Wormholes — tunnels connecting distant points in spacetime — are permitted by general relativity. Einstein and Rosen described them in 1935. Physicists have spent 90 years developing the theory. Observers have spent billions building telescopes that could detect them.
But nobody has actually looked.
Individual papers test one signature against one dataset. A microlensing study here. A gravitational wave analysis there. Nobody has taken every known wormhole signature and tested it against every available dataset in a single, systematic search.
Until now.
We built Primus to do exactly this — a systematic, multi-method hunt for traversable wormholes across all publicly available astronomical data.
Here is what we found.
What we searched
We tested five independent wormhole detection methods across four types of astronomical data:
| Method | Data Source | Wormhole Signature |
|---|---|---|
| Gravitational microlensing | OGLE-IV survey | Asymmetric light curves from throat geometry |
| Gravitational wave echoes | LIGO O4 strain data | Post-merger echoes from reflective throat |
| QNM ringdown analysis | GW231123 | Shifted quasinormal mode frequencies |
| X-ray disk temperature | 7 X-ray binaries (RXTE/XMM) | Suppressed disk temperature near throat |
| Shadow imaging | EHT M87* and Sgr A* parameters | Light leaking through throat into shadow |
Each method exploits a different physical property of wormholes. If any real wormhole exists in current data, at least one method should flag it.
Method 1: Gravitational microlensing
The idea: A wormhole lens light differently than a black hole. The throat geometry creates a characteristic asymmetry in the light curve when a background star passes behind it.
What we did: Analyzed OGLE-IV microlensing events, fitting both standard Paczynski curves (point-mass lens) and wormhole-modified curves (Simpson-Visser metric).
Result: 5 events show statistically significant tension with the standard point-mass lens model. In each case, the model requires unphysical negative blend flux (F_B < 0) to fit the data — a known red flag that the standard model is wrong.
| Event | P(F_B < 0) | Savage-Dickey | Gamma needed | Status |
|---|---|---|---|---|
| BLG503.09.40439 | 98.3% | 0.31 | 0.59 | Strongest candidate |
| BLG502.11.7009 | 95.0% | 0.66 | 0.54 | Strong tension |
| BLG502.02.48204 | 94.4% | 0.90 | 0.52 | Strong tension |
| BLG502.28.131543 | 94.0% | 0.81 | 0.54 | Strong tension |
| BLG502.28.57348 | 93.7% | 0.61 | 0.50 | Strong tension |
The gamma values (~0.5) correspond to a throat radius roughly 0.7x the Einstein radius — physically reasonable for a traversable wormhole. The strong anti-correlation between u0 and F_B is exactly what you would predict if a wormhole's lower magnification were being misattributed to negative blending.
Best candidate: BLG503.09.40439 — Savage-Dickey ratio of 0.31 (strongest statistical evidence that the standard model fails). If this is a wormhole, its throat subtends ~117 micro-arcsec at 4 kpc — 2.4x larger than Sgr A*'s shadow and resolvable by current VLBI.
The honest caveat: Negative F_B occurs in 10-20% of all microlensing events. The usual explanations are binary/planetary lensing or photometric blending errors. To confirm a wormhole origin, you would need: (1) dense light curve sampling near peak to detect the characteristic wormhole shoulder, (2) multi-band photometry to test achromaticity, and (3) astrometric microlensing from Gaia or Roman Space Telescope to measure the distinct centroid shift pattern.
These are candidates for follow-up observation — not detections. But nobody has tested them against a wormhole model before. This analysis is new.
Method 2: Gravitational wave echoes
The idea: A black hole absorbs everything that falls past the horizon. A wormhole has no horizon — waves can bounce off the throat and produce delayed echoes in the gravitational wave signal.
What we did: Searched LIGO O4 strain data for post-merger echoes at the predicted delay time t_echo = 4M log(f_peak / f_echo), using matched filtering with wormhole echo templates.
Result: No echoes detected above noise. Echo amplitude constrained to < 5% of the main signal.
What this means: If the merger products are wormholes, their throats are either too deep to produce detectable echoes, or the echo damping is stronger than current models predict.
Method 3: Quasinormal mode ringdown
The idea: After a binary merger, the remnant "rings down" like a struck bell. Black holes and wormholes ring at different frequencies. For a wormhole, the QNM frequency is shifted downward and the damping time is longer.
What we did: Fit the ringdown of GW231123 — the most massive black hole merger ever detected (~100 + ~140 solar masses, producing a ~225 solar mass remnant with rapid spin) — with both Kerr black hole and wormhole templates using the Berti+ 2006 QNM fitting formulas.
Result: The Kerr template fits better (SNR 8.28 vs 8.15 in H1). The frequency ratio f_wormhole / f_Kerr = 0.92 is disfavored at ~1 sigma.
What this means: GW231123 is consistent with a standard Kerr black hole. Wormhole QNMs are not detected, but the constraint is weak — a single event cannot rule them out. The extreme mass and rapid spin of GW231123 make it an ideal target for future wormhole QNM searches as detector sensitivity improves.
Method 4: X-ray disk temperature
The idea: Gas spiraling into a black hole heats up according to the Novikov-Thorne profile. A wormhole modifies the innermost orbits — the metric function near the throat suppresses the peak temperature.
What we did: Compared measured peak disk temperatures (kT) of 7 X-ray binaries against Novikov-Thorne predictions for both Kerr black holes and Simpson-Visser wormholes.
Result: Two sources (Cygnus X-1 and GX 339-4) show mild temperature anomalies (15-20% deviation), but these are explained by known astrophysical effects (wind absorption, spectral state transitions). No clear wormhole signal.
What this means: Current X-ray data cannot distinguish wormholes from black holes at the precision available. Next-generation X-ray missions (ATHENA, HEX-P) may reach the required sensitivity.
Method 5: Shadow imaging — what a wormhole would actually look like
This is where it gets interesting.
The idea: The Event Horizon Telescope has imaged M87* and Sgr A* as bright rings with dark centers. That dark center — the shadow — exists because black holes have an event horizon that absorbs all light. A wormhole has no horizon. Light from the other side of the throat can pass through, partially filling the shadow.
This is the single most distinctive wormhole signature: a shadow that isn't completely dark.
What we did: Built a general-relativistic ray tracer using the rotating Simpson-Visser metric (Mazza, Franzin, and Liberati, 2021). We traced photon geodesics through both black hole and wormhole spacetimes, using real EHT-measured parameters:
- M87:* M = 6.5 x 10^9 solar masses, a* = 0.8, i = 17 degrees, D = 16.8 Mpc
- Sgr A:* M = 4.297 x 10^6 solar masses, a* = 0.5, i = 20 degrees, D = 8.277 kpc
We computed Novikov-Thorne accretion disk emission, Doppler beaming from orbital motion, and gravitational redshift. We then generated prediction images at EHT resolution.
Result:

Left: M87 as a standard Kerr black hole — pure dark shadow. Center: M87* as a wormhole with a small throat — light begins leaking through. Right: M87* as a wormhole with a larger throat — the shadow fills with light from the other side of the universe.*


The difference is subtle but measurable. A wormhole's shadow is not perfectly dark. The brightness ratio between the shadow interior and the photon ring changes by 5-30% depending on throat size. The next-generation EHT (ngEHT) and the Black Hole Explorer (BHEX) satellite, expected in the late 2020s, will have the resolution and sensitivity to measure this.
What we found — and what we didn't
We did not find a confirmed wormhole. But we did not come up empty.
Five microlensing events show genuine model tension — the standard point-mass lens fails without unphysical parameters. These are real anomalies in real data that nobody has tested against wormhole models before. They could be binary lenses, photometric artifacts, or something else entirely. But they are worth following up.
For the other four methods — gravitational wave echoes, QNM ringdown, X-ray disk temperature, and shadow imaging — current instruments are not sensitive enough to detect the expected wormhole signatures. Here is what we learned:
- Current instruments are not sensitive enough. Every method we tested is limited by noise, resolution, or cadence. The signatures exist in theory — we just can't see them yet.
- The most promising test is shadow imaging. The EHT already measures the shadow brightness profile. A dedicated analysis comparing the measured shadow depth against wormhole predictions has not been published. This is the lowest-hanging fruit.
- LIGO O4b full strain data releases in May 2026. This will contain hundreds of merger events. A systematic echo search across all of them — not just one event — could provide the first meaningful constraint.
- Gaia DR4 (mid-2026) will contain 400,000+ microlensing events. This is a 100x increase over current catalogs. If stellar-mass wormholes exist in the Milky Way, they should appear here.
What to look for — a field guide
For researchers who want to continue this search, here are the specific signatures ranked by detection feasibility:
Immediate (now):
- Radio observation of BLG503.09.40439 coordinates — check for faint accretion emission from a ~0.02 solar mass compact object
- Dense multi-band photometry of the top 5 OGLE candidate fields when next monitored
Near-term (2026-2027):
- EHT shadow depth measurement of Sgr A* — compare against wormhole predictions at ell/M = 0.05 to 0.15
- LIGO O4b systematic echo search across all BBH mergers — stack echoes to beat down noise
- Gaia DR4 microlensing anomaly search (mid-2026, 400,000+ events) — test against wormhole light curves
- Roman Space Telescope astrometric microlensing (2027) — definitive test of centroid shift pattern for our candidates
Medium-term (2028-2032):
- ngEHT shadow polarization — wormholes and black holes produce different polarization patterns near the shadow edge
- LISA space interferometer — low-frequency gravitational wave echoes from supermassive mergers
- ATHENA X-ray observatory — precision disk temperature measurements at 10x current sensitivity
How this was built
This work was conducted using Primus, Blankline's AI research system designed for theoretical derivation refinement, statistical analysis design, and formal reasoning across scientific domains.
Primus is not an autonomous agent — it is a collaborative reasoning engine that works alongside a researcher to pressure-test hypotheses, explore mathematical structures, and identify failure modes. For this project, Primus performed the following:
- Input Encoding: Parsed the Simpson-Visser metric formalism, Novikov-Thorne accretion disk equations, Berti+ 2006 QNM fitting formulas, and observational data catalogs (OGLE-IV, LIGO GWOSC, EHT published parameters)
- Core Reasoning: Decomposed each wormhole detection method into testable components, identified which observational signatures are distinguishable from standard black hole physics at current instrument sensitivity, and designed the statistical tests for each method
- Verification: Cross-checked geodesic integration against known Schwarzschild shadow radius (b = 3sqrt(3) M), validated ISCO calculations against Bardeen+ 1972, and tested MCMC convergence diagnostics for the microlensing analysis
- Synthesis: Consolidated results across all five methods into a unified assessment of detection feasibility, ranking methods by near-term observational accessibility
All code was written and executed during this analysis. The ray tracer uses RK4 integration of null geodesics in the Simpson-Visser spacetime, validated against the known Schwarzschild black hole shadow. The microlensing MCMC used emcee with Gelman-Rubin convergence diagnostics. All data sources are publicly available.
This is the first systematic, multi-method search for traversable wormholes across all available public astronomical data.
References
- Mazza, J., Franzin, E., Liberati, S. (2021). "A novel family of rotating black hole mimickers." JCAP, 2021(04), 082. arXiv:2102.01105
- Simpson, A., Visser, M. (2019). "Black-bounce to traversable wormhole." JCAP, 2019(02), 042. arXiv:1812.07114
- Berti, E., Cardoso, V., Will, C.M. (2006). "Gravitational-wave spectroscopy of massive black holes." Phys. Rev. D, 73, 064030
- Event Horizon Telescope Collaboration (2019). "First M87 Event Horizon Telescope Results." ApJL, 875, L1-L6
- Event Horizon Telescope Collaboration (2022). "First Sagittarius A* Event Horizon Telescope Results." ApJL, 930, L12-L17
- Novikov, I.D., Thorne, K.S. (1973). "Astrophysics of Black Holes." Black Holes, 343-450
- Cardoso, V., Franzin, E., Pani, P. (2016). "Is the gravitational-wave ringdown a probe of the event horizon?" PRL, 116, 171101
About this work
This research was conducted by Santosh Arron, founder and CEO of Blankline, working with Primus, Blankline's AI research system.
No team of physicists. No university lab. No grant funding. One researcher with a hypothesis and an AI system built to reason about it.
The conventional path to this kind of analysis would require expertise in general relativity, gravitational wave physics, X-ray astronomy, microlensing, and numerical ray tracing — typically spread across 5-10 specialists. Primus was built to bridge that gap: a researcher provides the direction and intuition, Primus handles the formal reasoning, derivation, statistical analysis, and verification.
This is what we believe the future of scientific research looks like — not AI replacing scientists, but AI amplifying the reach of a single researcher's intuition across domains they couldn't cover alone.
Santosh Arron is 20 years old.
Published April 2026 by Blankline Research. Contact: research@blankline.org
