JWST Detects Atmospheric Clues for Water World on Exoplanet K2-18 b

October 19, 2025
JWST detects methane and CO2 on exoplanet K2-18 b, hinting at a habitable ocean world.
In a landmark discovery, NASA's James Webb Space Telescope (JWST) has identified key carbon-bearing molecules, including methane and carbon dioxide, in the atmosphere of the exoplanet K2-18 b. Situated 120 light-years away, this sub-Neptune exoplanet orbits within the habitable zone of its cool dwarf star, and these new findings bolster the hypothesis that it could be a 'Hycean' world—a planet with a water ocean beneath a hydrogen-rich atmosphere.
The Enigma of K2-18 b
K2-18 b has long been a target of intense scientific interest. With a radius 2.6 times that of Earth, it occupies a unique space between terrestrial planets and gas giants. Its position in the habitable zone—the region around a star where liquid water could exist on a planet's surface—makes it a prime candidate in the search for potentially habitable worlds beyond our solar system.
Webb's Spectroscopic Investigation
Using its advanced suite of instruments, particularly the Near-Infrared Spectrograph (NIRSpec) and Near-Infrared Imager and Slitless Spectrograph (NIRISS), JWST performed detailed observations of K2-18 b as it transited its host star. By analyzing the starlight filtered through the exoplanet's atmosphere, astronomers were able to decipher its chemical composition with unprecedented clarity.
- Methane and Carbon Dioxide Detected: The robust detection of these carbon-bearing molecules indicates a dynamic atmosphere and potential for organic chemistry.
- Lack of Ammonia: The scarcity of ammonia supports the theory of a liquid water ocean, as ammonia is highly soluble in water and would likely be depleted from a hydrogen-rich atmosphere above an ocean.
- Possible Dimethyl Sulfide (DMS): The data shows a tantalizing hint of a molecule called dimethyl sulfide. On Earth, DMS is produced almost exclusively by life, particularly marine phytoplankton.
Scientific Significance and Cautious Optimism
These findings represent a major step forward in the characterization of habitable-zone exoplanets. The combination of methane, CO2, and a lack of ammonia strongly supports the Hycean world model. However, astronomers emphasize that the potential detection of DMS is preliminary and requires further validation.
Our findings underscore the importance of considering diverse habitable environments in the search for life elsewhere. Traditionally, the search for life on exoplanets has focused primarily on smaller rocky planets, but the larger Hycean worlds are significantly more conducive to atmospheric observations.
Future Research and Next Steps
The research team plans to conduct follow-up observations with JWST's Mid-Infrared Instrument (MIRI) to further validate their findings, especially the potential presence of DMS, and to better constrain the atmospheric and surface conditions of K2-18 b. Confirming DMS would be a transformative moment in astrobiology.
While the discovery does not confirm the presence of life, it demonstrates the James Webb Space Telescope's profound capability to probe the atmospheres of distant worlds for potential biosignatures. The chemical portrait of K2-18 b opens a new and exciting chapter in humanity’s quest to answer the question: are we alone in the universe?
Frequently Asked Questions
A Hycean (a portmanteau of hydrogen and ocean) exoplanet is a theoretical type of world that is hot, covered by a liquid water ocean, and possesses a substantial hydrogen-rich atmosphere. They are considered promising candidates for finding biosignatures.
No, this discovery is not definitive proof of life. While the atmospheric composition is consistent with a world that could support life, and dimethyl sulfide (DMS) is a potential biosignature, the findings require further validation. It is a compelling but not conclusive result.
JWST uses a technique called transmission spectroscopy. When an exoplanet passes in front of its star (a transit), starlight filters through the planet's atmosphere. The telescope's instruments analyze this light to see which wavelengths have been absorbed by different molecules, revealing the atmosphere's chemical makeup.
On Earth, DMS is almost exclusively produced by biological processes, primarily from phytoplankton in marine environments. If confirmed on an exoplanet, it would be a very strong indicator of potential biological activity, though non-biological sources cannot be entirely ruled out without further study.