Dynamical origin of Theia, the last giant impactor on Earth
Duarte Branco, Sean N. Raymond, Pedro Machado

TL;DR
This study uses dynamical simulations to explore the origin of Theia, suggesting it could have been a carbonaceous or non-carbonaceous embryo, aligning with cosmochemical evidence of Earth's late accretion of CC material.
Contribution
It provides a dynamical validation for the cosmochemical hypothesis that Theia was a CC or NC embryo, matching multiple planetary formation constraints.
Findings
Approximately 50-50 chance Theia was a CC or NC embryo.
Simulations match Earth's and Mars's CC mass fractions and impact timing.
Total scattered CC mass was around 0.2-0.3 Earth masses.
Abstract
Cosmochemical studies have proposed that Earth accreted roughly 5-10% of its mass from carbonaceous (CC) material, with a large fraction delivered late via its final impactor, Theia (the Moon-forming impactor). Here, we evaluate this idea using dynamical simulations of terrestrial planet formation, starting from a standard setup with a population of planetary embryos and planetesimals laid out in a ring centered between Venus and Earth's orbits, and also including a population of CC planetesimals and planetary embryos scattered inward by Jupiter. We find that this scenario can match a large number of constraints, including i) the terrestrial planets' masses and orbits; ii) the CC mass fraction of Earth; iii) the much lower CC mass fraction of Mars, as long as Mars only accreted CC planetesimals (but no CC embryos); iv) the timing of the last giant (Moon-forming) impact; and v) a late…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Code & Models
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsPlanetary Science and Exploration · Astro and Planetary Science · Paleontology and Stratigraphy of Fossils
