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James Webb Detects Silicon Monoxide and Methane in WASP-121b’s Atmosphere

Vertical mixing coupled with a super-stellar carbon-to-oxygen ratio indicates WASP-121b formed beyond the water ice line before migrating inward.

This artistic impression depicts the stage at which WASP-121b accumulated most of its gas, as inferred from the latest results. Image credit: T. Müller, MPIA & HdA.

Overview

  • JWST’s Near-Infrared Spectrograph phase-curve observations captured water vapor, carbon monoxide and the first-ever detection of silicon monoxide in any planetary atmosphere.
  • Methane was observed on the cooler nightside despite ultra-hot conditions, implying robust vertical mixing that replenishes methane from deeper atmospheric layers.
  • Analysis of elemental ratios revealed a super-stellar carbon-to-oxygen ratio, suggesting WASP-121b formed in a cold, methane-rich region of its protoplanetary disk.
  • Silicon monoxide detection indicates late-stage accretion of rocky solids, shedding light on how refractory materials became incorporated during the planet’s assembly.
  • The chemical fingerprint supports a migration history from beyond the water ice line to its current 1.3-day orbit around its host star.