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LHS 1140 b is a small planet orbiting in the habitable zone of its M4. 5V dwarf host. Recent mass and radius constraints have indicated that it has either a thick H₂-rich atmosphere or substantial water by mass. Here we present a transmission spectrum of LHS 1140 b between 1. 7 and 5. 2 m, obtained using the NIRSpec instrument on JWST. By combining spectral retrievals and self-consistent atmospheric models, we show that the transmission spectrum is inconsistent with H₂-rich atmospheres with varied size and metallicity, leaving a water world as the remaining scenario to explain the planet's low density. Specifically, a H₂-rich atmosphere would result in prominent spectral features of CH₄ or CO₂ on this planet, but they are not seen in the transmission spectrum. Instead, the data favors a high-mean-molecular-weight atmosphere (possibly N₂-dominated with H₂O and CO₂) with a modest confidence. Forming the planet by accreting C- and N-bearing ices could naturally give rise to a CO₂- or N₂-dominated atmosphere, and if the planet evolves to or has the climate-stabilizing mechanism to maintain a moderate-size CO₂/N₂-dominated atmosphere, the planet could have liquid-water oceans. Our models suggest CO₂ absorption features with an expected signal of 20 ppm at 4. 2 m. As the existence of an atmosphere on TRAPPIST-1 planets is uncertain, LHS 1140 b may well present the best current opportunity to detect and characterize a habitable world.
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