Alphabeta Math
CounterexampleConstruction: Literature-sourcedVerification: AI-adaptedPipeline-generatedprecheck pass
How statement and proof provenance work

The first chip identifies the source of the statement or construction; the second identifies the source of its local proof or verification.

  • Literature-sourced: the exact statement appears in a cited source; only wording and notation differ.
  • AI-adapted: a semantically identical restatement of literature-sourced material, modulo indexing, notation, and boundary cases adopted by the library.
  • AI-generated: a genuinely novel statement formulated by AI, with no source for the claim itself.

These labels describe origin, not correctness: citations and verification chips remain separate evidence.

Vanishing stable characteristic classes do not make two embeddings isotopic

Statement refuted

FALSE: if two smooth embeddings of a closed oriented manifold into Euclidean space have isomorphic (even trivial) normal bundles and identical stable characteristic classes, then they are isotopic.

Assume AC. Let i:S2↪R3 be the standard inclusion of the unit sphere and let r:S2↪R3 be its reflection r(x1,x2,x3)=(x1,x2,−x3). Both are smooth embeddings of a closed oriented surface whose normal line bundle is trivial (computed below); hence the embeddings have isomorphic normal bundles and identical stable characteristic classes: wˉ=1, pˉ=1, and every characteristic-class test of this page (immersion or embedding, mod-two or rational) vanishes for both. Nevertheless i and r are not isotopic embeddings of S2 in R3. Indeed, an isotopy from i to r would extend by The isotopy extension theorem to an ambient isotopy H:R3×[0,1]→R3 with H0=id⁡ and H1∘i=r. The time-one map H1 is an orientation-preserving diffeomorphism of R3 and H1(S2)=S2; the diffeomorphism H1 permutes the connected components of R3∖S2. The image H1(int⁡B3) is a component whose closure H1(B3) is compact, hence it is the bounded component int⁡B3. Thus H1(B3)=B3. Its restriction to S2 therefore has degree +1 (Degree of an orientation-preserving or reversing diffeomorphism, Induced boundary orientation), whereas r∣S2 has degree −1 (Degree of identity constant reflection and antipodal sphere maps, Orientable manifolds); this contradicts H1∘i=r. Hence vanishing stable characteristic classes do not imply isotopy of embeddings.

Facts & Assumptions

Given: The unit sphere S2=∂B3⊆R3 with its standard orientation as a boundary (outward-normal-first), the standard inclusion i and the reflection r(x1,x2,x3)=(x1,x2,−x3); AC.

[F1]

Both i and r are smooth embeddings and oriented hypersurfaces of the oriented R3; their normal line bundles are trivial, and for the closed oriented surface S2 the normal classes are wˉ(S2)=1 and pˉ(S2)=1, with all higher normal classes vanishing by rank (the local calculation below, Smooth embeddings, Orientable manifolds).

[F2]

A smooth isotopy of a compact manifold M in a smooth manifold N extends to an ambient isotopy: for F:M×I→N an isotopy of embeddings constant near the ends and W a neighbourhood of the track, there is H:N×I→N with H0=id⁡N, every Ht a diffeomorphism, Ht∘F0=Ft for all t, and Ht=id⁡N outside W (The isotopy extension theorem, Smooth isotopies, diffeotopies and ambient isotopies). Here M=S2 is compact, N=R3, and the neighbourhood hypothesis is vacuous with W=N.

[F3]

A diffeomorphism H1 of R3 that is the time-one map of a diffeotopy from the identity preserves orientation: the orientation sign of Ht at each point is a continuous function of t with value +1 at t=0 and takes values in {±1} (Diffeomorphisms and local diffeomorphisms of manifolds, Orientable manifolds); changing coordinates does not affect the degree of a self-map of a connected closed oriented manifold (Degree of an orientation-preserving or reversing diffeomorphism).

[F4]

The reflection r restricts on S2⊆R3 to a single coordinate reflection of the sphere, hence has degree −1 as a self-map of S2; with the outward-normal-first orientation of S2=∂B3 this says exactly that r∣S2 is orientation-reversing (Degree of identity constant reflection and antipodal sphere maps, Degree of an orientation-preserving or reversing diffeomorphism, Induced boundary orientation). The closed ball B3 is compact and R3∖S2 has exactly two connected components, the bounded int⁡B3 and the unbounded one, with the latter containing points of arbitrarily large norm.

[F5]

AC implies the countable choice assumed by the isotopy extension theorem (AC implies DC implies countable choice, The Axiom of Countable Choice (ACω), The Axiom of Choice).

Counterexample

1.1givenconstructalgebra

For the standard embedding i(p)=p the radial field ni(p)=p spans its orthogonal normal line and is smooth and nowhere zero. For the reflected embedding r, the field nr(p)=r(p) is normal because reflection preserves inner products: ⟨r(p),drp(v)⟩=⟨p,v⟩=0. It is again a smooth nowhere-zero frame. Thus both normal lines are trivial. The embedding normal-bundle identity identifies their characteristic classes with the stable normal classes of S2, and the trivial line has total Stiefel--Whitney and Pontryagin class 1 and Euler class 0.

1.2F1

The two embeddings have identical stable characteristic classes. Both are embeddings of the same closed oriented surface S2 into R3 with trivial normal line bundle by [F1], so their normal bundles are isomorphic (both trivial). The normal classes wˉ(S2)=1 and pˉ(S2)=1 of [F1] are classes of the manifold S2 and therefore the same for both embeddings, and the codimension-one Euler class of the trivial normal line is zero. Consequently every characteristic-class test considered on this page — the mod-two normal classes, the rational normal Pontryagin classes and the oriented Euler class — evaluates trivially for both i and r, so no such test distinguishes them.

1.3F2F5

Suppose, for contradiction, that i and r were isotopic: there is a smooth isotopy of embeddings F:S2×I→R3 with F0=i and F1=r. Replacing F by a reparametrisation in t that is constant near the ends, the isotopy is constant near the ends without changing its endpoints; by [F2] and [F5] it extends to an ambient isotopy H:R3×I→R3 with H0=id⁡R3, every Ht a diffeomorphism, and Ht∘i=Ft for every t. In particular H1∘i=r.

2.1F3F4step 1.3

The time-one map H1 is an orientation-preserving diffeomorphism of R3 by [F3]. Since H1∘i=r and i,r have image S2, it satisfies H1(S2)=S2. As a diffeomorphism it maps the two connected components of R3∖S2 onto the two components, and H1(int⁡B3) is a component whose closure H1(B3) is compact because B3 is compact and H1 is continuous: hence H1(int⁡B3) is the bounded component int⁡B3 and H1(B3)=B3.

3.1F3F4step 2.1

Since H1 is an orientation-preserving diffeomorphism of R3 mapping B3 onto itself, it maps the boundary S2 to itself and its differential carries outward-pointing boundary vectors to outward-pointing boundary vectors; therefore the restriction H1∣S2:S2→S2 preserves the outward-normal-first boundary orientation. By [F3] and [F4], an orientation-preserving diffeomorphism of the connected closed oriented surface S2 has degree +1.

4.1F3F4F5step 1.3step 3.1∎

On the other hand H1∘i=r means H1∣S2=r∣S2 as maps S2→S2, and by [F4] the reflection has degree −1. This contradicts the degree +1 computed in step 3.1, so no isotopy from i to r exists. Hence two embeddings with identical (indeed trivial) normal bundles and identical stable characteristic classes need not be isotopic, and these characteristic classes do not determine isotopy. AC is inherited from the characteristic-class suppliers and supplies the countable choice used by isotopy extension.

Depends on

Used by

Nothing in the library uses this result yet.

Dependency tree · two levels

78 results within two dependency steps of this one, each drawn at its shortest distance from it. An arrow runs from a result to what uses it, so the chart reads left to right and ends at this result, which carries a heavier outline. Every node is a link to that result. Click elsewhere on the chart to enlarge it.

Sources