The Carbon Isotope Ratio Of β Pic b With High-resolution Spectroscopy
Isotopic ratios trace the formation and evolution of planets and link their atmospheres to the chemistry of their natal protoplanetary discs.
We measure 12C/13C=58+18−15 in the atmosphere of the young super-Jupiter β Pic b from 11 nights of CRIRES+ K-band spectroscopy (≈100,000) at the Very Large Telescope (VLT). We detect both 12CO and 13CO and constrain 12C/13C with a Bayesian retrieval jointly fitted with near-infrared photometry.
The inferred 12C/13C is consistent with the present-day interstellar medium (ISM), is below the solar value, and is comparable to measurements in other young super-Jupiters. We also retrieve Teff=1629+30−28K, near-solar to mildly super-solar metallicity ([M/H]=0.20+0.16−0.12), a solar-like carbon-to-oxygen ratio (C/O=0.52±0.03), and tentative evidence for thick clouds.
We analyse each night independently and combine the results of the six epochs with the highest signal-to-noise ratio (S/N), propagating night-to-night scatter into the final uncertainties. This provides an isotopic benchmark for a directly imaged planet interior to the CO snow line.
D. González Picos, I.A.G. Snellen, R. Landman, S. de Regt, N. Grasser, J. L. Birkby, T. Stolker, I. Koutalios, M.A. Kenworthy
Comments: Accepted to A&A
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2606.12401 [astro-ph.EP](or arXiv:2606.12401v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2606.12401
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Submission history
From: Darío González Picos
[v1] Wed, 10 Jun 2026 17:58:27 UTC (2,607 KB)
https://arxiv.org/abs/2606.12401
Astrobiology, Astrochemistry,