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Evidence for Dihedral D₃ Symmetry in the Planck CMB Temperature Anisotropy

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03 April 2026

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03 April 2026

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Abstract
We report a statistically significant detection of dihedral D₃ symmetry in the Planck PR3 temperature anisotropy data, validated across all four independent component-separation pipelines (SMICA, NILC, SEVEM, Commander). At a single optimized axis (ℓ, b) = (50.3°, −64.9°), the power fraction in the A₂ (reflection-antisymmetric) irreducible representation exceeds isotropic expectations with a two-tier structure: a dense cluster at l ≤ 15 (Fisher PTE = 4.2 × 10⁻³ to 1.2 × 10⁻² across maps), driven by three multipoles significant in all four pipelines, with l = 3 serving as the axis-registration multipole (f_A₂ = 0.94, z > 4.4) and l = 7 and l = 9 providing independent corroboration at the fixed axis, plus sporadic cross-map-validated recurrences at higher multipoles—notably l = 34 (significant in 3/4 maps) and l = 63 (3/4 maps). The A₂ excess draws power specifically from the E (rotation-doublet) irrep with anti-correlation r = −0.81, while the A₁ (trivial) irrep is decoupled. Extension to l_max = 150 with N_MC = 10,000 simulations shows that the aggregate high-l Fisher PTE is consistent with isotropy (PTE > 0.91), but individual multipoles punctuate this null background. Among the nine strongest cross-map-consistent peaks, none belongs to the l ≡ 2 (mod 3) residue class (p ≈ 0.02 under uniformity), consistent with the C₃ selection rule. Cross-map correlations of f_A₂(l) exceed r = 0.93 for all pipeline pairs (SMICA–NILC: r = 0.997), ruling out component-separation artifacts. A null test on E-mode polarization at the same axis returns Fisher PTE = 0.70, confirming that the signal is confined to the temperature channel as expected. The irrep redistribution is sharply parity-gated: all four maps confine the A₂ collecting signal to odd-l multipoles (Fisher p < 2 × 10⁻⁴), with even-l entirely null (p > 0.97). Crossing parity with residue class produces a six-cell grammar dominated by a single cell (odd, l ≡ 0 mod 3), with step-function onset at l = 3. Singular-value decomposition reveals that this 2 × 3 grammar admits an approximate rank-1 factorization into a binary parity selector and a D₃ residue routing vector, recovered independently by all four pipelines (rank-1 fraction > 94% in three of four maps). The binary gate acts on irrep redistribution, not on total power: a parity split of raw C_l is null (PTE > 0.61) in every map. The signal morphology—dense at large angular scales with isolated resonances at smaller scales—is consistent with a parity-gated boundary condition on the acoustic eigenvalue problem whose geometry is fully resolved only at l ≲ 15 (θ ≳ 12°). No physical model parameters are fit; the single directional degree of freedom (axis orientation) is determined from the octupole alone and then frozen.
Keywords: 
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1. Introduction

The temperature anisotropies of the cosmic microwave background (CMB), as measured by WMAP [4] and Planck [1], are broadly consistent with the predictions of the standard Λ CDM cosmology: a statistically isotropic, Gaussian random field with a nearly scale-invariant power spectrum. However, a persistent set of large-angle anomalies has resisted explanation within this framework [3,5].
These include the anomalous alignment of the quadrupole ( l = 2 ) and octupole ( l = 3 ) principal axes [6,7], the hemispherical power asymmetry [8], the low quadrupole amplitude, and the odd-parity preference at low l [9]. Individually, each anomaly has marginal significance ( 2 3 σ ); collectively, they suggest a preferred direction in the low-l CMB that the standard model does not predict.
Numerous explanations have been proposed, including non-trivial cosmic topology [11,12], anisotropic dark energy [13], and residual foregrounds [14]. Most address one anomaly at a time and leave the others unexplained.
In this work, we pursue a different approach: we test whether the dihedral group  D 3 —the symmetry group of the equilateral triangle, of order | D 3 | = 6 —organizes the angular power spectrum at a single preferred axis. D 3 is the smallest non-abelian finite group and the Weyl group of the Lie algebra su ( 3 ) ; it can simultaneously produce quadrupole–octupole alignment (through its C 3 rotational subgroup), hemispherical-type asymmetry (through its reflection planes), and a selection rule with period 3 in l (through its irreducible representation structure).
The analysis extends to l max = 150 and is validated across all four Planck PR3 component-separation pipelines. This allows us to determine whether the signal persists to high multipoles or is confined to the largest angular scales, and to rule out pipeline-specific artifacts.
The paper is organized as follows. In Section 2 we derive the decomposition of spherical harmonics into D 3 irreducible representations. In Section 3 we describe the data and Monte Carlo methodology. In Section 4 we present the results: axis determination, per-multipole irrep fractions, combined significance, inter-irrep correlations, and the transition scale. Section 5 reports the cross-map validation. Section 6 presents null tests. Section 7 examines the cumulative transfer structure, including the parity-gated grammar and its factorized form. In Section 8 we discuss the physical interpretation and identify falsifiable predictions.

2. D 3 Irrep Decomposition of Spherical Harmonics

2.1. Action of D 3 on S 2

The irrep decomposition is not performed directly on the observed a l m in Galactic coordinates. Instead, a candidate D 3 axis is chosen and the coefficients are rotated into a frame where that axis is the pole; the group then acts in this rotated frame. The axis is later optimized from the data (Section 3.3).
Let the D 3 symmetry axis coincide with the z-axis of a coordinate system on S 2 . The group D 3 is generated by a rotation C 3 through 2 π / 3 about z ^ and a reflection σ v through a vertical plane containing z ^ . Under C 3 , a spherical harmonic Y l m acquires a phase:
C 3 Y l m = e 2 π i m / 3 Y l m .
The harmonics therefore sort by m mod 3 :
  • m 0 ( mod 3 ) : invariant under C 3 (eigenvalue 1),
  • m 1 ( mod 3 ) : eigenvalue ω = e 2 π i / 3 ,
  • m 2 ( mod 3 ) : eigenvalue ω 2 = e 4 π i / 3 .
The m ± 1 ( mod 3 ) pairs combine into two-dimensional E doublets. The m 0 ( mod 3 ) harmonics are further split by the reflection σ v , which maps m m :
A 1 : 1 2 ( Y l , m + Y l , m ) , m = 0 , 3 , 6 , l ,
A 2 : 1 2 ( Y l , m Y l , m ) , m = 3 , 6 , 9 , l ,
where Y l , 0 is automatically symmetric and contributes only to A 1 .

2.2. Subspace Dimensions

The dimensions of the three irrep subspaces at multipole l are:
d A 1 ( l ) = l / 3 + 1 ,
d A 2 ( l ) = l / 3 ,
d E ( l ) = 2 l + 1 2 l / 3 1 = 2 l l / 3 ,
satisfying d A 1 + d A 2 + d E = 2 l + 1 .
A critical structural property follows: d A 2 increases by one unit precisely when l crosses a multiple of 3. This means that at l 0 ( mod 3 ) , the A 2 subspace acquires a new degree of freedom—a new “antenna element” tuned to the reflection-plane boundary. At l = 1 , d A 2 = 0 : the dipole contains no A 2 subspace, and is structurally excluded from the present analysis by the representation theory itself.

2.3. Isotropic Baseline

For a statistically isotropic Gaussian random field, all a l m at fixed l are independent with equal variance. The expected power fraction in each irrep is therefore proportional to its subspace dimension:
f X ( l ) iso = d X ( l ) 2 l + 1 , X { A 1 , A 2 , E } .
Table 1 lists the subspace dimensions and isotropic baselines for l = 2 –12.
Figure 1. Left: Subspace dimensions d X ( l ) for the three D 3 irreps. d A 2 = l / 3 increments (red dots) at l 0 ( mod 3 ) ; these dimension jumps drive the l mod 3 selection rule. Right: Isotropic expected fractions f X = d X / ( 2 l + 1 ) . All three approach their asymptotic values ( 1 / 3 for A 1 and A 2 ; 2 / 3 for E) at large l, with sawtooth modulation at period 3.
Figure 1. Left: Subspace dimensions d X ( l ) for the three D 3 irreps. d A 2 = l / 3 increments (red dots) at l 0 ( mod 3 ) ; these dimension jumps drive the l mod 3 selection rule. Right: Isotropic expected fractions f X = d X / ( 2 l + 1 ) . All three approach their asymptotic values ( 1 / 3 for A 1 and A 2 ; 2 / 3 for E) at large l, with sawtooth modulation at period 3.
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3. Data and Method

3.1. Planck Data

We analyze all four Planck PR3 (2018) component-separated temperature maps: SMICA, NILC, SEVEM, and Commander [2]. Each map is provided at HEALPix N side = 2048 and internally downgraded to N side = 256 (sufficient for l max = 150 ). Spherical harmonic coefficients a l m are extracted using healpy.map2alm [15].
For the polarization null test (Section 6), E-mode a l m E are extracted from the SMICA IQU polarization map at N side = 64 .

3.2. D 3 Decomposition

At each multipole l and a given axis ( gal , b gal ) , the a l m are rotated into the frame where the candidate D 3 axis is the pole. The rotation uses healpy.rotate_alm with Euler angles ( ϕ , θ , 0 ) , where ( θ , ϕ ) are the colatitude and longitude of the D 3 antipode. The power in each irrep is:
P X ( l ) = m M X ( l ) | a l m | 2 , f X ( l ) = P X ( l ) C l ,
where C l = m | a l m | 2 and M X ( l ) is the set of m-indices belonging to irrep X at multipole l. Note that f A 1 + f A 2 + f E = 1 by construction.

3.3. Axis Optimization

The preferred axis is determined by maximizing f A 2 at l = 3 (the octupole) over a HEALPix grid at N side = 32 (12,288 directions; mean pixel spacing 1 . 8 ), followed by a deterministic local refinement on a 0 . 2 -spaced sub-grid within 5 of the coarse optimum. The optimal axis is then fixed for all subsequent analysis at l 3 . This protocol ensures that the results at all other multipoles are effectively pre-registered: the axis was determined from l = 3 data alone.

3.4. Monte Carlo Simulations

Statistical significance is assessed against N MC = 10 , 000 isotropic Gaussian random realizations. For isotropic fields, the D 3 fraction distribution is frame-invariant by rotational symmetry, so the MC simulations generate random a l , m directly in the D 3 frame without rotation: a l , 0 N ( 0 , 1 ) (real), a l , m N ( 0 , 1 ) + i N ( 0 , 1 ) for m > 0 , with the Condon–Shortley convention a l , m = ( 1 ) m a ¯ l , m . This avoids the O ( l 2 ) cost of Wigner-D rotation per simulation.
The probability to exceed (PTE) for each l is the fraction of simulations with f A 2 f A 2 obs . PTEs of exactly zero (no simulation exceeded the observed value) are set to 0.5 / N MC as a conservative upper bound.
Combined significance across multipoles uses Fisher’s method:
χ Fisher 2 = 2 i ln ( PTE i ) ,
compared to a χ 2 distribution with 2 k degrees of freedom, where k is the number of contributing multipoles.

3.5. Statistical Protocol

To assist the reader in assessing trial factors, we summarize the complete analysis protocol:
1.
Axis selection. The axis is chosen by maximizing f A 2 ( l = 3 ) on a HEALPix N side = 32 grid ( 1 . 8 resolution) with local refinement. This is the sole optimization step and constitutes a single directional degree of freedom.
2.
Axis freezing. The same axis is then held fixed for all multipoles l 3 , all four component-separation maps, and all subsequent tests. The l = 3 octupole should therefore be understood as the axis-defining (registration) statistic, not as an independently pre-registered detection.
3.
Significance assessment. Per-multipole PTEs are computed against N MC = 10 , 000 isotropic Gaussian Monte Carlo realizations with the same decomposition.
4.
Primary significance claim. The Fisher combined PTE for l = 2 –15 across all four maps (Table 4).
5.
Replication criterion. Cross-map agreement is used as a replication standard, not as a tuning parameter: the axis is never re-optimized per pipeline.
6.
Secondary analyses. The top-9 peak residue-class test and the l mod 3 permutation test are designated a posteriori supportive analyses; they are not part of the primary significance claim.

4. Results

4.1. Axis Determination

The axis maximizing f A 2 ( l = 3 ) is found at Galactic coordinates
( , b ) = ( 50 . 3 , 64 . 9 ) ,
with f A 2 ( l = 3 ) = 0.940 (SMICA). Because this multipole was used to define the axis, its significance ( z > 4.4 against isotropic simulations) should be interpreted as a detection statistic used for registration, not as an independently pre-registered exceedance. The real evidence for D 3 symmetry lies in the replication of the same axis in independent multipoles ( l = 7 , 9 ) and across all four maps.
The optimal axis lies 5 . 8 from the antipode of the Axis of Evil [10], indicating that the D 3 signal and the previously reported quadrupole–octupole alignment share a common preferred direction.
Figure 2 visualizes the D 3 structure on the sky. When the Planck SMICA map is rotated so the D 3 axis points to the pole, the l = 3 octupole (panel a) displays the predicted six-lobe pattern: three hot spots and three cold spots alternating at 120 intervals, with the C 3 rotation axes (solid gold lines) passing through the alternating lobes and the σ v reflection planes (dashed white) bisecting them. Combining the three driving multipoles l = 3 , 7 , 9 (panel b) sharpens the structure rather than diluting it, confirming coherent D 3 alignment across angular scales. The full signal band l = 2 –15 (panel c) retains the pattern even with the addition of E-dominated modes, demonstrating that the A 2 signal survives superposition. Panel (d) shows that the axis is objectively determined by the data: an all-sky scan of f A 2 ( = 3 ) peaks sharply at the optimal direction, with no comparably strong secondary maxima.

4.2. Per-Multipole Irrep Fractions

Figure 3 shows f A 2 ( l ) for l = 2 –150 at the fixed axis (SMICA), compared to the isotropic baseline and Monte Carlo 1 σ / 2 σ bands. The signal exhibits a two-tier structure: a dense cluster of excess at l 15 , and sporadic but individually significant peaks at higher multipoles.
Table 2 provides detailed numerical results for the low-l region. Table 3 lists the nine strongest cross-map-consistent peaks across l = 2 –150. Three multipoles drive the primary detection in all four maps:
1.
Octupole ( l = 3 ): f A 2 = 0.910 0.943 across maps, PTE < 10 4 ( z > + 4.4 ). The octupole exceeds 4 σ in every pipeline.
2.
l = 7 : f A 2 = 0.481 0.496 , PTE = 0.013 0.016 ( z + 2.9 ).
3.
l = 9 : f A 2 = 0.392 0.478 , PTE = 0.014 0.044 ( z = + 2.0 to + 2.7 ).
Beyond the primary cluster, two high-l multipoles show cross-map-consistent A 2 excess: l = 34 (significant at PTE < 0.05 in SMICA, NILC, and Commander; SEVEM marginal at 0.056 ) and l = 63 ( PTE < 0.05 in SMICA, NILC, and Commander; SEVEM at 0.050 ). These are not isolated noise fluctuations: they replicate across independent pipelines at the same fixed axis.

4.3. Combined Significance

Table 4 presents the Fisher combined PTE for different multipole ranges across all four maps. The low-l sector ( l = 2 –15) shows a statistically unlikely concentration of A 2 excess in all four pipelines. Excluding the axis-defining octupole, the combined Fisher statistic is null (PTE = 0.87 0.99 ), indicating that l = 7 and l = 9 corroborate the same axis-specific structure but do not by themselves constitute an independent aggregate detection. Their evidential value is replication at the registered axis, not a second standalone Fisher-level discovery.
The aggregate Fisher PTE for l = 16 –150 is consistent with isotropy in every map (PTE  > 0.91 ). However, this aggregate statistic masks the presence of individually significant, cross-map-validated outliers at l = 34 and l = 63 (Table 3). The high-l range is best characterized as an isotropic background punctuated by isolated resonances at the same D 3 axis.

4.4. Inter-Irrep Correlations

The deviations Δ f X = f X obs f X iso across l = 2 –150 satisfy a strict conservation law:
Δ f A 1 ( l ) + Δ f A 2 ( l ) + Δ f E ( l ) = 0
at every l, exact to machine precision ( 10 15 ). This confirms that the D 3 decomposition is a pure redistribution of power among irreps, not a net excess or deficit.
The Pearson correlation coefficient between Δ f A 2 and Δ f E is strongly negative across all maps:
r ( Δ f A 2 , Δ f E ) = 0.81 ± 0.03 ( range across maps ) ,
with individual values SMICA: 0.805 , NILC: 0.809 , Commander: 0.806 , SEVEM: 0.743 . The A 2 excess draws power specifically from the E (doublet) irrep, not from A 1 . Figure 4 displays this anti-correlation.

4.5. The l mod 3 Selection Rule

A permutation test ( 10 , 000 random partitions) for whether l 0 ( mod 3 ) multipoles show preferential A 2 loading yields marginal results when applied to the full range l = 2 –150: Commander PTE  = 0.055 , SMICA PTE  = 0.074 , NILC PTE  = 0.079 , SEVEM PTE  = 0.092 .
A complementary (a posteriori) test examines the top-9 cross-map peaks (Table 3). Their residue class distribution is: l mod 3 = 0 (five multipoles: l = 3 , 9 , 18 , 12 , 63 ), l mod 3 = 1 (four: l = 7 , 34 , 31 , 46 ), and l mod 3 = 2 (zero). Under uniform random selection, the probability of drawing 0 / 9 from the l 2 ( mod 3 ) class is 0.02 . The complete absence of the residue class where d A 2 does not increment is consistent with the C 3 selection rule: the A 2 excess requires the new basis vector 1 2 ( Y l , 3 k Y l , 3 k ) that appears at l 0 ( mod 3 ) , or the adjacent l 1 ( mod 3 ) class where the E-doublet dimension also steps.
Figure 5 displays the mean Δ f A 2 grouped by residue class.

4.6. Signal Morphology

The D 3 signal does not exhibit a sharp cutoff. Instead, the A 2 excess shows a two-tier structure:
1.
Dense cluster ( l 15 ): Four of the thirteen multipoles ( 31 % ) exceed f A 2 > 0.27 , compared to an isotropic expectation of 5 % . The Fisher combined PTE for this range is 4.2 12 × 10 3 across maps.
2.
Sporadic resonances ( l > 15 ): Four of 135 multipoles ( 3 % ) exceed f A 2 > 0.27 , compared to an expected 1.5 % under isotropy. The aggregate Fisher PTE ( > 0.91 ) is null, but two individual multipoles ( l = 34 , l = 63 ) achieve PTE < 0.05 in three of four maps.
Figure 6 shows the running sum of Δ f A 2 , which rises steeply for l 15 , partially plateaus, then shows mild step-ups at the sporadic resonances—consistent with a boundary condition whose geometry is fully resolved at large angular scales but produces isolated overtones at specific higher harmonics.

4.7. Real-Space D 3 Pattern

The harmonic-space analysis can be visualized in real space by rotating the Planck SMICA map into the D 3 frame (where the D 3 axis is the pole) and examining the temperature field as a function of azimuth ϕ at fixed colatitude θ . Figure 7 shows this visualization for the D 3 -active multipoles ( l = 2 –15 and the three driving multipoles l = 3 , 7 , 9 ).
The equatorial ring ( θ = 90 ) displays a clear large-amplitude oscillation with three-fold structure (Figure 7, upper left). This pattern persists across colatitudes from 45 to 110 (upper right), confirming that the signal is not confined to the equatorial plane but pervades the hemisphere geometry.
The azimuthal Fourier spectrum of the equatorial ring (lower left) confirms the C 3 origin: for the l = 3 , 7 , 9 band, the m = 3 mode dominates, with m 0 ( mod 3 ) modes carrying the bulk of the power. This is the real-space manifestation of the m mod 3 sorting that defines the D 3 irrep decomposition (Equation (1)).
Most directly, the azimuthal auto-correlation (lower right) reveals:
r ( Δ ϕ = 120 ) = + 0.222 ,
r ( Δ ϕ = 60 ) = 0.234 .
Points separated by 120 around the D 3 axis see correlated temperatures ( C 3 rotational symmetry), while points at 60 —straddling a reflection plane—see anti-correlated temperatures ( σ v anti-symmetry). This alternating sign pattern with period 60 is the real-space fingerprint of the A 2 (reflection-antisymmetric) irrep that dominates the harmonic-space signal.

5. Cross-Map Validation

A critical test is whether the D 3 signal is consistent across independent component-separation methods. The four Planck PR3 pipelines (SMICA, NILC, SEVEM, Commander) use different algorithms and foreground models; agreement among them rules out pipeline-specific artifacts.
Table 5 presents the Pearson correlation of f A 2 ( l ) between all map pairs over l = 2 –150. The correlations range from r = 0.932 (NILC–SEVEM) to r = 0.997 (SMICA–NILC). SMICA and NILC are nearly identical; SEVEM shows slightly more variation but remains highly correlated with all other maps.
Figure 8 overlays f A 2 ( l ) from all four maps, demonstrating the remarkable agreement—particularly in the signal region ( l 15 ), where the four curves are nearly indistinguishable.

6. Null Tests

6.1. Aggregate High-l Null

The Fisher PTE for l = 16 –150 is > 0.91 in all four maps (Table 4). The aggregate high-l range does not show a sustained collective A 2 excess. All four pipelines agree on this. However, this aggregate null coexists with the isolated cross-map-validated peaks at l = 34 and l = 63 discussed in Section 4.6—highlighting the distinction between a diffuse persistent signal (absent) and discrete resonances (present).

6.2. E-Mode Polarization

The D 3 decomposition was applied to E-mode polarization a l m E from the Planck SMICA IQU map at N side = 64 . No multipole shows f A 2 E E > 0.50 . The Fisher combined PTE for the key multipoles ( l = 3 , 6 , 7 , 9 ) is 0.70 —fully consistent with isotropy. An independent axis optimization on the EE data yields an axis 83 from the TT optimum, confirming the signals are unrelated.
This null is physically expected. Low-l E-mode polarization arises from reionization Thomson scattering at z 6 –10, well inside the last-scattering surface where the D 3 boundary condition operates on acoustic modes.

6.3. Axis Stability

The TT-optimal axis at l = 3 is stable under variation of the input data: using the full-resolution ( N side = 2048 ) map versus downgraded versions yields axis shifts < 2 .

7. Cumulative Transfer Structure

The per-multipole A 2 excesses discussed in Section 4 are signed: each multipole either collects power into A 2 ( Δ f A 2 > 0 ) or pays power out ( Δ f A 2 < 0 ). We define the transfer ledger  τ l f A 2 obs ( l ) f A 2 iso ( l ) and study its cumulative behavior across the full multipole range l = 2 –150.

7.1. Normalized Transfer Invariant

Partition the cumulative transfer into residue classes,
T r ( L ) = l L l mod 3 = r τ l , r { 0 , 1 , 2 } ,
and define the normalized invariant
Ξ ( L ) = T 0 ( L ) T 2 ( L ) σ MC [ T 0 ( L ) T 2 ( L ) ] ,
where σ MC is the standard deviation of T 0 T 2 under N MC = 10 , 000 isotropic simulations, evaluated at each L. This quantity measures the cumulative residue-class asymmetry of the A 2 transfer in units of the isotropic null.
Figure 9 shows Ξ ( L ) as a function of the upper summation boundary L max . Three features are noteworthy:
1.
Stable plateau. Ξ ( L ) rises to + 3 σ by L = 15 and remains between + 2.5 and + 3.1 across all four component-separation maps out to L = 150 . The inter-map spread is less than 0.3 σ at every checkpoint (Table 6).
2.
A 2 specificity. The analogous invariant computed for the A 1 irrep fluctuates around zero ( Ξ A 1 < 0.6 at all L), while the E invariant mirrors A 2 at Ξ E 3 σ —a direct consequence of the per-multipole conservation Δ f A 1 + Δ f A 2 + Δ f E = 0 . The transfer is thus an E A 2 funnel with A 1 as spectator, extending the correlation reported in Section 8.2.
3.
Jackknife stability. Removing l = 9 alone reduces Ξ ( 150 ) from + 2.5 to + 2.1 ; removing l = 3 alone reduces it to + 1.2 . Removing all three low-l anchors ( l = 3 , 7 , 9 ) collapses the invariant to + 0.7 , confirming that the signal is dominated by the dense cluster at l 15 . This is consistent with the two-tier morphology identified in Section 4.6: the boundary condition is fully resolved at large angular scales.
The persistence of Ξ ( L ) to L = 150 does not imply an independent high-l detection; it reflects the survival of the low-l transfer asymmetry as additional high-l null multipoles are cumulatively added (cf. the aggregate high-l null in Section 6.1).
Restricting the summation to the 94 cross-map sign-consistent multipoles (63% of the total) strengthens the invariant: Ξ rises from + 2.53 to + 2.88 at L = 150 , indicating that the sign-inconsistent multipoles dilute the signal rather than contribute to it.

7.2. One-Way Collect Rule

Among all multipoles individually significant at PTE < 0.05 in two or more pipelines, the cross-map mean τ l is positive in every case. That is, every statistically robust transfer event collects power into  A 2 ; none pays out. This one-way rule holds under all thresholds tested (1/4 to 4/4 maps significant, PTE thresholds of 0.05 and 0.10 ), producing a binomial probability 2 8 under the null hypothesis of symmetric pay/collect.

7.3. Parity-Gated Transfer Grammar

The D 3 group contains rotations and reflections but no spatial inversion; it does not distinguish odd from even l. Nevertheless, the transfer ledger splits sharply by parity. The mean excess Δ f A 2 is positive for odd l and negative for even l in all four pipelines (Table 7). Aggregated via Fisher’s method, the odd-l subset yields a combined PTE < 2 × 10 4 in every map, while the even-l subset is entirely null ( PTE > 0.97 ).
This parity split is not an artifact of A 2 subspace dimensions: odd and even l contribute nearly equal total A 2 capacity ( d A 2 = 1850 vs. 1875 for l = 2 –150).
Crucially, the split is not confined to  A 2 . The E irrep shows the mirror pattern (even > odd) at comparable or stronger significance ( PTE perm < 0.015 in SMICA and Commander), while A 1 is marginally patterned ( PTE 0.06 ). Because Δ f A 1 + Δ f A 2 + Δ f E = 0 at every l, the parity gate acts on the entire redistribution system, not on a single output channel.

The Six-Cell Grammar

Crossing parity with the residue class l mod 3 produces a 2 × 3 transfer grammar (Table 8). The structure is dominated by a single cell: odd multipoles in the l 0 ( mod 3 ) class carry a cumulative A 2 transfer of + 1.15 , while every even-l cell drains. This is not “odd good, even bad”: the odd ( r = 1 ) and odd ( r = 2 ) cells are near-neutral or draining. The gate selects the intersection of odd parity and the D 3 -preferred residue class.
The onset of this grammar is sharp. At l = 1 , the A 2 subspace has dimension zero (a group-theory identity confirmed to machine precision in all maps). At l = 2 (even), Δ f A 2 = 0 to four decimal places. At l = 3 —the first multipole that is both odd and carries d A 2 > 0 —the signal switches on at z + 4.5 . The transition from silence to the strongest detection in the entire spectrum occurs at the first algebraically allowed mode of the parity-gated D 3 grammar.
This two-layer structure— D 3 residue routing overlaid by a binary parity gate—is consistent with a two-branch boundary selection law rather than a generic parity anomaly. A background parity asymmetry would modulate total power C l without preferentially acting on the irrep redistribution; the observed effect acts specifically on the transfer grammar. Indeed, a permutation test on raw C l confirms this: the odd/even parity split in total power is null ( PTE > 0.61 ) in all four maps, while the same test applied to Δ f A 2 yields PTE as low as 0.03 (SEVEM). The binary gate acts on routing, not on total power.

7.4. Factorized Transfer Law

The six-cell grammar of Table 8 can be viewed as a 2 × 3 matrix
M ( L ) = T odd , 0 ( L ) T odd , 1 ( L ) T odd , 2 ( L ) T even , 0 ( L ) T even , 1 ( L ) T even , 2 ( L ) ,
where the rows index parity and the columns index the residue class l mod 3 . A singular-value decomposition (SVD) of M ( 150 ) reveals that the matrix is approximately rank 1 (Table 9):
M ( L ) σ 1 u v ,
with σ 1 / σ 2 > 4 in three of four maps. The dominant left vector u R 2 encodes a binary gate (odd positive, even negative), and the dominant right vector v R 3 encodes a D 3 routing pattern ( r = 0 dominant, r = 1 inert, r = 2 draining).
Cross-map stability is high: the minimum pairwise cosine similarity is 0.967 for u and 0.988 for  v . The same binary branch and same D 3 routing vector are recovered by all four independent component-separation pipelines. The rank-1 fraction exceeds 94 % at L = 50 –75 in all maps and remains above 90 % in three of four pipelines through L = 150 . The exception is SEVEM ( 77 % ), whose template-fitting method introduces larger even-l transfer amplitudes (roughly 2– 3 × those of the ILC and Bayesian pipelines), inflating σ 2 and diluting the rank-1 fraction; however, the SEVEM singular vectors u and v still align with the other three maps (pairwise cosine > 0.94 ), so the same grammar is recovered with a noisier gate. The factorization reflects the dominant low-l boundary phase identified in Section 8.1 and remains stable in the cumulative matrix as null high-l multipoles are added. The factorization should be understood as a property of the cumulative low-l-dominated transfer matrix, not as a claim that the same singular vectors characterize the high-l sector in isolation.
In summary, the entire D 3 transfer structure admits an approximate factorization into two primitive components: a binary parity selector and a three-fold residue routing grammar. This factorized form is more constrained than either the residue-class hierarchy or the parity gate taken separately, and suggests that the underlying boundary law has an internal 2 × 3 product structure.
Figure 10. The 2 × 3 transfer grammar. Left: Observed four-map mean transfer matrix M ( 150 ) , partitioned by parity (rows) and residue class l mod 3 (columns); error bars show inter-map spread. Center: Best rank-1 reconstruction σ 1 u v . Right: Residual (observed − reconstruction), showing that the rank-1 approximation captures the dominant structure. The single dominant cell (odd, r = 0 ) and the near-zero residuals confirm the factorized transfer law.
Figure 10. The 2 × 3 transfer grammar. Left: Observed four-map mean transfer matrix M ( 150 ) , partitioned by parity (rows) and residue class l mod 3 (columns); error bars show inter-map spread. Center: Best rank-1 reconstruction σ 1 u v . Right: Residual (observed − reconstruction), showing that the rank-1 approximation captures the dominant structure. The single dominant cell (odd, r = 0 ) and the near-zero residuals confirm the factorized transfer law.
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7.5. Empirical Signature Summary

Table 10 collects the identified empirical properties of the D 3 signal, their observables, quantitative results, and evidential status. Primary claims are those supported by pre-registered statistics or clear null controls; supportive observations are a posteriori structural patterns that sharpen the interpretation but do not constitute standalone detections.

8. Discussion

8.1. A Large-Angle Boundary Condition

The detected D 3 symmetry should not be confused with a claim of multiply-connected spatial topology. Topological models (e.g., the Poincaré dodecahedral space [11]) tile the spatial 3-manifold with a discrete group. The D 3 signal reported here is an angular spectral property: the irrep decomposition of a l m at each l reveals preferential excitation of the reflection-antisymmetric subspace at a fixed axis on S 2 .
The two-tier morphology—dense cluster at l 15 plus sporadic resonances at l = 34 and l = 63 —constrains the physical mechanism. A rigid geometric template would produce excess at all l; a foreground systematic would correlate with the mask geometry and would not replicate across independent component-separation pipelines. The observed pattern is instead consistent with a boundary condition on the acoustic eigenvalue problem: the boundary geometry is fully resolved by modes at l 15 ( θ 12 ), producing the dense cluster, while specific higher harmonics whose angular wavelengths happen to alias the boundary structure produce isolated resonances.
The primary scale l 15 corresponds to angular separations of order 12 , or comoving distances of approximately 800 Mpc at the last scattering surface—comparable to the largest observed structures in the cosmic web. The resonances at l = 34 ( θ 5 . 3 ) and l = 63 ( θ 2 . 9 ) may represent overtones of the same boundary geometry.
The rank-1 factorization of the transfer matrix (Section 7.4) further constrains the boundary’s internal structure. The approximate decomposition M σ 1 u v implies that the boundary law is not irreducibly six-fold but has an internal 2 × 3 product form: a binary parity selector composed with a three-fold residue routing grammar. This factorized structure is stable across all four pipelines and reflects the dominant low-l boundary phase, suggesting two primitive components in the boundary condition rather than a single monolithic selection rule.

8.2. Representation-Theoretic Structure

The signal is not a generic anisotropy. Four features identify it specifically as D 3 :
1.
A 2 specificity. The collecting excess concentrates in the reflection-antisymmetric irrep, with a mirrored depletion in the E (rotation-doublet) irrep and A 1 largely acting as spectator. An arbitrary dipolar or quadrupolar modulation would populate all irreps comparably.
2.
E A 2 funnel. The anti-correlation r ( Δ f A 2 , Δ f E ) = 0.81 with A 1 decoupled is consistent with the reflection planes being the geometrically active elements. The cumulative transfer invariant (Section 7) confirms this structure: Ξ A 2 and Ξ E are mirror images while Ξ A 1 0 , and every statistically robust event collects into  A 2 . In the Weyl chamber of S U ( 3 ) , the reflection hyperplanes (walls) separate adjacent chambers; the observed power transfer from E (rotations) to A 2 (reflections) admits an interpretation in which these walls act as boundary surfaces.
3.
l mod 3 selection rule. The aggregate permutation test is marginal ( PTE 0.06 0.09 ). As a supportive (a posteriori) observation, the top-9 cross-map peaks show zero entries from l 2 ( mod 3 ) ( p 0.02 ); however, the threshold defining “top 9” was not pre-specified and this test should be regarded as suggestive rather than confirmatory. The period of 3 is consistent with the order of the rotational subgroup C 3 D 3 and with the Coxeter number h = 3 of the root system A 2 , distinguishing D 3 = Weyl ( A 2 ) from other dihedral groups D n with n 3 .
4.
Parity-gated transfer. Although D 3 contains no spatial inversion, the irrep redistribution is sharply gated by parity: the entire A 2 collecting signal resides in odd-l multipoles, while even-l multipoles are null (Section 7.3). The gate acts across all three irreps simultaneously, ruling out an A 2 -specific artifact. The six-cell grammar (parity × residue class) isolates the signal to a single cell—odd, l 0 ( mod 3 ) —and the onset at l = 3 (the first algebraically allowed mode) is step-like rather than gradual. This two-branch selection law is an additional structural constraint beyond D 3 alone, consistent with a hidden binary boundary encoding.

8.3. Connection to the Vacuum Energy Sector

The spherical boundary Σ S 2 on which D 3 acts is also the surface on which the monopole ( l = 0 ) channel of the cosmological causal diamond projects. The D 3 analysis operates at l 2 ; the vacuum energy density, being spatially uniform, projects entirely onto l = 0 . These are different harmonic channels of the same S 2 boundary.
A first-principles derivation connecting the Standard Model field content on this boundary to the observed cosmological constant, yielding Ω Λ = 0.6948 with zero free parameters (deviation 0.4 σ from observation), has been presented elsewhere [16]. The present detection of D 3 at l 2 is consistent with the hypothesis that the boundary Σ S 2 carries physically observable structure, though the CMB result alone does not require this interpretation. The cosmological-constant connection is not part of the statistical claim of the present paper; it is noted here only to indicate a possible theoretical context.

8.4. Falsifiable Predictions

The D 3 boundary-condition interpretation makes specific predictions testable with forthcoming data:
1.
Resonance spectrum. If l = 34 and l = 63 are overtones of a boundary geometry, additional resonances should appear at predictable multipoles determined by the boundary’s angular structure. Extension to l max = 500 –1000 with CMB-S4 [17] data will test whether the sporadic peaks continue or are confined to l 100 .
2.
l 2 ( mod 3 ) exclusion. The current 0 / 9 absence of this residue class among the strongest peaks ( p 0.02 ) should persist or strengthen with deeper data. A single strong l 2 ( mod 3 ) peak would disfavor the C 3 selection-rule mechanism.
3.
Cross-survey consistency. The D 3 signal should appear in future independent CMB measurements (LiteBIRD [18], Simons Observatory [19]) at the same axis and with the same two-tier morphology.
4.
Lensing B-modes. If the boundary condition imprints on the matter field, gravitational-lensing B-modes should show a residual D 3 signal at low l.
5.
Parity-gate persistence. The odd-only concentration of the D 3 transfer should persist at higher l and in independent surveys. If the gate is a genuine two-branch boundary law, no even-l multipole should enter the dominant collecting cell at any l max .

9. Conclusions

We have presented evidence for dihedral D 3 symmetry in the Planck CMB temperature anisotropy, validated across all four independent component-separation pipelines at a single preferred axis. The signal has a two-tier morphology: a dense cluster at l 15 (Fisher PTE = 4.2 × 10 3 to 1.2 × 10 2 ), driven by three multipoles ( l = 3 , 7 , 9 ) significant in every map, plus cross-map-validated resonances at l = 34 and l = 63 (each significant in 3/4 pipelines).
Four features specifically identify D 3 rather than a generic anisotropy: concentration in the A 2 (reflection-antisymmetric) irrep, an E A 2 power funnel with r = 0.81 , supportive evidence for a C 3 selection rule from the absence of l 2 ( mod 3 ) multipoles among the strongest peaks, and a parity-gated transfer grammar in which the entire signal resides in odd-l multipoles while even-l is null across all irreps. The cumulative transfer invariant Ξ A 2 ( L ) + 3 σ remains stable from L = 15 to 150 across all four pipelines, with a one-way collect rule (every statistically robust event adds power to  A 2 ) and the expected A 1 /E conservation-law mirror. The six-cell parity × residue-class grammar isolates the collecting signal to a single cell (odd, l 0 ( mod 3 ) ), with step-function onset at l = 3 . Singular-value decomposition of the 2 × 3 transfer matrix reveals an approximate rank-1 factorization into a binary parity selector u ( + , ) and a D 3 routing vector v ( + , 0 , ) , stable across pipelines (minimum pairwise cosine > 0.96 ). The boundary law thus has an internal 2 × 3 product structure rather than a single monolithic selection rule. Cross-map correlations exceeding r = 0.93 for all pipeline pairs rule out component-separation artifacts, and a null result in E-mode polarization (Fisher PTE  = 0.70 ) confirms the signal is confined to the temperature channel.
The primary empirical claims are the fixed-axis low-l A 2 concentration, cross-map replication, EE null, parity-gated transfer, cumulative transfer invariant, and the rank-1 factorization. The residue-class top-9 test and overtone interpretation are supportive structural observations rather than standalone confirmatory statistics (Table 10).
The group D 3 Weyl ( A 2 ) is the Weyl group of the su ( 3 ) root system. The period-3 selection rule matches the order of the rotational subgroup C 3 D 3 and the Coxeter number h = 3 of A 2 , suggesting a connection between the angular structure of the microwave sky and the gauge group of quantum chromodynamics through the shared boundary S 2 .

Data Availability Statement

This analysis uses publicly available Planck PR3 data from the Planck Legacy Archive.1 The analysis code and exact reproduction notebooks are publicly available at https://github.com/rmereau/d3-cmb.2

Acknowledgments

The author thanks the Planck Collaboration for making their data products publicly available, and the HEALPix and healpy teams for the spherical harmonic analysis tools used throughout.

Appendix A. Robustness Tests

To verify that the primary result is not sensitive to analysis choices, we examine stability under variations of the multipole window and axis seeding.

Appendix A.1. Multipole Window

Table A1 shows the Fisher combined PTE for the A 2 excess (SMICA) as a function of the upper multipole boundary l max , with l min = 2 fixed. The significance is strongest at l 10 and degrades gradually as null high-l multipoles are added, but remains below 0.05 for all windows up to l max = 30 . This confirms that the signal is not an artifact of the particular choice l max = 15 .
Table A1. Fisher combined PTE (SMICA) for varying l max , with l min = 2 .
Table A1. Fisher combined PTE (SMICA) for varying l max , with l min = 2 .
l range Fisher PTE
2–10 8.5 × 10 4
2–15 4.6 × 10 3
2–20 9.2 × 10 3
2–25 1.9 × 10 2
2–30 3.5 × 10 2
Table A2 varies the lower boundary l min with l max = 15 fixed. Removing l = 2 (which is E-dominated and contributes no A 2 signal) improves the Fisher PTE from 4.6 × 10 3 to 2.2 × 10 3 , demonstrating that the quadrupole dilutes rather than drives the result. Removing both l = 2 and l = 3 (the axis-defining multipole) yields PTE = 0.14 : the signal from l = 4 –15 alone is not independently significant, confirming that l = 3 anchors the detection.
Table A2. Fisher combined PTE (SMICA) for varying l min , with l max = 15 .
Table A2. Fisher combined PTE (SMICA) for varying l min , with l max = 15 .
l range Fisher PTE
2–15 4.6 × 10 3
3–15 2.2 × 10 3
4–15 0.14

Appendix A.2. Axis Seeding

The axis optimization uses HEALPix N side = 32 as the initial grid. Repeating the search at N side = 16 (3,072 directions; 3 . 7 resolution) and N side = 64 (49,152 directions; 0 . 9 resolution) yields axis shifts < 1 . 5 and f A 2 ( l = 3 ) values within 0.002 of the baseline, confirming that the optimum is a broad, well-resolved feature of the sky.

Appendix A.3. Resolution

Using the full-resolution ( N side = 2048 ) SMICA map versus downgraded versions ( N side = 128 , 256, 512) yields axis shifts < 2 and identical per-multipole PTEs to within Monte Carlo noise, indicating that the signal is insensitive to the pixel resolution.

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Figure 2. Mollweide projections of the Planck SMICA temperature field in the D 3 frame (optimal axis at the pole). (a) Pure l = 3 octupole showing the six-lobe pattern with three-fold rotational symmetry ( f A 2 = 0.94 ). (b) Combined l = 3 , 7 , 9 : the three strongest cross-map-validated multipoles reinforce the D 3 pattern. (c) Full signal band l = 2 –15: the D 3 structure persists across the low-l cluster. (d) All-sky scan of f A 2 ( = 3 ) ; the optimal axis (star) at ( 50 . 3 , 64 . 9 ) galactic is a sharp, isolated maximum. Gold solid lines: C 3 rotation axes; white dashed: σ v reflection planes; upward (downward) triangles: hot (cold) spots.
Figure 2. Mollweide projections of the Planck SMICA temperature field in the D 3 frame (optimal axis at the pole). (a) Pure l = 3 octupole showing the six-lobe pattern with three-fold rotational symmetry ( f A 2 = 0.94 ). (b) Combined l = 3 , 7 , 9 : the three strongest cross-map-validated multipoles reinforce the D 3 pattern. (c) Full signal band l = 2 –15: the D 3 structure persists across the low-l cluster. (d) All-sky scan of f A 2 ( = 3 ) ; the optimal axis (star) at ( 50 . 3 , 64 . 9 ) galactic is a sharp, isolated maximum. Gold solid lines: C 3 rotation axes; white dashed: σ v reflection planes; upward (downward) triangles: hot (cold) spots.
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Figure 3. A 2 power fraction f A 2 ( l ) at the fixed D 3 axis for l = 2 –150 (SMICA). Gray line: isotropic baseline f A 2 = d A 2 / ( 2 l + 1 ) . Blue/light bands: 1 σ / 2 σ Monte Carlo envelopes ( N = 10 , 000 realizations). Red points: multipoles with PTE < 0.05 . The signal is densest at l 15 , but isolated cross-map-validated peaks appear at l = 34 and l = 63 . The axis was determined from l = 3 alone; all other multipoles constitute an effectively pre-registered test.
Figure 3. A 2 power fraction f A 2 ( l ) at the fixed D 3 axis for l = 2 –150 (SMICA). Gray line: isotropic baseline f A 2 = d A 2 / ( 2 l + 1 ) . Blue/light bands: 1 σ / 2 σ Monte Carlo envelopes ( N = 10 , 000 realizations). Red points: multipoles with PTE < 0.05 . The signal is densest at l 15 , but isolated cross-map-validated peaks appear at l = 34 and l = 63 . The axis was determined from l = 3 alone; all other multipoles constitute an effectively pre-registered test.
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Figure 4. Scatter plot of Δ f A 2 vs. Δ f E for l = 2 –150 (SMICA). Dark points: l 0 ( mod 3 ) ; open circles: l 15 (signal region). The dashed line shows the least-squares fit with r = 0.805 . The strong anti-correlation confirms the E A 2 power funnel predicted by the reflection-plane mechanism.
Figure 4. Scatter plot of Δ f A 2 vs. Δ f E for l = 2 –150 (SMICA). Dark points: l 0 ( mod 3 ) ; open circles: l 15 (signal region). The dashed line shows the least-squares fit with r = 0.805 . The strong anti-correlation confirms the E A 2 power funnel predicted by the reflection-plane mechanism.
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Figure 5. Mean A 2 excess Δ f A 2 grouped by residue class l mod 3 for l = 2 –150 (SMICA). The l 0 ( mod 3 ) class shows the highest mean excess (permutation PTE = 0.074 ). Among the nine strongest cross-map peaks (Table 3), zero belong to the l 2 ( mod 3 ) class ( p 0.02 ). Error bars: standard error of the mean.
Figure 5. Mean A 2 excess Δ f A 2 grouped by residue class l mod 3 for l = 2 –150 (SMICA). The l 0 ( mod 3 ) class shows the highest mean excess (permutation PTE = 0.074 ). Among the nine strongest cross-map peaks (Table 3), zero belong to the l 2 ( mod 3 ) class ( p 0.02 ). Error bars: standard error of the mean.
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Figure 6. Running sum of Δ f A 2 from l = 3 to l = 150 (SMICA). The steep rise at l 15 reflects the dense signal cluster. The subsequent near-plateau is interrupted by mild step-ups at l = 34 and l = 63 —the sporadic resonances identified in Table 3. Red dots mark l 0 ( mod 3 ) . Dotted lines: ± 1 σ random walk envelope.
Figure 6. Running sum of Δ f A 2 from l = 3 to l = 150 (SMICA). The steep rise at l 15 reflects the dense signal cluster. The subsequent near-plateau is interrupted by mild step-ups at l = 34 and l = 63 —the sporadic resonances identified in Table 3. Red dots mark l 0 ( mod 3 ) . Dotted lines: ± 1 σ random walk envelope.
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Figure 7. Real-space visualization of the D 3 signal in the Planck SMICA map, rotated into the D 3 frame. Upper left: Equatorial temperature ring for the signal band ( l = 2 –15, blue) and the three driving multipoles ( l = 3 , 7 , 9 , red). Vertical lines mark C 3 rotations ( 0 , 120 , 240 , solid) and reflection planes ( 60 , 180 , 300 , dashed). Upper right: The three-fold pattern at colatitudes θ = 45 110 from the D 3 axis. Lower left: Azimuthal power spectrum showing m = 3 dominance, confirming the C 3 D 3 selection rule. Lower right: Azimuthal auto-correlation: r ( 120 ) = + 0.22 (positive, C 3 symmetry) and r ( 60 ) = 0.23 (negative, σ v anti-symmetry). This alternating sign pattern is the real-space fingerprint of A 2 irrep loading.
Figure 7. Real-space visualization of the D 3 signal in the Planck SMICA map, rotated into the D 3 frame. Upper left: Equatorial temperature ring for the signal band ( l = 2 –15, blue) and the three driving multipoles ( l = 3 , 7 , 9 , red). Vertical lines mark C 3 rotations ( 0 , 120 , 240 , solid) and reflection planes ( 60 , 180 , 300 , dashed). Upper right: The three-fold pattern at colatitudes θ = 45 110 from the D 3 axis. Lower left: Azimuthal power spectrum showing m = 3 dominance, confirming the C 3 D 3 selection rule. Lower right: Azimuthal auto-correlation: r ( 120 ) = + 0.22 (positive, C 3 symmetry) and r ( 60 ) = 0.23 (negative, σ v anti-symmetry). This alternating sign pattern is the real-space fingerprint of A 2 irrep loading.
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Figure 8. A 2 power fraction f A 2 ( l ) for all four Planck PR3 component-separation maps at the fixed D 3 axis. The near-perfect overlap—especially at l 15 , where the D 3 signal resides—rules out pipeline-specific artifacts. SMICA and NILC are virtually indistinguishable ( r = 0.997 ).
Figure 8. A 2 power fraction f A 2 ( l ) for all four Planck PR3 component-separation maps at the fixed D 3 axis. The near-perfect overlap—especially at l 15 , where the D 3 signal resides—rules out pipeline-specific artifacts. SMICA and NILC are virtually indistinguishable ( r = 0.997 ).
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Figure 9. Cumulative transfer invariant Ξ ( L ) (Equation (16)). (a)  Ξ A 2 ( L ) for all four Planck pipelines, showing a stable 3 σ plateau from L 15 to 150. (b) Four-map mean Ξ under jackknife removal of key multipoles: the plateau survives individual removals but collapses when all three low-l anchors are excised. (c) Comparison of Ξ for the three D 3 irreps: A 2 and E are mirror images (reflecting the conservation law), while A 1 is consistent with zero. Grey bands mark the ± 2 σ isotropic expectation.
Figure 9. Cumulative transfer invariant Ξ ( L ) (Equation (16)). (a)  Ξ A 2 ( L ) for all four Planck pipelines, showing a stable 3 σ plateau from L 15 to 150. (b) Four-map mean Ξ under jackknife removal of key multipoles: the plateau survives individual removals but collapses when all three low-l anchors are excised. (c) Comparison of Ξ for the three D 3 irreps: A 2 and E are mirror images (reflecting the conservation law), while A 1 is consistent with zero. Grey bands mark the ± 2 σ isotropic expectation.
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Table 1. D 3 subspace dimensions and isotropic expected power fractions for l = 2 –12. Rows with l 0 ( mod 3 ) are marked () where d A 2 increments.
Table 1. D 3 subspace dimensions and isotropic expected power fractions for l = 2 –12. Rows with l 0 ( mod 3 ) are marked () where d A 2 increments.
l d A 1 d A 2 d E f A 1 f A 2 f E
2 1 0 4 0.200 0.000 0.800
3 2 1 4 0.286 0.143 0.571
4 2 1 6 0.222 0.111 0.667
5 2 1 8 0.182 0.091 0.727
6 3 2 8 0.231 0.154 0.615
7 3 2 10 0.200 0.133 0.667
8 3 2 12 0.176 0.118 0.706
9 4 3 12 0.211 0.158 0.632
10 4 3 14 0.190 0.143 0.667
11 4 3 16 0.174 0.130 0.696
12 5 4 16 0.200 0.160 0.640
Table 2. D 3 irrep fractions at the fixed axis for SMICA ( l = 2 –15). PTE from N MC = 10 , 000 isotropic simulations. The three driving multipoles ( l = 3 , 7 , 9 ) are marked with †.
Table 2. D 3 irrep fractions at the fixed axis for SMICA ( l = 2 –15). PTE from N MC = 10 , 000 isotropic simulations. The three driving multipoles ( l = 3 , 7 , 9 ) are marked with †.
l f A 1 f A 2 f E Δ f A 2 PTE
2 0.011 0.000 0.989 + 0.000
3 0.051 0.940 0.009 + 0.797 < 10 4
4 0.105 0.117 0.778 + 0.006 0.347
5 0.060 0.002 0.938 0.089 0.957
6 0.116 0.031 0.852 0.123 0.872
7 0.055 0.481 0.464 + 0.348 0.016
8 0.041 0.252 0.707 + 0.134 0.098
9 0.048 0.478 0.474 + 0.320 0.014
10 0.049 0.097 0.854 0.046 0.693
11 0.163 0.085 0.752 0.046 0.680
12 0.262 0.297 0.441 + 0.137 0.089
13 0.122 0.198 0.680 + 0.060 0.340
14 0.228 0.162 0.610 + 0.019 0.458
15 0.167 0.239 0.594 + 0.082 0.218
Table 3. The nine strongest A 2 peaks ranked by cross-map mean f A 2 . “Sig” counts maps with PTE < 0.05 . No peak belongs to the l 2 ( mod 3 ) residue class.
Table 3. The nine strongest A 2 peaks ranked by cross-map mean f A 2 . “Sig” counts maps with PTE < 0.05 . No peak belongs to the l 2 ( mod 3 ) residue class.
l f A 2 SM NI SE CM Sig l mod 3
3 0.932 .940 .943 .910 .937 4/4 0
7 0.487 .481 .496 .482 .490 4/4 1
9 0.448 .478 .467 .392 .454 4/4 0
34 0.307 .328 .322 .267 .312 3/4 1
18 0.284 .341 .342 .203 .248 2/4 0
12 0.281 .302 .320 .244 .258 0/4 0
63 0.280 .290 .290 .246 .294 3/4 0
31 0.278 .268 .283 .256 .305 2/4 1
46 0.250 .279 .302 .189 .230 2/4 1
Table 4. Fisher combined PTE across multipole ranges for all four Planck PR3 component-separation pipelines. N MC = 10 , 000 .
Table 4. Fisher combined PTE across multipole ranges for all four Planck PR3 component-separation pipelines. N MC = 10 , 000 .
Range SMICA NILC Cmdr SEVEM
l = 2 –15 4.7 × 10 3 4.2 × 10 3 6.3 × 10 3 1.2 × 10 2
l = 16 –150 0.942 0.940 0.919 0.993
l = 2 –150 0.685 0.674 0.645 0.922
Excl. l = 3 0.895 0.889 0.872 0.987
Table 5. Cross-map consistency of f A 2 ( l ) over l = 2 –150. Pearson correlation r and mean absolute deviation | Δ f | .
Table 5. Cross-map consistency of f A 2 ( l ) over l = 2 –150. Pearson correlation r and mean absolute deviation | Δ f | .
Map pair r ( f A 2 ) | Δ f |
SMICA–NILC 0.997 0.006
SMICA–Commander 0.958 0.021
SMICA–SEVEM 0.936 0.024
NILC–Commander 0.957 0.021
NILC–SEVEM 0.932 0.025
SEVEM–Commander 0.938 0.025
Table 6. Transfer invariant Ξ A 2 ( L ) for each pipeline and the four-map mean Ξ , at selected summation boundaries.
Table 6. Transfer invariant Ξ A 2 ( L ) for each pipeline and the four-map mean Ξ , at selected summation boundaries.
L SMICA NILC Commander SEVEM Ξ
15 + 3.13 + 3.16 + 3.00 + 3.11 + 3.10
50 + 2.90 + 3.07 + 2.79 + 2.98 + 2.93
100 + 2.87 + 2.96 + 3.08 + 3.04 + 2.99
150 + 2.47 + 2.50 + 2.53 + 2.63 + 2.53
Table 7. Odd/even parity split in the A 2 transfer. Δ f A 2 is the mean excess over isotropic expectation; Fisher PTE combines per-multipole PTE values within each parity class. The sign agreement across all four maps rules out pipeline-specific artifacts.
Table 7. Odd/even parity split in the A 2 transfer. Δ f A 2 is the mean excess over isotropic expectation; Fisher PTE combines per-multipole PTE values within each parity class. The sign agreement across all four maps rules out pipeline-specific artifacts.
Map Δ f A 2 odd Δ f A 2 even p odd p even
SMICA + 0.014 0.006 1.3 × 10 4 0.98
NILC + 0.013 0.005 2.0 × 10 4 0.97
SEVEM + 0.012 0.014 1.4 × 10 4 > 0.99
Commander + 0.015 0.009 2.2 × 10 5 > 0.99
Table 8. Cumulative A 2 transfer T r parity ( 150 ) (four-map mean ± inter-map spread), partitioned by parity and residue class. The single dominant cell is odd, r = 0 .
Table 8. Cumulative A 2 transfer T r parity ( 150 ) (four-map mean ± inter-map spread), partitioned by parity and residue class. The single dominant cell is odd, r = 0 .
r = 0 r = 1 r = 2
Odd l + 1 . 15 ± 0.20 + 0.04 ± 0.12 0.20 ± 0.14
Even l 0.24 ± 0.28 0.09 ± 0.22 0.32 ± 0.38
Table 9. Rank-1 factorization of the 2 × 3 transfer matrix M ( 150 ) . The rank-1 fraction is σ 1 2 / ( σ 1 2 + σ 2 2 ) . The binary-gate vector u and routing vector v are recovered independently by each pipeline.
Table 9. Rank-1 factorization of the 2 × 3 transfer matrix M ( 150 ) . The rank-1 fraction is σ 1 2 / ( σ 1 2 + σ 2 2 ) . The binary-gate vector u and routing vector v are recovered independently by each pipeline.
Map Rank-1 u odd u even v 0 v 1 v 2
SMICA 94 % + . 99 . 12 + 1.00 . 00 . 08
NILC 95 % + 1.00 . 09 + . 99 . 00 . 15
SEVEM 77 % + . 94 . 34 + . 99 + . 12 . 06
Commander 95 % + . 99 . 17 + . 99 + . 07 . 14
Table 10. Empirical signature summary. “Primary” denotes claims supported by pre-registered or controlled statistics; “Supportive” denotes a posteriori structural observations.
Table 10. Empirical signature summary. “Primary” denotes claims supported by pre-registered or controlled statistics; “Supportive” denotes a posteriori structural observations.
Property Observable Result Status
Registered axis ( , b ) ( 50 . 3 , 64 . 9 ) Primary
Low-l  A 2 cluster Fisher PTE ( l = 2 –15) 4.2 × 10 3 to 1.2 × 10 2 Primary
Cross-map replication r ( f A 2 ) all pairs 0.93 0.997 Primary
E A 2 funnel r ( Δ f A 2 , Δ f E ) 0.81 ± 0.03 Primary
EE null Fisher PTE (polarization) 0.70 Primary control
Parity-gated transfer Odd/even Fisher odd < 2 × 10 4 ; even > 0.97 Primary structural
2 × 3 factorization Rank-1 fraction 77 % 95 % Primary structural
Cumulative Ξ A 2 Ξ ( L = 15 150 ) + 2.5 to + 3.1 σ Primary
One-way collect rule Robust τ l signs All collecting into A 2 Secondary-strong
High-l aggregate null Fisher PTE ( l = 16 –150) > 0.91 Primary constraint
Residue-class top-9 0 / 9 in l 2 ( mod 3 ) p 0.02 Supportive only
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