Rachel Joanne
Goodband‡
and
Margarita
Staykova
*
Department of Physics, Durham University, South Rd, DH1 3LE, Durham, UK. E-mail: margarita.staykova@durham.ac.uk
First published on 4th February 2025
Most studies on pore formation in lipid membranes focus on lipid vesicles under isotropic tension. These models however fail to replicate the anisotropic stresses encountered by living cells and the complex rheological properties of the cell membrane arising from its interactions with the underlying cytoskeleton. Here, we employ a custom-built device to impose uniaxial stretch on PDMS-supported lipid membranes. We show that in contrast to the circular pores in vesicles, supported membranes under uniaxial loading open elliptical pores that are aligned perpendicularly to the direction of stretch. We discuss the constraints on tension diffusion in supported membranes, and how tension distribution determines the density and the shape of the membrane pores in relation to the applied strain rate and strain magnitude. Our paper shows for the first time that lipid membranes can exhibit a fracture behavior similar to the fracture of soft gels under tensile loading.
Membrane rupture of substrate-supported lipid bilayers (SLBs) differs significantly from that in vesicles. We argue that SLB models are a more realistic biomimetic model for studying response to tension because they capture the frictional interaction of the cell membrane to other structures (cyoskeleton, protein anchors) and reflect its obstructed dynamics. SLBs have been successfully used to explain the formation of noncircular pores in adhering cells.10 When spreading on solid substrates with low density of pinning points, both cellular and artifical membranes develop floral pores due to growing membrane fingering instabilities.10–13 In contrast, spreading on substrates with high pinning points density induces a fractal membrane rupture behvaiour, consistent with invasion percolation in disordered media.10,12
In this work, we set out to explore the fracture behavior of lipid membranes under anisotropic stretch. We take advantage of our previous work on coupling membranes to deformable polydimethylsiloxane (PDMS) which have examined the membrane area regulation under stretch and compression.14,15 Here we develop a simple PDMS stretching device that can deliver uni-directional stretch on SLBs. To our surprise, we find that SLBs open elliptical pores oriented perpendicularly to the stretch direction, contrasting with simulations that predict circular pores in unsupported membranes under uniaxial stretch.16,17 These elliptical pores suggest a previously undiscussed analogy between membrane poration and the fracture mechanisms of soft gels under tensile loading.
Elsewhere, we have shown that the deformation of the PDMS substrate induces a stretch on the SLB via a frictional coupling.14,15 The coupling between the PDMS substrate and the lipid bilayer depends on the hydrophobicity of the PDMS substrate, which can be controlled by the duration of plasma exposure prior to vesicle fusion. In these experiments, we use a longer plasma exposure and hydrophilic PDMS substrates onto which the lipid mobility is retained, albeit significantly restricted due to the friction with the substrate.15
To characterise the membrane strain due to the PDMS subtrate deformation we track the distance between small membrane defects, usually unfused vesicles. We label the membrane strains along and perpendicular to the directions of the PDMS stretch as longitudinal strain (ε‖) and lateral strain (ε⊥), respectively (Fig. 1a). Fig. 1b shows thatthe membrane strain closely follow the PDMS strain; ε‖ increases continuously to 10–15% throughout the operation of the pump, while the lateral strain, ε⊥, decreases slightly by 1–2%.
We note that the strain rate and strain magnitude may differ slightly across devices, even when we apply the same pump settings. This variation is mainly due to differences in the thickness of the PDMS sheet and how it is deposited on the acrylic post. To account for this, we continuously image the bilayers while they are being stretched and compare their response either at a fixed strain magnitude or for a fixed pore size.
All pores initially appear as circles but as the strain increases, they elongate more rapidly in the direction perpendicular to the applied stretch (Fig. 2a). This can be seen by the increase in their aspect ratio with strain (Fig. 2a and c). Interestingly, pores that open later grow perpendicular to the stretch but very little along it. At the end of the stretch process, there is a clear correlation between the time a pore opens, its size and aspect ratio (Fig. 2d). In general, the later a pore opens, the smaller its final area and the larger its aspect ratio. This dependence is also observed for other samples stretched at different strain rates (ESI,† Fig. S3).
Fig. 3a shows images of membrane samples stretched at slow, medium and fast strain rates. The corresponding movies are shown in the ESI,† Movies S1–S3. The membrane strain determined by tracking immobile defects on these bilayers is 12% (slow), 12% (medium) and 15% (fast). The percentage of combined pore area vs. total area is 11.7%, 12.15% and 15.2%, respectively. The close mapping between pore area and membrane strain for all samples indicates that (1) the dominant mechanism for membrane tension release is pore formation, and (2) the extent of membrane rupture, i.e. the total fracture area depends only on the stretch magnitude, and not on the strain rate. Strain rate however clearly affects the way SLBs rupture, as seen from the differences in the pore size and the pore number density between the samples on Fig. 3a.
Membranes stretched at slower rates appear to have fewer and much larger pores compared to higher strain rate samples (Fig. 3b). The large variation within and between samples at slow strain rate, can be attributed to the relatively small number of pores, and to the larger effect that late pores have on the average pore size distribution. Despite the large error bars, there is a clear statistical difference between the mean pore sizes as a function of strain rate, verified using 5% significance level t-test.
In conjunction with pore area, strain rate affects the inter-pore distance (Fig. 3c). Our experiments show that higher strain rate results in higher density of smaller pores, in agreement with previous experiments on membrane patches subjected to bi-axial stretch.15 The decrease in inter-pore distance with strain rate can be fitted with a power-law function. Fig. 3c shows two fits to the data: one with a fixed power of −0.5, and another with a free power (see Discussion for more information). The best-fit power law was y = 7.13x−0.335, with a standard error of regression of 2.46 μm and the best fit using a function with a fixed power of −0.5 was y = 4.02x−0.5, with a standard error of regression of 2.93 μm.
We then look at whether the strain rate has an effect on the shape of the pores. As discussed previously, the aspect ratio of individual pores depends on the applied strain magnitude, and on when in the stretch process a pore appears (Fig. 2c and d). Therefore to compare pore shape across samples, we select only early pores and measure their aspect ratio for a fixed pore area of 10 μm2. This small reference pore size is set by the maximum pore size reached in the high strain rate samples. With these considerations, our results show that the strain rate does not affect the aspect ratio of pores (Fig. 3c) using a 5% significance level t-test. In other words, fast strain rates do not lead to more elongated pores. It must be noted however that at this small reference pore size, pore asymmetry is in general small and the measurement uncertainty high, which puts our conclusion under question.
Tension-driven lipid flows in supported lipid bilayers and in biological membranes underlined by the cell cytoskeleton are shown to be opposed both by viscous and friction forces.8,11 The ratio between the viscosity of the bilayer (μ) and the membrane sliding friction with the substrate (ζ) defines a characteristic length-scale, , which indicates the relative significance of these forces in lipid flows. Large scale flows on length scale exceeding L, are limited by the friction of the membrane with the supporting substrate, whereas local lipid rearrangement is governed by viscous forces. Taking literature values for μ ≈ 1 × 10−10 Pa m s (ref. 21) and ζ ≈ 1 × 108 Pa s m−1 (ref. 15,22) we obtain a value of L in the range of a few tens of nanometers, which falls within the length-scale relevant for pore formation. We therefore expect that small-scale lipid rearrangement in the vicinity of growing pores will be governed mostly by viscous forces, whereas the larger scale lipid dynamics, which sets the pore size and inter-pore distance will predominantly depend on the membrane-substrate sliding friction.
In our experiments, we apply gradually increasing uniaxial strain to lipid bilayers by stretching the underlying membrane support. As a result, the tension in the bilayer increases and once it reaches a critical value (usually at 1–2% strain), the bilayer opens pores to release its tension (Fig. 2a and b). The growth of pores with increasing membrane strain is opposed by viscous and frictional drag forces, which lead to further accumulation of membrane tension and opening of new (‘late’) pores (Fig. 2b). In contrast to vesicle systems, pores in SLBs can have irregular shape10,11 and can stay open for a long time15 (ESI,† Fig. S2), even if the membrane tension is low. This is due to the strong frictional coupling between the membrane and the substrate, which effectively counteracts the edge tension acting to minimise the pore perimeter. Previous studies have presented scaling arguments that support these observations.10,11
The density of pores on the SLB, and the inter-pore distance respectively, R, depend on the rates of tension increase and tension dissipation as , where K [J m−2] is the membrane elastic modulus, ζ is the friction coefficient, and
[s−1] is the applied strain rate.8,15R can also be understood as the distance over which a pore reduces the membrane tension in its vicinity. Higher strain rates correspond to shorter times for lipid relaxational flow, hence shorter R. As a result, SLBs stretched at higher rates exhibit a higher density of smaller pores. Fig. 3c confirms the expected square-root dependence between inter-pore distance and strain rate. The deviation of the perfect fit from the predicted powerlaw of −½ can be ascribed to a non-homogeneous pore distribution (Fig. 3a), possibly arising from pre-existing membrane and substrate defects that lower the threshold for pore nucleation.
All pores initially have a circular shape but quickly transform into ellipsoids as they grow faster in the direction perpendicular to the applied stretch (Fig. 2a). Although such behavior has not been observed, nor predicted16,17 for fluid bilayers, it has been well characterised in the context of elastic fracture mechanics in solid materials. Defects and cracks in solid materials induce inhomogeneities in the stress field, with stress concentrating at the crack tip. Stress concentration may lead to spontaneous crack propagation and material failure in solids at much smaller tensile loads.23 Similarly, tension in the bilayer is amplified at the lateral sides of the pores (Fig. 4a) causing them to grow into ellipsoids oriented perpendicular to the strain direction.
![]() | ||
Fig. 4 (a) Schematic drawing of the tension distribution in the membrane, with dark shades of grey indicating stress concentration at the tip of the pores. R corresponds to the tension diffusion length. (b) Microscopic images of a supported lipid bilayer patch made of DOPC lipids before and after the stretch. Full video in ESI.† The red box shows the dimensions of the sample achieved after the stretch. (c) Image of membrane pores with viscoelastic trumpet shapes. Scale bar is 20 μm. (d) Viscoelastic trumpet structure characteristic of the failure behaviour of materials with rate dependent properties. The tip of the crack is characterised by large tension, high elastic modulus (K), and a sharp crack propagation. Away from the pore tip, membrane behaves as a deformable material with lower elastic modulus, K*. |
A close examination of the membrane pore profile reveals a combination of responses and a complex membrane rheology. Most membrane pores, especially the early ones, exhibit a wide ellipsoidal profile (relatively small aspect ratio), characteristic for the fracture of soft elastic solids, such as rubber or gels.20,24,25 We suggest that the apparent softness of the otherwise inextensible membrane stems from tension relaxational flows within the membrane plane. Such flows have been previously visualised in isolated SLB patches that simultaneously slide and form pores in response to substrate deformation.15 Tracking the edge of the patches under uni-axial stretch reveals that they elongate in the direction of the stretch, at the expense of an incoming flow of lipids from the sides (Fig. 4b and ESI,† Movie S4). But the membrane pores are not completely ellipsoidal. At the tip of the pores, we see a much narrower crack profile that characterises the fracture behaviour of stiff materials (Fig. 4c and d). Such pore profiles, called ‘visco-elastic trumpets’20 have been described in visco-elastic solids, and reflect different strain rates and different material responses around the crack. At the sides of the pore (facing the stretch direction), the membrane responds as a soft deformable material with effectively lower elastic modulus, K* due to creep flows. At the tip however, the speed of the pore propagation and the strain rate are highest, and the membrane behaves elastically with its high elastic modulus (K). Interestingly, pores that open later in the stretch process have a much narrower opening profile and a higher aspect ratio (Fig. 2c and d). This suggests that the capacity of the SLB for large-scale relaxational flow may be exhausted as the stretch progresses.
Our data do not show a significant correlation between the mean aspect ratio of the pores and the rate of stretching applied to the membrane (Fig. 3d). Moreover, we observe trumpet-shaped pores at all strain rates (Fig. 3a). Previous analysis of cracks in visco-elastic materials has argued that trumpet shapes appear at rates of crack propagation comparable to the relaxation rate of the visco-elastic material.20 In our membrane experiments however, a fast strain rate becomes compensated by a larger density of pores and not by faster pore growth rate.
Our results on the gel-like fracture of supported lipid membranes agree with previous research showing that cell membranes behave more like a semi-solid gel than a viscous fluid.8,9 These studies reported a very slow tension equilibration on the cell surface, caused by membrane-cytoskeleton attachments hindering the lipid flow. In relation to cell membrane rupture and healing, our study implies that the shape of the pores in cells will strongly depend on the local distribution of the membrane tensile stress, and that edge tension will have little effect on the pore shape and its closure. It remains to be studied whether the irregularity of pore perimeter and the variation in the pore edge curvature may control the pore closure process by facilitating protein and lipid recruitment.1,2
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4sm01410c |
‡ Present address: Department of Mechanical and Manufacturing Engineering, School of Engineering, Trinity College Dublin, Ireland. E-mail: goodbanr@tcd.ie |
This journal is © The Royal Society of Chemistry 2025 |