A new benchmark in exoplanet science
The planet — a sub-Neptune orbiting a K-dwarf star roughly 120 light-years from Earth — was observed during multiple transits over several months. The resulting spectrum revealed clear absorption features from carbon dioxide (CO₂), methane (CH₄), and water (H₂O), alongside a tentative detection of carbon monoxide.
The simultaneous presence of CO₂ and CH₄ is particularly striking. In equilibrium chemistry at the temperatures inferred for this planet (~300 K in the observable atmosphere), methane should dominate. Finding both implies either disequilibrium chemistry — driven by biological or geological processes — or an unusual metallicity in the atmosphere. The science team has published their analysis in Nature Astronomy, noting the result is consistent with a "Hycean" world hypothesis: a rocky or water-rich interior beneath a hydrogen-dominated atmosphere.
Why this matters for the search for life
No single detection constitutes a biosignature — confirmed evidence of life. But the technique demonstrated here — stacking many transit observations to build a high signal-to-noise spectrum — represents the methodological pathway to future biosignature searches. JWST's follow-up programme will now target a dozen more sub-Neptunes in the habitable zones of nearby stars, building a statistical picture of this most common planetary class.
To understand how planets like this are discovered and classified, see our exoplanets overview guide. The transit detection method is explained in detail in our how we find exoplanets guide. For the dictionary entry on exoplanets, see our glossary.
Detected molecules
The James Webb Space Telescope is operated by NASA, ESA, and the Canadian Space Agency. All atmospheric spectra data are publicly archived via the MAST archive.