Magnetic fields are proposed to have played a critical role in some of the most enigmatic processes of planetary formation by mediating the rapid accretion of disk material onto the central star and the formation of the first solids. However, there have been no experimental constraints on the intensity of these fields. We have been studying meteoritic materials from the early solar system to infer the existence intensity of nebular magnetic fields. We recently showed that chondrules in the Semarkona meteorite were magnetized in a nebular field of ~5-50 μT (Fu et al. 2014) at ~2 million years after solar system formation. This field strength is sufficient to account for the rates of stellar accretion observed in protoplanetary disks.
Because nebular gas is required for the sustenance of nebular magnetism, paleomagnetic methods can also be used to trace the lifetime of the nebula itself. We have recently shown that volcanic angrites, the oldest known well-preserved basaltic rocks, are essentially not magnetized (Wang et al. 2017). This indicates the solar nebular field and gas had likely dissipated by just 3.8 million years after solar system formation. Combined with our Semarkona measurements (see above) his times the birthdate of the Sun, Jupiter and Saturn to ~2-3.8 million years after the formation of the oldest solids.