A JWST Transmission Spectrum of the Temperate Sub-Neptune TOI-732 c
Frances E. Rigby, Nikku Madhusudhan, Subhajit Sarkar, Lorenzo Pica-Ciamarra, Måns Holmberg, Julianne I. Moses
TL;DR
This study presents the first JWST transmission spectrum of TOI-732 c, a temperate sub-Neptune, across 0.9–12 μm to probe atmospheric composition and interior structure. Using NIRISS, NIRSpec, and MIRI data with two retrieval frameworks (AURA and POSEIDON), the authors robustly detect CH$_4$ in a hydrogen-rich atmosphere and place stringent upper limits on NH$_3$ and HCN, while uncovering evidence for excess absorption from one or more complex trace species. A comprehensive survey of up to 250 molecules reveals moderate to strong evidence for several candidate absorbers, with two compounds—isobutylene and 1-pentene—showing consistent, albeit degenerate, signals in both NIR and MIR analyses. Clouds/hazes at the terminator are inferred, and a photospheric temperature around ~310 K at 10 mbar is retrieved, suggesting a cold trap is possible but not required. The results illuminate the degeneracies between atmospheric composition and interior structure for temperate sub-Neptunes and motivate further observations and theoretical work to robustly characterize such worlds and their potential habitability.
Abstract
In recent years, JWST has facilitated detections of carbon-bearing molecules in the atmospheres of temperate sub-Neptunes orbiting M dwarfs, ushering in a new era in the characterization of this intriguing planetary regime. We report the transmission spectrum of the temperate sub-Neptune TOI-732 c, observed with JWST NIRISS, NIRSpec G395H and MIRI LRS between 0.9-12 $μ$m. The observations provide evidence for methane (CH$_4$) in a H$_2$-rich atmosphere, at a volume mixing ratio of $\sim$1\%, and non-detection of NH$_3$ and HCN, along with nominal constraints on other prominent molecules H$_2$O, CO and CO$_2$, which are typically expected in H$_2$-rich atmospheres. We conduct a comprehensive survey of 250 chemical species and find moderate to strong evidence (up to $\ln B\sim 5.9$, $3.9σ$) for additional absorption due to one or more complex molecules including higher-order hydrocarbons and/or sulfur-bearing molecules. The spectral features are strongly degenerate among these molecules and with methane, which we find at $\ln B=3.2-8.8$ (up to $3.0-4.6$$σ$) significance. Two complex molecules are preferred with at least moderate evidence ($\ln B \gtrsim 2.5$) in both the near- and mid-infrared, while several others show such evidence in at least one of the two wavelength ranges. The preferred molecules are found in trace quantities on Earth, with no significant sources identified in other planetary atmospheres, requiring future work to assess their physical plausibility in this planet. Future observations are required to resolve the degeneracies and place more robust constraints on these species. We highlight the need for further theoretical and experimental work to robustly characterize the atmospheric and internal composition of TOI-732 c and similar sub-Neptunes.
