ISSN 1364-0380 (on line) 1465-3060 (printed) 935 Geometry & Topology G T GG T T T Volume 9 (2005) 935–970 G T G T G T G T Published: 25 May 2005 T G T G T G T G T G G G G T T Symplectomorphism groups and isotropic skeletons Joseph Coffey Courant Institute for the Mathematical Sciences, New York University 251 Mercer Street, New York, NY 10012, USA Email:
[email protected] Abstract The symplectomorphism group of a 2–dimensional surface is homotopy equiv- alent to the orbit of a filling system of curves. We give a generalization of this statement to dimension 4. The filling system of curves is replaced by a decomposition of the symplectic 4–manifold (M,ω) into a disjoint union of an isotropic 2–complex L and a disc bundle over a symplectic surface Σ which is Poincare dual to a multiple of the form ω. We show that then one can recover the homotopy type of the symplectomorphism group of M from the orbit of the pair (L, Σ). This allows us to compute the homotopy type of certain spaces of Lagrangian submanifolds, for example the space of Lagrangian RP2 ⊂ CP2 isotopic to the standard one. AMS Classification numbers Primary: 57R17 Secondary: 53D35 Keywords: Lagrangian, symplectomorphism, homotopy Proposed: Leonid Polterovich Received: 25 June 2004 Seconded: Yasha Eliashberg, Tomasz Mrowka Revised: 24 September 2004 c Geometry & Topology Publications 936 Joseph Coffey 1 Introduction 1.1 Surface diffeomorphisms A finite set L = {γi} of simple, closed, transversally intersecting parametrized curves on a surface X fills if X\{γi} consists solely of discs.