesicles were purified from unencapsulated dye by using a gravity-flow size exclusion column (Sepharose 4B). Myristoleic acid/monomyristolein vesicles were prepared by mixing 0.5 equivalents of neat monomyristolein with fatty acid, and then following the above procedure.
Fatty Acid Micelles. Fatty acid micelles were prepared by using alkali hydroxide as described (3). For stock solutions of oleatearginine micelles, neat fatty acid was added to a 1315% methanol solution containing one equivalent of arginine. This addition was necessary because micelles prepared without methanol formed a gel. The final concentration of methanol in growth reactions was <0.6%. This amount did not affect HPTS fluorescence or cause detectable leakage of encapsulated dye. DLS of oleate-arginine micelles was measured by an ALV/DLS/SLS-5000 compact goniometer system (ALV-GmbH, Langen, Germany) with a CW argon-ion laser and a detection angle of 90°. Data were analyzed by the method of cumulants (36, 37).
pH Measurement. A pH meter (pH-25, Corning) was used to determine the pH of buffer solutions and vesicle solutions during preparation. Encapsulated HPTS was used to monitor internal vesicle pH. HPTS was excited at 402 and 460 nm and the emission was detected at 510 nm. The ratio of these emissions depends on the pH (38), and a standard curve was made by using vesicles prepared at different pH. All fluorescence measurements were performed by using a Cary Eclipse fluorimeter (Varian).
Assay for Surface Area Growth in Vesicles. FRET efficiencies (
) were approximated as 1 Fv/Ft, where Fv is donor fluorescence in vesicles and Ft is donor fluorescence after the addition of 1% Triton X-100 (39, 40). Donor fluorescence was measured at 530 nm with excitation at 430 nm. A standard curve was generated by using known dye concentrations in vesicles.
Stopped-Flow Kinetics. Vesicles were diluted to a concentration between 1.5 and 6 mM and were loaded into a 2.5-ml syringe of the RX-2000 rapid mix accessory to the fluorimeter (Applied Photophysics, Surrey, U.K.). In pH gradient decay experiments, buffer of the appropriate pH was loaded into a 2.5-ml syringe. The observed rate constant (k) of pH gradient decay was used to calculate a permeability coefficient by using the formula P = k(V/S), where V and S are the calculated volume and surface area of a 100-nm diameter vesicle, respectively. In growth experiments, micelles were loaded into a 100-µl syringe in 25-fold excess of the desired final concentration. Stopped-flow mixing was performed according to manufacturer's instructions. Fluorescence data were converted to internal vesicle pH or relative surface area by using the standard curves. Time course curves were fit to first-order exponential decay equations by using nonlinear regression.
Arginine Permeability Assay. A quantity of 3H-arginine (2 µCi; 1 Ci = 37 GBq) was encapsulated by addition to buffer before resuspension with oleic acid. Vesicles were purified from unencapsulated 3H-arginine by size exclusion chromatography (Sepharose 4B). Size exclusion chromatography was repeated at different time points and the radioactivity in encapsulated and unencapsulated fractions was quantified by scintillation counting.
Determination of Cac. Oleate vesicles were prepared by diluting a micelle stock into 0.2 M bicine, pH 8.5. After mixing for 3 h, the turbid solution was serially diluted in the concentration range from 1 µM to 2 mM. The 90° light scattering was measured by a PDDLS/Batch system (Precision Detectors, Bellingham, MA). Scattering intensities at low and high concentrations were log-transformed and were fit to straight lines, and the point of intersection was used to estimate the cac.
| Results |
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Our data for pure fatty acid vesicles are consistent with a mode of cation transport analogous to proton transport by fatty acid flip-flop, in which anionic oleate acts as an ionophore (47). To test this hypothesis, we prepared membranes composed of fatty acids with shorter acyl chains, which should exhibit faster flip-flop and therefore faster cation transport. This finding was verified by using myristoleate and palmitoleate vesicles prepared with K+ (Table 1). This transport pathway avoids the electrostatic barrier to transport of ions by diffusion through the hydrophobic core (48), and it allows fast cation permeation through fatty acid vesicles, relative to model membranes composed of phospholipids, which have flip-flop lifetimes of several hours (49).
We were initially motivated to study the decay of pH gradients in pure fatty acid vesicles because we predicted that vesicle growth would generate a pH gradient. Growth should acidify the vesicle interior because half of the fatty acid that is initially incorporated into the outer leaflet of the membrane must transfer to the inner leaflet. This action presumably occurs through the flip-flop of the protonated acid, which is much faster than the flip-flop of negatively charged oleate (50). Fatty acid added to the inner leaflet would then equilibrate with the vesicle interior, causing acidification (20). This process would store some of the energy released during spontaneous vesicle growth in the form of a pH gradient (Fig. 2).
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6 sec) in oleate vesicles. Arginine slowed the decay to a time scale much longer than growth (t1/2
16 h, Fig. 3A), which agreed with the observed arginine permeability time scale. As expected, no fluorescence changes were observed when oleate-arginine vesicles were mixed with buffer prepared at the same pH. Oleatearginine micelles were examined by DLS, which indicated an average hydrodynamic radius of 1.8 nm, compared with 1.3 nm for Na+-oleate micelles.
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7%). For comparison, oleate-Na+ vesicles show an
70% surface area increase under similar growth conditions. We therefore tested whether oleate-arginine vesicles were for some reason only capable of incorporating a small amount of fatty acid. At a lower buffer concentration, a fixed amount of growth should translate into a larger internal pH drop due to the decreased buffering capacity. However, the same pH drop (
0.3 units) was observed at low (50 mM) and high (0.2 M) bicine buffer concentrations. We also verified that oleate-arginine vesicles are stable over the pH range explored (pH 7.18.3), as shown by size exclusion chromatography of encapsulated HPTS, indicating that acidification did not cause gross destabilization of the membrane.
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In a further search for factors that could limit the growth of oleate-arginine vesicles, we asked whether the state of the added micelles could influence the extent of fatty acid incorporation into preformed membranes. Micelles diluted into an intermediate pH are rapidly transformed into metastable structures, which slowly evolve into vesicles (33). Because the energetically favorable micelle-to-vesicle transition drives growth, the driving force for growth decreases as the micelles are gradually altered in the low pH environment. We hypothesized that if a second aliquot of freshly prepared micelles was added to vesicles that had been previously grown to equilibrium, further vesicle growth should occur. As predicted, further acidification was observed upon addition of fresh micelles (Table 2). Taken together, these results indicate that vesicle growth was not limited by intrinsic properties of the membrane, but rather that growth stops when the "back pressure" of the proton gradient equals the driving force for growth (52, 53).
| Discussion |
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We determined the rate of decay of a pH gradient in the presence of different alkali metal cations. Because large changes in proton concentration were necessary to change the pH of the buffered solution in these experiments, proton flux was effectively limited by cation flux in the opposite direction. The decay of the pH gradient was therefore an indirect measure of the simultaneous decay of the cation gradient. Na+ was found to be most permeable, followed by K+, and Rb+, and Cs+ (Fig. 1B). Alkali metal cations were more permeant to fatty acid vesicles than to phospholipid vesicles by several orders of magnitude. These data are consistent with a pathway in which oleate acts as an ionophore associating with alkali metal ions (47). The affinities of the alkali metal cations for negatively charged phospholipid liposomes follow the trend Na+>K+>Rb+>Cs+ (5557). A higher affinity of Na+ for the fatty acid membrane may result in a greater effective concentration of the cation-ionophore pair, leading to faster cation permeation.
The pathway for cation transport may be written as follows, where subscripts i and o on chemical species denote the volumes on the inside and outside of the vesicle respectively, C+ denotes a cation, and FA denotes a deprotonated fatty acid (e.g., oleate).
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Assuming that pH gradient decay is limited by cation transport, the apparent rate constant (kapp) for pH gradient decay is
. k1/k1 is the association constant of cation and fatty acid, which is affected by the identity of the cation. The fatty acid chain length affects k2, because short chains should allow faster flip-flop, as observed. This mechanism maintains mass balance of the inner and outer leaflets during pH gradient decay, avoiding the need to invoke transmembrane movement of charged oleate anions. Because the concentration of ionized fatty acid on the inner leaflet,
, is itself a function of the internal pH, kapp may be expected to change during the course of pH gradient decay. Our failure to observe a significant departure from single-exponential decay of the pH gradient may simply reflect the noise in our experimental data, but could also reflect a degree of cooperativity in the ionization of lamellar phase fatty acid, which would limit changes in
over the measured pH range (27).
We studied the generation of a transmembrane pH gradient during growth by using oleate-arginine vesicles (Fig. 2), because pH gradients across oleate-arginine vesicles did not decay significantly on the experimental time scale. We observed the expected acidification of vesicle interiors upon addition of oleate micelles to preformed vesicles, but the surface area increase of oleate-arginine vesicles was significantly less than that of oleate-Na+ vesicles. The pH drop itself limited further gradient formation, and when an opposing pH gradient was experimentally imposed, we were able to significantly increase the magnitude of the pH drop. By using an assay based on FRET between two lipid-incorporated probes, we verified that an increase in vesicle surface area (i.e., membrane growth) occurs simultaneously with and at the same rate as the pH drop.
The conversion of micelles to vesicles is exergonic, and some of this energy was transduced into a transmembrane pH gradient. To estimate the efficiency of this conversion, the free energy of the micelle to vesicle transition was estimated from the cac of oleic acid in our system (82 µM, Fig. 4), by using a phase transition model for micelle-vesicle equilibrium at large aggregation numbers. The standard free energy released per mole of oleate converted from micelles to vesicles is given by
RTln(cac), in which the cac is given in units of mol fraction (58, 59). The factor of 1.5 is an adjustment for the difference in the degree of ionization between micelles and vesicles, assuming that one-half equivalent of cations is released during the transition from micelles to vesicles (31). For the addition of 1.5 mM micelles,
Gtransition =11 kJ/mol. Given the size of the vesicle (100 nm diameter) and the approximate amount of growth, we estimated that 1.9 x 1016 J are released per vesicle during growth.
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Ggradient = 2.3 RT(
pH) =1.7 kJ/mol. The titration of 0.2 M bicine from pH 8 to 7.7 requires the addition of 25 mM H+. Given the volume of a vesicle, 2.2 x 1017 J are stored in the pH gradient per vesicle. Thus, the overall efficiency of energy transfer from the micelle to vesicle transition into the pH gradient was
12%. Part of this energetic loss is a necessary consequence of the process of growth. Approximately half of the fatty acid molecules incorporated into a preformed vesicle will be incorporated into the inner leaflet. Of these, approximately half will dissociate to produce a proton and the corresponding anion, because the solution is near the pKa of the membrane-incorporated fatty acid. Given these losses, the theoretical maximum efficiency for the conversion of energy into the pH gradient would be 25%. The remainder of the energy loss may be due to several factors, including the fast relaxation of micelles into metastable structures and entropic increases resulting from alterations in the structure of water surrounding the micelle or vesicle. The observed energy efficiency is similar to that of other energy transduction systems based on pH gradients (52); for example, the energy efficiency of photosynthetic conversion of absorbed red light into reduced carbon is 34% (60). In comparison with these systems, however, energy transduction is achieved in oleate-arginine vesicles with only a few chemical components, namely oleate and a buffer by using an impermeant cation.
This simple chemical system demonstrates energy storage in the form of a pH gradient created by spontaneous vesicle growth. In a prebiotic context, growing vesicles might gain a selective advantage if the gradient could be used to drive other useful processes, such as uptake of metabolically useful amines (61). From a systems perspective, this process may couple growth of one protocellular component, the membrane, to the growth of other components that are able to use the stored energy. These studies also emphasize that the maintenance of a substantial transmembrane pH gradient in fatty acid vesicles is contingent on a membrane with low cation permeability. To use the energy released during membrane growth, early protocells using fatty acid membranes would have had to exist in the absence of a substantial concentration of alkali cations, which seems unlikely. Therefore, the ability to use energy stored in pH gradients may not have been possible until the evolution of membranes composed of less permeable membrane components, such as phosphate or glycerol esters, and with relatively low steady-state levels of free fatty acids.
Finally, our observation that the development of an internally acidic pH gradient is strongly inhibitory to further membrane growth suggests that the evolution of less permeable membranes may have required the coevolution of ionophores to relax the inhibitory pH gradient. Further advantage may have been obtained through the evolution of a proton "pump," requiring energetic input, that could generate an alkaline vesicle interior to increase the rate of membrane growth (61, 62). Such a pump, running in reverse, could have been co-opted later as part of a mechanism to couple a transmembrane gradient to the formation of energy-rich bonds.
| Acknowledgements |
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| Footnotes |
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Abbreviations: DLS, dynamic light scattering; FRET, fluorescence resonance energy transfer; HPTS, 8-hydroxypyrene-1,3,6-trisulfonic acid; cac, critical aggregate concentration.
* To whom correspondence should be addressed. E-mail: szostak{at}molbio.mgh.harvard.edu.
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