
A big sub-Neptune-sized planet revolving round a purple dwarf star 124 gentle years away has been the subject of debate amongst a number of scientists in current months.
In line with fashions from a bunch of Cambridge scientists utilizing knowledge from the James Webb House Telescope (JWST), there have been indicators of dimethyl sulfide (DMS) and dimethyl disulfide (DMDS) within the planet’s ambiance. These molecules are recognized to solely be produced by dwelling organisms on Earth. However shortly after the announcement, a number of different teams analyzing the identical knowledge claimed that their analyses didn’t again up these claims.
These early observations additionally gave some perception into the atmospheric composition of the planet, known as K2-18 b. It was discovered to have a hydrogen-rich ambiance, containing methane and probably carbon dioxide. There was restricted proof for the existence of ammonia and water vapor, however extra observations have been wanted to get a clearer image. The scientists concerned within the debate over DMS and DMDS have been additionally wanting to make clear whether or not the attainable signatures for these molecules can be current in future knowledge.
Now, a number of of those scientists have gotten collectively and analyzed new knowledge from 4 newer JWST near-infrared transit observations and mixed these with earlier JWST and Hubble knowledge. Their research was lately posted to the arXiv preprint server. The brand new outcomes present no proof for the DMS or DMDS signatures, however they do assist to create a extra strong image of the planet’s construction.
The most important consequence to come back out of the examine is the knowledge that K2-18 b is a quite water-rich planet. The group discovered a strong detection of methane and carbon dioxide in K2-18 b’s ambiance, however no water vapor.
They clarify, “The simultaneous presence of CH4 and CO2 on the noticed abundances can solely be defined by both an enormous ambiance with roughly 100× photo voltaic metallicity and a bulk H2O content material of 10–25% by quantity, or a small ambiance overlaying a liquid-water ocean. No matter whether or not the planet hosts a liquid-water ocean, our outcomes conclusively show that K2-18 b has a water-rich inside.”
Ammonia and carbon monoxide have been additionally absent within the planet’s ambiance. The examine authors say that the shortage of ammonia within the ambiance is according to a liquid ocean, however it isn’t conclusive, and extra observations are wanted to get helpful details about the carbon dioxide to carbon monoxide ratio. The outcomes additionally present that the absence of atmospheric water vapor may recommend a chilly entice, seemingly because of water vapor condensation occurring earlier than reaching the altitudes probed by their devices.
As traditional, extra observations will assist to refine the atmospheric fashions in these research and provides a clearer image of whether or not the water on K2-18 b exists as a layer of gasoline, a liquid ocean and even a part of an icy core. Whichever state it is in, the examine signifies that there is no such thing as a proof of something dwelling in it. Nonetheless, this specific planet is a captivating examine for a lot of scientists.
The examine authors write,”K2-18 b—a cool, water-rich world—stands out as one of the crucial promising temperate sub-Neptunes for exploring the emergence of liquid-water environments in non-Earth-like planets, motivating additional characterization of its ambiance and inside.”
Written for you by our writer Krystal Kasal, edited by Stephanie Baum, and fact-checked and reviewed by Andrew Zinin—this text is the results of cautious human work. We depend on readers such as you to maintain impartial science journalism alive.
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Extra data:
Renyu Hu et al, A water-rich inside within the temperate sub-Neptune K2-18 b revealed by JWST, arXiv (2025). DOI: 10.48550/arxiv.2507.12622
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Planet K2-18b might not host alien life, however it’s residence to a water-rich inside (2025, July 28)
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