Constraints on the Distances and Timescales of Solid Migration in the Early Solar System from Meteorite Magnetism

The migrations of solid objects throughout the solar system are thought to have played key roles in disk evolution and planet formation. However, our understanding of these migrations is limited by a lack of quantitative constraints on their timings and distances recovered from laboratory measuremen...

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Bibliographic Details
Published in:The Astrophysical journal 2020-06, Vol.896 (2), p.103
Main Authors: Bryson, James F. J., Weiss, Benjamin P., Biersteker, John B., King, Ashley J., Russell, Sara S.
Format: Article
Language:English
Subjects:
Aluminum
Asteroid belt
Asteroids
Astrophysics
Calcium
Calcium-aluminum-rich inclusions
Chondrites
Chondrules
Constraints
Isotope composition
Isotopes
Kuiper belt
Magnetic fields
Magnetism
Meteorites
Meteoritic composition
Meteors & meteorites
Olivine
Oxygen
Planet formation
Planetary evolution
Primordial magnetic fields
Protoplanetary disks
Solar system
Solar system evolution
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Summary:The migrations of solid objects throughout the solar system are thought to have played key roles in disk evolution and planet formation. However, our understanding of these migrations is limited by a lack of quantitative constraints on their timings and distances recovered from laboratory measurements of meteorites. The protoplanetary disk supported a magnetic field that decreased in intensity with heliocentric distance. As such, the formation distances of the parent asteroids of ancient meteorites can potentially be constrained by paleointensity measurements of these samples. Here, we find that the WIS 91600 ungrouped C2 chondrite experienced an ancient field intensity of 4.4 2.8 T. Combined with the thermal history of this meteorite, magnetohydrodynamical models suggest the disk field reached 4.4 T at ∼9.8 au, indicating that the WIS 91600 parent body formed in the distal solar system. Because WIS 91600 likely came to Earth from the asteroid belt, our recovered formation distance argues that this body previously traveled from ∼10 au to 2-3 au, supporting the migration of asteroid-sized bodies throughout the solar system. WIS 91600 also contains chondrules, calcium-aluminum-rich inclusions and amoeboid olivine aggregates, indicating that some primitive millimeter-sized solids that formed in the innermost solar system migrated outward to ∼10 au within ∼3-4 Myr of solar system formation. Moreover, the oxygen isotopic compositions of proposed distal meteorites (WIS 91600, Tagish Lake and CI chondrites) argue that the CM, CO, and CR chondrites contain micrometer-scale dust and ice that originated in the distal solar system.
ISSN:0004-637X
1538-4357
DOI:10.3847/1538-4357/ab91ab