Abstract:Let a and b be two simple closed curves on an orientable surface S such that their geometric intersection number is greater than 1. The group generated by corresponding Dehn twists ta and t b is known to be isomorphic to the free group of rank 2. In this paper we extend this result to the case of a nonorientable surface.
Let N g denote a closed nonorientable surface of genus g. For g ≥ 2 the mapping class group M(N g ) 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.
Let N g denote a closed nonorientable surface of genus g. For g ≥ 2 the mapping class group M(N g ) 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.
“…It follows that F commutes with Y i , T α i , T β j , and thus by Theorem 3.3 it belongs to the center of M(N g ) which is trivial, according to [18,Corollary 6.3]. Hence F = 1 and Let N g−1 be the surface obtained by replacing the leftmost crosscap in Fig.…”
Section: Lemma 34 the Involution R Belongs To Y(n )mentioning
Crosscap slide is a homeomorphism of a nonorientable surface of genus at least 2, which was introduced under the name Y-homeomorphism by Lickorish as an example of an element of the mapping class group which cannot be expressed as a product of Dehn twists. We prove that the subgroup of the mapping class group of a closed nonorientable surface N generated by all crosscap slides is equal to the level 2 subgroup consisting of those mapping classes which act trivially on H 1 (N ; Z 2 ). We also prove that this subgroup is generated by involutions.
“…For M = M −2 the statement is trivial, hence assume that M = M −2 . By Proposition 3.4 of [13] and Lemma 4.1 of [16] there exists a circle b, generic in N, such that I(a, b) > 0. In particular b is not a boundary circle of N, hence by Proposition 2.2 and Theorem 3.6, the twist t b is nontrivial in M, that is b is generic in M.…”
Section: Subsurfaces and Injectivitymentioning
confidence: 97%
“…The mapping class group of a Klein bottle is generated by a twist and a crosscap slide [9], and is isomorphic to Z 2 × Z 2 . The description of mapping class groups of a Klein bottle with one puncture and a Klein bottle with one hole can be found in the appendix to [16]. In particular, we will use the following proposition.…”
Section: 1mentioning
confidence: 99%
“…It is known [13] that an orientable surface has a pantalon decomposition if and only if 2g + r + s > 2 and M = M 3 0 . As observed in Section 5 of [16], one needs to add two more "pieces" in order to decompose nonorientable surfaces, namely a Möbius strip with one puncture and a Möbius strip with an open disk removed. We call these surfaces a skirt of type I and II, respectively (cf Figure 2).…”
Abstract. Let M be a surface (possibly nonorientable) with punctures and/or boundary components. The paper is a study of "geometric subgroups" of the mapping class group of M , that is subgroups corresponding to inclusions of subsurfaces (possibly disconnected). We characterise the subsurfaces which lead to virtually abelian geometric subgroups. We provide algebraic and geometric conditions under which two geometric subgroups are commensurable. We also describe the commensurator of a geometric subgroup in terms of the stabiliser of the underlying subsurface. Finally, we show some applications of our analysis to the theory of irreducible unitary representations of mapping class groups.
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