4.6-Billion-Year-Old Meteorite Reveals a Surprisingly Strong Primordial Magnetic Field
MIT researchers have found evidence, preserved in a pristine Antarctic meteorite, that the early solar system had a magnetic field three to 12 times stronger than Earth's today, before the Sun had fully formed.
Step by step
- 1
Solar nebula collapses into a disk
- 2
Magnetic field forms within the disk
- 3
CAI grains record the field's strength
- 4
Grains preserved inside meteorite for eons
- 5
Meteorite found, grains measured on Earth
Researchers led by the Massachusetts Institute of Technology (MIT) have found evidence of a surprisingly strong magnetic field during the solar system's first 200,000 years, before the Sun had fully formed. The evidence comes from microscopic mineral grains preserved inside a meteorite found in Antarctica in 2008. The findings, led by MIT professor Benjamin Weiss and Borlina, a former MIT graduate student now an assistant professor at Purdue University, appear in the Proceedings of the National Academy of Sciences (PNAS).
The researchers examined DOM 08006, a meteorite found in 2008 in the Dominion Range along the East Antarctic Ice Sheet. It is one of the most primitive meteorites known, having changed far less than most others over its roughly 4.6-billion-year history. Inside it, the team identified calcium-aluminum-rich inclusions (CAIs) β tiny mineral grains that formed during the solar system's first 200,000 years and are the oldest known material from that period.
Some of the CAIs contained naturally magnetic minerals, including iron, capable of recording the strength of any magnetic field present when they formed β a property called . The measurements indicate the early solar system's magnetic field measured roughly 150 to 600 microteslas, about three to 12 times stronger than Earth's magnetic field today.
The finding pushes evidence of solar-system magnetism further back than before. The researchers had previously found signs of magnetic fields from about 2 million years after formation began, when the Sun had already formed and planets were assembling. Weiss said the shift from a spherical cloud to a is among the most significant events in solar system history, and that while gravity has long been credited, the new measurements show magnetism likely played a role too.
Borlina said the fields likely helped move gas from the protoplanetary disk inward toward the forming Sun, working alongside gravity β a factor he said should be included in explaining how the Sun and planets formed.
Terms explained
The story so far
- MIT Engineers Turn Bacteria Into Living Transistors to Build Biological Circuits
- Researchers Record Arctic Under-Ice Sounds and Test a Through-Ice Radio
- Antarctica Gained a Record 695 Billion Tons of Ice, Study Finds
- Rattlesnake Blood Proteins Point to More Powerful Antivenom
- Fossils Reveal the Songs of Jurassic-Era Insects
- Earth May Not Be a Cosmic Fluke, New Solar System Simulations Suggest
- 4.6-Billion-Year-Old Meteorite Reveals a Surprisingly Strong Primordial Magnetic Field
