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Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets

Abstract

The petrology record on the Moon suggests that a cataclysmic spike in the cratering rate occurred ∼700 million years after the planets formed1; this event is known as the Late Heavy Bombardment (LHB). Planetary formation theories cannot naturally account for an intense period of planetesimal bombardment so late in Solar System history2. Several models have been proposed to explain a late impact spike3,4,5,6, but none of them has been set within a self-consistent framework of Solar System evolution. Here we propose that the LHB was triggered by the rapid migration of the giant planets, which occurred after a long quiescent period. During this burst of migration, the planetesimal disk outside the orbits of the planets was destabilized, causing a sudden massive delivery of planetesimals to the inner Solar System. The asteroid belt was also strongly perturbed, with these objects supplying a significant fraction of the LHB impactors in accordance with recent geochemical evidence7,8. Our model not only naturally explains the LHB, but also reproduces the observational constraints of the outer Solar System9.

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Figure 1: Disk location and LHB timing.
Figure 2: The planetary orbits and the positions of the disk particles, projected on the initial mean orbital plane.
Figure 3: Planetary migration and the associated mass flux towards the inner Solar System from a representative simulation.

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Acknowledgements

R.G. thanks Conselho Nacional de Desenvolvimento Científico e Tecnológico for support for his sabbatical year in the OCA observatory in Nice. K.T. was supported by an EC Marie Curie Individual Fellowship. A.M. and H.F.L. thank the CNRS and the NSF for funding collaboration between the OCA and the SWRI groups. H.F.L. was supported by NASA's Origins and PG&G programmes.

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Correspondence to A. Morbidelli.

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Gomes, R., Levison, H., Tsiganis, K. et al. Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets. Nature 435, 466–469 (2005). https://doi.org/10.1038/nature03676

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