Bifurcation of planetary building blocks during Solar System formation

Author:

Lichtenberg Tim1ORCID,Dra̧żkowska Joanna2ORCID,Schönbächler Maria3ORCID,Golabek Gregor J.4ORCID,Hands Thomas O.5ORCID

Affiliation:

1. Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, Oxford, UK.

2. University Observatory, Faculty of Physics, Ludwig-Maximilians-Universität München, Munich, Germany.

3. Institute for Geochemistry and Petrology, Department of Earth Sciences, ETH Zurich, Zurich, Switzerland.

4. Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany.

5. Institute for Computational Science, University of Zurich, Zurich, Switzerland.

Abstract

Two-part formation of the Solar System Measurements of meteorites have shown that the inner and outer Solar System formed from two distinct reservoirs of material. Existing models have proposed that these were split by Jupiter forming first, which would open a gap in the protoplanetary disc. Lichtenberg et al. instead argue that the snow line, the boundary between regions containing water vapor and solid ice, migrated first outward and then inward, forming two separate populations of planetesimals. Those planetesimals then grew through collisions to form the planets. Their simulation of this model explains the meteorite data and is consistent with astronomical observations of protoplanetary disks around other stars. Science , this issue p. 365

Funder

Simons Foundation

H2020 European Research Council

Swiss National Science Foundation

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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