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Sheaves on quoric manifolds

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Abstract

Quoric manifolds are quaternionic analogues of quasitoric manifolds introduced by Hopkinson. Given a quoric manifold over a simple polytope, we study the stratification induced by the faces of the polytope. We then show that the equivariant derived category of constructible sheaves with respect to the face stratification is equivalent to the derived category of constructible DG-modules over a DG-algebra defined on the orbit space. Finally, we prove that the associated DG-algebra is formal.

Introduction

There were two motivations for this work. The first was to study quoric manifolds [15] from a sheaf-theoretic perspective and in particular, to understand how their equivariant topology is reflected in the associated categories of equivariant and constructible sheaves. The second was to investigate whether Lunts’ techniques for toric varieties [19] can be applied to quoric manifolds. In particular, we wanted to determine whether the equivariant derived category of constructible sheaves on quoric manifolds admits a description in terms of the geometry of the orbit space and the isotropy data of the underlying group action.

In this paper we show that the equivariant derived category of constructible sheaves on a quoric manifold is equivalent to the derived category of constructible DG-modules over a sheaf of DG-algebras on the face poset of the orbit polytope. We further show that this sheaf of DG-algebras is formal, that is, quasi-isomorphic to its cohomology sheaf.

Equivariant derived categories of sheaves

Sheaf theory was introduced by Leray in the 1940s and developed in the following decade. Its basic principle is to organise local data on a space XX into global invariants: sheaves on XX form an abelian category Sh⁡(X)\operatorname{Sh}(X), and the global sections functor assigns to each sheaf its global invariants. This functor, and more generally the direct image f∗f_* along a continuous map ff, is only left exact, and its failure to preserve short exact sequences is measured by higher direct images, in particular by sheaf cohomology. These higher terms are organised in the derived category, obtained from complexes of sheaves by localising at quasi-isomorphisms. There they become single functors f∗f_*, which together with f∗f^*, ⊗\otimes, f!f_!, f!f^! and Verdier duality form the six operations [18].

This formalism is especially fruitful when XX carries extra structure. If XX is stratified, one restricts to complexes whose cohomology sheaves are constructible, that is, locally constant of finite rank along the strata. For suitable stratifications this subcategory is stable under the six operations and relates the local topology of the strata to the global structure of XX. If a group GG acts on XX, one obtains the abelian category Sh⁡G(X)\operatorname{Sh}_G(X) of GG-equivariant sheaves. Its naive derived category does not retain equivariant cohomology: for connected GG and X=ptX = \mathrm{pt} it gives D(Vect⁡)D(\operatorname{Vect}), whereas the equivariant cohomology of a point is H∗(BG)H^*(BG). This was addressed by Bernstein and Lunts [4], who define DG(X)D_G(X) by resolving XX by the free GG-spaces X×EX \times E and descending to the quotients X×GEX \times_G E, where EE approximates EGEG. The resulting category carries the functors f∗f^*, f∗f_*, f!f^!, f!f_! and the usual adjunctions. Combining the two structures gives the equivariant derived category DG,c(X)D_{G,c}(X) of constructible sheaves.

Toric varieties are the model case in which the group action, the stratification and the equivariant derived category are all controlled by combinatorics. A normal toric variety X=XΣX = X_\Sigma is a complex algebraic variety with an action of the algebraic torus Tn:=(C∗)nT^n := (\mathbb{C}^*)^n and a dense open orbit. It has finitely many TnT^n-orbits OσO_\sigma, in bijection with the cones σ\sigma of the fan Σ\Sigma, with dim⁡Oσ=n−dim⁡σ\dim O_\sigma= n - \dim\sigma. Lunts [19] described the bounded TnT^n-equivariant derived category DTn,cb(X)D^b_{T^n,c}(X) of sheaves constructible with respect to the orbit stratification algebraically. It is equivalent to the derived category of DG-modules over a differential graded algebra, which is the Ext-algebra of the direct sum of the simple equivariant perverse sheaves attached to the orbits, and which is formal. Lunts also conjectured that an analogous description holds for a complex reductive group acting on a projective variety with finitely many orbits; this conjecture was extended in a number of directions [14 Bal09, 23 Jos22a]

In this paper we take a first step towards a real-topological analogue of this conjecture. We replace the complex reductive group by the compact Lie group QnQ^n, a product of copies of the group Q≅SU(2)Q \cong\mathrm{SU}(2) of unit quaternions, and the projective variety by a quoric manifold M4nM^{4n}, the quaternionic analogue of a quasitoric manifold, the latter being a topological analogue of a toric variety [8]. This is a 4n4n-dimensional manifold with an action of QnQ^n whose orbit space is a simple nn-polytope PnP^n. As in the toric case, the faces of PnP^n induce a finite stratification of M4nM^{4n}. Our results are an equivalence of DQn,cb(M4n)D^b_{Q^n,c}(M^{4n}) with the derived category of DG-modules over a sheaf of DG-algebras on the face poset of PnP^n (Theorem 4.13), and the formality of this sheaf of DG-algebras (Theorem 5.6).

Quoric manifolds, stratifications and the Borel construction

Quoric manifolds were introduced by Hopkinson [15], building on earlier work of Scott [24], as quaternionic analogues of the quasitoric manifolds of Davis and Januszkiewicz [8], which are themselves topological analogues of toric varieties [10]. A quoric manifold is a smooth 4n4n-dimensional manifold with a smooth locally regular action of Qn=(S3)nQ^n = (S^3)^n whose orbit space is a simple nn-dimensional polytope (Definition 2.11). This contrasts with a 2n2n-dimensional quasitoric manifold, which carries an action of the compact torus Tn=(S1)nT^n = (S^1)^n. The identification of the orbit space with the polytope is understood to preserve the face structure.

As in toric topology [5], the face structure of the orbit polytope records the isotropy data of the action (§ 3.2). Since QnQ^n is non-abelian, stabilisers are recorded up to conjugacy. Over the relative interior of each face their conjugacy class is constant, although the stabiliser subgroups need not be equal, and distinct faces may carry the same conjugacy class. Thus the partition by stabiliser conjugacy classes need not have connected pieces.

Let π:M4n→Pn\pi:M^{4n}\to P^n be the orbit map, let F(Pn)\mathcal{F}(P^n) be the set of nonempty faces of PnP^n including PnP^n, and for a face FF with relative interior F˚\mathring{F} put MF:=π−1(F˚)M_F:=\pi^{-1}(\mathring{F}). Then M4n=⋃F∈F(Pn)MFM^{4n}=\bigcup_{F\in\mathcal{F}(P^n)}M_F. We encode this decomposition by a finite topological space: the face poset (F(Pn),⊆)(\mathcal{F}(P^n),\subseteq), ordered by inclusion, with the Alexandrov topology whose open sets are the up-sets (§ 3.3). Denote it by F≤\mathcal{F}_{\leq}. The map ρP:Pn→F≤\rho_P:P^n\to\mathcal{F}_{\leq}, $\rho_P(x)=F for x∈F˚x \in\mathring{F}, is continuous and open, and so is

πF:=ρP∘π:M4n⟶F⪯,\pi_{\mathcal{F}} := \rho_P \circ\pi: M^{4n} \longrightarrow\mathcal{F}_{\preceq},

whose fibres are precisely the subsets MFM_F. Our first main result is the following.

Theorem (Theorem 2.27). Let M4nM^{4n} be a quoric manifold over a simple polytope PnP^n. Then πF:M4n⟶F⪯\pi_{\mathcal{F}}: M^{4n} \longrightarrow\mathcal{F}_{\preceq} defines a poset-stratified space, and the decomposition M4n=⋃FπF−1(F)M^{4n} = \bigcup_F \pi_{\mathcal{F}}^{-1}(F) is a finite stratification of M4nM^{4n}.

The face stratification coincides with the connected components of the orbit-type Whitney stratification (Corollary 2.31) and extends to the Borel construction. Let ENQn=(S4N+3)nE_NQ^n = (S^{4N+3})^n and EQn=⋃NENQnEQ^n = \bigcup_N E_NQ^n. In § 3.5 we study the Borel space construction of a quoric manifold

MQ:=EQn×QnM4n=⋃NENQn×QnM4nM_Q := EQ^n \times_{Q^n} M^{4n} = \bigcup_N E_NQ^n \times_{Q^n} M^{4n}

together with the projection bQ:MQ⟶F⪯b_Q: M_Q \longrightarrow\mathcal{F}_{\preceq}, [e,m]↦πF(m)[e,m] \mapsto\pi_{\mathcal{F}}(m). For a face FF let UF={G∈F(Pn)∣F⪯G}U_F = \{G \in\mathcal{F}(P^n) \mid F \preceq G\} be its minimal open neighborhood and VF,Q:=bQ−1(UF)V_{F,Q} := b_Q^{-1}(U_F) the corresponding open star. Our second main result is the following.

Theorem (Propositions 2.33 and 2.34). Let FF be a face of PnP^n of codimension kk and f∈F˚f \in\mathring{F}. Then EQn×QnMF≃Bλb(F)≃BQkEQ^n \times_{Q^n} M_F \simeq B\lambda^b(F) \simeq BQ^k, and the open star VF,QV_{F,Q} deformation retracts onto EQn×QnOf≃Bλb(F)EQ^n \times_{Q^n} O_f \simeq B\lambda^b(F), where Of=π−1(f)O_f = \pi^{-1}(f) and λb(F)≅Qk\lambda^b(F) \cong Q^k is the isotropy group of the stratum over FF. In particular, both are connected and simply connected.

This is the topological input for the sheaf of DG-algebras of § 5.2.

Sheaves on quoric manifolds

Sheaves that retain information about both the QnQ^n-action and the face stratification are our main interest. In § 4 we study QnQ^n-equivariant sheaves on M4nM^{4n}, with the face stratification {MF}F∈F(Pn)\{M_F\}_{F\in\mathcal{F}(P^n)} as the organising structure. The aims are to compute the categories of sheaves and local systems on orbits and strata, and to use this to describe constructible and perverse sheaves.

Every stabiliser of the QnQ^n-action is connected, being isomorphic to Qk=SU(2)kQ^k = \mathrm{SU}(2)^k, and each stratum splits equivariantly as MF≅F˚×Qn/λb(F)M_F \cong\mathring{F} \times Q^n/\lambda^b(F). Since SU(2)\mathrm{SU}(2) is simply connected and F˚\mathring{F} is contractible, every stratum is simply connected. This gives two computations.

  • Orbits. The equivariant category of an orbit Qn/HQ^n/H is Rep⁡(π0(H))\operatorname{Rep}(\pi_0(H)), and π0(H)\pi_0(H) is trivial for every stabiliser. Hence Sh⁡Qn(Qn⋅m)\operatorname{Sh}_{Q^n}(Q^n \cdot m), Loc⁡(Qn⋅m)\operatorname{Loc}(Q^n \cdot m) and Loc⁡Qn(Qn⋅m)\operatorname{Loc}_{Q^n}(Q^n \cdot m) are all equivalent to Vect⁡C\operatorname{Vect}_{\mathbb{C}}, so an equivariant sheaf on an orbit is constant.

  • Strata. Sh⁡Qn(MF)≃Sh⁡(F˚)\operatorname{Sh}_{Q^n}(M_F) \simeq\operatorname{Sh}(\mathring{F}), so the group action carries no extra data on a stratum, and Loc⁡(MF)≃Loc⁡Qn(MF)≃Vect⁡C\operatorname{Loc}(M_F) \simeq\operatorname{Loc}_{Q^n}(M_F) \simeq\operatorname{Vect}_{\mathbb{C}}. The proofs use the vanishing of π1\pi_1 of the stratum and of its Borel construction EQn×QnMF≃Bλb(F)EQ^n \times_{Q^n} M_F \simeq B\lambda^b(F).

All of the above have been well studied in general. Our aim is to carry out explicit calculations in the case of quoric manifolds. Our third main result is the following.

Theorem (Theorem 3.37). Let M4nM^{4n} be a quoric manifold with the natural face stratification {MF}F∈F(Pn)\{M_F\}_{F\in\mathcal{F}(P^n)}.

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