Exoplanets, -moons, -comets

Formation Of Cold Giant Planets Around Late M Dwarfs Via Core Accretion And The Fate Of Inner Rocky Worlds

By Keith Cowing
Status Report
astro-ph.EP
December 11, 2025
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Formation Of Cold Giant Planets Around Late M Dwarfs Via Core Accretion And The Fate Of Inner Rocky Worlds
Normalized torques as a function of planetary mass and semimajor axis, assuming circular and coplanar orbits. The different migration regimes are indicated, separating inward from outward migration. The mass required to open a gap in the disk (dashed white line), the planet-to-star mass ratio (q) of 0.002, and the gas depth criterion K = 104 are over-plotted (dashed black lines). — astro-ph.EP

Modeling the formation of cold giant planets around M dwarfs is difficult because their disks may not contain enough solids to form massive cores and because forming giants are expected to migrate inward through disk interactions.

It is also unclear whether inner rocky planets can survive in systems hosting a cold giant, with implications for the habitability of close-in worlds. We investigated the conditions that allow giant planets to form at 1-3 au around a 0.1 M star and explored when a close-in rocky planet can survive.

We perform N-body simulations in which embryos grow through pebble and gas accretion in a disk with a local turbulent viscosity of αt=10−4. Planet-disk interactions are included using a prescription that triggers outward migration when the planet-to-star mass ratio (q) exceeds 0.002.

We find that a cold giant can form even in a disk with an initial pebble mass of 6 M if the disk gas mass is 10% of the stellar mass. This requires a compact 20 au disk with a dense inner region set by αg=10−4, the assembly of a ∼5 M core within 1 Myr, and a disk lifetime of 10 Myr. A close-in rocky planet can survive if it reaches the inner cavity before the outer body becomes a giant.

Thus, giant planet formation around very low-mass stars does not require high dust masses as previously thought. A combination of planet-planet collisions, efficient pebble accretion, and a long disk lifetime plays a key role in enabling the formation of cold giant planets with masses between those of Saturn and Jupiter.

Mariana Sanchez, Nienke van der Marel, Michiel Lambrechts, Sijme-Jan Paardekooper, Yamila Miguel

Comments: Accepted for publication in A&A
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2512.06115 [astro-ph.EP] (or arXiv:2512.06115v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2512.06115
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Submission history
From: Mariana Belen Sanchez Mrs
[v1] Fri, 5 Dec 2025 19:44:16 UTC (1,246 KB)
https://arxiv.org/abs/2512.06115
Astrobiology, Exoplanet, Astrogeology,

Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) 🖖🏻