Icy Surprise from a Dying Star: JWST Finds CO2 Crystals express

Original: "Detection of CO$$_2$$ ice in the planetary nebula NGC 6302"
arXiv:2602.22366 · 2026-02-25 · CC BY 4.0 · 1 min
JWST spotted crystalline carbon dioxide ice in the most unexpected place.

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In a blazing foundry, any ice cube would vanish instantly. But tucked inside a thick mitten, it survives. Nature pulled a similar trick in the planetary nebula NGC 6302. A dying star floods its surroundings with deadly ultraviolet light, yet inside a dense dust ring, the JWST spotted something unexpected: pure crystalline ice made of carbon dioxide. Its giveaway: spectral lines exactly matching those of dry ice used to create theater fog.

At around –250°C, this ice is colder than Pluto's surface, though it lies in a radiation zone millions of times brighter than the Sun.

Scientists once believed ices don't form in such old systems. But spectroscopy data revealed an abundance of CO₂ gas, with a gas-to-ice ratio dozens of times higher than in the cradles of newborn stars. Apparently, ice crystallizes directly onto dust grains — like frost on a window, but sheltered inside a protective dust "mitten." The discovery forces a rewrite of dying stars' chemistry.

Original abstract

as written by the authors arXiv:2602.22366

Using JWST/MIRI observations, we report the detection of CO$$_2$$ ice in the dusty torus of the planetary nebula NGC 6302, an environment generally considered hostile to fragile molecular species and ices due to intense UV irradiation. This detection accompanies cold (20-50 K) gas-phase CO$$_2$$ along the same sightlines. The ice absorption profile exhibits a double-peak profile, a characteristic of pure, crystalline CO$$_2$$ ice. The CO$$_2$$ gas-to-ice ratio is more than an order of magnitude higher than in young stellar objects, pointing to distinct ice formation or processing mechanisms in evolved stellar environments. This discovery demonstrates that the dusty torus provides sufficient shielding to harbour ice chemistry, and that ice-mediated surface reactions must be incorporated into chemical models of planetary nebulae.

Dry ice on Earth doesn't melt; it sublimates directly from solid to gas. It behaves the same way in space, so its crystals can survive for billions of years.

Scientists
Ludwig BoltzmannJames JeansCecilia Payne-GaposchkinTheodore LymanHans BetheNancy Grace Roman
Concepts
cold gas sulfur dioxide torus snow line young stellar object stellar nursery gas cloud cosmic dust icecube neutrino detection liquid argon dust ring large magellanic cloud water ice dayside titanium oxide crab nebula crust hot jupiter atmospheres carbon dioxide nebula