An MIT-led team reports remanent magnetization in calcium-aluminum-rich inclusions from an Antarctic meteorite, pushing the earliest known nebular field ten times closer to time zero.
Reality
- Evidence58
- Adoption
- Not scored
- Hype gap+20
- Incentives
- Not scored
- Confidence60
Meteorite grains from the solar system's first 200,000 years recorded a field stronger than Earth's
MIT researchers found magnetic traces in meteorite grains from the solar system's first 200,000 years that point to a field stronger than Earth's today. That places magnetism in the nebula while the sun was forming, though how much of the collapse it drove is still an estimate.
Reality
- Evidence40
- Adoption
- Not scored
- Hype gap+25
- Incentives35
- Confidence55
Half a gram of Bennu puts its birthplace at the solar system's water-ice line
An ETH Zurich lab measured iron, titanium and chromium in its share of the OSIRIS-REx return and found the same dust reservoir that produced Ryugu and the rare CI meteorites, a composition matching neither the inner nor the outer solar system.
Reality
- Evidence66
- Adoption30
- Hype gap+12
- Incentives55
- Confidence62
Iron meteorite chemistry puts the earliest planetesimals at 8 to 17 percent icy dust
Yale researchers read the original makeup of planetesimals that melted so thoroughly their textures vanished, and place the Solar System's preference for heat-formed rock beads inside the first million years.
Reality
- Evidence58
- Adoption
- Not scored
- Hype gap+25
- Incentives70
- Confidence48
Melted meteorites date the sorting of rock over ice to the solar system's first million years
A Yale-led team could not sample planetesimals from the first million years, because every one of them melted, so it reconstructed their make-up from sulfur and iron oxidation in iron meteorites and got 8% to 17% icy dust.
Reality
- Evidence62
- Adoption
- Not scored
- Hype gap+18
- Incentives55
- Confidence58