HomeScienceAstronomers spot carbon-heavy disk around young star, challenging planet formation models

Astronomers spot carbon-heavy disk around young star, challenging planet formation models

Conventional models predict water vapour in a disk’s inner regions, as icy pebbles drift inward and vaporise. But Webb’s MIRI instrument revealed a strong carbon dioxide signal instead.

September 01, 2025 / 13:46 IST
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An image of the star-forming region NGC 6357 highlights the young star XUE 10. Using JWST/MIRI, scientists detected a planet-forming disk rich in four distinct forms of carbon dioxide but with little water, offering fresh insights into the chemical conditions where planets are beginning to form. (Image: Stockholm University (SU) and María Claudia Ramírez-Tannus, Max Planck Institute for Astronomy (MPIA))
An image of the star-forming region NGC 6357 highlights the young star XUE 10. Using JWST/MIRI, scientists detected a planet-forming disk rich in four distinct forms of carbon dioxide but with little water, offering fresh insights into the chemical conditions where planets are beginning to form. (Image: Stockholm University (SU) and María Claudia Ramírez-Tannus, Max Planck Institute for Astronomy (MPIA))

Astronomers studying a young star system have found something unexpected: a planet-forming disk unusually rich in carbon dioxide, but with hardly any water. The finding, made with the James Webb Space Telescope, challenges long-held ideas about how planets are born.

What did scientists discover in the planet-forming disk?
A team led by Jenny Frediani at Stockholm University found strikingly high amounts of carbon dioxide in regions where rocky planets might one day emerge. “Unlike most planet-forming disks, where water dominates, this one is surprisingly carbon dioxide rich,” Frediani said. “Water is so scarce it is barely detectable.”

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NGC 6357 with the star XUE 10 (Image: Stockholm University (SU) and María Claudia Ramírez-Tannus, Max Planck Institute for Astronomy (MPIA))

Conventional models predict water vapour in a disk’s inner regions, as icy pebbles drift inward and vaporise. But Webb’s MIRI instrument revealed a strong carbon dioxide signal instead. “This challenges current models because such high levels of carbon dioxide compared with water cannot be explained easily,” Frediani explained.