Impact bombardment chronology of the terrestrial planets from 4.5 Ga to 3.5 Ga

Abstract

Subsequent to the Moon's formation, late accretion to the terrestrial planets modified their silicate crusts and mantles. We combine dynamical N-body and Monte Carlo simulations to determine impact probabilities, impact velocities, and expected mass augmentation onto the terrestrial planets from three sources: planetesimals left over from primary accretion, asteroids from the E-belt, and comets arriving from the outer Solar System. We present estimates of the amount of cometary material striking the terrestrial planets in an early episode of planetesimal-driven giant planet migration (Mojzsis et al., 2019). The Moon and Mars suffer proportionally higher cometary accretion than Venus and Earth. The background mass addition from small leftover planetesimals to Earth and Mars is far less than independent estimates based on their mantle abundances of highly-siderophile elements. This supports the theory that both planets were struck by single large bodies that delivered most of their mass augmentation since primary accretion. We present fits to the impact chronologies valid from 4500 Ma to ca. 3700 Ma. The lunar timeline thus obtained is at odds with both the calibrated Neukum (Neukum et al., 2001) and Werner (Werner et al., 2014; Werner, 2019) chronologies. For Mars, the match with its calibrated Werner chronology is no better; by increasing the mass of the E-belt by a factor of four the dynamical lunar and martian chronologies are in line with that of Werner (2019) and match constraints from the current population of Hungaria asteroids. Yet, neither of our dynamical timelines fit well with that of Neukum. The dynamical lunar and martian chronologies are also different from each other. Consequently, the usual extrapolation of such chronologies from one planetary body to the other is technically inappropriate.

Accepted in Icarus

References in corpus (21)

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Cited by in corpus (21)

• Early Bombardment of the Moon: Connecting the Lunar Crater Record to the Terrestrial Planet Formation
• Reduced atmospheres of post-impact worlds: The early Earth
• The terrestrial planet formation paradox inferred from high-resolution N-body simulations
• Did Mars possess a dense atmosphere during the first ~400 million years?
• Reduced late bombardment on rocky exoplanets around M-dwarfs
• Habitable planet formation around low-mass stars: Rapid accretion, rapid debris removal and the essential contribution of external giants
• A new martian crater chronology: Implications for Jezero crater
• Born extra-eccentric: A broad spectrum of primordial configurations of the gas giants that match their present-day orbits
• The early instability scenario: Mars' mass explained by Jupiter's orbit
• Modification of the composition and density of Mercury from late accretion
• Eta-Earth Revisited II: Deriving a Maximum Number of Earth-like Habitats in the Galactic Disk
• Rethinking the role of the giant planet instability in terrestrial planet formation models
• Escape and accretion by cratering impacts: Formulation of scaling relations for high-speed ejecta
• Origin of Mars's moons by disruptive partial capture of an asteroid
• Mercury's formation within the Early Instability Scenario
• A new estimate for the age of highly-siderophile element retention in the lunar mantle from late accretion
• Terrestrial planet formation during giant planet formation and giant planet migration I: The first 5 million years
• The plausibility of origins scenarios requiring two impactors
• Constraining the survival of HCN during cometary impacts
• Gyr-timescale destruction of high-eccentricity asteroids by spin and why 2006 HY51 has been spared
• Impact chronology of leftover planetesimals