There’s always a lot of extraterrestrial dust floating down to Earth, but this dust is normally only a tiny fraction of the other dust in our atmosphere such as volcanic ash, dust from deserts and sea salt. But when a 93-mile (150 km) wide asteroid broke apart in the main asteroid belt between Mars and Jupiter some 466 million years ago (the middle of the Ordovician period), it created way more dust than usual. Schmitz et al argue that the mid-Ordovician...
