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Published in final edited form as: Phys Rev E. 2021 Feb 1;103(2-1):022411. doi: 10.1103/PhysRevE.103.022411

Morphoelasticity of large bending deformations of cell sheets during development

Pierre A Haas 1,2,*, Raymond E Goldstein 1,
PMCID: PMC7616142  EMSID: EMS196597  PMID: 33736073

Abstract

Deformations of cell sheets during morphogenesis are driven by developmental processes such as cell division and cell shape changes. In morphoelastic shell theories of development, these processes appear as variations of the intrinsic geometry of a thin elastic shell. However, morphogenesis often involves large bending deformations that are outside the formal range of validity of these shell theories. Here, by asymptotic expansion of three-dimensional incompressible morphoelasticity in the limit of a thin shell, we derive a shell theory for large intrinsic bending deformations and emphasize the resulting geometric material anisotropy and the elastic role of cell constriction. Taking the invagination of the green alga Volvox as a model developmental event, we show how results for this theory differ from those for a classical shell theory that is not formally valid for these large bending deformations and reveal how these geometric effects stabilize invagination.

I. Introduction

Cell division, cell shape changes, and related processes can drive deformations of cell sheets during animal and plant development [16]. In elastic continuum theories of the development of the green alga Volvox [710], of tissue folding in Drosophila [11,12], or of more abstract active surfaces [13], these driving processes appear as changes of the reference or intrinsic geometry of thin elastic shells.

Just as classical thin shell theories arise from an asymptotic expansion of bulk elasticity in the small thickness of the shell [1416], these morphoelastic shell theories should be asymptotic limits of a bulk theory. While there is now a well-established framework of three-dimensional morphoelasticity [17,18], based on a multiplicative decomposition of the deformation gradient tensor into intrinsic and elastic deformations [19], studies of this asymptotic limit have mostly been restricted to the case of flat morphoelastic plates. Extensions of the classical Föppl–von Kármán equations [20,21] have been derived and residual stresses in Kirchhoff plate theories [22] have been studied in this case. A theory of non-Euclidean plates [23] has been developed in parallel. Apart from a general geometric theory of morphoelastic surfaces [24], studies of morphoelastic shells have remained more phenomenological, however: Some models [7,8,1113] simply replaced the elastic strains in classical shell theories [15,25,26] with measures of the difference of the intrinsic and deformed geometries. Other studies [9,10] took a more geometric approach, mirroring geometric derivations of classical shell theories [25] based on the so-called Kirchhoff “hypothesis”. This is the asymptotic result [15] that the normals of the midsurface of the undeformed shell remain, at leading order, normal to the deformed midsurface.

There is, however, one more serious limitation of these models: Tissues in development undergo large bending deformations (Fig. 1) that are outside the formal range of validity of the underlying thin shell theories, which assume that the thickness of the shell is much smaller than all length scales of the midsurface of the shell [15,25,26]. However, even if the thickness of the cell sheet is much smaller than its undeformed radius of curvature, this radius of curvature may become comparable, locally, to the thickness of the cell sheet as it deforms (Fig. 1). This is associated with cells contracting at one cell pole to splay and thereby bend the cell sheet [4].

Fig. 1.

Fig. 1

Large bending deformations during morphogenesis: Even if the thickness of the cell sheet is small compared to the undeformed radius of curvature, the local radius of curvature need not remain large compared to the cell sheet thickness as the sheet deforms. (a) Cross section of ventral furrow formation in Drosophila, reproduced from Ref. [29]. (b) Midsagittal cross section of invagination in the spherical alga Volvox globator, reproduced from Ref. [8]. Inset: Cartoon of constricted triangular cells in the bend region. Scale bars: 20 μm.

Here, we derive a theory of thin incompressible morphoelastic shells undergoing large bending deformations by asymptotic expansion of three-dimensional elasticity. We reveal how, even in a constitutively isotropic material, this biological scaling limit of large bending deformations induces, in the thin shell limit, a geometric anisotropy absent from classical shell theories: different deformation directions exhibit different deformation responses. We stress how this geometric effect is associated with the geometric singularity of cell constriction, i.e., the limit of wedged triangular cells [Fig. 1(b), inset] associated with these large bending deformations. Specializing to the invagination of the green alga Volvox [27,28], we then show how results for this theory differ from those for a classical theory that is not formally valid in this large bending limit and reveal how invagination is stabilized by the geometry of large bending deformations.

II. Elastic Model

In this section, we describe large bending deformations of a thin incompressible morphoelastic shell, starting from three-dimensional morphoelasticity. We shall have to distinguish between three configurations of the shell [Fig. 2(a)]: (i) the undeformed configuration of the shell, (ii) the deformed configuration of the shell, and (iii) the intrinsic configuration of the shell that encodes the local, intrinsic deformations of the shell, i.e., the cell shape changes or cell division in the biological system. These intrinsic deformations are not in general compatible with the global geometry of the shell: in other words, this intrinsic configuration cannot, in general, be embedded into three-dimensional Euclidean space [17]. Elasticity must therefore intervene to “glue” the intrinsically deformed infinitesimal patches of cell sheet back together, as illustrated in Fig. 2(a). Configurations (i) and (ii) are related by the geometric deformation gradient F˜. This tensor decomposes multiplicatively into an intrinsic contribution F0 that relates configurations (i) and (iii), and an elastic contribution F=F˜(F0)1. This is the multiplicative decomposition of morphoelasticity [17,18].

Fig. 2. Morphoelasticity of an axisymmetric shell.

Fig. 2

(a) The undeformed (top), deformed (left), and intrinsic (right) configurations of the shell are related by the three tensors F˜,F0, and F=F˜(F0)1. The geometric and intrinsic midsurface stretches are fs˜,f˜ϕ and fs0,fϕ0. (b) Undeformed configuration V of an axisymmetric shell of thickness εh(s), described by coordinates r(s), z(s), where s is arclength, with respect to the basis {ur, uϕ, uz} of cylindrical polars. (c) Cross section of the undeformed shell, defining a basis = {es, eϕ, n} and the transverse coordinate ζ. The surfaces of the undeformed shell are at ζ = ±h±(s), where the tangent vectors are es±,eϕ±, and the normal is n±. (d) Deformed configuration V˜ of the shell: After a torsionless deformation, the shell has thickness εh˜(s), arclength s˜, and is described by coordinates r˜(s),z˜(s) with respect to cylindrical polars. (e) Cross section of the deformed shell, defining a basis ˜={e˜s,e˜ϕ,n˜}. Normals to the midsurface rotate so that a point at a distance εζ from the undeformed midsurface 𝒮 is at a distance εζ˜(s,ζ) from the deformed midsurface S˜ and displaced by a distance εζ˜(s,ζ) parallel to S˜. At the surfaces ζ˜=±h˜±(s) of the deformed shell, the tangent vectors are e˜s±,e˜ϕ±, and the normal is ñ±. (f) The intrinsic midsurface S0, on which ζ 0 = 0, embeds, locally, into three-dimensional space to define an intrinsic basis 0 = {Es, Eϕ, N}.

In this section, we restrict to torsionless deformations of an axisymmetric shell. The analysis can be extended to more general deformations of the shell, and, for the sake of completeness, we do so in Appendix A, but the restriction to axisymmetric deformations eschews the mire of tensorial notation that arises in the general case.

The derivation of the shell theory for large bending deformations divides, like derivations of classical shell theories, into two steps: First, in Sec. II A, we describe the kinematics of the deformation and derive expressions for the geometric, intrinsic, and elastic deformations gradients. Second, in Sec. II B, we analyze the mechanics of the shell and expand the three-dimensional elastic energy and equilibrium conditions asymptotically. At the end of this section, in Sec. II C, we discuss the limit of small bending deformations that gives rise to classical shell theories.

A. Axisymmetric deformations of an elastic shell

We consider an elastic shell of undeformed thickness εh, where ε ≪ 1 is a small asymptotic parameter expressing the thinness of the shell compared to other length scales associated with its midsurface. Large bending deformations will be introduced in Sec. II B by allowing one of the intrinsic radii of curvature of the shell to be of order O(ε). We begin by deriving an expression for the elastic deformation gradient F for torsionless deformations of an axisymmetric shell.

1. Undeformed configuration of the shell

We will describe the undeformed configuration 𝒱 of the shell with reference to a midsurface S that we will choose later. With respect to the basis {ur, uϕ, uz} of cylindrical coordinates, we define the position vector of a point on 𝒮,

ρ(s,ϕ)=r(s)ur(ϕ)+z(s)uz, (1)

with s denoting arclength and ϕ being the azimuthal coordinate [Fig. 2(b)]. The tangent angle ψ (s) of 𝒮 is defined by

r(s)=cosψ(s),z(s)=sinψ(s), (2)

in which dashes denote differentiation with respect to s. The vectors

es(s,ϕ)=cosψ(s)ur(ϕ)+sinψ(s)uz,eϕ(ϕ)=uϕ(ϕ) (3)

thus constitute a basis of the tangent space of 𝒮 [Fig. 2(c)], which we extend to a (right-handed) orthonormal basis = {es, eϕ, n} for 𝒱 by adjoining the normal to 𝒮,

n(s,ϕ)=cosψ(s)uzsinψ(s)ur(ϕ). (4)

In particular, n = es × eϕ. We complete the description of 𝒮 by computing its curvatures,

ϰs(s)=ψ(s),ϰϕ(s)=sinψ(s)r(s). (5)

Now, the position of a point in 𝒱 is

r(s,ϕ,ζ)=ρ(s,ϕ)+εζn(s,ϕ), (6)

where we have introduced the transverse coordinate ζ, which is such that the shell surfaces are at ζ = ±h±(s) [Fig. 2(c)]. Noting the derivatives ∂n/s = −ϰses and ∂n/ϕ = −ϰϕeϕ, we obtain the tangent basis of 𝒱,

rs=(1εϰsζ)es,rϕ=r(1εϰϕζ)eϕ,rζ=εn, (7)

from which follows the expression for the Riemannian metric of the undeformed configuration,

χs2ds2+χϕ2dϕ2+χζ2dζ2, (8a)

with associated scale factors

χs=1εϰsζ,χϕ=r(1εϰϕζ),χζ=ε, (8b)

and hence volume element

dV=χsχϕχζdsdϕdζ=ε(1εϰsζ)(1εϰϕζ)rdsdϕdζ. (8c)

The position vectors of the surfaces ζ = ±h±(s) of the undeformed shell are

r±(s,ϕ,ζ)=ρ(s,ϕ)±εh±(s)n(s,ϕ) (9a)

so, using commata to denote partial differentiation,

r±s=(1εϰsh±)es±εh,s±n. (9b)

The unit tangent vectors to the shell surfaces are es±r±/s and eϕ±=eϕ, in which the symbol || expresses parallelism and hides a normalization factor for the unit vector on the left-hand side. By definition, the unit normals n± to the undeformed shell surfaces [Fig. 2(c)] obey n±es±×eϕ±. Now introducing the normalization factor explicitly, we find

n±=nv±es1+v±2withv±=εh,s±1εϰsh±. (10)

2. Deformed configuration of the shell

As the shell deforms into its deformed configuration V˜, the midsurface 𝒮 maps to the deformed midsurface S˜ [Fig. 2(d)], with position vector

ρ˜(s,ϕ)=r˜(s)ur(ϕ)+z˜(s)uz, (11)

where, in particular, s is again the undeformed arclength. Denoting by s˜ the deformed arclength, we define the stretches

f˜s(s)=ds˜ds,f˜ϕ(s)=r˜(s)r(s), (12)

which enable us to define the tangent angle ψ˜(s) of S˜ by

r˜(s)=f˜scosψ˜(s),z˜(s)=f˜ssinψ˜(s), (13)

where dashes still denote differentiation with respect to s. Similarly to the analysis of the undeformed configuration, we introduce the tangent vectors

e˜s(s,ϕ)=cosψ˜(s)ur(ϕ)+sinψ˜(s)uz,e˜ϕ(ϕ)=uϕ(ϕ), (14)

and the normal vector

n˜(s,ϕ)=cosψ˜(s)uzsinψ˜(s)ur(ϕ), (15)

so n˜=e˜s×e˜ϕ. This defines a (right-handed) orthonormal basis ˜={e˜s,e˜ϕ,n˜} describing V˜ [Fig. 2(e)]. The curvatures of the deformed shell are

κ˜s(s)=ψ˜(s)f˜s(s),κ˜ϕ(s)=sinψ˜(s)r˜(s). (16)

As the shell deforms, the normals to 𝒮 need not remain normal to S˜, and so a point in 𝒱 at a distance εζ from 𝒮 will end up, in V˜, at a distance εζ˜ from S˜, and displaced by a distance ε𝜍˜ parallel to S˜ [Fig. 2(e)]. By definition of the midsurface, ζ˜=𝜍˜=0 if ζ = 0. The position of a point in V˜ is thus

r˜(s,ϕ,ζ)=ρ˜(s,ϕ)+εζ˜(s,ζ)n˜(s,ϕ)+ε𝜍˜(s,ζ)e˜s(s,ϕ). (17)

Continuing to use commata to denote partial differentiation, we find

r˜s=[f˜s(1εκ˜sζ˜)+ε𝜍˜,s]e˜s+ε(ζ˜,s+f˜sκ˜s𝜍˜)n˜ (18a)

and

r˜ϕ=[r˜(1εκ˜ϕζ˜)+ε𝜍˜cosψ˜]e˜ϕ,r˜ζ=ε(ζ˜,ζn˜+𝜍˜,ζe˜s). (18b)

Noting that r˜=f˜ϕr from definitions (12), the Riemannian metric of V˜ is therefore

{[f˜s(1εκ˜sζ˜)+ε𝜍˜,s]2+ε2(ζ˜,s+f˜sκ˜s𝜍˜)2}ds2+[f˜ϕr(1εκ˜ϕζ˜)+ε𝜍˜cosψ˜]2dϕ2+ε2[(ζ˜,ζ)2+(𝜍˜,ζ)2]dζ2+2ε{𝜍˜,ζ[f˜s(1εκ˜sζ˜)+ε𝜍˜,s]+εζ˜,ζ(ζ˜,s+f˜sκ˜s𝜍˜)}dsdζ. (19a)

From ζ˜=𝜍˜=0 on ζ = 0, it follows that ζ˜,s=𝜍˜,s=0 on ζ = 0. Hence the metric of S˜ is simply

f˜s2ds2+f˜ϕ2r2dϕ2. (19b)

At the surfaces ζ˜=±h˜±(s) of the deformed shell, the unit tangent vectors are e˜s± and e˜ϕ±=e˜ϕ. They define the normals n˜±e˜s±×e˜ϕ± [Fig. 2(e)].

3. Intrinsic configuration of the shell: Incompatibility

To specify the intrinsic configuration 𝒱0 of the shell, we introduce the intrinsic stretches fs0,fϕ0 and the intrinsic curvatures κs0,κϕ0 and the intrinsic normal displacement ζ 0. We assume that fs0,fϕ0 and κs0,κϕ0 are functions of s only, while ζ 0(s, ζ) is strictly increasing in ζ, with ζ 0 = 0 on ζ = 0. Further, we assume that the analog of the displacement parallel to the midsurface vanishes, 𝜍0 = 0.

Although we have named these functions with reference to similar quantities defined for the deformed configuration, they lack a geometric meaning at this stage. In fact, the Riemannian metric that we can write down by analogy with Eq. (19a),

{[fs0(1εκs0ζ0)]2+ε2(ζ,s0)2}ds2+[fϕ0(1εκϕ0ζ0)]2r2dϕ2+ε2(ζ,ζ0)2dζ2+2ε2ζ,ζ0ζ,s0dsdζ, (20a)

is not in general compatible: Its Riemann curvature tensor does not vanish in general, so it cannot, in general, be embedded into three-dimensional Euclidean space [17]. Mechanically, this means that relieving all stresses in the shell requires an infinite number of cuts [17]. This is not surprising because, in the biological system, each cell undergoes independent shape changes or division in general and, since cells are infinitesimal in this continuum description, isolating these infinitesimal building blocks requires infinitely many cuts.

We now define the intrinsic midsurface S0 of the shell by its Riemannian metric, which is, by analogy with Eq. (19b) and consistently with Eq. (20a),

(fs0)2ds2+(fϕ0)2r2dϕ2. (20b)

It follows from a local embedding theorem for Riemannian metrics [30,31] that this two-dimensional metric can be embedded, at least locally, into three-dimensional Euclidean space. In particular, this means that there exists a local (right-handed) orthonormal intrinsic basis 0 = {Es, Eϕ, N} of three-dimensional space such that Es, Eϕ = uϕ are tangent to 𝒮0, and N is normal to it [Fig. 2(f)]. From this basis, we compute the curvatures of S0, ϰs0=EsN,s and ϰϕ0=EϕN,ϕ. The intrinsic curvatures κs0,κϕ0 are specified independently from these as they do not enter the definition of 𝒮0 in Eq. (20b). In particular, κs0,κϕ0 are in general different from ϰs0,ϰϕ0. This expresses the incompatibility of metric (20a). While Eq. (20b) assigns a geometric meaning to the intrinsic stretches fs0,fϕ0, these intrinsic curvatures therefore remain without the direct geometric realisation that would result from an embedding into three-dimensional Euclidean space, as does the intrinsic normal displacement ζ 0.

We specify the latter by requiring the intrinsic deformations to conserve volume. This assumption is, for example, appropriate for Volvox inversion [Fig. 1(b)]: the cell measurements of Ref. [28] suggest that the cell shape changes driving inversion preserve volume. For other developmental processes that include cell division, the assumption of intrinsic volume conservation would be replaced with a position-dependent constraint that takes account of this growth. Since ζ 0(s, ζ) is increasing and can hence be inverted to yield ζ (s, ζ 0), Eq. (20a) becomes, on changing coordinates from {s, ϕ, ζ} to {s, ϕ, ζ0},

(χs0)2ds2+(χϕ0)2dϕ2+(χζ00)2(dζ0)2, (21a)

with scale factors

χs0=fs0(1εκs0ζ0),χϕ0=fϕ0r(1εκϕ0ζ0),χζ00=ε. (21b)

Its volume element is therefore

dV0=χs0χϕ0χζ00dsdϕdζ0=εfs0fϕ0(1εκs0ζ0)(1εκϕ0ζ0)rdsdϕdζ0. (21c)

Intrinsic volume conservation requires dV = dV 0, so Eqs. (8c) and (21c) combine to yield a differential equation for ζ 0 as a function of ζ, which we will eventually integrate in Sec. II B under the scaling assumptions of our shell theory.

At this stage, 𝒮, S˜, and 𝒮0 are defined to be corresponding surfaces within the shell. Indeed, it would it be possible to develop a shell theory for any choice of surfaces that correspond to each other in this way. We add that there is no obvious correspondence between the shell theories that result from different choices of the intrinsic midsurface 𝒮0 belonging to 𝒱0 since the latter cannot be embedded into three-dimensional space.

We now make a particular choice of the surfaces 𝒮, S˜, and 𝒮0 that, as we shall see in the discussion at the end of Sec. II B, justifies referring to these surfaces as midsurfaces. We do so by imposing the following condition: the surfaces of the shell, at ζ = ±h±(s) and ζ˜=±h˜±(s) in 𝒱 and V˜ respectively, correspond to ζ 0 = ±h0(s)/2; the calculations in Sec. II B will show that this choice can be made. We stress that, like ζ 0, the intrinsic thickness h0(s) lacks a direct geometric realization.

We close by noting that ζ 0(s, ζ) and hence h0(s) can also be specified without reference to the incompatible metric (20a), by imposing the condition det F0 = 1. Indeed, with the intrinsic deformation gradient F0 defined as in Eq. (24) below, this is easily seen to be equivalent with dV = dV 0. Conversely, the condition det F0 =1 can be used to define the intrinsic volume element dV 0 without reference to Eq. (20a).

4. Calculation of the deformation gradient tensors

The geometric deformation gradient is F˜=Gradr˜ [17], in which the gradient with respect to the undeformed configuration is [17]

Grad=1χs2srs+1χϕ2ϕrϕ+1χζ2ζrζ. (22)

Combining Eqs. (7), (8b), and (18), we thus obtain the geometric deformation gradient,

F˜=(f˜s(1εκ˜sζ˜)+ε𝜍˜,s1εϰsζ0𝜍˜,ζ0f˜ϕ(1εκ˜ϕζ˜)+ε𝜍˜cosψ˜/r1εϰϕζ0ε(ζ˜,s+f˜sκ˜s𝜍˜)1εϰsζ0ζ˜,ζ), (23)

expressed here with respect to the mixed basis ˜. We now complete specifying the intrinsic configuration 𝒱0 by writing down an analogous expression for the intrinsic deformation gradient with respect to the mixed basis 0, viz.,

F0=(fs0(1εκs0ζ0)1εϰsζ000fϕ0(1εκϕ0ζ0)1εϰϕζ0εζ,s01εϰsζ0ζ,ζ0). (24)

The elastic deformation gradient is, therefore, with respect to the natural mixed basis ˜0,

F=F˜(F0)1=(f˜s(1εκ˜sζ˜)+ε(𝜍˜,s+𝜍˜,ζ0ζ,s0)fs0(1εκs0ζ0)0𝜍˜,ζ00f˜ϕ(1εκ˜ϕζ˜)+ε𝜍˜cosψ˜/rfϕ0(1εκϕ0ζ0)0ε(ζ˜,s+f˜sκ˜s𝜍˜ζ,s0ζ˜,ζ0)fs0(1εκs0ζ0)0ζ˜,ζ0). (25)

B. Thin shell theory for large bending deformations

In this subsection, we derive the effective elastic energy for the shell by asymptotic expansion of three-dimensional elasticity. We assume the simplest constitutive law, that the shell is made of an incompressible neo-Hookean material [17], so its elastic energy is

=V0edV0,withe=C2(13), (26)

wherein C > 0 is a material parameter, and 1 is the first invariant of the right Cauchy–Green tensor C = FF [17]. The integration of the strain energy density e is over the intrinsic configuration 𝒱0 of the shell, with volume element dV 0. As we have noted above, this can be defined from the condition det F0 = 1, independently of the incompatible metric (20a).

The force on an area element dS˜ with unit normal m˜ of the deformed configuration is Tm˜dS˜ [17,32]. In this expression, T is the Cauchy stress tensor, which, for this neo–Hookean material, is related to the deformation gradient by [21]

T=C(FFpI), (27)

in which I is the identity and the Lagrange multiplier p is proportional to pressure and imposes the incompressibility condition det F = 1. To this area element of the deformed configurations corresponds, in the undeformed configuration, an area element dS with unit normal m. Nanson’s relation [17,32] states that m˜dS˜=J˜F˜mdS, where J˜=detF˜=detFdetF0=1. We introduce the tensor

P=TF˜=CQwithQ=F(F0)pF˜. (28)

In particular, if F0 = I, then P =TF−T is the familiar (first) Piola–Kirchhoff tensor [17]. By definition, Tm˜dS˜=PmdS, and hence, similarly to the derivation of the familiar Cauchy equation of classical elasticity [17,32], the configuration of the shell minimizing the energy (26) is determined by

DivQ=0, (29a)

where the divergence (with respect to the undeformed configuration of the shell) is defined by contracting the first and last indices of the gradient in Eq. (22). Since is independent of ζ by definition, and using the nabla operator to denote the gradient on 𝒮, this becomes, on separating the components parallel and perpendicular to the midsurface,

(Qn),ζε+Q=0. (29b)

1. Scaling assumptions

At this point, we break the complete generality of our description by making scaling assumptions appropriate for a shell theory of large intrinsic bending deformations.

First, we introduce large intrinsic bending deformations explicitly by scaling the intrinsic curvatures so as to allow small radii of curvature in the meridional direction, viz.,

κs0=fs0fϕ0λs0ε,κϕ0=fs0fϕ0λϕ0, (30)

in which the scaled intrinsic curvatures λs0,λϕ0 are assumed to be O(1) quantities. This scaling regime in which the meridional intrinsic radius of curvature becomes comparable to the thickness of the cell sheet is, as shown in Fig. 1(b), the one relevant for Volvox invagination, which we shall analyze in Sec. III. Appendix A treats the general case in which all components of the curvature tensor are allowed to be large.

Second, we make the standard scaling assumptions of shell theory, that the elastic strains are small, i.e., that the stretches and curvatures in the deformed configuration do not differ “too much” from the intrinsic stretches and curvatures. In particular, while we have allowed the radius of curvature 1/κs0 to become comparable to the shell thickness in Eqs. (30), we shall assume the deviations from this to remain small. More formally, we introduce the shell strains Es, Eϕ by writing

f˜s=fs0(1+εEs),f˜ϕ=fϕ0(1+εEϕ), (31)

and the curvature strains Ls, Lϕ by letting

κ˜s=fs0fϕ0(λs0ε+Ls),κ˜ϕ=fs0fϕ0(λϕ0+Lϕ). (32)

Finally, we introduce the scaled variables

Z0=fs0fϕ0ζ0,Z=fs0fϕ0ζ˜,S=fs0fϕ0ζ˜. (33)

While we will come back to discussing the factors fs0fϕ0 that arise in Eqs. (30), (32), and (33), we note, for now and from Eq. (20b), the following: the intrinsic midsurface 𝒮0 has surface element dS0=fs0fϕ0rdrdϕ=fs0fϕ0dS, with dS the surface element of the undeformed midsurface 𝒮. Hence these rescalings by fs0fϕ0 absorb the intrinsic stretching of the midsurface. This will turn out to simplify expressions that arise in subsequent calculations.

2. Boundary and incompressibility conditions

We solve the Cauchy equation (29b) subject to the incompressibility condition det F =1 and force-free boundary conditions. These boundary conditions, that there be no external forces on the surfaces of the shell, are relevant for many problems in developmental biology, where deformations are, as discussed in the Introduction, driven by changes of the intrinsic geometry only; including external forces does not pose any additional difficulty though.

These force-free boundary conditions read T±ñ± = 0 [17], where T± are the Cauchy tensors evaluated on the surfaces ζ˜=±h˜± of V˜. By the above, these are equivalent with P±n± = 0, where, from Eq. (28), P± = CQ± are evaluated on the surfaces ζ = ±h± of V, the normal vectors n± of which are given by Eqs. (10). The latter yields the expansion

n±=nεh,s±es+O(ε2). (34)

The incompressibility condition is det F = 1. Since the bases ˜ and 0 are orthonormal, there exist rotations, represented by proper orthogonal matrices R˜ and R0, that map the standard Cartesian basis χ onto ˜ and 0, respectively. Hence, if F denotes the matrix in Eq. (25) that represents F with respect to the mixed basis ˜0, then F is represented by R˜FR0 with respect to χχ. Since det R˜=det R0=1, detF=det(R˜FR0)=detF. The incompressibility condition can therefore be evaluated using the matrix in Eq. (25), but it is important to recognize that incompressibility is a tensorial condition. For the general, nonaxisymmetric deformations discussed in Appendix A, we shall indeed have to distinguish more carefully between tensors and the matrices representing them with respect to mixed nonorthogonal bases, which is why we have already introduced different notations, based on Ogden’s [32], for matrices (sans serif font) and tensors (bold sans serif font) that could be used interchangeably here.

3. Intrinsic volume conservation

Before expanding the boundary and incompressibility conditions asymptotically, we determine the dependence of ζ 0 and hence Z0 on ζ that results from the condition dV = dV 0 of intrinsic volume conservation. On recalling that κs0=O(ε1), the expressions for dV in Eq. (8c) and dV 0 in Eq. (21c) yield, at leading order, a differential equation for Z0(ζ),

(1λs0Z0)Z,ζ0=1Z0=1λs0(112λs0ζ), (35)

where we have imposed Z0 = 0 at ζ = 0. Let H0=h0fs0fϕ0. Since ζ 0 = ±h0/2 ⇔ Z0 = ±H 0/2 at ζ = ±h± by definition, Eq. (35) implies

h±=H02(1λs04H0)h=h++h=H0, (36)

wherein h is again the undeformed thickness of the cell sheet [Fig. 2(c)]. We note that Eq. (36) is a leading-order result only, since we have ignored O(ε) corrections in Eq. (35).

4. Expansion of the boundary and incompressibility conditions

To expand the incompressibility and boundary conditions in the small parameter ε, we posit regular expansions

Z=Z(0)+εZ(1)+O(ε2),S=S(0)+O(ε), (37)

for the scaled transverse and parallel displacements. Throughout this paper, we shall use subscripts in parentheses in this way to denote the different terms in asymptotic expansions in ε. We further expand

Q=Q(0)+εQ(1)+O(ε2),p=p(0)+O(ε). (38)
(a). Expansion at order O(1)

At leading order, Eq. (29b) yields (Q(0)n),ζ = 0, so Q(0)n = Q(s) is independent of ζ. It follows that 0=Q±n±=Q(0)±n+O(ε)=±Q+O(ε) using Eq. (34). Thus 0Q=Q(0)n=(q(0)s,0,q(0)n). Expanding definition (28) using Eqs. (23)–(25), this yields [33]

0=q(0)s=fs0fϕ0(1λs0Z0)λs0S(0)[p(0)(S(0),Z0)2]+(1λs0Z(0))S(0),Z0Z(0),Z0(1λs0Z(0))Z(0),Z0λs0S(0)S(0),Z0, (39a)
0=q(0)n=fs0fϕ0(1λs0Z0)(1λs0Z(0))[(Z(0),Z0)2p(0)]λs0S(0)S(0),Z0Z(0),Z0(1λs0Z(0))Z(0),Z0λs0S(0)S(0),Z0, (39b)

where we have used (ζ0,ζ)1=fs0fϕ0(1λs0Z0)+O(ε), which follows from Eq. (35) on recalling the rescalings (33). Moreover, on expanding the incompressibility condition using Eq. (25), we find

1=detF=11λs0Z0(1λs0Z(0))Z(0),Z0+λs0S(0)S(0),Z01λs0Z0+O(ε). (40)

Equations (39) and (40) define a system of three simultaneous linear algebraic equations for p(0),Z(0),Z0, and S(0),Z0, with solution

p(0)=(1λs0Z0)2(1λs0Z(0))2+(λs0S(0))2, (41a)
Z(0),Z0=(1λs0Z0)(1λs0Z(0))(1λs0Z(0))2+(λs0S(0))2, (41b)
S(0),Z0=λs0S(0)(1λs0Z0)(1λs0Z(0))2+(λs0S(0))2. (41c)

Equation (40) or Eqs. (41b) and (41c) imply

2Z(0),Z0(1λs0Z(0))+2λs0S(0)S(0),Z0=2(1λs0Z0). (42a)

Integrating and using the fact that Z(0) = S(0) = 0 at Z0 = 0 by definition of the midsurfaces, we obtain

(1λs0Z(0))2+(λs0S(0))2=(1λs0Z0)2. (42b)

Equation (41a) now becomes p(0) = 1. Moreover, on substituting Eq. (42b) into Eq. (41b),

Z(0)Z0=1λs0Z(0)1λs0Z01λs0Z(0)1λs0Z0=const., (43)

which, using Z(0) = 0 at Z0 = 0 again, yields Z(0)Z0. Hence S(0) ≡ 0 from Eq. (42b). The last equality is the Kirchhoff “hypothesis” [15]: normals to the intrinsic midsurface remain, at lowest order, normal to the deformed midsurface.

(b). Expansion at order O(ε)

We now expand the incompressibility condition further, finding

0=detF1=ε(Es+EϕLϕZ0+Z(1)Z0LsZ0+λs0Z(1)1λs0Z0)+O(ε2). (44)

On solving the resulting differential equation for Z(1) by imposing Z(1) = 0 at Z0 = 0, we obtain

Z(1)=Z0{6(Es+Eϕ)3Z0[Ls+Lϕ+λs0(Es+Eϕ)]+2λs0Lϕ(Z0)2}6(1λs0Z0). (45)
(c). Expansion at order O(ε2)

It will turn out not to be necessary to expand the deformation gradient explicitly beyond order O(ε). Indeed, it will suffice to consider a formal expansion,

F=(1+εa(1)+ε2a(2)+O(ε3)0εv(1)+O(ε2)01+εb(1)+ε2b(2)+O(ε3)0εw(1)+O(ε2)01+εc(1)+ε2c(2)+O(ε3)), (46)

with the leading-order terms found from Eq. (25). This also yields, using Eq. (45),

a(1)=6Es6[Ls+λs0(EsEϕ)]Z0+3λs0[LsLϕ+λs0(EsEϕ)](Z0)2+2(λs0)2Lϕ(Z0)36(1λs0Z0)2,b(1)=EϕZ0Lϕ. (47)

Expressions for a(2), b(2), c(1), c(2), v(1), w(1) could similarly be obtained in terms of the expansions (37), but, as announced, will turn out to be of no consequence. Using Eq. (46), the incompressibility condition becomes

1=detF=1+ε(a(1)+b(1)+c(1))+ε2(a(2)+b(2)+c(2)+a(1)b(1)+b(1)c(1)+c(1)a(1)v(1)w(1))+O(ε3). (48)

Next, using Eq. (24), we introduce an analogous formal expansion for the intrinsic deformation gradient, viz.,

F0=(a(0)0+O(ε)000b(0)0+O(ε)0εw(1)0+O(ε2)0c(0)0+O(ε)), (49)

Where c(0)0=[fs0fϕ0(1λs0Z0)]1 using Eq. (35), and the values of a(0)0,b(0)0,w(1)0 are of no consequence. Hence, using Eq. (46),

F˜=FF0=(a(0)0+O(ε)0εc(0)0v(1)+O(ε2)0b(0)0+O(ε)0ε(w(1)0+a(0)0w(1))+O(ε2)0c(0)0+O(ε).), (50)

and thus, since p = 1 + O(ε),

Q=(O(ε)0ε(v(1)+w(1))/c(0)0+O(ε2)0O(ε)0O(ε)0O(ε).)Q(0)=O,Q(1)n=((v(1)+w(1))/c(0)00O(1)). (51)

In particular, Eq. (29b) at order O(1) is just (Q(1)n),ζ = 0. Moreover 0=Q±n±=εQ(1)±n+O(ε2), since Q(0) = O and using Eq. (34). Similarly to above, this implies Q(1)n0. From this and from Eq. (48), we infer

w(1)=v(1),c(1)=(a(1)+b(1)), (52a)
c(2)=a(1)2+a(1)b(1)+b(1)2a(2)b(2)+v(1)w(1). (52b)

5. Asymptotic expansion of the constitutive relations

On computing the expansion of C = FF from Eq. (46) and hence that of 1= tr C, and simplifying using Eqs. (52), we obtain

1=3+ε[2(a(1)+b(1)+c(1))]+ε2[a(1)2+b(1)2+c(1)2+v(1)2+w(1)2+2(a(2)+b(2)+c(2))]+O(ε3)=3+ε2[4(a(1)2+a(1)b(1)+b(1)2)]+O(ε3). (53a)

Hence, from Eqs. (47) and on introducing x=λs0Z0,

1=3+ε2(1x)4{[1+(1x)2]2Es2+2[1+(1x)2]EsEϕ+(412x+18x212x3+3x4)Eϕ21λs0[2x(46x+4x2x3)EsLs2x(2x)EϕLs2x3(612x+11x25x3+x4)EsLϕ2x3(1239x+55x236x3+9x4)EϕLϕ]+1(λs0)2[x2(2x)2Ls2+2x23(69x+5x2x3)LsLϕ+x29(36126x+177x2114x3+28x4)Lϕ2]}+O(ε3). (53b)

This determines the leading-order term in the asymptotic expansion of the energy density in Eqs. (26). On defining, from Eq. (46), the (symmetric) effective two-dimensional deformation gradient and associated two-dimensional strain,

F^=(1+εa(1)001+εb(1))+O(ε2),E^=F^F^I2ε, (54)

wherein I is again the identity, we rewrite Eq. (53a) as

13=2ε2[(trE^)2+trE^2]+O(ε3) (55)

This shows how, at leading order, the energy density depends only on the two invariants of the effective two-dimensional strain. In the asymptotic limit of a thin shell, the constitutive relations have thus become effectively two-dimensional.

6. Derivation of the thin shell theory

We are now set up to average out the transverse coordinate and thus obtain the thin shell theory. We compute, from Eq. (21c), the leading-order expansion for the volume element in the intrinsic configuration:

dV0=ε(1λs0Z0)rdsdϕdZ0+O(ε2)=1xλs0εrdsdϕdx+O(ε2). (56)

Moreover, we introduce η=λs0h/2, so that the shell surfaces ζ 0 = ±h0/2 correspond to x = ±η.

On substituting Eqs. (53b) and (56) into Eqs. (26), integrating with respect to x, and using axisymmetry, we then obtain

=Se^rdsdϕ=2πCe^rds, (57a)

with the first integration over the undeformed axisymmetric midsurface 𝒮 and the second over the curve 𝒞 generating 𝒮. The effective two-dimensional energy density ê in Eq. (57a) is

e^=ελs0ηηe(x)(1x)dx=C2ε3{h[αssEs2+(αsϕ+αϕs)EsEϕ+αϕϕEϕ2]+2h2[βssEsLs+βsϕEsLϕ+βϕsEϕLs+βϕϕEϕLϕ]+h3[γssLs2+(γsϕ+γϕs)LsLϕ+γϕϕLϕ2]}+O(ε4), (57b)

wherein

αss=η42η2+2(1η2)2+2tanh1ηη, (58a)
αsϕ=αϕs=1(1η2)2+tanh1ηη, (58b)
αϕϕ=3η46η2+4(1η2)2, (58c)
βss=η(2η2)2(1η2)2, (58d)
βsϕ=η6+4η411η2+318η(1η2)2tanh1η6η2, (58e)
βϕs=12η(1η2)2+tanh1η2η2, (58f)
βϕϕ=3η55η3+η6(1η2)2, (58g)
γss=η42η2+24η2(1η2)2tanh1η2η3, (58h)
γsϕ=γϕs=η62η4+η2+336η2(1η2)2tanh1η12η3, (58i)
γϕϕ=10η421η2+1236(1η2)2 (58j)

are functions of the large bending parameter

η=λs02h=κs02fs0fϕ0(εh)=κs02(εh0) (59)

only. Moreover, from Eqs. (31) and (32), the shell strains in Eq. (57b) are

εEs=f˜sfs0fs0,εEϕ=f˜ϕfϕ0fϕ0, (60)

while the curvature strains are

Ls=κ˜sκs0fs0fϕ0=Ks2ηhEs+O(ε), (61a)
Lϕ=κ˜ϕκϕ0fs0fϕ0=Kϕ+O(ε), (61b)

where we have defined

Ks=f˜sκ˜sfs0κs0(fs0)2fϕ0,Kϕ=f˜ϕκ˜ϕfϕ0κϕ0fs0(fϕ0)2. (62)

Shell theories are expressed more naturally in terms of the alternative curvature strains Ks, Kϕ. Indeed, Ks, Kϕ vanish for pure stretching deformations, whereas Ls, Lϕ do not: Consider a shell, the undeformed (and intrinsic) configuration of which is a sphere of radius R, and which deforms into a sphere of radius R′ = f R, for example because of a pressure difference between the inside and outside. For this deformation, fs0=fϕ0=1, κs0=κϕ0=1/R, while f˜s=f˜ϕ=f,κ˜s=κ˜ϕ=1/fR and so Ls = Lϕ = (1 − f)/f 3R ≠ 0 for f ≠ 1, but Ks = Kϕ = 0. Reference [15] has also discussed this point, noting that Ls, Lϕ and Ks, Kϕ can be used interchangeably in classical shell theories. However, Eq. (61a) shows that, in the large bending limit considered here, LsKs = O(1). Even at leading order, the stretching deformations associated with changes in curvature cannot therefore be neglected in this limit. In terms of the alternative curvature strains Ks, Kϕ, Eq. (57b) becomes

e^=C2ε3{h[α¯ssEs2+(α¯sϕ+α¯ϕs)EsEϕ+αϕϕEϕ2]+2h2[β¯ssEsKs+β¯sϕEsKϕ+βϕsEϕKs+βϕϕEϕKϕ]+h3[γssKs2+(γsϕ+γϕs)KsKϕ+γϕϕKϕ2]}+O(ε4), (63)

where αϕϕ, βϕs, βϕϕ, γss, γ = γϕs, γϕϕ are still given by Eqs. (58), while

α¯ss=αss4ηβss+4η2γss=4(1η2)2, (64a)
α¯sϕ=α¯ϕs=αsϕ2ηβϕs=2(1η2)2, (64b)
β¯ss=βss2ηγss=1η(1η2)2+tanh1ηη2, (64c)
β¯sϕ=βsϕ2ηγsϕ=η(2η2)3(1η2)2. (64d)

This completes the derivation of the elastic energy (57a) of a thin shell undergoing large axisymmetric bending deformations. In Appendix B, we derive the associated governing equations, using the expression (63) of the energy density in terms of the alternative curvature strains defined in Eqs. (62).

7. Discussion

Several features of the shell theory that we have obtained here are worth discussing in some detail.

(a). Stretching, coupling, and bending energies

The terms that appear in the elastic energy (63) separate into stretching, coupling, and bending terms, viz.,

e^=e^stretch+e^couple+e^bend+O(ε4), (65)

with

e^stretch=Ch2ε3[α¯ssEs2+(α¯sϕ+α¯ϕs)EsEϕ+αϕϕEϕ2], (66a)
e^couple=Ch2ε3[β¯ssEsKs+β¯sϕEsKϕ+βϕsEϕKs+βϕϕEϕKϕ], (66b)
e^bend=Ch32ε3[γssKs2+(γsϕ+γϕs)KsKϕ+γϕϕKϕ2]. (66c)

As (α¯sϕ+α¯ϕs)24α¯ssα¯ϕϕ=48(1η2)2<0 for |η| < 1, the stretching energy êstretch is positive semidefinite. Numerically, we also find that (γ + γϕs)2 − 4γssγϕϕ < 0 for |η| < 1, and hence the bending energy êbend is positive semidefinite, too. However, the coupling energy êcouple can clearly be of either sign, though ê is of course positive semidefinite.

(b). Constriction limit: Divergence

All of the coefficient functions in Eqs. (58) and (64) diverge as η → ±1. More precisely, the coefficients diverge like (1 − |η|)−2, and so Eq. (63) loses asymptoticity when 1|η|=O(ε), and hence the shell theory is not formally valid in this limit. This is mirrored by a similar breakdown of asymptoticity at other places in the analysis: for example, Eqs. (47) show that the expansion of the deformation gradient in Eq. (46) also breaks down when 1|η|=O(ε). However, this divergence, absent from theories not valid for large bending deformations, is not surprising in the first place. Indeed, the limit η → ± 1 corresponds to constricted cells, i.e., wedge-shaped, triangular cells [Fig. 1(b), inset] for which the intrinsic meridional radius of curvature is half the intrinsic cell sheet thickness: one of the surfaces of the shell has contracted to a point in the intrinsic configuration, so is geometrically singular. As the intrinsic configuration approaches this constricted limit somewhere, deviations from the intrinsic configuration become more and more expensive energetically there compared to other positions in the shell, unless the divergence of ê as η → ±1 is suppressed. This happens if êcouple ≈ − (êstretch + êbend) < 0 or the divergence of each of êstretch, êcouple, êbend is suppressed, which is possible for special values of Es, Eϕ, Ks, Kϕ, as discussed in more detail below.

(c). Geometric anisotropy

Plots of the coefficient functions in Eqs. (58) and (64), arbitrarily scaled with α¯ss to absorb their divergence as η → ±1, are shown in Fig. 3. These illustrate how the relative importance of different deformation modes depends on the amount of intrinsic bending. In other words, large bending deformations break the material isotropy, so that different directions of stretching have different effective stretching moduli; similarly, different effective bending moduli are associated with different directions of bending. This anisotropy is therefore geometric. It is not perhaps surprising since it mirrors the curvature anisotropy of the intrinsic configuration but, as discussed below, this effect is absent from the classical theories not valid for large bending deformations.

Fig. 3.

Fig. 3

Effective two-dimensional energy density. Plots of the coefficients in Eq. (63), defined in Eqs. (58) and (64), against η. All coefficients are arbitrarily scaled with α¯ss to absorb their divergence in the constriction limit η → ±1. (a) Plot of the stretching coefficients α¯ss,α¯sϕ,α¯ϕs, αϕϕ. Inset: Unscaled plot of α¯ss against η, diverging as η → ±1. (b) Plot of the mixed co-efficients β¯ss,β¯sϕ, βϕs, βϕϕ. (c) Plot of the bending coefficients γss, γ, γϕs, γϕϕ.

(d). Midsurfaces

The leading-order solution above shows that ζ˜=ζ0+O(ε). This implies that h˜±=h0/2+O(ε), and hence (h˜+h˜)/2=O(ε). The middle surface ζ˜=(h˜+h˜)/2 of the deformed configuration V˜ therefore coincides with ζ˜=0, i.e., with the midsurface S˜at leading order, which is the order to which the shell theory is valid. However, (h+h)/2=λs0h2/8+O(ε)=O(1), from Eq. (36), and so S, defined by ζ = 0, is not the middle surface ζ = (h+h)/2 of the undeformed configuration 𝒱. We could have derived a shell theory with similar properties to the one obtained here but in which the midsurfaces correspond to the middle surface of 𝒱 but not to that of V˜. Since the middle surface of V˜ is the one that is ultimately observed, our choice is perhaps the more natural one, and we are justified in referring to 𝒮, S˜, 𝒮0 as midsurfaces.

C. Limit of small bending deformations

We conclude our calculations by taking the limit η → 0, in which the bending deformations become small compared to the thickness of the shell. The energy density in Eq. (63) then limits to the form familiar from classical shell theories [15],

e^0=2Cε3[h(Es2+EsEϕ+Eϕ2)+h312(Ks2+KsKϕ+Kϕ2)], (67)

up to corrections of order O(ε4). This is the energy density of a thin Hookean shell [15,25,26] with Poisson’s ratio ν = 1/2, implying incompressibility, and elastic modulus E = 3C. In particular, our analysis also provides a formal derivation of the morphoelastic version of this classical shell theory. Again, the energy density separates into stretching and bending terms,

e^0=e^0,stretch+e^0,bend, (68)

with

e^0,stretch=12(4Ch)ε3[Es2+EsEϕ+Eϕ2], (69a)
e^0,stretch=12(Ch33)ε3[Ks2+KsKϕ+Kϕ2] (69b)

but there is no term that couples the strains and curvature strains. Such coupling terms do arise in the expansion corresponding to Eq. (53b), but are odd functions of Z0, so disappear on integration over [−H0, H0] and hence from Eq. (67).

In this classical theory, the same stretching modulus E(εh)/(1 − ν2) = 4C(εh) and the same bending modulus E(εh)3/[12(1 − ν2)] = C(εh)3/3 are associated with all directions of stretching or bending; to pick up on a point made earlier, it is this isotropy resulting from the constitutively assumed isotropy of the material that is broken by the geometry of large bending deformations.

Of course, Eq. (67) could be derived directly by imposing different scalings, of small intrinsic bending, replacing those for large bending deformations in Eqs. (30); these scalings would considerably simplify the solutions of Eqs. (39), (40), and (44). Indeed, the structure of these calculations would be broadly similar to the earlier asymptotic derivation of the classical shell theories in Ref. [16]. We emphasize that, in either derivation, the terms at order O(ε2) in the expansion (46) of the deformation gradient need not be computed explicitly.

1. Stretching and bending energies for small and large bending

We compare the stretching and bending energies in the small and large bending limits by observing that

e^stretch=e^0,stretch+η2(2η2)(1η2)2(2Es+Eϕ)2, (70a)
e^bend=e^0,bend+η2(32η2)36(1η2)2(3Ks+Kϕ)(k(η)Ks+Kϕ), (70b)

where we have used Eqs. (58) and (64) and defined

k(η)=η(4η611η4+10η26)+6(1η2)2tanh1ηη5(32η2). (71)

This shows that the classical theory underestimates the stretching energy of large bending deformations: êstretchê0,stretch from Eq. (70a). Moreover, êstretch diverges as |η| → 1 unless the deformations are such that Eϕ = −2Es.

The classical theory may, however, overestimate the bending energy of large bending deformations. Indeed, numerically, we find 13/5 = k(0) < k(η) < k(±1) = 3 for |η| < 1, and hence, from Eq. (70b), êbend < ê0,bend if and only if KsKϕ < 0 and k(η) |Ks| < |Kϕ| < 3 |Ks|. Also from Eq. (70b), êbend diverges as |η| →1 unless Kϕ = −3Ks.

In particular, êstretch and êbend are both bounded as |η| → 1 if and only if Eϕ = −2Es and Kϕ= −3Ks. In this case, Eq. (66b) shows that êcouple is also bounded as |η| → 1. The conditions Eϕ = −2Es, Kϕ = −3Ks thus define the special deformations that allow the stretching, bending, and coupling energies to remain bounded as |η| → 1 that we mentioned earlier.

2. Other elastic shell theories

The energy density in Eq. (67) has the same structure as the elastic energy densities used in the models referenced in the Introduction, but the morphoelastic definitions of the shell and curvature strains in Eqs. (60) and (62) differ from those in these previous models: In models not based on morphoelasticity and its multiplicative decomposition of the deformation gradient [7,8,1113], the shell and curvature strains are simply differences of stretches or curvatures, missing the scaling factors of fs0,fϕ0 that appear in Eqs. (60) and (62). We also note that the expressions for the curvature strains in Eqs. (62) differ by a factor of g0=fs0fϕ0, from those in Refs. [9,10], which, as discussed in the Introduction, used a geometric approach to derive a morphoelastic shell theory. Earlier, we noted that this factor corresponds to the stretching of the intrinsic midsurface. Moreover, since h˜±=h0/2+O(ε) as noted above, the deformed cell sheet has thickness h˜=h˜++h˜=h0+O(ε) Equation (36) therefore yields h/h˜=h/h0+O(ε)=g0+O(ε). The fact that the curvature strains in Eqs. (62) decrease as g0 increases therefore expresses the fact that the shell becomes easier to bend as it thins as a result of this stretching of the midsurface, with e^bend,e^0,bendg02. This geometric role of the factor g0 has been noticed previously in the context of uniform growth of an elastic shell [34].

The geometric approach in Refs. [9,10] also leads to additional terms in the energy density. The present analysis proves that these terms are not leading-order terms in the thin shell limit. However, there is no reason to expect this geometric approach to yield all terms at next order in the asymptotics. A complete expansion could in principle be obtained by continuing the asymptotic analysis presented here. Taking the analysis to higher orders in this way would in particular answer the question: at what order does the Kirchhoff hypothesis break down, i.e., at what order do the normals to the deformed midsurface diverge from those to the undeformed midsurface? This would permit asymptotic justification of the so-called shear deformation theories [35] in which the normals to the undeformed midsurface need not remain normals in the deformed configuration, but we do not pursue this further here.

III. INVAGINATION IN VOLVOX

A. Biological background

The green algal genus Volvox [36] has become a model for the study of the evolution of multicellularity [37,38], for biological fluid dynamics [39], and for problems in developmental biology [40,41]. Adult Volvox colonies [Fig. 4(a)] are spheroidal, consisting of several thousand biflagellated somatic cells that enclose a small number of germ cells [36]. Each germ cell undergoes several rounds of cell division to form a spherical embryonic cell sheet [Figs. 4(b) and 4(e)], at which stage those cell poles whence will emanate the flagella point into the sphere [36]. To acquire motility, the embryo turns itself inside out in a process called inversion [27,42].

Fig. 4. Invagination in Volvox.

Fig. 4

(a) Volvox colony, with somatic cells and one embryo labeled. (b) Light-sheet microscopy image of a spherical Volvox embryo before inversion. (c) Corresponding image at an early stage of inversion, when a circular invagination (I) has formed. (d) Splaying of cells and bending of the cell sheet result from the formation of wedge-shaped cells and the rearrangement of the cytoplasmic bridges (CBs); red lines indicate position of CBs. (e) Midsagittal cross section of a Volvox embryo before inversion. (f) Corresponding cross section during invagination, with the regions where wedge-shaped cells (W) and contracted spindle-shaped cells (C) have formed labeled. (g) Plot of the intrinsic curvature κs0 against arclength s, defined in the inset. The plot defines the model parameters κp, κb, κa, s0, and w. Regions of cell shape changes (W, C) as in (f) are also indicated. (h) Corresponding plot of the intrinsic Stretches fs0,fϕ0, defining additional model parameters fp, fa. Panels (a)–(f) include microscopy images by Stephanie Höhn and have been redrawn from Ref. [8]. Scale bars: (a) 50 μm; (e), (f) 20 μm.

In some species of Volvox [27,28], inversion starts with the formation of a circular invagination [Figs. 4(c) and 4(f)], reminiscent of the cell sheet folds associated with processes such as gastrulation or neurulation in higher organisms. At the cell level, this invagination results from two types of cell shape changes [7,28]: (1) cells near the equator become wedge-shaped [Fig. 4(d)], while the cytoplasmic bridges (cell-cell connections resulting from incomplete division) rearrange to connect the cells at their thin wedge ends, and (2) cells in the posterior hemisphere narrow in the meridional direction. These cell shape changes arise simultaneously, with (1) splaying the cells and thereby bending the cell sheet [Fig. 4(d)] and (2) contracting the posterior hemisphere to facilitate the subsequent inversion of the posterior hemisphere inside the as yet uninverted anterior hemisphere.

At later stages of inversion, other cell shape changes arise in different parts of the cell sheet [9,28] to ease the peeling of the anterior hemisphere over the inverted posterior and thus complete inversion. In particular, the anterior hemisphere of the cell sheet thins as cells there stretch anisotropically [9,28].

B. Results

Following our earlier work [710], we model Volvox inversion by considering the deformations of an incompressible elastic spherical shell under quasistatic axisymmetric variations of its intrinsic stretches and curvatures representing the cell shape changes driving inversion. The slow speed of inversion—it takes about an hour for a Volvox embryo to turn itself inside out [27,28]—justifies this quasistatic approximation. In more detail, Figs. 4(g) and 4(h) show functional forms of the intrinsic stretches and curvatures encoding the cell shape changes driving invagination and define the model parameters κp, κb, κa, fp, fa, s0, and w that encode the intrinsic curvatures and intrinsic stretches of different regions of the cell sheet and the extent of these regions. In numerical calculations, we regularize the step discontinuities in the definitions of the intrinsic stretches and curvatures in Figs. 4(g) and 4(h), we nondimensionalize all lengths with the preinversion radius R of the embryo, and we take εh = 0.15, appropriate for Volvox globator [7,9].

We solve the governing equations derived in Appendix B numerically using the boundary value problem solver bvp4c of MATLAB (The MathWorks, Inc.) and the continuation software AUTO [43].

During the invagination stage, the radius of curvature in the bend region of wedge-shaped cells [Fig. 4(f)] becomes comparable to the thickness of the cell sheet: This is the scaling limit of large bending deformations studied in Sec. II. We therefore compare the resulting elastic model, with energy density (63), to the classical theory, in which the energy density is given by Eq. (67). For weakly invaginated stages of Volvox inversion (corresponding to small values of η in the large bending theory), the two models yield, unsurprisingly, very similar shapes [Fig. 5(a)], mirrored by very similar profiles of meridional shell strain [Fig. 5(b)] and meridional curvature strain [Fig. 5(c)]. The contraction of the posterior hemisphere leads to thickening of the cell sheet there [Fig. 5(a)]. However, the more the intrinsic configuration of the cell sheet approaches the limit of cell constriction, the more the shapes resulting from the two models differ [Fig. 5(d)]. Correspondingly, the meridional shell strain [Fig. 5(e)] and meridional curvature strain [Fig. 5(f)] in the two models differ increasingly. It may seem counterintuitive that these strains are larger in the bend region of nearly constricted cells for the large-bending model than for the classical model [Figs. 5(e) and 5(f)], since the stretching and bending cost of these larger strains is much higher in the large-bending model than in the classical model. Indeed, on computing the stretching and bending energies (not shown) of the shapes in Fig. 5(d), we find them to be much larger in the large-bending model than in the classical model. However, these large energies are balanced by a correspondingly large and negative coupling energy: for example, Es < 0 and Ks > 0 in the bend region [Figs. 5(e) and 5(f)], while η<0β¯ss>0 [Fig. 3(b)], and so β¯ssEsKs<0. This negative coupling energy therefore explains the large strains in the bend region that arise in the large-bending model.

Fig. 5.

Fig. 5

Comparison of the elastic model for large bending deformations and the classical model. Solid lines: Large bending model with energy density given by Eq. (63); dashed lines: classical model with energy density given by Eq. (67). (a) Early invagination stage: the two models yield very similar shapes. Thick lines: Midline of the cell sheet. Thin lines and shaded area: Transverse extent of the shell, illustrating the thickness variations resulting from the cell shape changes. Dotted line: midline of the undeformed spherical shell. Parameter values: κp = κa = 1, κb = −2, fp = 0.8, fa = 1, s0 =1.5, w = 0.2. (b) Corresponding plot of the meridional shell strain Es. The grey shaded area marks the bend region s0w < s < s0. (c) Corresponding plot of the meridional curvature strain Ks. (d) Later invagination stage: As the cells in the bend region approach the constriction limit, the shapes resulting from the two models differ increasingly. Parameter values are as in (a), except κb = −8.5, w = 0.5. (e) Corresponding plot of the meridional shell strain Es. (f) Corresponding plot of the meridional curvature strain Ks. (g) Bifurcation diagram, for different values of w, in (k, d) space, where k = −κb and d is the posterior displacement defined in the axis inset. Different lines correspond to parameter values w = 0.3, 0.5, 0.6, 0.7, 0.8, 0.9. Other parameter values are as in (a). The vertical line |η| = 1 corresponding to the constriction limit is also shown. For w > w* (in the large bending model) or w>w0 (in the classical model), discontinuous jumps in d, denoted by vertical arrows, arise as k is increased. The thick lines correspond to w = 0.6 and show that w>w0.

The largest curvature strains [Fig. 5(f)] arise, however, in the anterior fold, i.e., in the second bend region that arises as a passive mechanical consequence of the wedge-shaped cells in the bend region just next to it [7,9]. As a result of the contraction of the posterior hemisphere, the cell sheet is thinner in the anterior [Fig. 5(d)], and hence is easier to bend there, as discussed earlier. In fact, around the invagination stage in Fig. 5(d), cells in the anterior fold begin to stretch in the meridional direction [9,28], leading to further thinning and increased bendability of the cell sheet there.

The examples in Figs. 5(a) and 5(d) indicate that the results of the two models differ at a quantitative, if not at a qualitative level. We extend this observation by plotting, for both models, k = −κb against the displacement d of the posterior pole [Fig. 5(g), inset] for different values of the width w of the bend region in Fig. 5(g). Again, the solution curves show similar behavior in the two models, but differ at a quantitative level. They confirm what one observes in Fig. 5(d), that the cell sheet is more invaginated, at the same parameter values and for sufficiently large k, in the classical model than in the large-bending model. Nonetheless, the cell sheet invaginates completely even in the large-bending model as w increases [Fig. 5(g)], i.e., as more cells become wedge-shaped and the bend region widens, as observed during Volvox inversion [28]. Moreover, one can argue that invagination is actually more stable in the large-bending model: There is a critical bend region width, w* in the large-bending model and w0 in the classical model, such that the solution curves in the (k, d) diagram are single-valued for w < w* or w<w0, but become multivalued for w > w* or w<w0, respectively, leading to discontinuous jumps in d as k is varied. Where multiple solutions exist for a given value of k, the one with the lowest value of d has the lowest energy (not shown). For the classical theory, we have discussed this bifurcation behavior in Ref. [8], and rationalized it by constructing an effective energy that estimates different elastic contributions. It is therefore not surprising that, here, we find qualitatively identical bifurcation behavior in the two models, but that again, there are quantitative differences in the bifurcation behavior. However, Fig. 5(g) shows that w*>w0. In other words, continuous invagination is possible in a larger region of parameter space in the large bending theory than in the classical theory: in this sense, invagination is stabilized in the large-bending theory.

This discussion shows how the geometry of large bending deformations modifies the mechanical picture of invagination suggested by the classical theory. When we introduced the problem of large bending deformations, we argued that classical shell theories cannot describe these deformations because of the assumption of large radii of curvature inherent in them. At this stage, we must therefore ask: can the large-bending theory derived here provide a complete description of the mechanics of invagination? This is first a question of self-consistency: Is the intrinsic configuration not too incompatible? In other words, are the deformations resulting from the imposed intrinsic stretches and curvatures consistent with the scalings (31) and (32) assumed in the derivation of the shell theory? Even for the late invagination stage in Fig. 5(d), the meridional shell strain remains small [Fig. 5(e)], although the meridional curvature strain reaches values of order O(1/ε) [Fig. 5(f)]. Of course, the invagination stage in Fig. 5(d) does not satisfy the restriction 1|η|ε of our shell theory discussed earlier. This kind of condition is particularly restrictive for biological tissues in which ε is not “that small” (Fig. 1). While results remain qualitatively unchanged for somewhat smaller values of |η| within that range of validity, this hints that understanding the elasticity of the constriction limit |η| → 1 remains a key open problem for future work.

VI. Conclusion

In this paper, we have derived a morphoelastic shell theory valid for the large bending deformations that are commonly observed in developmental biology (Fig. 1), and have shown how this scaling limit of large bending deformations induces a purely geometric effective material anisotropy absent from classical shell theories. Taking the invagination of the green alga Volvox as an example, we have compared this large-bending theory to a simpler, classical theory not formally valid for large bending deformations. Since the classical theory does not account for the geometric material anisotropy or the singularity of cell constriction, it differs, for strongly invaginated shapes as in Figs. 1(b), 4(c), and 4(f), from the theory for large bending deformation at a quantitative, if not at a qualitative level. In particular, we have argued that these geometric effects stabilize Volvox invagination.

This and the growing interest in quantitative rather than merely qualitative analyses of morphogenesis [44,45] emphasize the importance of this scaling limit of large bending deformations for studies of the mechanics of developmental biology. The theory we have derived here is not, however, the most general theory of these large bending deformations. Indeed, when writing down the expression for the intrinsic deformation gradient in Eq. (24), we assumed that there is no intrinsic displacement parallel to the midsurface, 𝜍0 = 0. The nonlinear differential equations extending Eqs. (39) and (40) that arise in the expansions of the boundary and incompressibility conditions for 𝜍0 ≠ 0 still admit a trivial solution p(0) = 1, Z(0)Z0, S(0)S0, where S0=fs0fϕ0𝜍0.We were, however, unable to extend our calculations in Sec. II to prove that this solution is unique; a similar issues arises when extending the calculations of this paper to more general constitutive relations, as discussed below and in Appendix C. It therefore remains unclear what form the extension of the Kirchhoff “hypothesis” [15] to this case takes.

In this paper, we assumed the simplest, incompressible neo-Hookean constitutive relations when deriving our shell theory for large bending deformations. The restriction to incompressible elastic materials is justified by the biological context of our analysis, in which the models derived here describe sheets of fluid-filled cells that are therefore indeed incompressible to a first approximation. However, the bulk elastic response of biological materials such as brain tissue is not linear [4648]. The restriction to linear neo-Hookean relations may therefore appear to be a limitation of the analysis, but that turns out not to be the case: in the thin shell limit, general hyperelastic constitutive relations reduce to neo-Hookean relations. This result has been established previously for thin plates [20,49], and, in Appendix C, we (partially) extend it to the large bending deformations of thin shells considered here. In the context of shell theories, the problem of specifying the nonlinear constitutive relations of biological tissues does not therefore arise. However, we have recently shown that the continuum limit of a class of discrete models of cell sheets involves not only nonlinear elastic, but also non-local, nonelastic terms [50]. Moreover, adding the geometric singularity of apical constriction (corresponding to triangular cells in the underlying discrete model) as a constraint to the variational problem that arises in this continuum limit remains an important open problem [50]. Solving this may provide a regularization of the singularity that breaks asymptoticity as |η| →1 in the theory derived here, and hence a yet more complete mechanical picture of the bend region of wedge-shaped cells in Volvox invagination [Fig. 4(d)]. Meanwhile, all of this suggests that the journey toward understanding the continuum mechanics of biological materials, on which we have taken another step with the present analysis of large bending deformations of thin elastic shells, will continue to abound with new problems in nonlinear mechanics.

Supplementary Material

Supplementary Materials

Acknowledgments

We thank two anonymous referees for helpful reports and, in particular, incisive questions bearing on the definition of the intrinsic configuration. We also thank S. S. M. H. Höhn for discussions about Volvox inversion, M. Gomez for comments on the paper, and A. Goriely and C. P. Turner for a discussion of tensor algebraic matters. We gratefully acknowledge support from the Engineering and Physical Sciences Research Council (Established Career Fellowship EP/M017982/1 to R.E.G.), the Wellcome Trust (Investigator Award 207510/Z/17/Z to R.E.G.), Magdalene College, Cambridge (Nevile Research Fellowship to P.A.H.), and a Hooke Research Fellowship (P.A.H.).

References

  • [1].Keller R, Davidson LA, Shook DR. How we are shaped: The biomechanics of gastrulation. Differentiation. 2003;71:171. doi: 10.1046/j.1432-0436.2003.710301.x. [DOI] [PubMed] [Google Scholar]
  • [2].Leptin M. Gastrulation movements: The logic and the nuts and bolts. Dev Cell. 2005;8:305. doi: 10.1016/j.devcel.2005.02.007. [DOI] [PubMed] [Google Scholar]
  • [3].Lecuit T, Lenne P-F. Cell surface mechanics and the control of cell shape, tissue patterns and morphogenesis. Nat Rev Mol Cell Biol. 2007;8:633. doi: 10.1038/nrm2222. [DOI] [PubMed] [Google Scholar]
  • [4].Keller R, Shook D. The bending of cell sheets—From folding to rolling. BMC Biol. 2011;9:90. doi: 10.1186/1741-7007-9-90. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [5].Lecuit T, Lenne P-F, Munro E. Force generation, transmission, and integration during cell and tissue morphogenesis. Annu Rev Cell Dev Biol. 2011;27:157. doi: 10.1146/annurev-cellbio-100109-104027. [DOI] [PubMed] [Google Scholar]
  • [6].Tada M, Heisenberg C-P. Convergent extension: Using collective cell migration and cell intercalation to shape embryos. Development. 2012;139:3897. doi: 10.1242/dev.073007. [DOI] [PubMed] [Google Scholar]
  • [7].Höhn S, Honerkamp-Smith AR, Haas PA, Khuc Trong P, Goldstein RE. Dynamics of a Volvox Embryo Turning Itself Inside Out. Phys Rev Lett. 2015;114:178101. doi: 10.1103/PhysRevLett.114.178101. [DOI] [PubMed] [Google Scholar]
  • [8].Haas PA, Goldstein RE. Elasticity and glocality: Initiation of embryonic inversion in Volvox. J R Soc Interface. 2015;12:20150671. doi: 10.1098/rsif.2015.0671. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [9].Haas PA, Höhn SSMH, Honerkamp-Smith AR, Kirkegaard JB, Goldstein RE. The noisy basis of morphogenesis: Mechanisms and mechanics of cell sheet folding inferred from developmental variability. PLoS Biol. 2018;16:e2005536. doi: 10.1371/journal.pbio.2005536. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [10].Haas PA, Goldstein RE. Embryonic inversion in Volvox carteri: The flipping and peeling of elastic lips. Phys Rev E. 2018;98:052415. doi: 10.1103/PhysRevE.98.052415. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [11].Heer NC, Miller PW, Chanet S, Stoop N, Dunkel J, Martin AC. Actomyosin-based tissue folding requires a multicellular myosin gradient. Development. 2017;144:1876. doi: 10.1242/dev.146761. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [12].Yevick HG, Miller PW, Dunkel J, Martin AC. Structural redundancy in supracellular actomyosin networks enables robust tissue folding. Dev Cell. 2019;50:586. doi: 10.1016/j.devcel.2019.06.015. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [13].Miller PW, Stoop N, Dunkel J. Geometry of Wave Propagation on Active Deformable Surfaces. Phys Rev Lett. 2018;120:268001. doi: 10.1103/PhysRevLett.120.268001. [DOI] [PubMed] [Google Scholar]
  • [14].Ciarlet PG. An introduction to differential geometry with applications to elasticity. J Elasticity. 2005;78:1. [Google Scholar]
  • [15].Audoly B, Pomeau Y. Elasticity and Geometry. Oxford University Press; Oxford, UK: 2010. Chap. 6, pp. 159–213; Chap. 12, pp. 35–453; and App. D, pp. 571–581. [Google Scholar]
  • [16].Steigmann DJ. Koiter’s shell theory from the perspective of three-dimensional nonlinear elasticity. J Elasticity. 2013;111:91. [Google Scholar]
  • [17].Goriely A. The Mathematics and Mechanics of Biological Growth. Springer; Berlin, Germany: 2017. Chap. 11, pp. 261–344 and Chap. 12, pp. 345–373. [Google Scholar]
  • [18].Ambrosi D, Ben Amar M, Cyron CJ, De Simone A, Goriely A, Humphrey JD, Kuhl E. Growth and remodelling of living tissues: Perspectives, challenges and opportunities. J R Soc Interface. 2019;16:20190233. doi: 10.1098/rsif.2019.0233. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [19].Rodriguez EK, Hoger A, McCulloch AD. Stress-dependent finite growth in soft elastic tissues. J Biomech. 1994;27:455. doi: 10.1016/0021-9290(94)90021-3. [DOI] [PubMed] [Google Scholar]
  • [20].Dervaux J, Ben Amar M. Morphogenesis of Growing Soft Tissues. Phys Rev Lett. 2008;101:068101. doi: 10.1103/PhysRevLett.101.068101. [DOI] [PubMed] [Google Scholar]
  • [21].Dervaux J, Ciarletta P, Ben Amar M. Morphogenesis of thin hyperelastic plates: A constitutive theory of biological growth in the Föppl–von Kármán limit. J Mech Phys Solids. 2009;57:458. [Google Scholar]
  • [22].McMahon J, Goriely A, Tabor M. Nonlinear morphoelastic plates I: Genesis of residual stress. Math Mech Solids. 2011;16:812. [Google Scholar]
  • [23].Efrati E, Sharon E, Kupferman R. Elastic theory of unconstrained non-Euclidean plates. J Mech Phys Solids. 2009;57:762. [Google Scholar]
  • [24].Sadik S, Angoshtari A, Goriely A, Yavari A. A geometric theory of nonlinear morphoelastic shells. J Nonlinear Sci. 2016;26:929. [Google Scholar]
  • [25].Ventsel E, Krauthammer T. Thin Plates and Shells: Theory, Analysis, and Applications. Marcel Dekker; New York, NY: 2001. Chap. 12, pp. 325–347. [Google Scholar]
  • [26].Libai A, Simmonds JG. The Nonlinear Theory of Elastic Shells. 2nd ed. Cambridge University Press; Cambridge, UK: 2005. Chap. V, pp. 1597#x2013;342. [Google Scholar]
  • [27].Hallmann A. Morphogenesis in the family Volvocaceae: Different tactics for turning an embryo right-side out. Protist. 2006;157:445. doi: 10.1016/j.protis.2006.05.010. [DOI] [PubMed] [Google Scholar]
  • [28].Höhn S, Hallmann A. There is more than one way to turn a spherical cellular monolayer inside out: Type B embryo inversion in Volvox globator. BMC Biol. 2011;9:89. doi: 10.1186/1741-7007-9-89. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [29].Conte V, Ulrich F, Baum B, Muñoz J, Veldhuis J, Brodland W, Miodownik M. A biomechanical analysis of ventral furrow formation in the Drosophila melanogaster embryo. PLoS ONE. 2012;7:e34473. doi: 10.1371/journal.pone.0034473. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [30].Janet M. Sur la possibilité de plonger un espace riemannien donné dans un espace euclidien. Ann Soc Pol Math. 1926;5:38. [Google Scholar]
  • [31].Cartan É. Sur la possibilité de plonger un espace riemannien donné dans un espace euclidien. Ann Soc Pol Math. 1927;6:1. [Google Scholar]
  • [32].Ogden RW. Non-linear Elastic Deformations. Dover; Mineola, NY: 1997. Chap. 1, pp. 1–72; Chap. 2.2, pp. 83–121; Chap. 3.4, pp. 152–155; and Chap. 6.1, pp. 328–351. [Google Scholar]
  • [33].Expansions were carried out using MATHEMATICA (Wolfram, Inc.) to assist with manipulating the complicated algebraic expressions that arise in these calculations.
  • [34].Pezzulla M, Stoop N, Jiang X, Holmes DP. Curvature-driven morphing of non-Euclidean shells. Proc R Soc A. 2017;473:20170087. doi: 10.1098/rspa.2017.0087. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [35].Reddy JN. Theory and Analysis of Elastic Plates and Shells. 2nd ed. CRC Press; Boca Raton, FL: 2007. Chap. 10, pp. 359–402. [Google Scholar]
  • [36].Kirk DL. Volvox: Molecular-Genetic Origins of Multicellularity and Cellular Differentiation. Cambridge University Press; Cambridge, UK: 1998. [Google Scholar]
  • [37].Kirk DL. A twelve-step program for evolving multicellularity and a division of labor. BioEssays. 2005;27:299. doi: 10.1002/bies.20197. [DOI] [PubMed] [Google Scholar]
  • [38].Herron MD. Origins of multicellular complexity: Volvox and the volvocine algae. Mol Ecol. 2016;25:1213. doi: 10.1111/mec.13551. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [39].Goldstein RE. Green algae as model organisms for biological fluid dynamics. Annu Rev Fluid Mech. 2015;47:343. doi: 10.1146/annurev-fluid-010313-141426. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [40].Kirk DL, Nishii I. Volvox carteri as a model for studying the genetic and cytological control of morphogenesis. Dev Growth Differ. 2001;43:621. doi: 10.1046/j.1440-169x.2001.00612.x. [DOI] [PubMed] [Google Scholar]
  • [41].Matt G, Umen J. Volvox: A simple algal model for embryogenesis, morphogenesis and cellular differentiation. Dev Biol. 2016;419:99. doi: 10.1016/j.ydbio.2016.07.014. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [42].Desnitskiy AG. Comparative analysis of embryonic inversion in algae of the genus Volvox (Volvocales, Chlorophyta) Russ J Dev Biol. 2018;49:129. [Google Scholar]
  • [43].Doedel EJ, Oldman BE, Champneys AR, Dercole F, Fairgrieve T, Kuznetsov Y, Paffenroth R, Sandstede B, Wang X, Zhang C. AUTO-07P: Continuation and Bifurcation Software for Ordinary Differential Equations Tech Rep. Concordia University; Montreal, Canada: 2012. [Google Scholar]
  • [44].Cooper WJ, Albertson RC. Quantification and variation in experimental studies of morphogenesis. Dev Biol. 2008;321:295. doi: 10.1016/j.ydbio.2008.06.025. [DOI] [PubMed] [Google Scholar]
  • [45].Oates AC, Gorfinkel N, González-Gaitán M, Heisenberg C-P. Quantitative approaches in developmental biology. Nat Rev Gen. 2009;10:517. doi: 10.1038/nrg2548. [DOI] [PubMed] [Google Scholar]
  • [46].Mihai LA, Chin L, Janmey PA, Goriely A. A comparison of hyperelastic constitutive models applicable to brain and fat tissues. J R Soc Interface. 2015;12:20150486. doi: 10.1098/rsif.2015.0486. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [47].Mihai LA, Budday S, Holzapfel GA, Kuhl E, Goriely A. A family of hyperelastic models for human brain tissue. J Mech Phys Solids. 2017;106:60. [Google Scholar]
  • [48].Budday S, Sommer G, Birkl C, Langkammer C, Haybaeck J, Kohnert J, Bauer M, Paulsen F, Steinmann P, Kuhl E, Holzapfel GA. Mechanical characterization of human brain tissue. Acta Biomater. 2017;48:319. doi: 10.1016/j.actbio.2016.10.036. [DOI] [PubMed] [Google Scholar]
  • [49].Erbay HA. On the asymptotic membrane theory of thin hyperelastic plates. Int J Eng Sci. 1997;35:151. [Google Scholar]
  • [50].Haas PA, Goldstein RE. Nonlinear and nonlocal elasticity in coarse-grained differential-tension models of epithelia. Phys Rev E. 2019;99:022411. doi: 10.1103/PhysRevE.99.022411. [DOI] [PMC free article] [PubMed] [Google Scholar]
  • [51].Kreyszig E. Introduction to Differential Geometry and Riemannian Geometry. University of Toronto Press; Toronto, ON: 1968. Chap. 4, pp. 78–99 and Chap. 6, pp. 125–136. [Google Scholar]
  • [52].Block matrices will represent tensors with respect to tensor products of a left tangent basis and right dual basis, so can be multiplied without incurring metric factors and traces can be computed without raising or lowering indices. In fact, the indices of the entries of these block matrices (and also of the matrices that appear as their components) will never be raised or lowered. In particular, transposes are understood to be matrix transposes, so do not change the covariant or contravariant nature of indices
  • [53].Bernstein DS. Matrix Mathematics: Theory, Facts, and Formulas. 2nd ed. Princeton University Press; Princeton, NJ: 2009. Chap. 2.8, pp. 115–119 and Chap. 4.4, pp. 261–267. [Google Scholar]
  • [54].Yavari A, Goriely A. Riemann–Cartan geometry of nonlinear dislocation mechanics. Arch Ration Mech Anal. 2012;205:59. This result is doubtless known in the solid mechanical literature: e.g., it appears without proof as Eq. (5.8) of. [Google Scholar]
  • [55].The indices in Eq. (A28) are raised or lowered with different metrics, g˜ and g0, which are asymptotically close to each other by Eq. (A26b). Hence taking tensor transposes explicitly by multiplying matrices by the appropriate metrics enables us to impose the asymptotic scaling (A26b) during the asymptotic expansion. This is the reason why transposes in our block matrix notation [52] are matrix transposes rather than tensor transposes
  • [56].Horn RA, Johnson CR. Matrix Analysis. Cambridge University Press; Cambridge, UK: 1985. Chap. 1.3, pp. 44–57; Chap. 4.1, pp. 169–176; and Chap. 7.2, pp. 402–411. [Google Scholar]
  • [57].Gregory AL, Lasenby J, Agarwal A. The elastic theory of shells using geometric algebra. R Soc Open Sci. 2017;4:170065. doi: 10.1098/rsos.170065. [DOI] [PMC free article] [PubMed] [Google Scholar]

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