Metallicity regulates planet formation across all masses
Max Nguyen, Vardan Adibekyan
TL;DR
The paper addresses how the total heavy-element content of planet-building disks, quantified by the heavy-element mass fraction $Z$, governs planet occurrence, multiplicity, and mass across the full planetary spectrum. It estimates $Z$ from host-star abundances using a stoichiometric model with $Z_igodot=1.25\%$ and analyzes RV-detected planets alongside non-host control samples to identify metallicity-planet formation trends. The findings show that higher $Z$ environments preferentially form planets across all masses, with stronger signals for more massive planets and higher planetary multiplicity, consistent with core accretion and challenging a dominant gravitational-instability interpretation for the bulk of planets. The study also demonstrates the robustness of $Z$ as a disk-metallicity proxy across data sets and uncertainty thresholds, and highlights the nuanced difference between $Z$ and [Fe/H] as tracers. Overall, metallicity—via $Z$—shapes the entire planetary mass spectrum and system architectures, supporting a predominantly core-accretion–driven formation pathway with limited GI influence.
Abstract
The role of stellar metallicity in shaping planetary systems is central to our understanding of planet formation. While the core accretion paradigm is widely accepted as the dominant mechanism for forming low- and intermediate-mass planets, the origin of the most massive planets remains debated, with gravitational instability often invoked to explain their existence. In this study, we analyze the dependence of planet formation on metallicity using the total heavy-element mass fraction (Z), which is a proxy for the composition of the protoplanetary disk inferred from stellar photospheres. We show that even the most massive planets form preferentially in metal-rich environments. Z correlates not only with the presence of planets, but also with planetary system multiplicity and total planetary mass. The most massive planets are found in the most metal-rich environments, and, in agreement with core-accretion theory, only the upper end of the planetary mass distribution shows a clear positive correlation with metallicity. These findings suggest that the chemical enrichment of protoplanetary disks plays a central role in shaping the full spectrum of planetary masses.
