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

From papers

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 cc\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.

Progress summary

Open

The conjecture remains open: only coordinate coalescence and matching first two moments have been established, not the proposed beta limits.

The conjecture asks whether, as cc\to\infty, both coordinates approach the same beta distribution in the two-island and seed-bank settings. It appears as Conjecture 2.7 in a 2024 preprint.

Known results

  • The stationary coordinates satisfy XY0X-Y\to 0 in probability as cc\to\infty.
  • The first and second stationary moments match those of the conjectured beta laws.
  • The exact stationary distribution is generally unknown, and these observations are given only as motivation, not as a proof.

Current status (as of August 2026): The conjectured beta limits for both the two-island and seed-bank cases remain unproved, with no verified counterexample or resolution found.

Sources
Sources & referencesView supporting material

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).

Solutions 1

Counterexample

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(yx)]fx+α2x(1x)fxx+[b1(b1+b2)y+γc(xy)]fy+β2y(1y)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 cc\to\infty,

(Xc,Yc)(Z,Z),ZBeta(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 (xy)2(x-y)^2 gives

E(XcYc)2=O(c1).\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 hC2[0,1]h\in C^2[0,1],

E[{u1(u1+u2)W}h(W)+K2(1+γ)W(1W)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+r1θ1+θ2+r1mr1,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

ZBeta(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

ZBeta(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

limcEXc2=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 .

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