Pulsatile Lipid Vesicles under Osmotic Stress

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Pulsatile Lipid Vesicles under Osmotic Stress Morgan Chabanon, James C.S. Ho, Bo Liedberg, Atul N. Parikh, Padmini Rangamani  Biophysical Journal  Volume 112, Issue 8, Pages 1682-1691 (April 2017) DOI: 10.1016/j.bpj.2017.03.018 Copyright © 2017 Biophysical Society Terms and Conditions

Figure 1 Homogeneous GUVs made of POPC with 1 mol % Rho-DPPE exhibit swell-burst cycles when subject to hypotonic conditions. (A) Schematic of a swell-burst cycle of a homogeneous GUV under hypotonic conditions. Dashed blue arrows represent osmotic influx of solvent through the lipid membranes, while solid blue arrows represent the leak-out of the inner solution through the transient pore. (B) Micrographs of a swollen (left), ruptured (middle), and resealed (right) GUV. Scale bars represent 10 μm. Pictures extracted from Movie S1. (C) Typical evolution of a GUV radius with time during swell-burst cycles in 200 mM sucrose hypotonic conditions. The GUV radius increases continuously during swelling phases, and drops abruptly when bursting events occur. Pore opening events are indicated by red triangles. Dashed line represents the estimated initial radius R0. See also Movie S2. More GUV radius measurements are shown in Fig. S1. (D) Experimental area strain ϵexp as a function of time. To see this figure in color, go online. Biophysical Journal 2017 112, 1682-1691DOI: (10.1016/j.bpj.2017.03.018) Copyright © 2017 Biophysical Society Terms and Conditions

Figure 2 Lytic tension is a dynamic quantity governed by thermodynamic fluctuations. (A) The energy required to open a pore of radius r in a GUV without fluctuations, for various membrane tensions. The energetic cost to open a pore in a tense GUV shows a local maximum, which has to be overcome for a pore to open. (B) For a given strain ϵ, the energy barrier is located at a pore radius rb = γ/σ(ϵ) = γ/(κeffϵ) (where κeff = 2 × 10−3 N/m as discussed in the text). (C and E) If the critical strain is fixed at a constant value, ϵ∗, as in the deterministic approach, then a pore is nucleated whenever the strain reaches ϵ∗, regardless of the strain rate. Prescribing various linear strain rates (ϵ=ϵ˙t+ϵ0, with ϵ˙= 10−2, 10−3, and 10−4 s−1, ϵ0 = 0.05) does not alter the strain at which a pore will form (C) and the pore nucleation radius rb will be constant (E). (D and F) In the stochastic approach, however, the nucleation threshold is replaced by a fluctuating pore (blue line in (F) as computed by Eq. 2), inducing a dependence of the lytic strain on the strain rate (D). This is due to the fact that, for lower strain rates, the probability of a large pore fluctuation to reach rb is higher (F), producing a lower lytic tension on average. To see this figure in color, go online. Biophysical Journal 2017 112, 1682-1691DOI: (10.1016/j.bpj.2017.03.018) Copyright © 2017 Biophysical Society Terms and Conditions

Figure 3 Dynamics of swell-burst cycles from the model for a GUV of radius 14 μm in 200 mM hypotonic stress. (A and C) GUV radius and (B and D) pore radius as a function of time. The model captures the dynamics of multiple swell-burst cycles, in particular the decrease of maximum GUV radius and increase of cycle period with cycle number (A). Looking closely at a single pore opening event corresponding to the gray region, the model predicts a three-stage pore dynamics (C and D), namely opening, closing, and resealing, with a characteristic time of a few hundred milliseconds. Numerical reconstruction of the GUV is shown in Movies S3 and S4. Results for R0 = 8 and 20 μm are shown in Fig. S3. To see this figure in color, go online. Biophysical Journal 2017 112, 1682-1691DOI: (10.1016/j.bpj.2017.03.018) Copyright © 2017 Biophysical Society Terms and Conditions

Figure 4 Diffusion of sucrose through a transient pore produces a stepwise decrease of the inner solute concentration. (A) In hypotonic conditions, the model predicts a stepwise decrease of solute concentration differential with time (blue line), which is solely due to diffusion of solute through the transient pore. In comparison, when diffusion is neglected in the model (gray line), the solute concentration differential decreases smoothly (also see Fig. S6 for further analysis on the effect of diffusion). In isotonic conditions (dashed line), the solute concentration differential is constant with time (here t0 = 40 s.) (B) Time evolution of the normalized fluorescence intensity of a GUV in hypotonic condition, encapsulating fluorescent glucose analog. ΔI is the difference in mean intensity between the inside of the GUV and the background. In hypotonic conditions (solid lines) the normalized intensity decreases with time due to the constant influx of water through the membrane, and shows sudden drops in intensity at each pore opening (indicated by arrows), due to diffusion of sucrose through the pore (see Movie S5). In comparison, GUVs in an isotonic environment (dashed lines) exhibit a rather constant fluorescence intensity (see Movie S6). (C) Micrographs of a GUV in hypotonic condition, encapsulating fluorescent glucose analog, just before bursting (left panel), with an open pore (middle panel), and just after pore resealing (right panel). The leakout of fluorescent dye is observed in the middle frame, coinciding with a drop of the GUV radius. Frames were extracted from Movie S7. (D) Same as (C), with the images processed to increase contrast and attenuate noise. The blue, red, and white lines are the isocontours of the 90, 75, and 60 grayscale values, respectively, highlighting the leakout of fluorescent dye. To see this figure in color, go online. Biophysical Journal 2017 112, 1682-1691DOI: (10.1016/j.bpj.2017.03.018) Copyright © 2017 Biophysical Society Terms and Conditions

Figure 5 Cycle period and strain rate are exponential functions of cycle number, and power-law functions of solute concentration. (A and C) Cycle period and (B and D) strain rates as functions of cycle number (n) (A and B) and solute concentration (C and D). Insets show the same data in log scale. Each model point is the mean of 10 numerical experiments; error bars represent mean ± SD. The analytical expressions for the cycle period and strain rate (Eq. 5) with ϵ∗ = 0.15, are plotted in (C and D) for comparison. To see this figure in color, go online. Biophysical Journal 2017 112, 1682-1691DOI: (10.1016/j.bpj.2017.03.018) Copyright © 2017 Biophysical Society Terms and Conditions

Figure 6 The pulsatile dynamics is characterized by the characteristic timescale τ. (A and B) The data from Fig. 5 are scaled by the characteristic time associated with swelling defined as τ. Insets show the same data in log scale. The nondimensionalization by τ allows cycle periods and the strain rates to collapse onto a single curve. (C and D) The analytical expressions for the cycle period and strain rate (Eq. 5) with ϵ∗ = 0.15, are plotted for comparison. To see this figure in color, go online. Biophysical Journal 2017 112, 1682-1691DOI: (10.1016/j.bpj.2017.03.018) Copyright © 2017 Biophysical Society Terms and Conditions