Algebraic and Topological Properties of Big Mapping Class Groups
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[Math.GT] 9 Jul 2003
LOW-DIMENSIONAL HOMOLOGY GROUPS OF MAPPING CLASS GROUPS: A SURVEY MUSTAFA KORKMAZ Abstract. In this survey paper, we give a complete list of known re- sults on the first and the second homology groups of surface mapping class groups. Some known results on higher (co)homology are also men- tioned. 1. Introduction n Let Σg,r be a connected orientable surface of genus g with r boundary n components and n punctures. The mapping class group of Σg,r may be defined in different ways. For our purpose, it is defined as the group of the n n isotopy classes of orientation-preserving diffeomorphisms Σg,r → Σg,r. The diffeomorphisms and the isotopies are assumed to fix each puncture and the n points on the boundary. We denote the mapping class group of Σg,r by n Γg,r. Here, we see the punctures on the surface as distinguished points. If r and/or n is zero, then we omit it from the notation. We write Σ for the n surface Σg,r when we do not want to emphasize g,r,n. The theory of mapping class groups plays a central role in low-dimensional n topology. When r = 0 and 2g + n ≥ 3, the mapping class group Γg acts properly discontinuously on the Teichm¨uller space which is homeomorphic to some Euclidean space and the stabilizer of each point is finite. The quotient of the Teichm¨uller space by the action of the mapping class group is the moduli space of complex curves. Recent developments in low-dimensional topology made the algebraic structure of the mapping class group more important. -
NOTES on the TOPOLOGY of MAPPING CLASS GROUPS Before
NOTES ON THE TOPOLOGY OF MAPPING CLASS GROUPS NICHOLAS G. VLAMIS Abstract. This is a short collection of notes on the topology of big mapping class groups stemming from discussions the author had at the AIM workshop \Surfaces of infinite type". We show that big mapping class groups are neither locally compact nor compactly generated. We also show that all big mapping class groups are homeomorphic to NN. Finally, we give an infinite family of big mapping class groups that are CB generated and hence have a well-defined quasi-isometry class. Before beginning, the author would like to make the disclaimer that the arguments contained in this note came out of discussions during a workshop at the American Institute of Mathematics and therefore the author does not claim sole credit, espe- cially in the case of Proposition 10 in which the author has completely borrowed the proof. For the entirety of the note, a surface is a connected, oriented, second countable, Hausdorff 2-manifold. The mapping class group of a surface S is denoted MCG(S). A mapping class group is big if the underlying surface is of infinite topological type, that is, if the fundamental group of the surface cannot be finitely generated. 1.1. Topology of mapping class groups. Let C(S) denote the set of isotopy classes of simple closed curves on S. Given a finite collection A of C(S), let UA = ff 2 MCG(S): f(a) = a for all a 2 Ag: We define the permutation topology on MCG(S) to be the topology with basis consisting of sets of the form f · UA, where A ⊂ C(S) is finite and f 2 MCG(S). -
The Birman-Hilden Theory
THE BIRMAN{HILDEN THEORY DAN MARGALIT AND REBECCA R. WINARSKI Abstract. In the 1970s Joan Birman and Hugh Hilden wrote several papers on the problem of relating the mapping class group of a surface to that of a cover. We survey their work, give an overview of the subsequent developments, and discuss open questions and new directions. 1. Introduction In the early 1970s Joan Birman and Hugh Hilden wrote a series of now- classic papers on the interplay between mapping class groups and covering spaces. The initial goal was to determine a presentation for the mapping class group of S2, the closed surface of genus two (it was not until the late 1970s that Hatcher and Thurston [33] developed an approach for finding explicit presentations for mapping class groups). The key innovation by Birman and Hilden is to relate the mapping class group Mod(S2) to the mapping class group of S0;6, a sphere with six marked points. Presentations for Mod(S0;6) were already known since that group is closely related to a braid group. The two surfaces S2 and S0;6 are related by a two-fold branched covering map S2 ! S0;6: arXiv:1703.03448v1 [math.GT] 9 Mar 2017 The six marked points in the base are branch points. The deck transforma- tion is called the hyperelliptic involution of S2, and we denote it by ι. Every element of Mod(S2) has a representative that commutes with ι, and so it follows that there is a map Θ : Mod(S2) ! Mod(S0;6): The kernel of Θ is the cyclic group of order two generated by (the homotopy class of) the involution ι. -
Roots of Crosscap Slides and Crosscap Transpositions
Period Math Hung DOI 10.1007/s10998-017-0210-3 Roots of crosscap slides and crosscap transpositions Anna Parlak1 · Michał Stukow1 © The Author(s) 2017. This article is an open access publication Abstract Let Ng denote a closed nonorientable surface of genus g.Forg ≥ 2 the mapping class group M(Ng) is generated by Dehn twists and one crosscap slide (Y -homeomorphism) or by Dehn twists and a crosscap transposition. Margalit and Schleimer observed that Dehn twists on orientable surfaces have nontrivial roots. We give necessary and sufficient conditions for the existence of roots of crosscap slides and crosscap transpositions. Keywords Mapping class group · Nonorientable surface · Punctured sphere · Elementary braid · Crosscap slide · Crosscap transposition Mathematics Subject Classification 57N05 · 20F38 · 57M99 1 Introduction n Let Ng,s be a connected nonorientable surface of genus g with s boundary components and n punctures, that is a surface obtained from a connected sum of g projective planes Ng by removing s open disks and specifying the set ={p1,...,pn} of n distinguished points in the interior of Ng.Ifs or/and n equals zero, we omit it from notation. The mapping class M( n ) : n → n group Ng,s consists of isotopy classes of self-homeomorphisms h Ng,s Ng,s fixing () = M( n ) boundary components pointwise and such that h . The mapping class group Sg,s of an orientable surface is defined analogously, but we consider only orientation-preserving Both authors are supported by Grant 2015/17/B/ST1/03235 of National Science Centre, Poland. B Michał Stukow [email protected] Anna Parlak [email protected] 1 Institute of Mathematics, Faculty of Mathematics, Physics and Informatics, University of Gda´nsk, 80-308 Gda´nsk, Poland 123 A. -
Math.GT] 11 Aug 1998 Nec Once Opnn of Component Connected Each on Hr Xsssc an Such Exists There Has Let Ubro Udul Onsi O 2
QUADRUPLE POINTS OF REGULAR HOMOTOPIES OF SURFACES IN 3-MANIFOLDS TAHL NOWIK 1. Introduction Definition 1.1. Let F be a (finite) system of closed surfaces and M a 3-manifold. A regular homotopy Ht : F → M, t ∈ [0, 1] will be called closed if H0 = H1. We will denote a closed generic regular homotopy by CGRH. The number mod 2 of quadruple points of a generic regular homotopy Ht will be denoted by q(Ht) (∈ Z/2.) Max and Banchoff in [MB] proved that any generic regular homotopy of S2 in R3 which “turns S2 inside out,” has an odd number of quadruple points. The main point was showing that any CGRH of S2 in R3 has an even number of quadruple points. Goryunov in [G] expresses this from the Vassiliev Invariants point of view, as follows: Let Imm(S2, R3) be the space of all immersions of S2 in R3, and let ∆ ⊆ Imm(S2, R3) be the subspace of all non-generic immersions. Choose some 2 3 2 3 generic immersion f0 : S → R as a base immersion. For any generic immersion f : S → R let Q(f) ∈ Z/2 be defined as q(Ht) where Ht is some generic regular homotopy between f0 and f. 2 3 There exists such an Ht since Imm(S , R ) is connected, and this is well defined since any CGRH has q = 0. Furthermore, since generic immersions do not have quadruple points, Q will be constant on each connected component of Imm(S2, R3) − ∆. [G] then raises the question whether such a Q may be defined for any surface in R3, that is, whether for any CGRH of any surface in R3 the number of quadruple points is 0 mod 2. -
Arxiv:1706.08798V1 [Math.GT] 27 Jun 2017
WHAT'S WRONG WITH THE GROWTH OF SIMPLE CLOSED GEODESICS ON NONORIENTABLE HYPERBOLIC SURFACES Matthieu Gendulphe Dipartimento di Matematica Universit`adi Pisa Abstract. A celebrated result of Mirzakhani states that, if (S; m) is a finite area orientable hyperbolic surface, then the number of simple closed geodesics of length less than L on (S; m) is asymptotically equivalent to a positive constant times Ldim ML(S), where ML(S) denotes the space of measured laminations on S. We observed on some explicit examples that this result does not hold for nonorientable hyperbolic surfaces. The aim of this article is to explain this surprising phenomenon. Let (S; m) be a finite area nonorientable hyperbolic surface. We show that the set of measured laminations with a closed one{sided leaf has a peculiar structure. As a consequence, the action of the mapping class group on the projective space of measured laminations is not minimal. We determine a partial classification of its orbit closures, and we deduce that the number of simple closed geodesics of length less than L on (S; m) is negligible compared to Ldim ML(S). We extend this result to general multicurves. Then we focus on the geometry of the moduli space. We prove that its Teichm¨ullervolume is infinite, and that the Teichm¨ullerflow is not ergodic. We also consider a volume form introduced by Norbury. We show that it is the right generalization of the Weil{Petersson volume form. The volume of the moduli space with respect to this volume form is again infinite (as shown by Norbury), but the subset of hyperbolic surfaces whose one{sided geodesics have length at least " > 0 has finite volume. -
An Introduction to Mapping Class Groups. In: Clay, M
Brendle, T., and Childers, L. (2015) Surfaces and their symmetries: an introduction to mapping class groups. In: Clay, M. and Margalit, D.(eds.) Office Hours With a Geometric Group Theorist. Princeton University Press. Copyright © 2015 Princeton University Press A copy can be downloaded for personal non-commercial research or study, without prior permission or charge Content must not be changed in any way or reproduced in any format or medium without the formal permission of the copyright holder(s) When referring to this work, full bibliographic details must be given http://eprints.gla.ac.uk/101049/ Deposited on: 9 January 2015 Enlighten – Research publications by members of the University of Glasgow http://eprints.gla.ac.uk SURFACES AND THEIR SYMMETRIES: AN INTRODUCTION TO MAPPING CLASS GROUPS TARA E. BRENDLE AND LEAH CHILDERS 1. Introduction An overarching theme in mathematics is that one can learn a vast deal about an object by studying its group of symmetries. For example, in abstract algebra we study two fundamental objects in mathematics, a finite set, and a regular polygon, via symmetric groups and dihedral groups, respectively. The primary goal of this chapter is to introduce the mapping class group Mod(S), that is, the group of symmetries of another fundamental object: a surface S. We will acquaint the reader with a few of its fascinating properties and give a brief glimpse of some active research related to this class of groups. We do not assume a background in topology. Therefore in Section 2 we give an introduction to surfaces and explain the concept of a homeomorphism, our working notion of \sameness" for surfaces. -
Volume Growth in the Component of the Dehn–Seidel Twist
VOLUME GROWTH IN THE COMPONENT OF THE DEHN–SEIDEL TWIST URS FRAUENFELDER AND FELIX SCHLENK Abstract. We consider an entropy-type invariant which mea- sures the polynomial volume growth of submanifolds under the iterates of a map, and we show that this invariant is at least 1 for every diffeomorphism in the symplectic isotopy class of the Dehn– Seidel twist. Contents 1. Introduction and main results 1 2. Proofs 5 2.1. Idea of the proof of Theorem 1 5 2.2. P -manifolds 6 2.3. Twists 7 2.4. LagrangianFloerhomology 10 m 2.5. Computation of HF∗ (ϑ (Dx),Dy) 15 2.6. EndoftheproofofTheorem1 23 2.7. Proof of Corollary 1 25 2.8. A remark on smoothness 26 2.9. Differential topology of twists 26 References 29 1. Introduction and main results The complexity of a compactly supported smooth diffeomorphism ϕ of a smooth manifold M can be measured in the following way: Fix a Riemannian metric g on M. For i ∈ {1,..., dim M} denote by Σi the set of smooth embeddings σ of the cube Qi = [0, 1]i into M, and i by µg(σ) the volume of σ (Q ) ⊂ M computed with respect to the measure on σ (Qi) induced by g. Following [21], we define for each i ∈ Date: January 12, 2005. 2000 Mathematics Subject Classification. Primary 53D35, Secondary 37B40, 53D40. 1 2 Volume growth in the component of the Dehn–Seidel twist {1,..., dim M} the i-dimensional slow volume growth si(ϕ) ∈ [0, ∞] by n log µg (ϕ (σ)) si(ϕ) = sup lim inf . -
Actions of Mapping Class Groups Athanase Papadopoulos
Actions of mapping class groups Athanase Papadopoulos To cite this version: Athanase Papadopoulos. Actions of mapping class groups. L. Ji, A. Papadopoulos and S.-T. Yau. Handbook of Group Actions, Vol. I, 31, Higher Education Press; International Press, p. 189-248., 2014, Advanced Lectures in Mathematics, 978-7-04-041363-2. hal-01027411 HAL Id: hal-01027411 https://hal.archives-ouvertes.fr/hal-01027411 Submitted on 21 Jul 2014 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. ACTIONS OF MAPPING CLASS GROUPS ATHANASE PAPADOPOULOS Abstract. This paper has three parts. The first part is a general introduction to rigidity and to rigid actions of mapping class group actions on various spaces. In the second part, we describe in detail four rigidity results that concern actions of mapping class groups on spaces of foliations and of laminations, namely, Thurston’s sphere of projective foliations equipped with its projective piecewise-linear structure, the space of unmeasured foliations equipped with the quotient topology, the reduced Bers boundary, and the space of geodesic laminations equipped with the Thurston topology. In the third part, we present some perspectives and open problems on other actions of mapping class groups. -
The Stable Mapping Class Group and Stable Homotopy Theory
THE STABLE MAPPING CLASS GROUP AND STABLE HOMOTOPY THEORY IB MADSEN AND MICHAEL WEISS Abstract. This overview is intended as a lightweight companion to the long article [20]. One of the main results there is the determination of the rational cohomology of the stable mapping class group, in agreement with the Mum- ford conjecture [26]. This is part of a recent development in surface theory which was set in motion by Ulrike Tillmann’s discovery [34] that Quillen’s plus construction turns the classifying space of the stable mapping class group into an infinite loop space. Tillmann’s discovery depends heavily on Harer’s homo- logical stability theorem [15] for mapping class groups, which can be regarded as one of the high points of geometric surface theory. 1. Surface bundles without stable homotopy theory We denote by Fg,b an oriented smooth compact surface of genus g with b bound- ary components; if b = 0, we also write Fg. Let Diff(Fg,b; ∂) be the topological group of all diffeomorphisms Fg,b → Fg,b which respect the orientation and restrict to the identity on the boundary. (This is equipped with the Whitney C∞ topol- ogy.) Let Diff1(Fg,b; ∂) be the open subgroup consisting of those diffeomorphisms Fg,b → Fg,b which are homotopic to the identity relative to the boundary. Theorem 1.1. [10], [11]. If g > 1 or b > 0, then Diff1(Fg,b; ∂) is contractible. Idea of proof. For simplicity suppose that b = 0, hence g > 1. Write F = Fg = Fg,0. Let H(F ) be the space of hyperbolic metrics (i.e., Riemannian metrics of constant sectional curvature −1) on F . -
On Open Book Embedding of Contact Manifolds in the Standard Contact Sphere
ON OPEN BOOK EMBEDDING OF CONTACT MANIFOLDS IN THE STANDARD CONTACT SPHERE KULDEEP SAHA Abstract. We prove some open book embedding results in the contact category with a constructive ap- proach. As a consequence, we give an alternative proof of a Theorem of Etnyre and Lekili that produces a large class of contact 3-manifolds admitting contact open book embeddings in the standard contact 5-sphere. We also show that all the Ustilovsky (4m + 1)-spheres contact open book embed in the standard contact (4m + 3)-sphere. 1. Introduction An open book decomposition of a manifold M m is a pair (V m−1; φ), such that M m is diffeomorphic to m−1 m−1 2 m−1 MT (V ; φ)[id @V ×D . Here, V , the page, is a manifold with boundary, and φ, the monodromy, is a diffeomorphism of V m−1 that restricts to identity in a neighborhood of the boundary @V . MT (V m−1; φ) denotes the mapping torus of φ. We denote an open book, with page V m−1 and monodromy φ, by Aob(V; φ). The existence of open book decompositions, for a fairly large class of manifolds, is now known due the works of Alexander [Al], Winkelnkemper [Wi], Lawson [La], Quinn [Qu] and Tamura [Ta]. In particular, every closed, orientable, odd dimensional manifold admits an open book decomposition. Thurston and Winkelnkemper [TW] have shown that starting from an exact symplectic manifold (Σ2m;!) 2m as page and a boundary preserving symplectomorphism φs of (Σ ;!) as monodromy, one can produce a 2m+1 2m contact 1-form α on N = Aob(Σ ; φs). -
Arxiv:Math/0309299V2 [Math.GT] 13 Oct 2003 Rvdtesm Eut Hwn Ht3 Licko That Later, Showing Century Result, Quarter Same About the Proved Twists
GENERATING THE SURFACE MAPPING CLASS GROUP BY TWO ELEMENTS ∗ MUSTAFA KORKMAZ Abstract. Wajnryb proved in [W2] that the mapping class group of an orientable surface is generated by two elements. We prove that one of these generators can be taken as a Dehn twist. We also prove that the extended mapping class group is generated by two elements, again one of which is a Dehn twist. Another result we prove is that the mapping class groups are also generated by two elements of finite order. 1. Introduction Let Σ be a compact connected oriented surface of genus g with one bound- 1 ary component. We denote by Modg the mapping class group of Σ, the group of isotopy classes of orientation-preserving diffeomorphisms Σ → Σ which restrict to the identity on the boundary. The isotopies are also required to fix the points on the boundary. If the diffeomorphisms and the isotopies are allowed to permute the points on the boundary of Σ, then we get the ∗ group Modg,1. The extended mapping class group Modg,1 of Σ is defined to be the group of isotopy classes of all (including orientation-reversing) dif- feomorphisms of Σ. These three groups are related to each other as follows: ∗ Modg,1 is contained in Modg,1 as a subgroup of index two and the groups 1 Modg and Modg,1 fit into a short exact sequence Z 1 1 → → Modg → Modg,1 → 1, Z 1 where is the subgroup of Modg generated by the Dehn twist about a simple closed curve parallel to the boundary component of Σ.