The Taurid meteor streams have a reputation for generating impressive fireball meteors.
The Great Oxidation Event, which occurred between 2.1 and 2.4 billion years ago, fundamentally transformed Earth's atmosphere and made complex life possible. Before this period, oxygen producing cyanobacteria had evolved hundreds of millions of years earlier, yet atmospheric oxygen levels remained low for an extended period. Scientists have long wondered over this delay, exploring various explanations from volcanic gases to microbial activity. A recent study from Okayama University in Japan offers a fresh view on this ancient mystery by examining two unlikely culprits, nickel and urea.

