Dynamical evidence for an early giant planet instability
arXiv:1912.10879 · doi:10.1016/j.icarus.2019.113605
Abstract
The dynamical structure of the Solar System can be explained by a period of orbital instability experienced by the giant planets. While a late instability was originally proposed to explain the Late Heavy Bombardment, recent work favors an early instability. We model the early dynamical evolution of the outer Solar System to self-consistently constrain the most likely timing of the instability. We first simulate the dynamical sculpting of the primordial outer planetesimal disk during the accretion of Uranus and Neptune from migrating planetary embryos during the gas disk phase, and determine the separation between Neptune and the inner edge of the planetesimal disk. We performed simulations with a range of migration histories for Jupiter. We find that, unless Jupiter migrated inwards by 10 AU or more, the instability almost certainly happened within 100 Myr of the start of Solar System formation. There are two distinct possible instability triggers. The first is an instability that is triggered by the planets themselves, with no appreciable influence from the planetesimal disk. Of those, the median instability time is Myr. Among self-stable systems -- where the planets are locked in a resonant chain that remains stable in the absence of a planetesimal's disk-- our self-consistently sculpted planetesimal disks nonetheless trigger a giant planet instability with a median instability time of 37-62 Myr for a reasonable range of migration histories of Jupiter. The simulations that give the latest instability times are those that invoked long-range inward migration of Jupiter from 15 AU or beyond; however these simulations over-excited the inclinations of Kuiper belt objects and are inconsistent with the present-day Solar System. We conclude on dynamical grounds that the giant planet instability is likely to have occurred early in Solar System history.
arXiv comment46 pages, 26 figures, Article reference YICAR_113605, https://authors.elsevier.com/tracking/article/details.do?aid=113605&jid=YICAR&surname=Ribeiro
References in corpus (88)
- Disk Frequencies and Lifetimes in Young Clusters
- A low mass for Mars from Jupiter's early gas-driven migration
- REBOUND: An open-source multi-purpose N-body code for collisional dynamics
- Planetary Candidates Observed by Kepler, III: Analysis of the First 16 Months of Data
- Dynamical Outcomes of Planet-Planet Scattering
- Rapid growth of gas-giant cores by pebble accretion
- IAS15: A fast, adaptive, high-order integrator for gravitational dynamics, accurate to machine precision over a billion orbits
- Masses, Radii, and Orbits of Small Kepler Planets: The Transition from Gaseous to Rocky Planets
- Origins of Eccentric Extrasolar Planets: Testing the Planet-Planet Scattering Model
- WHFast: A fast and unbiased implementation of a symplectic Wisdom-Holman integrator for long term gravitational simulations
- Forming the cores of giant planets from the radial pebble flux in protoplanetary discs
- Separating gas-giant and ice-giant planets by halting pebble accretion
- Collisions Between Gravity-Dominated Bodies: 1. Outcome Regimes and Scaling Laws
- Collisions between Gravity-Dominated Bodies: 2. The Diversity of Impact Outcomes during the End Stage of Planet Formation
- Breaking the Chains: Hot Super-Earth systems from migration and disruption of compact resonant chains
- Statistical Study of the Early Solar System's Instability with 4, 5 and 6 Giant Planets
- Reversing type II migration: resonance trapping of a lighter giant protoplanet
- The Mass and Size Distribution of Planetesimals Formed by the Streaming Instability. I. The Role of Self-Gravity
- The HARPS search for southern extra-solar planets XXXIV. Occurrence, mass distribution and orbital properties of super-Earths and Neptune-mass planets
- On the orbital evolution and growth of protoplanets embedded in a gaseous disc
- Dynamics of the giant planets of the solar system in the gaseous proto-planetary disk and relationship to the current orbital architecture
- Dynamical Evolution of the Early Solar System
- Origin of water in the inner Solar System: Planetesimals scattered inward during Jupiter and Saturn's rapid gas accretion
- A Sawtooth-like Timeline for the First Billion Year of Lunar Bombardment
- Formation of planetary systems by pebble accretion and migration: How the radial pebble flux determines a terrestrial-planet or super-Earth growth mode
- The timeline of the Lunar bombardment - revisited
- Growing the gas-giant planets by the gradual accumulation of pebbles
- Probabilistic Mass-Radius Relationship for Sub-Neptune-Sized Planets
- Three-dimensional simulations of multiple protoplanets embedded in a protostellar disc
- The Absolute Magnitude Distribution of Kuiper Belt Objects
- Capture of Trojans by Jumping Jupiter
- Exotic Earths: Forming Habitable Worlds with Giant Planet Migration
- Evidence from the asteroid belt for a violent past evolution of Jupiter's orbit
- The Different Evolution of Gas and Dust in Disks around Sun-like and Cool Stars
- Cavity opening by a giant planet in a protoplanetary disc and effects on planetary migration
- Modeling the Formation of Giant Planet Cores I: Evaluating Key Processes
- Mars' Growth Stunted by an Early Giant Planet Instability
- Debris disks as signposts of terrestrial planet formation
- Young Solar System's Fifth Giant Planet?
- The Evidence for Slow Migration of Neptune from the Inclination Distribution of Kuiper Belt Objects
- Planet-planet scattering in planetesimal disks II: Predictions for outer extrasolar planetary systems
- Constraints on resonant-trapping for two planets embedded in a protoplanetary disc
- Merging Criteria for Giant Impacts of Protoplanets
- On disc protoplanet interactions in a non-barotropic disc with thermal diffusion
- Migration and Dynamical Relaxation in Crowded Systems of Giant Planets
- Constructing the secular architecture of the solar system II: The terrestrial planets
- Cataclysm no more: New views on the timing and delivery of lunar impactors
- Neptune's Orbital Migration Was Grainy, Not Smooth
- The formation of Uranus and Neptune among Jupiter and Saturn
- Jumping Neptune Can Explain the Kuiper Belt Kernel
- On the Migration of Jupiter and Saturn: Constraints from Linear Models of Secular Resonant Coupling with the Terrestrial Planets
- NOTE: Explaining why the Uranian satellites have equatorial prograde orbits despite the large planetary obliquity
- Gas giant planets as dynamical barriers to inward-migrating super-Earths
- Resonant inclination excitation of migrating giant planets
- Capture of Irregular Satellites at Jupiter
- The early instability scenario: terrestrial planet formation during the giant planet instability, and the effect of collisional fragmentation
- The Orbital Stability of Planets Trapped in the First-Order Mean-Motion Resonances
- Unstable Planetary Systems Emerging Out Of Gas Disks
- Rocky super-Earths or waterworlds: the interplay of planet migration, pebble accretion and disc evolution
- The Fragility of the Terrestrial Planets During a Giant Planet Instability
- Oligarchic and giant impact growth of terrestrial planets in the presence of gas giant planet migration
- Constraining the giant planets' initial configuration from their evolution: implications for the timing of the planetary instability
- Accretion of Uranus and Neptune from inward-migrating planetary embryos blocked by Jupiter and Saturn
- Disk Dispersal and Planet Formation Time Scales
- Outward migration of Jupiter and Saturn in 3:2 or 2:1 resonance in radiative disks: implications for the Grand Tack and Nice models
- Toward a new paradigm for Type II migration
- The evolution of asteroids in the jumping-Jupiter migration model
- The Grand Tack model: a critical review
- Consequences of Giant Impacts on Early Uranus for Rotation, Internal Structure, Debris, and Atmospheric Erosion
- Prograde rotation of protoplanets by accretion of pebbles in a gaseous environment
- A collisionless scenario for Uranus tilting
- Two phase, inward-then-outward migration of Jupiter and Saturn in the gaseous Solar Nebula
- Analysis of terrestrial planet formation by the Grand Tack model: System architecture and tack location
- Modeling the Historical Flux of Planetary Impactors
- Planetesimal-driven planet migration in the presence of a gas disk
- The excitation of a primordial cold asteroid belt as an outcome of the planetary instability
- Excitation and depletion of the asteroid belt in the early instability scenario
- Is the Grand Tack model compatible with the orbital distribution of main belt asteroids?
- Extrasolar Planet Eccentricities from Scattering in the Presence of Residual Gas Disks
- Application of gas dynamical friction for planetesimals: I. Evolution of single planetesimals
- Runaway gas accretion and gap opening versus type~I migration
- Tilting Saturn without tilting Jupiter: Constraints on giant planet migration
- Formation of planetary systems by pebble accretion and migration: Hot super-Earth systems from breaking compact resonant chains
- Instabilities in the Early Solar System due to a Self-gravitating Disk
- Checking the Compatibility of the Cold Kuiper Belt with a Planetary Instability Migration Model
- Considerations on the accretion of Uranus and Neptune by mutual collisions of planetary embryos in the vicinity of Jupiter and Saturn
- Jumping Jupiter can explain Mercury's orbit
- Dynamical effects on the classical Kuiper Belt during the excited-Neptune model
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- Venusian Habitable Climate Scenarios: Modeling Venus through time and applications to slowly rotating Venus-Like Exoplanets
- Early Solar System instability triggered by dispersal of the gaseous disk
- The Role of Early Giant Planet Instability in the Terrestrial Planet Formation
- 1I/'Oumuamua as an N2 ice fragment of an exo-pluto surface. II. Generation of N2 ice fragments and the origin of 'Oumuamua
- Born eccentric: constraints on Jupiter and Saturn's pre-instability orbits
- Growing Mars fast: High-resolution GPU simulations of embryo formation
- The terrestrial planet formation paradox inferred from high-resolution N-body simulations
- Did Mars possess a dense atmosphere during the first ~400 million years?
- An interstellar origin for high-inclination Centaurs
- Direct measurement of decimeter-sized rocky material in the Oort cloud
- Origin and dynamical evolution of the asteroid belt
- Dynamical avenues for Mercury's origin I: The lone survivor of a primordial generation of short-period proto-planets
- Implications of Jupiter Inward Gas-Driven Migration for the Inner Solar System
- Survivor bias: divergent fates of the Solar System's ejected vs. persisting planetesimals
- Born extra-eccentric: A broad spectrum of primordial configurations of the gas giants that match their present-day orbits
- Hint of an exocomet transit in the CHEOPS lightcurve of HD 172555
- The early instability scenario: Mars' mass explained by Jupiter's orbit
- The Dissipation of the Solar Nebula Constrained by Impacts and Core Cooling in Planetesimals
- Dynamical avenues for Mercury's origin II: in-situ formation in the inner terrestrial disk
- A race against the clock: Constraining the timing of cometary bombardment relative to Earth's growth
- Collision Chains among the Terrestrial Planets. II. An Asymmetry between Earth and Venus
- Origin of Water in the Terrestrial Planets: Insights from Meteorite Data and Planet Formation Models
- Very Slow Rotators from Tidally Synchronized Binaries
- Rethinking the role of the giant planet instability in terrestrial planet formation models
- Effects of early intense bombardment on megaregolith evolution and on lunar (and planetary) surface samples
- Terrestrial planet and asteroid belt formation by Jupiter-Saturn chaotic excitation
- Mercury's formation within the Early Instability Scenario
- Generating metal-polluting debris in white dwarf planetary systems from small-impact crater ejecta
- Mars' formation can constrain the primordial orbits of the gas giants
- Orbital Dynamics and the Evolution of Planetary Habitability in the AU Mic System
- An early giant planet instability recorded in asteroidal meteorites
- Can narrow disks in the inner solar system explain the four terrestrial planets?
- Dynamical evolution of a self-gravitating planetesimal disk in the distant trans-Neptunian region
- Can the orbital distribution of Neptune's 3:2 mean motion resonance result from stability sculpting?
- Crash Chronicles: relative contribution from comets and carbonaceous asteroids to Earth's volatile budget in the context of an Early Instability
- Collisional Growth Within the Solar System's Primordial Planetesimal Disk and the Timing of the Giant Planet Instability
- Very-wide-orbit planets from dynamical instabilities during the stellar birth cluster phase
- Planet formation: key mechanisms and global models
- From Planetesimals to Dwarf Planets by Pebble Accretion
- Collisional heating of icy planetesimals. I. Catastrophic collisions
- A Crater Chronology for the Jupiter's Asteroids
- Oort Cloud Ecology. III. The Sun left the parent star cluster shortly after the giant planets formed
- Formation of the four terrestrial planets in the Jupiter-Saturn chaotic excitation scenario: fundamental properties and water delivery
- Asteroids fail to retain cometary impact signatures
- On the interstellar origin of high-inclination Centaurs
- Inclination pathways of planet-crossing asteroids
- Protoplanetary disk formation from the collapse of a prestellar core
- Shaken, not stirred: inefficient mixing of CM- and CI-like materials
- Dust Dynamics in Hall-effected Protoplanetary Disks. I. Background Drift Hall Instability
- Acceleration of planetary migration: Resonance crossing and planetesimal ring