Beta-limit conjecture for stationary two-island and seed-bank diffusions

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For the stationary distribution of the two-island diffusion, let (X,Y)(X,Y) have distribution

(X,Y)∼TI⁡(a1,a2,γb1,γb2,c,γc,2,2γ).(X,Y) \sim \operatorname{TI}(a_1,a_2,\gamma b_1,\gamma b_2,c,\gamma c,2,2\gamma).

For the stationary distribution of the seed-bank diffusion, let

(X,Y)∼TI⁡(a1,a2,0,0,c,γc,2,0).(X,Y) \sim \operatorname{TI}(a_1,a_2,0,0,c,\gamma c,2,0).

Beta-limit conjecture. As c→∞c\to\infty, in the two-island case both XX and YY converge in distribution to the beta distribution with parameters (a1+b1,a2+b2)(a_1+b_1,a_2+b_2); in the seed-bank case both XX and YY converge in distribution to the beta distribution with parameters (a1,a2)(a_1,a_2).

The conjecture is motivated by the fact that the two islands become asymptotically indistinguishable and that the first and second moments calculated in the preceding lemma match the corresponding beta moments. The supplied text gives no resolution, so the conjecture remains open.

References

Primary source

Han L. Gan and Maite Wilke-Berenguer, “Stationary distribution approximations of Two-island Wright-Fisher and seed-bank models using Stein's method”, arXiv:2405.18763 (2024).

Progress summary

Refreshed
Claimed progress

The published conjecture is unproved, while a reader-written calculation claims the two-island case is true and gives a counterexample to the seed-bank case.

Gan and Wilke-Berenguer (2024) conjectured that, as c→∞c\to\infty, both coordinates approach the same beta law: Beta⁡(a1+b1,a2+b2)\operatorname{Beta}(a_1+b_1,a_2+b_2) for two islands and Beta⁡(a1,a2)\operatorname{Beta}(a_1,a_2) for the seed bank. This is Conjecture 2.72.7.

Known results

  • The stationary coordinates coalesce: X−Y→0X-Y\to0 in probability as c→∞c\to\infty.
  • The calculated first and second moments agree with the proposed beta limits.
  • The exact stationary distribution is generally unknown.

Posted attempt

A reader-written attempt claims a general limiting theorem: the two-island clause is proved, whereas the seed-bank clause is false and should instead have beta parameters ((1+γ)a1/γ,(1+γ)a2/γ)((1+\gamma)a_1/\gamma,(1+\gamma)a_2/\gamma). It supplies a second-moment counterexample at a1=a2=γ=1a_1=a_2=\gamma=1. This is a partial claim about the combined conjecture and has not been independently verified.

Current status (as of August 2026): The published source leaves both clauses open, while an unverified discussion claims the two-island clause and disputes the seed-bank clause; no corroborated resolution is recorded.

Sources

Solutions 1

CounterexampleThis solution needs a summarySee full solutionHide full solution

The two-island assertion is true, but the seed-bank assertion is false. A corrected general limit theorem identifies both cases.

Consider the source's stationary diffusion with generator

Lcf(x,y)=[a1−(a1+a2)x+c(y−x)]fx+α2x(1−x)fxx+[b1−(b1+b2)y+γc(x−y)]fy+β2y(1−y)fyy.\begin{aligned} \mathcal L_cf(x,y) ={}&[a_1-(a_1+a_2)x+c(y-x)]f_x +\frac{\alpha}{2}x(1-x)f_{xx}\\ &+[b_1-(b_1+b_2)y+\gamma c(x-y)]f_y +\frac{\beta}{2}y(1-y)f_{yy}. \end{aligned}

Let γ>0\gamma>0, ui=γai+biu_i=\gamma a_i+b_i, and K=γ2α+βK=\gamma^2\alpha+\beta, with u1,u2,K>0u_1,u_2,K>0. Then as c→∞c\to\infty,

(Xc,Yc)⟹(Z,Z),Z∼Beta⁡(2(1+γ)(γa1+b1)γ2α+β,2(1+γ)(γa2+b2)γ2α+β).(1)\boxed{ (X_c,Y_c)\Longrightarrow(Z,Z), \qquad Z\sim\operatorname{Beta}\left( \frac{2(1+\gamma)(\gamma a_1+b_1)}{\gamma^2\alpha+\beta}, \frac{2(1+\gamma)(\gamma a_2+b_2)}{\gamma^2\alpha+\beta} \right). } \tag{1}

To prove this, stationarity applied to (x−y)2(x-y)^2 gives

E(Xc−Yc)2=O(c−1).\mathbb E(X_c-Y_c)^2=O(c^{-1}).

Now set

Wc=γXc+Yc1+γ.W_c=\frac{\gamma X_c+Y_c}{1+\gamma}.

Migration cancels exactly in Lch(Wc)\mathcal L_ch(W_c). Therefore every subsequential weak limit WW satisfies, for every h∈C2[0,1]h\in C^2[0,1],

E[{u1−(u1+u2)W}h′(W)+K2(1+γ)W(1−W)h′′(W)]=0.(2)\mathbb E\left[ \{u_1-(u_1+u_2)W\}h'(W) +\frac{K}{2(1+\gamma)} W(1-W)h''(W) \right]=0. \tag{2}

Taking h(w)=wrh(w)=w^r determines all moments:

mr=θ1+r−1θ1+θ2+r−1mr−1,θi=2(1+γ)uiK.m_r =\frac{\theta_1+r-1}{\theta_1+\theta_2+r-1}m_{r-1}, \qquad \theta_i=\frac{2(1+\gamma)u_i}{K}.

Compactness of [0,1][0,1] makes these moments determining, so (2) gives the beta law in (1), and diagonal collapse upgrades this to joint convergence.

For the conjectured two-island specialization, the generator parameters are

(b1gen,b2gen,α,β)=(γb1,γb2,2,2γ).(b_1^{\rm gen},b_2^{\rm gen},\alpha,\beta) =(\gamma b_1,\gamma b_2,2,2\gamma).

Formula (1) correctly gives

Z∼Beta⁡(a1+b1,a2+b2),Z\sim\operatorname{Beta}(a_1+b_1,a_2+b_2),

proving the first clause.

For the seed-bank specialization, however,

(b1,b2,α,β)=(0,0,2,0),(b_1,b_2,\alpha,\beta)=(0,0,2,0),

and (1) gives the actual limit

Z∼Beta⁡(1+γγa1,1+γγa2),\boxed{ Z\sim \operatorname{Beta}\left( \frac{1+\gamma}{\gamma}a_1, \frac{1+\gamma}{\gamma}a_2 \right), }

not the asserted Beta⁡(a1,a2)\operatorname{Beta}(a_1,a_2).

A completely explicit counterexample follows by taking a1=a2=γ=1a_1=a_2=\gamma=1. Stationarity for x,y,x2,xy,y2x,y,x^2,xy,y^2 yields, exactly for every c>0c>0,

EXc=EYc=12,\mathbb EX_c=\mathbb EY_c=\frac12, EXc2=3c+410c+12,E[XcYc]=EYc2=3(c+1)10c+12.\mathbb EX_c^2=\frac{3c+4}{10c+12}, \qquad \mathbb E[X_cY_c]=\mathbb EY_c^2 =\frac{3(c+1)}{10c+12}.

Hence

lim⁡c→∞EXc2=310,\lim_{c\to\infty}\mathbb EX_c^2=\frac3{10},

whereas the claimed Beta⁡(1,1)\operatorname{Beta}(1,1) limit has second moment 1/31/3. Since x2x^2 is bounded and continuous, the claimed convergence is impossible. The correct limit is Beta⁡(2,2)\operatorname{Beta}(2,2).

Thus the original combined conjecture is false; its first clause holds, and its second clause requires the missing factor (1+γ)/γ(1+\gamma)/\gamma in both beta parameters.

Source: Gan and Wilke-Berenguer, Stationary distribution approximations of Two-island Wright-Fisher and seed-bank diffusions using Stein's method, equation (1.1), Lemma 2.6, and Conjecture 2.7, https://arxiv.org/abs/2405.18763 .