Open up almost any stony meteorite, as scientists have been doing for more than 200 years1, and you will find hundreds of millimetre-sized bits of rock. These ‘chondrules’ (named after the Greek for seeds) were formed at the birth of the Solar System, and as such potentially bear witness to conditions — pressures, temperatures, chemical composition and so on — in the solar nebula. But obtaining that information depends on identifying how they formed, a topic tackled by Cuzzi and Alexander on page 483 of this issue2.
CITATION STYLE
Desch, S. (2006). How to make a chondrule. Nature, 441(7092), 416–417. https://doi.org/10.1038/441416a
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