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✓ 4 results · all verified · 1 also independently AI-judged
Every result on this page is machine-checked by a proof checker and read in full and owner-audited; the judge is an additional, independent cross-model AI review of the proofs. The 3 not AI-judged were verified by owner audit (typically over a confirmed judge false positive), not failures.

Isotopy Extension and Embedding Theory Beyond Whitney — Examples

1 · Prerequisites

2 · Summary

These examples exercise the A page's theory in its simplest concrete cases. The visible motion of a round circle in R3 — translation, scaling, rotation about a moving axis — is an explicit isotopy of embeddings to which the isotopy extension theorem applies, and every round circle is carried to every other by a compactly supported ambient isotopy. Isotopic submanifolds share their normal bundles and their complements, so the ambient diffeomorphism supplied by the extension theorem is the source of the two embedding invariants; the converse fails, and the page records that failure.

The counterexample is the reflection of the standard sphere S2⊆R3: it is regularly homotopic to the standard inclusion because all immersions S2→R3 are regularly homotopic, but it is not isotopic, because an isotopy would extend ambiently to a diffeomorphism of the ball preserving the boundary orientation of S2 and hence of degree +1, while the reflection has degree −1. Finally the dimension count for surfaces is computed in four- and five-space: in R4 the double points are isolated and finite, so the algebraic obstruction has content, while in R5 self-transversality already forces an embedding.

3 · Logical flowchart

4 · Definitions, theorems and proofs

None yet.

5 · Examples, counterexamples and false statements

LemmaStatement: Literature-sourcedProof: Literature-sourcedprecheck passjudge pass (gpt-6.1-sol)Open item page →

An ambient isotopy preserves the orientation of an invariant round sphere

Statement

Let H:R3×I→R3 be an ambient isotopy with H0=id (Smooth isotopies, diffeotopies and ambient isotopies) and suppose H1 maps the closed unit ball B3⊆R3 to itself. Then H1 restricts to a diffeomorphism of the unit sphere S2=∂B3 of degree +1; that is, H1∣S2 preserves the boundary orientation of S2 (Induced boundary orientation). Consequently, if r:R3→R3 is a linear reflection in a plane through the origin (so det⁡r=−1 and r preserves S2), there is no such ambient isotopy with H1∣S2=r∣S2.

Facts & Assumptions

Given: An ambient isotopy H:R3×I→R3 with H0=id and H1(B3)=B3.

[F1]

Each Ht is a diffeomorphism of R3 and H is smooth; in particular every differential dHt(x) is an invertible linear map (Smooth isotopies, diffeotopies and ambient isotopies, Diffeomorphisms and local diffeomorphisms of manifolds).

[F2]

The entries of the Jacobian matrix of the smooth map (x,t)↦Ht(x) are partial derivatives of a C∞ function of several variables and are therefore continuous; the determinant is a polynomial in the matrix entries (Ck maps and multi-index derivative notation in Euclidean space, Directional derivatives and partial derivatives of a map U⊆Rm→Rn, For every fixed finite size at least one, the determinant of a real square matrix is a polynomial in its matrix entries).

[L1]

A continuous real function on I=[0,1] that never vanishes and is positive at 0 is positive everywhere (Intermediate value theorem, by bisection with a canonical left-half rule: a continuous function on [a,b] takes every value between f(a) and f(b)).

[L2]

A diffeomorphism of manifolds with boundary maps the boundary onto the boundary and the interior onto the interior (Diffeomorphisms preserve interior and boundary).

[L3]

The boundary orientation of S2=∂B3 is the outward-normal-first orientation of Induced boundary orientation applied to the oriented closed ball; S2 is a nonempty connected orientable boundaryless manifold (Orientable manifolds).

[L4]

A diffeomorphism between nonempty connected oriented boundaryless manifolds has degree +1 if it preserves orientation and −1 if it reverses it (Degree of an orientation-preserving or reversing diffeomorphism). A linear reflection r with det⁡r=−1 restricts to a diffeomorphism of S2 that reverses the outward-normal-first boundary orientation, since r maps the ball onto itself, carries outward normals to outward normals, and reverses the ambient orientation; hence r∣S2 has degree −1 by the same proposition.

Proof

technique · direct
1.1F1F2L1

Fix x∈R3 and put φ(t):=det⁡dHt(x) for t∈I. The function φ is continuous on I by [F2], and it never vanishes because each dHt(x) is invertible by [F1]; since φ(0)=det⁡id=1>0, the intermediate value property [L1] gives φ(t)>0 for every t∈I. Hence dHt(x) is orientation-preserving at every (x,t), and in particular H1 preserves the orientation of R3 at every point.

2.1F1L2step 1.1

Since H1 is a diffeomorphism and H1(B3)=B3, [L2] shows that H1 maps the interior of B3 onto the interior and the sphere S2=∂B3 onto itself; thus H1∣S2:S2→S2 is a diffeomorphism. Moreover dH1 carries the outward transverse direction of S2 at each p to the outward transverse direction at H1(p): the interior maps to the interior, so a tangent vector pointing into the ball maps to a vector pointing into the ball, and an outward transverse vector maps to an outward transverse vector: the inward boundary coordinate of the image vanishes at the boundary, is positive on the interior side, and has nonzero normal derivative by invertibility, so that derivative is positive. Orthogonality to the sphere need not be preserved.

3.1L3L4step 1.1step 2.1

The restriction H1∣S2 preserves the outward-normal-first boundary orientation of [L3]: if (v1,v2) is a positive basis of TpS2, so that (np,v1,v2) is a positive basis of TpR3 with np outward, then step 1.1 makes (dH1(np),dH1(v1),dH1(v2)) positive at H1(p), and dH1(np) is an outward vector by step 2.1, so (dH1(v1),dH1(v2)) is a positive basis of TH1(p)S2. Hence H1∣S2 is an orientation-preserving diffeomorphism of S2, and [L4] gives deg⁡(H1∣S2)=+1.

4.1L4step 3.1∎

Let r:R3→R3 be a linear reflection, det⁡r=−1, preserving S2. By [L4] the restriction r∣S2 reverses the boundary orientation and has degree −1, while every diffeomorphism H1∣S2 arising as above has degree +1 by step 3.1; therefore H1∣S2=r∣S2 is impossible, and no such ambient isotopy can restrict to the reflection.

ExampleConstruction: Literature-sourcedVerification: Literature-sourcedprecheck passOpen item page →

Extending a visible isotopy of an unknotted circle in R3

Example

Assume ACω. Let S1⊆R2×{0}⊆R3 be the unit circle with inclusion map f0, and let f1:S1→R3 be a round circle of radius λ>0 centred at c∈R3, written as the affine image f1(x)=c+λQf0(x) of f0 for some Q∈SO(3). Then there is a compactly supported ambient isotopy H of R3 with H0=id and H1∘f0=f1: every round circle is carried to every other by an ambient isotopy supported in any prescribed open neighbourhood of the entire isotopy image F(S1×I) constructed below. The example exhibits the hypothesis check of The isotopy extension theorem in the simplest case (M=S1 compact, N=R3 without boundary, no boundary stratum, no properness issue) and shows that the visible motion of a round circle is always realisable ambiently.

Facts & Assumptions

Given: The unit circle S1 with inclusion f0, a round circle f1=c+λQf0 with λ>0, c∈R3 and Q∈SO(3), and a prescribed open neighbourhood W of the entire image of the affine isotopy F constructed below.

[F1]

An ordered orthonormal pair in R3 is completed to an element of SO(3) by its cross product. Step 1.1 constructs a smooth path of rotations using a fixed axis; mere topological path connectedness is not used as a smooth-path theorem.

[F2]

A smooth isotopy of embeddings is a smooth map whose slices are smooth embeddings; an ambient isotopy of R3 is a smooth family of diffeomorphisms with H0=id, and it is compactly supported when it fixes a compact set's complement (Smooth isotopies, diffeotopies and ambient isotopies, Smooth embeddings).

[L1]

Under ACω every smooth isotopy of a compact manifold into R3 extends to an ambient isotopy supported in any prescribed neighbourhood of the track (The isotopy extension theorem, clause 4). [F2]

[A1]

Countable choice is inherited from [L1]; the explicit affine family below selects nothing (The Axiom of Countable Choice (ACω)).

Verification

technique · direct
1.1F2A1constructalgebra

An orthogonal 3×3 matrix Q of determinant one has a unit fixed axis a: its eigenvalues have modulus one, the nonreal ones occur in conjugate pairs, and their product together with the real eigenvalues is one, so one real eigenvalue is +1. On a⊥ its restriction is a plane rotation through some angle θ. Fix an orthonormal basis of that plane and let Qt fix a and rotate the plane through tθ; its sine and cosine entries give a smooth path with Q0=I, Q1=Q. Define Ft(x)=tc+((1−t)+tλ)Qtf0(x). Each slice is the restriction of an invertible affine map because (1−t)+tλ>0, hence is an embedding. The family is smooth and satisfies F0=f0, F1=f1.

2.1F1L1L2step 1.1construct

By compactness of S1, [L1] extends F to an ambient isotopy supported in a compact subset of W, with H1∘f0=f1. Every affine parametrization of a round circle has the form c+λ(ucos⁡s+vsin⁡s) for an ordered orthonormal pair u,v; completing it by u×v gives a matrix in SO(3), including when the circle parameter orientation is reversed. Thus the construction covers all such round circles. The neighbourhood must contain the whole motion, since a disconnected neighbourhood of disjoint endpoint circles cannot support a motion between its components.

3.1step 1.1step 2.1∎

Steps 1.1 and 2.1 exhibit the required compactly supported ambient isotopy carrying f0 to f1, verifying the hypothesis check of The isotopy extension theorem in this example.

ExampleConstruction: Literature-sourcedVerification: Literature-sourcedprecheck passOpen item page →

Compact isotopic submanifolds have isomorphic normal bundles and diffeomorphic complements

Example

Assume ACω. Let N be a smooth manifold without boundary, let M be a compact smooth manifold and let f0,f1:M→N be isotopic embeddings with normal bundles ν0=f0∗TN/TM and ν1=f1∗TN/TM (Normal and conormal bundles of an embedded submanifold). Then ν0≅ν1 as smooth vector bundles over M and N∖f0(M)≅N∖f1(M); under AC every characteristic class defined on these normal bundles agrees (for orientation-dependent classes, use orientations transported by the displayed bundle isomorphism) and the complements are diffeomorphic. The example verifies the two embedding invariants supplied by isotopy: the ambient diffeomorphism of Isotopic embeddings of a compact manifold have diffeomorphic complements intertwines the normal bundles, and The isotopy extension theorem is the source of that diffeomorphism. (The converse fails: trivial normal bundles do not force isotopy, as the reflected-sphere counterexample on this page shows.)

Facts & Assumptions

Given: Countable choice, a boundaryless N, a compact M, isotopic embeddings f0,f1:M→N with normal bundles ν0,ν1.

[F1]

Isotopic embeddings are joined by a smooth isotopy of embeddings (Smooth isotopies, diffeotopies and ambient isotopies, Smooth embeddings).

[L1]

Under ACω there is a diffeomorphism H:N→N with H∘f0=f1, restricting to a diffeomorphism of pairs and of complements (Isotopic embeddings of a compact manifold have diffeomorphic complements, The isotopy extension theorem).

[L2]

Under countable choice the normal quotients have their smooth bundle structures by Assuming countable choice, normal and conormal bundles are smooth vector bundles. The chain rule is The chain rule for differentials of smooth maps. Under AC a characteristic class is natural in the bundle isomorphism class (Characteristic class as a universal natural bundle class). The normal bundle of the embedding fi is the fibrewise quotient fi∗TN/TM, with tangent maps dfi as in Normal and conormal bundles of an embedded submanifold, The tangent bundle as a disjoint union and The differential of a smooth map; a diffeomorphism H carries TN∣f0(M) isomorphically onto TN∣f1(M) by its differential.

[A1]

Countable choice is inherited from [L1]; the bundle isomorphism below is an explicit induced map and selects nothing. The characteristic-class clauses additionally assume AC (The Axiom of Choice) (The Axiom of Countable Choice (ACω)).

Verification

technique · direct
1.1F1L1L2A1

By [L1] let H be an ambient diffeomorphism with H∘f0=f1. Its differential restricts to a smooth bundle isomorphism dH:TN∣f0(M)→TN∣f1(M) covering f1∘f0−1.

2.1L2step 1.1

On the level of M the map dH induces a bundle map ν0→ν1 over the identity of M: by the chain rule, dH carries the summand df0(TM)⊆TN∣f0(M) isomorphically onto df1(TM)⊆TN∣f1(M), so it descends to an isomorphism of the fibrewise quotients ν0=f0∗TN/TM→ν1=f1∗TN/TM over idM. A bundle map that is a linear isomorphism on each fibre is a bundle isomorphism, so ν0≅ν1; consequently the characteristic classes natural under this bundle isomorphism agree. For the characteristic-class construction assume additionally AC. Orientation-dependent classes agree when orientations are transported by it; unrelated choices of orientations are not being compared.

2.2L1step 1.1

The complement statement is the second conclusion of [L1]: H restricts to a diffeomorphism N∖f0(M)→N∖f1(M) with smooth inverse. For the standard sphere and its reflection, the radial vectors at their image points give nowhere-zero smooth frames of the normal line bundles, so both are trivial. The reflected-sphere counterexample on this page proves they are not isotopic, establishing the parenthetical failure of the converse.

3.1step 2.1step 2.2∎

The normal bundles are isomorphic and the complements diffeomorphic, which is what the example claims.

CounterexampleConstruction: Literature-sourcedVerification: AI-adaptedprecheck passOpen item page →

A reflected sphere embedding is regularly homotopic but not isotopic to the standard one

Statement refuted

Every pair of regularly homotopic embeddings of a closed manifold into Euclidean space is isotopic; equivalently, regular homotopy of embeddings and isotopy of embeddings define the same equivalence relation.

Facts & Assumptions

Given: The standard inclusion ι:S2↪R3 of the unit sphere and a linear reflection r:R3→R3 with det⁡r=−1.

[F1]

Regular homotopy is a smooth family of immersions, while isotopy is a smooth family of embeddings (Regular homotopy of immersions, Smooth isotopies, diffeotopies and ambient isotopies, Smooth embeddings).

[L1]

For m=2 and n=3 the Smale classification of sphere immersions records that all immersions S2→R3 are regularly homotopic, because π2(SO(3))=0 (Smale's classification of sphere immersions in Euclidean space, Regular homotopy classes of immersions are formal homotopy classes); for the standard inclusion and its reflection this formal-data homotopy is computed directly in Standard and reflected two-sphere immersions have homotopic formal data in R^3, whose vanishing class in π2(SO(3)) is the obstruction to homotoping the two formal data.

[L2]

Under ACω every smooth isotopy of the compact S2 in the boundaryless R3 extends to an ambient isotopy, whose final restriction is the prescribed sphere map (The isotopy extension theorem).

[L3]

A diffeomorphism between nonempty connected oriented boundaryless manifolds has degree +1 if it preserves orientation and −1 if it reverses it (Degree of an orientation-preserving or reversing diffeomorphism); a linear reflection r with det⁡r=−1 preserves the unit ball and reverses the outward-normal-first boundary orientation of S2=∂B3, so r∣S2 has degree −1.

[A1]

Countable choice is inherited from the Smale classification chain and the extension theorem; the reflection computations select nothing (The Axiom of Countable Choice (ACω)).

Counterexample

technique · direct
1.1F1L3

Both ι and r∘ι are smooth embeddings of S2 into R3: ι is the inclusion of an embedded submanifold, and r is a linear isomorphism, hence a diffeomorphism of R3 whose composite with ι is again an embedding.

2.1L1step 1.1A1

The two embeddings are regularly homotopic: by [L1], applied with m=2 and n=3, all immersions S2→R3 are regularly homotopic because π2(SO(3))=0, and ι and r∘ι are such immersions; the reflection is, up to an orientation-preserving rotation of the target, the antipodal reparametrisation of the standard inclusion, and the direct formal-data computation identifies the obstruction as a class in π2(SO(3))=0, so the two formal data are homotopic and the formal-data criterion gives the regular homotopy. Hence clause 1 of the counterexample holds.

2.2F1L2step 1.1

The two embeddings are not isotopic. Suppose an isotopy of embeddings from ι to r∘ι existed. Since S2 is compact and R3 is boundaryless, [L2] produces an ambient isotopy H of R3 with H0=id and H1∘ι=r∘ι, that is H1∣S2=r∣S2.

3.1F1step 2.2construct

The sphere complement has precisely the two connected components U={∣x∣<1} and V={∣x∣>1}: U is convex, and in V radial paths to a common large sphere followed by great-circle arcs on that sphere (for antipodal endpoints choose a perpendicular unit vector by normalizing the first nonzero coordinate-vector projection) connect any two points. Since H1(S2)=S2, the homeomorphism permutes these components. It cannot send U to V, since H1(U‾) is compact and therefore bounded, whereas V is unbounded. Consequently H1(U)=U and H1(B3)=B3.

4.1L3L4step 3.1construct

For every x, the function t↦det⁡dHt(x) is continuous, never zero, and equals one at zero, so [L4] makes it positive for all t. Thus H1 preserves the ambient orientation. Because it maps the ball's interior onto itself, its differential takes an outward transverse vector to an outward transverse vector at the sphere: in a boundary chart the inward normal coordinate has positive inward derivative, by invertibility and preservation of the interior. The outward-normal-first rule in [L4] therefore makes H1∣S2 orientation preserving. By [L3] its degree is +1, contradicting the reflection's degree −1. This proves the orientation argument locally, without a B-page prerequisite.

5.1step 2.2step 4.1∎

Therefore ι and r∘ι are regularly homotopic but not isotopic, so the statement refuted is false: regular homotopy of embeddings is strictly coarser than isotopy of embeddings for S2 in R3. The historically first instance, a knotted circle versus the round circle in R3, is recorded as a boundary rather than proved here, because its non-isotopy invariant π1(R3∖L) belongs to the low-dimensional knot track and not to this run's closure.

ExampleConstruction: AI-adaptedVerification: AI-adaptedOpen item page →

The double point dimension count for surfaces in four- and five-space

Example

Assume ACω. Let M2 be a closed connected surface (m=2). Then:

  1. for a self-transverse immersion f:M2↬R4 the expected dimension is 2m−n=0: the double point locus is a closed 0-dimensional submanifold of M×M∖ΔM, the double point set is finite, and the selected branch pairs are isolated and transverse; several pairs may initially have the same collision image;
  2. for a self-transverse immersion f:M2↬R5 the expected dimension is −1<0: the double point locus is empty, so f is an injective immersion, and since M is closed f is an embedding.

The example shows why dimension four is the critical case for surfaces: it is exactly there that the double points are isolated rather than absent, so that the algebraic branch-pair count can be nonzero; the m≥3 disjunction theorem does not cover this surface-in-four-space case. In five-space the configuration space argument already forbids double points.

Facts & Assumptions

Given: Countable choice, a closed connected surface M and a self-transverse immersion f:M2↬Rn with n=4 or n=5.

[F1]

For a self-transverse immersion f:Mm→Xn, Δ2(f) is a closed embedded submanifold of M×M∖ΔM of pure dimension 2m−n when 2m−n≥0, and it is empty when 2m−n<0; the double point set is Σ(f)=f(pr⁡1Δ2(f)) (The double point locus has the expected dimension 2m−n, Self-transverse immersions and the double point locus).

[F2]

A self-transverse immersion f:Mm→Xn with n>2m is injective (A self-transverse immersion has no double points when n>2m).

[F3]

A proper injective immersion of smooth manifolds is a smooth embedding (A proper injective immersion is a smooth embedding); an immersion is locally an embedding, and a self-transverse immersion is in particular an immersion (Every immersion is locally an embedding, Immersions, submersions, and constant-rank maps).

[F5]

An embedded submanifold of dimension 0 has each point isolated: in a slice chart at the point the submanifold meets the chart in that single point (Embedded submanifolds and slice charts).

[A1]

Countable choice is inherited from the transversality machinery used in [F1]; the finite compactness argument below selects nothing (The Axiom of Countable Choice (ACω)).

Verification

technique · direct
1.1F1F5A1

Clause 1: with m=2 and n=4 the expected dimension is 2m−n=0, so [F1] makes Δ2(f) a closed embedded 0-dimensional submanifold of M×M∖ΔM; by [F5] each of its points is isolated.

1.2F3F4

A neighbourhood of the diagonal free of double points: by [F3] every x∈M belongs to an open set U on which f is injective. Thus the family of all U×U with this property is an ambient-open cover of ΔM. By [F4] finitely many U1×U1,…,Uk×Uk cover the compact diagonal; their union N is an open neighbourhood of ΔM. If (y,z)∈N∩Δ2(f), then (y,z)∈Ui×Ui for some i and f(y)=f(z) with y≠z, contradicting injectivity on Ui. Hence N∩Δ2(f)=∅. No family of neighbourhoods indexed by all source points was selected.

1.3F1F2F3F4

Clause 2: with m=2 and n=5 one has n>2m, so [F2] makes f injective; equivalently the expected dimension 2m−n=−1 is negative and [F1] gives Δ2(f)=∅ directly. Since M is closed, every compact subset of R5 has compact preimage under the continuous map f (the preimage is closed in the compact space M and hence compact by [F4]), so f is proper; being a proper injective immersion, f is a smooth embedding by [F3].

2.1F1step 1.1step 1.2

Finiteness of the double point set: by step 1.2 one has Δ2(f)⊆M×M∖N; the set M×M∖N is closed in M×M∖ΔM because N is open and contains ΔM, and Δ2(f) is closed in M×M∖ΔM by step 1.1, so Δ2(f) is closed in M×M∖N, while M×M∖N is compact by [F4] as a closed subset of the compact space M×M; hence Δ2(f) is compact. By step 1.1 it is a discrete subspace, and a compact discrete subspace is finite, so Σ(f)=f(pr⁡1Δ2(f)) is finite as the image of a finite set. The double points are isolated by step 1.1 and transverse because f is self-transverse by hypothesis and the branch tangents span the target tangent space at each double point.

3.1step 1.1step 1.2step 2.1step 1.3∎

Both clauses hold: clause 1 is steps 1.1, 1.2 and 2.1, and clause 2 is step 1.3. Hence the critical dimension for surfaces is four, where the double point locus is a finite set, while in five-space self-transversality already forces an embedding.

Sources