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Oxford-Led Study Identifies Sulfur-Rich Magma-Ocean Planet, Proposing a New Exoplanet Class

Computer models tied to JWST spectra explain the planet’s low density by coupling a deep molten mantle to a hydrogen‑sulfur atmosphere.

Overview

  • Published in Nature Astronomy on March 16, the analysis finds L 98-59 d—about 1.6 times Earth’s radius—has a bulk density near 40% of Earth’s while orbiting a nearby red dwarf 34–35 light-years away.
  • JWST and ground-based observations reveal hydrogen sulfide and sulfur dioxide in a hydrogen-rich envelope, with ultraviolet light driving sulfur chemistry high in the atmosphere.
  • Simulations reconstruct nearly five billion years of evolution, indicating a global magma ocean thousands of kilometers deep that stores vast sulfur reservoirs and helps retain the atmosphere despite stellar X-ray loss.
  • The team reports surface temperatures exceeding roughly 1,500°C and a relatively small core, with the molten layer spanning about 70–90% of the interior radius, rendering the world inhospitable to life as we know it.
  • Researchers propose L 98-59 d may be the first recognized member of a broader population of sulfurous magma-ocean worlds and call for follow-up with JWST, ESA’s Ariel, and PLATO to assess their prevalence.