History of the solar nebula from meteorite paleomagnetism.
basic_science · Level V
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- Record sourced from PubMed, PMID 33523830.
- Also identified by DOI 10.1126/sciadv.aba5967 and PMC identifier 7775786.
- Licence recorded as CC BY-NC.
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Abstract
We review recent advances in our understanding of magnetism in the solar nebula and protoplanetary disks (PPDs). We discuss the implications of theory, meteorite measurements, and astronomical observations for planetary formation and nebular evolution. Paleomagnetic measurements indicate the presence of fields of 0.54 ± 0.21 G at ~1 to 3 astronomical units (AU) from the Sun and ≳0.06 G at 3 to 7 AU until >1.22 and >2.51 million years (Ma) after solar system formation, respectively. These intensities are consistent with those predicted to enable typical astronomically observed protostellar accretion rates of ~10<sup>-8</sup> <i>M</i> <sub>⊙</sub>year<sup>-1</sup>, suggesting that magnetism played a central role in mass transport in PPDs. Paleomagnetic studies also indicate fields <0.006 G and <0.003 G in the inner and outer solar system by 3.94 and 4.89 Ma, respectively, consistent with the nebular gas having dispersed by this time. This is similar to the observed lifetimes of extrasolar protoplanetary disks.