Connected sum of oriented manifolds Created 2026-10-05 Updated 2026-10-07
For connected oriented closed -dimensional manifolds with , their connected sum removes an open -dimensional ball from each and identifies the resulting boundary spheres by an orientation-reversing diffeomorphism. The remaining orientations fit together. Collapsing the separating sphere gives a pinch map to the wedge sum of the two closed manifolds, and projection to either summand has degree of a continuous mapping one. In intermediate positive degrees the cohomology is the direct sum of the summand groups. Products of classes from different summands vanish; products landing in top degree use the single common orientation class. These statements follow from excision, the Mayer–Vietoris sequence and the degree-one projections.
A symplectomorphism is a diffeomorphism, so it preserves the genus of a surface. It also preserves the orientation determined by the symplectic form and, by integration of a pullback of a differential form, preserves the symplectic area.
Conversely, equal genus of a surface gives a diffeomorphism . We can choose to preserve the orientations determined by : if necessary, compose with an orientation-reversing diffeomorphism of the standard closed orientable surface of that genus of a surface, obtained by reflection of a symmetric handle model. On put . Both and are positive volume forms for the same orientation, and their integrals agree. By top-degree de Rham cohomology, .
The family consists of positive volume forms, hence symplectic forms in dimension two, with constant de Rham cohomology class. Moser theorem supplies with . Consequently
Therefore the genus of a surface and symplectic area classify compact connected symplectic surfaces.
There is an orientation convention in this statement: the two volume forms must be positive for one fixed orientation, as is usual in Moser theorem for volume forms. Without that convention, the stated necessity is false. For example, on an oriented two-sphere, take a positive volume form and an orientation-reversing diffeomorphism , and set . Then but . We prove the intended result with a common orientation.
If , positivity forces to preserve the orientation, and integration of the pullback of a differential form gives equality of the integrals.
For sufficiency, top-degree de Rham cohomology gives a differential form of degree with . Put . Positivity makes every a volume form. The interior product of a differential form gives an linear isomorphism
Thus there is a unique smooth time-dependent vector field satisfying . Since is compact, its local flow exists throughout and defines a smooth isotopy starting at the identity. By Cartan's magic formula, and since a top-degree differential form has zero exterior derivative,
Hence
The zero-dimensional case, a single point, is immediate from equality of the integrals.
An abstract smooth surface is a Hausdorff second-countable topological space with an atlas of charts to open subsets of whose transition maps are smooth. It is orientable when it has such an atlas for which every transition map has positive Jacobian determinant. A map is a smooth map when every coordinate representation
is smooth wherever it is defined.
The map is a smooth involution with no fixed point: the equation
would force , which is impossible on . For each , choose a sufficiently small coordinate neighbourhood such that
Then the quotient projection restricts to a homeomorphism
Transporting a smooth chart across this homeomorphism gives the quotient chart
On an overlap, a lift lies either in another chosen neighbourhood or in its image under . The corresponding transition map is therefore a transition map on , possibly composed with the diffeomorphism , and is smooth. Since this is a free action of the finite group , the quotient is Hausdorff and second countable. This constructs the smooth quotient by a free finite group action, and in these charts is locally the identity. Hence is a local diffeomorphism, in particular smooth.
To test orientability, parametrize the cylinder by
The involution acts in these coordinates as
whose derivative has determinant . Thus is an orientation-reversing diffeomorphism of the cylinder.
If the quotient surface were orientable, its orientation would pull back through the local diffeomorphism to an orientation of . The identity would then force to preserve that pulled-back orientation, contradicting the negative determinant above. Therefore