Cited by 939Astro and Planetary ScienceStellar, planetary, and galactic studiesSpace Satellite Systems and Control

Chaotic capture of Jupiter's Trojan asteroids in the early Solar System

Morbidelli, A., Levison, H. F., Tsiganis, K., Gomes, R.·2005·Nature

Abstract

Jupiter's Trojans are asteroids that follow essentially the same orbit as Jupiter, but lead or trail the planet by an angular distance of approximately 60 degrees (co-orbital motion). They are hypothesized to be planetesimals that formed near Jupiter and were captured onto their current orbits while Jupiter was growing, possibly with the help of gas drag and/or collisions. This idea, however, cannot explain some basic properties of the Trojan population, in particular its broad orbital inclination distribution, which ranges up to approximately 40 degrees (ref. 8). Here we show that the Trojans could have formed in more distant regions and been subsequently captured into co-orbital motion with Jupiter during the time when the giant planets migrated by removing neighbouring planetesimals. The capture was possible during a short period of time, just after Jupiter and Saturn crossed their mutual 1:2 resonance, when the dynamics of the Trojan region were completely chaotic. Our simulations of this process satisfactorily reproduce the orbital distribution of the Trojans and their total mass.

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Crossref · 10.1038/nature03540

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  • The Nice model can explain the structure of the asteroid belt, some compositional variations therein, and the structure of Jupiter and Neptune's trojan populations.

    “The Nice model can also explain not only the structure of the asteroid belt but also some of the compositional variations observed therein (Levison et al., 2009), along with the structure of both Jupiter and Neptune's trojan population (Morbidelli et al., 2005; Tsiganis et al., 2005; Sheppard and Trujillo, 2010).”

    From The Astrobiology Primer v2.0 (2016) · cites this paper as Morbidelli et al., 2005

  • Two dominant models have emerged under the planetary accretion paradigm to explain the formation of planets and long-term evolution of the Solar System: the Grand Tack model and the Nice model.

    “Two dominant models have emerged under the planetary accretion paradigm to explain the formation of planets and long-term evolution of the Solar System: the Grand Tack model, which focuses on planet formation (Walsh et al., 2011), and the Nice model, which focuses on long-term evolution (Gomes et al., 2005; Morbidelli et al., 2005; Tsiganis et al., 2005; Levison et al., 2011).”

    From The Astrobiology Primer v2.0 (2016) · cites this paper as Morbidelli et al., 2005

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Authors
Morbidelli, A., Levison, H. F., Tsiganis, K., & Gomes, R.
Affiliations
  • Observatoire de la Côte d’Azur (FR)
  • Southwest Research Institute (US)
  • Universidade Federal do Rio de Janeiro (BR)
Corresponding author
Morbidelli, A.
Venue
Nature
Published
2005-05
Volume
435
Issue
7041
Pages
462-465
ISSN
  • 0028-0836 (ISSN-L)
  • 1476-4687
OpenAlex
W2041775599
Cited by
939
References
1
Citations by year
2026: 24 · 2025: 32 · 2024: 43 · 2023: 39 · 2022: 37 · 2021: 50 · 2020: 50 · 2019: 45 · 2018: 75 · 2017: 45 · 2016: 56 · 2015: 51 · 2014: 57 · 2013: 33 · 2012: 53
FWCI
21.31
Type
journal article
Language
en
Open access
closed
Locations
  • Nature (publishedVersion)
  • PubMed (publishedVersion)
  • HAL (submittedVersion)
  • RePEc: Research Papers in Economics (submittedVersion)
Funders
National Aeronautics and Space Administration
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Stellar, planetary, and galactic studies
  • Physical Sciences › Engineering › Aerospace Engineering › Space Satellite Systems and Control
Keywords
giant planet migration, early solar system dynamics, Late Heavy Bombardment, orbital inclination distribution, 1:2 resonance, planetesimals, orbital evolution

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