Significance
Long-range fluid flows are crucial for the functioning of many organisms, as they provide forcing for migration and development and spread resources and signals. How flows can span vastly different scales is unclear. Here, we develop a minimal, two-component model, coupling the mechanics of a cell’s cortex to a contraction-triggering chemical. The chemical itself is spread with the fluid flows that arise due to the cortex contractions. Through theoretical and numerical analysis, we find that the oscillatory component of the flows can give rise to robust scaling of contraction waves with system size—much beyond predicted length scales. This mechanism is likely to work in a broad class of systems.
Keywords: active matter, pattern formation, fluid mechanics
Abstract
Flows over remarkably long distances are crucial to the functioning of many organisms, across all kingdoms of life. Coordinated flows are fundamental to power deformations, required for migration or development, or to spread resources and signals. A ubiquitous mechanism to generate flows, particularly prominent in animals and amoebas, is actomyosin cortex-driven mechanical deformations that pump the fluid enclosed by the cortex. However, it is unclear how cortex dynamics can self-organize to give rise to coordinated flows across the largely varying scales of biological systems. Here, we develop a mechanochemical model of actomyosin cortex mechanics coupled to a contraction-triggering, soluble chemical. The chemical itself is advected with the flows generated by the cortex-driven deformations of the tubular-shaped cell. The theoretical model predicts a dynamic instability giving rise to stable patterns of cortex contraction waves and oscillatory flows. Surprisingly, simulated patterns extend beyond the intrinsic length scale of the dynamic instability—scaling with system size instead. Patterns appear randomly but can be robustly generated in a growing system or by flow-generating boundary conditions. We identify oscillatory flows as the key for the scaling of contraction waves with system size. Our work shows the importance of active flows in biophysical models of patterning, not only as a regulating input or an emergent output, but also as a full part of a self-organized machinery. Contractions and fluid flows are observed in all kinds of organisms, so this concept is likely to be relevant for a broad class of systems.
Fluid flows are fundamental to the functioning of all organisms. They play an important role in homeostasis, by spreading resources and biochemical signals (1–3). They power deformations driving migration of many motile cells (4–6) and can even directly impact organism size (7). Surprisingly, even in the absence of a pacemaker like a heart, flows are coordinated on vastly different scales ranging from the size of a single migrating cell of about 20 m (8, 9), via the Caenorhabditis elegans gonad of about 450 m (10, 11), to the Drosophila embryos of about 500 m (12), to acellular slime molds of more than 2 cm in size (13). The physical mechanism of how coordinated flows can self-organize particularly in a single cellular envelope remains unknown.
Animal and slime mold cells are lined with an actomyosin cortex situated just below their cellular envelope, enclosing the cells’ fluid cytoplasm. This actomyosin meshwork forms an active viscoelastic material (14, 15). It contracts under myosin motor activity and thereby drives the enclosed cytoplasm to flow into a less contracted part of the cell (1, 16). Long-range flows adapting to system size therefore require a spatial organization of cortex contractility. The mechanism driving the coordination of cortex contraction across a cell or an organism is unclear.
Already in the early 1980s Oster and Odell (17, 18) explored the idea that a contraction-triggering chemical, like calcium, could explain dynamic, oscillatory patterns of actomyosin activity in the cell cortex. However, the dynamic patterns’ spatial component was not investigated. Calcium is necessary to generate actomyosin contractions in many biological systems (19–22). Additionally, calcium is regulated by mechanical stretching, via mechanosensitive channels (23–26). Consequently, cortex expansion triggers the influx of calcium which in turn leads to contraction. Due to the widespread importance of cortex activity in developmental processes, this feedback is of general interest, investigated in mechanochemical models (27). Models describing the cortex as a fluid (28) or as a poroelastic medium (29), where active stress is up-regulated by a chemical immersed in this medium, account for short-range traveling waves of contractions and oscillatory flows. However, the mechanistic insight is missing that can account for coordination of contractions on scales beyond the intrinsic length scale of the dynamic system and thus account for very long-range fluid flows scaling with system size.
Particularly, the slime mold Physarum polycephalum is renowned for long-range coordination of cortex contractions. Here, fluid flows scale with organism size from 2 mm to at least 2 cm (13). Again, flows are known to power organism migration (6, 30). Moreover, stimulants that alter cortex contractility have recently been found to be advected with the fluid flows inside the cell (2). This observation suggests that the physical transport by fluid flows is the key to long-range spatial coordination of cortex contractions and fluid flows.
Here, we investigate in a tubular geometry the self-organization of cortex contractions, coupled to a contraction-triggering chemical which is advected with the flows of the fluid cytoplasm. The simple two-component model is unstable toward self-sustained cortex oscillations as cortex stretching triggers the increase of the contraction-triggering chemical concentration. A linear analysis of the model predicts traveling-wave solutions of cortex shape and the intrinsic wavelength of the dynamic instability is derived. In contrast to our analytic prediction, numerical solutions of the model in a tube with periodic boundaries show a probabilistic distribution of five different patterns of traveling waves. Although the tube is twice as long as the expected intrinsic wavelength, in one of these patterns the traveling wave scales with tube length. Further analysis shows that scaling can be robustly generated in growing tubes with periodic boundary conditions or by flow-generating boundary conditions in nongrowing tubes. We identify oscillatory flows as the key to the scaling of contraction waves with system size. The ubiquity of fluid flows in biological and nonliving systems suggests that this nontrivial scaling could be broadly relevant in active matter.
Results
Coupling of Tubular-Shaped Cortex with Contraction-Triggering Chemical.
A cell showing coordinated cytoplasmic fluid flows in general has a distinctive viscous fluid phase separated from a surrounding viscoelastic actomyosin cortex. The nature of long-range flows typically entails a tubular cell shape. We here consider as a minimal model an active, viscoelastic tube of length , filled with a fluid. Tube shape is fully defined by the tube’s radius along the tube’s axial position and over time . The tube’s temporal evolution directly follows from the conservation of the fluid volume within the tube,
| [1] |
where denotes the cross-sectionally averaged fluid flow velocity along the tube. Fluid flow is powered by contractions of the tube and thus by the stress acting radially within the tube’s cross-section (Fig. 1). We distinguish , the contractile stress stemming from actomyosin activity within the cortex, and , the counteracting viscoelastic restoring stress of the cell. For long slender tubes, , lubrication approximation applies. The Stokes equation for the fluid velocity simplifies to
| [2] |
where denotes the dynamic viscosity of the fluid. We approximate the cell’s material properties to be dominated by a linear viscoelastic response following a Kelvin–Voigt model with a small nonlinearity to suppress potential divergences. Abbreviating radial deformation as with respect to the constant equilibrium radius , the restoring stress is given by
| [3] |
where and denote the tube’s effective elastic modulus and viscosity, respectively, and is the strength of the nonlinear response. Note that and incorporate both the elastic properties and the thickness of the cell cortex.
Fig. 1.
Illustration of the model predicting self-sustained contraction waves. (A) A tubular-shaped cell lined with an actomyosin cortex (blue) enclosing the liquid cytoplasm carrying a contraction-triggering chemical (orange). Chemically controlled contractile cortex stress is balanced by viscoelastic restoring stress. Small cortex contractions self-amplify as more actin overlaps in a contracted cortex, shown in variations in cortex density. Cortex stretch leads to inflow of contraction-triggering chemical, allowing for self-sustained oscillations. Contractions are coupled spatially as the chemical is advected with the cytoplasmic flows (parabolic lines) resulting from cortex deformations. (B) Phase diagram depicting a region of uniform, stationary pattern and oscillatory patterns.
In light of the role of calcium in coordinating actomyosin activity, we describe the strength of the cortex contractile stress to be proportional to the concentration of a contraction-triggering chemical . In addition, contractions may self-amplify as more actin fibers overlap in a contracted cortex following observations for low myosin concentrations typical for nonmuscle cells (31, 32). Inversely, overlap decreases in an expanded cortex, reducing potential contractility. Consequently, the contractile stress is represented by
| [4] |
Here, represents the chemical concentration integrated across the cross-section of the cell, is the equilibrium concentration, describes the active tension at equilibrium, and is the typical deformation for the change in fiber overlap to become significant for contractility. The chemical itself constantly cycles between an inactive state and an active state in the cytoplasm with release rate and capture rate . We assume the amount of inactive chemical to be abundant and therefore not limiting the dynamics here. Importantly, motivated by our knowledge of calcium regulation by mechanical deformations (23–26), additional chemical is released at the cell’s membrane upon cortex stretch with denoting the corresponding typical deformation scale. Now, we further incorporate spatial coupling as we account for the advection and diffusion of the contraction-triggering chemical. Reflecting the tubular cell shape we assume the chemical to average out quickly across the tube’s cross-section by diffusion, with diffusivity , compared with the advective transport with velocity along the tube of length , . This assumption warrants the use of Taylor dispersion for a tube of varying radius (33),
| [5] |
Here, the factor in the kinetics term stems from chemical release at the surface of the tube. Note, that chemical release in the bulk, i.e., a factor of instead, does not alter the model’s dynamics described below (SI Appendix, Linear Stability Analysis).
Stretch-Activated Chemical Inflow Controls Self-Sustained Oscillations.
At zero fluid flow the tube’s radius is uniformly at its rest value of . Similarly, the chemical concentration is at a constant value of throughout the tube. This uniform state is unstable with respect to small perturbations as a small deformation of the tube radius grows when the contractile stress of scale exceeds restoring stress (Fig. 1B). Thus, the relative stretch parameterized by drives the short wave instability of the system. A stretched cortex additionally ignites the inflow of the contraction-triggering chemical. Chemical inflow results in contractions, thus decreasing the deformation and initiating the oscillation. Consistent with this intuitive reasoning, linear stability analysis shows that the uniform state is unstable if is large enough compared with the tube’s elastic modulus , diffusion , and capture rate , all factors limiting the development of fluctuations,
| [6] |
(SI Appendix, Instability Condition). The wavelength of the most unstable mode is given by
| [7] |
The scale of coordinated flows set by this intrinsic wavelength here arises from the competition between diffusion and viscosity , increasing the wavelength by filtering out perturbations on a short scale, and contractility, amplifying the fluctuations locally and controlled essentially by . Approximating , the linear analysis also gives a constraint for an oscillatory instability
| [8] |
(Fig. 1B). The oscillation frequency can be derived (SI Appendix, Eq. S1). The result confirms the intuitive idea that oscillations occur if the stretch-activated chemical release, controlled by , is strong enough to counterbalance the self-amplifying deformation of the tube. Based on these analytical results we expect the system to generate spontaneous contractile waves of a wave size given by the most unstable mode .
Multiple Patterns of Contractions Arise in a Periodic Tube.
To study the self-organization of contractile waves in organisms of varying sizes, we numerically solve model Eqs. 1 and 5 in tubes of different lengths and measure the sizes of the contractile wave patterns (Fig. 2). As model parameters, we choose physiological values for calcium kinetics and actomyosin cortex mechanics (Materials and Methods). Tube radius is chosen to match P. polycephalum—most renowned for scaling contraction waves. The model is further verified by comparing the numerically observed phase relationship between fluid flow and contraction-triggering chemical to experimental data of P. polycephalum (34). The model predicts the nontrivial change of phase relationship along the tube (SI Appendix, Fig. S3), robust against changes in model parameters. Among ambiguous observations on the role of calcium in P. polycephalum (35, 36), complemented by theoretical models (37), this experimental verification of our model promotes that calcium activates actin–myosin contractions in P. polycephalum as is common in living organisms.
Fig. 2.
Contraction wave can scale with tube length. (A and B) Size of self-sustained contraction waves for tubes of different lengths , for closed (A) and periodic (B) boundary conditions. Linear stability analysis predicts wave size to be bound by the intrinsic wavelength of the most unstable mode (dotted line) as observed numerically for a closed tube. However, wave size can scale with tube length (arrows in B) for periodic boundary conditions. Each data point denotes an individual simulation.
To determine the size of the waves, we computed the power spectral density of the radius averaged over 10 oscillation periods and identified the dominant mode. As “wave size” we denote the inverse of the dominant mode. Note that wave size is not always equivalent to wavelength, in particular if the patterns are antisymmetric (see Fig. 3 B and E, for examples of patterns with different wavelength and equal wave size). Simulations with closed boundary conditions (Fig. 2A) fully match our expectations from linear stability analysis, namely waves increasing with tube length up to an upper bound given by the intrinsic wavelength corresponding to the most unstable mode . Surprisingly, in simulations with periodic boundary conditions (Fig. 2B) we observe waves exceeding , scaling with tube length instead.
Fig. 3.
Stable wave patterns in a periodic tube twice as large as the intrinsic wavelength . (A–E) Tube radius (Top) and resulting fluid flow rate (Bottom) along a tube (horizontal axis) and time (vertical axis). Probability of each pattern in 300 independent runs is denoted above the radius plots.
Characterizing more precisely the variety of wave patterns, we screen multiple runs with different initial perturbations, for the intermediate tube length , with periodic boundary conditions (Fig. 3 and SI Appendix, Fig. S2). Observed wave patterns can be divided into five cases, by wave size and period-averaged flow rate along the tube (see SI Appendix, Fig. S6 for details on the identification of the patterns). There are one, two, or three waves traveling in the same direction (Fig. 3 A, B, or C, respectively), two antisymmetric waves (Fig. 3E), or two asymmetric waves (Fig. 3D). The single wave matching tube length (Fig. 3A) generates the strongest net fluid flow, exceeding unidirectional multiple wave patterns (Fig. 3 B and C) and asymmetric waves (Fig. 3D). Patterns with antisymmetric waves (Fig. 3E) do not create a net flow due to their invariance under space flipping, thus not providing any mass transport or long-range mixing. Patterns occur with very different probabilities with only 12% showing the most efficient pattern regarding mixing and transport, where the wave scales with tube length. In general, net flow and maximum flow increase with wave size (38) (SI Appendix, Fig. S5), and thus generating waves scaling with system size is fundamental for organisms whose size varies vastly. What measures can make this most efficient pattern more robust? What mechanism drives the scaling of the contractions with the size of the tube?
Growth of the Tube Leads to the Robust Scaling of the Wave.
To investigate robustness and the mechanism behind the scaling of contractile waves we performed simulations of growing tubes and measured wave size for periodic or closed boundaries (Fig. 4). Tubes grow linearly, starting from in length.
Fig. 4.
Scaling of the contraction wave in growing, periodic tubes. Shown is wave size for tubes with periodic (blue circles) and closed (red diamonds) boundaries, grown to different lengths . While wave size in closed tubes saturates at (dotted line) as predicted from linear stability analysis, waves in tubes with periodic boundaries scale robustly with tube length up to sevenfold the predicted length (blue vertical line). Each data point represents an independent run of a tube grown from an initial .
In agreement with linear stability analysis we find that waves in tubes with closed boundaries grow with tube length only up to the upper bound . However, for periodic boundary conditions, waves scale with the length of the tube up to sevenfold (Fig. 4). From linear stability analysis the wavelength is an unstable but not oscillating state (SI Appendix, Fig. S1), suggesting another mechanism beyond linear stability analysis at play. Above this limit to the scaling , the wave splits into six or seven smaller waves matching roughly (Fig. 4). Note that while the wave size scales with system size, the period of contractions barely changes (SI Appendix, Fig. S5), in accordance with observations (39). Results are robust against variations in parameters. Particularly, changing the fluid viscosity varies the scaling limit and the factor of mode multiplication . Contrary to previous reaction–diffusion systems capable of mode doubling or tripling when simulated on growing domains (40), many values of are accessible; see SI Appendix, Fig. S7 for . From Eq. 7, we can see that the predicted wavelength scales like . On the other hand, a dimensional analysis of the advective term in Eq. 5 leads to a typical scale proportional to , consistent with our simulations showing (SI Appendix, Fig. S7). As and scale differently with viscosity, the mode-multiplication factor changes accordingly. Noteworthy, decreasing the viscosity increased the scaling limit. A lower viscosity does not change any mechanical properties of the tube but increases the flow velocity and thus advection of the contraction-triggering chemical. This suggests that flow-driven transport is crucial for the observed scaling mechanism and the upper scaling limit.
Scaling of the Wave Is Due to Oscillatory Flows.
To distinguish the role of net flow and oscillatory flow in establishing the scaling, we investigated dynamics in tubes with an imposed inflow of on one end of the tube. To limit our study to a 2D parameter space, we set to the natural angular frequency of our system (SI Appendix, Eq. S1). The values of and were chosen to be comparable with the values generated spontaneously in simulations of periodic tubes (SI Appendix, Fig. S8).
Imposed flow boundary conditions result in long-range contraction patterns (Fig. 5). Interestingly, and have different effects on the observed wave size. Contrary to our expectations, the net flow has little impact on contraction wave size. The oscillatory part of the flow , on the other hand, increases sharply the wavelength for any value of . Interestingly, the time necessary to establish a stable pattern of contractions is shorter as the wave size grows (SI Appendix, Fig. S8). Thus, we find that oscillating flow at the boundary, rather than net flow, is the key to scaling with system size much beyond the intrinsic length scale of the instability.
Fig. 5.
Scaling of wave with system size governed by an oscillatory flow component at the tube boundary. Shown is a heat map of wave sizes in tubes of with an imposed flow at one boundary. Full scaling arises at high oscillatory flow almost independent of net flow .
Discussion
We have studied the self-organization of long-range fluid flows in tubular-shaped cells, due to the coupling of cortex contractions to an advected, contraction-triggering chemical. Our minimal two-component model system describing cortex and chemical dynamics predicts self-sustained contraction waves of wave size . Numerical simulations of the model confirm these predictions in tubes with closed boundaries. However, in tubes with periodic boundary conditions we find flows to scale with tube length much beyond the predicted wave size . Robust scaling is observed when tubes are grown longer than , “mode multiplying” at a scaling limit , . Simulations of fluids with different viscosities and tubes with imposed inflow show that the oscillatory flow is the key to this unexpected scaling on such long length scales.
From a dynamical systems point of view, previous work accounted for scaling contraction waves only when also the period of contraction scaled (41), whereas in our mechanism the period barely changes. Also the observation of mode multiplying at factors of up to 8 vastly exceeds previous observations of mode doubling or mode tripling (40). Within our model we find that mode multiplying is determined by the ratio between the scaling limit and the linearly unstable wavelength . The impact of the viscosity of the cytoplasm, as an example, was investigated, and the different scaling with viscosity, and , explained the splitting of the contraction wave to different modes.
The oscillatory nature of fluid flows allowed by periodic boundary conditions or by imposed flow is crucial to generate scaling beyond the intrinsic wavelength (Eq. 7). The value of the intrinsic wavelength may vary broadly between different systems. Assuming our representative parameter values, that contractility is of the same order as stiffness , and taking into account only that cell elastic modulus and cortex viscosity scale with cortex thickness over cell radius , a rule of thumb for the intrinsic wavelength is . This rule of thumb implies that only based on the intrinsic wavelength, a doubling in system size would requires a 16-fold increase in radius to allow the intrinsic wavelength to match the doubled system size. Alternatively, oscillatory flow boundary conditions are required to allow for scaling with system size beyond the intrinsic wavelength as the system grows. Given the possible range of biological parameters, this rule of thumb sets a scale for the radius over which long-range scaling due to oscillatory flows is likely to be at work. Note that the scale predicted here is only a rough estimate as our mechanochemical model accounts for only the role of calcium and additional cortex regulation machinery might be important in a specific system (5). Moreover, measurements of the mechanical and geometrical properties of the cell cortex show large variations and increase further the uncertainty. The key insight is that oscillatory fluid flows can generate scaling contraction waves and that it may be worth checking for their role in large systems, exceeding the intrinsic wavelength.
For the system best studied for its cortex-driven cytoplasmic flows, P. polycephalum, and with parameter values inferred from related organisms where necessary (Materials and Methods), the predicted wave size is , about an order of magnitude smaller than the coordinated contraction waves observed on scales of up (13), but well within the range of , in agreement with our predictions. At these large scales P. polycephalum forms a network of tubes with more viscous bags pooling fluid at the growing fronts. It is fascinating to speculate how the network morphology impacts the dynamics of contractile waves. It is likely that the contractions of the viscous bags at the growing fronts here do serve as pumps very much similar to the imposed flow boundary conditions we implemented. The growing fronts could thereby also account for the resurrection of scaling contraction waves after contraction stopped due to harmful external stimuli (42). In contrast to P. polycephalum to date detailed quantitative data are lacking in other systems to allow for quantitative comparison. However, cortex contractions and oscillatory flows are very general components for many other systems, even beyond the single cell. Thus, the interplay of fluid flows and mechanical oscillations resulting in scaling might be broadly relevant.
In general, our model broadens the budding understanding of the fundamental role of cytoplasmic flows in a large class of biophysical systems (1, 43–45). In very diverse systems, flows appear to be a fundamental part of a self-organized machinery. In our case, their oscillations are crucial to drive and organize patterns of contractions on a large scale, a mechanism likely present in many other biological systems. More fundamentally, our result opens perspectives on how including active advection in classical reaction–diffusion frameworks leads to unexpected observations such as scaling.
Materials and Methods
Implementation.
Numerical solutions of the model equations were explored with a custom-written Crank–Nicholson scheme implemented in MATLAB (The Mathworks). Simulations started from the spatially uniform equilibrium value for tube radius and chemical concentration. To perturb the stable state, uncorrelated, Gaussian fluctuations of SD 0.01 were added to the radius. Three kinds of boundary conditions were implemented: periodic, closed, or flow. For flow boundary conditions, the radius and the chemical concentration at the boundaries of the tube are both assumed to be equal to their value at the uniform equilibrium, and fluid flow is imposed on one end of the tube. In growing tubes, linear growth is simulated by changing dynamically the mesh size used for spatial discretization. The mesh is refined when the length of the tube doubled. The growth rate is small compared with the contraction period to decouple the dynamics of the system from growth. When tubes reach their target lengths, simulations are continued for roughly 200 additional contraction periods to ensure that growth has no impact on the simulated pattern.
Parameters.
Simulations parameters were for the viscosity of the cytoplasm (46), for the radius of the viscoelastic tube, for its effective stiffness [assuming a Young’s modulus of (47, 48) and a thickness of the tubes of ], for its effective viscosity (47, 49, 50), for the nonlinear elasticity, for the active stress (48, 51), (37, 52) for the diffusion of the tension activator in the cytoplasm, (23, 24) for the timescale of its regulation, for the threshold of its stretch-activated supply, and for the stretch inhibition of the active stress. The mechanical parameters, particularly and , were chosen to result in deformations of about 10%, typical for P. polycephalum (13). The resulting flow velocities in our simulations were around ms−1 to 30 ms−1, matching cytoplasmic flows for P. polycephalum (2).
Supplementary Material
Acknowledgments
This work was supported by the Max Planck Society.
Footnotes
The authors declare no conflict of interest.
This article is a PNAS Direct Submission.
This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1805981115/-/DCSupplemental.
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