Biogeochemists say new evidence linking glacial events during the "Snowball Earth" period to the rise of early animals.
The controversial
Snowball Earth hypothesis, which originated in 1964 due to the discovery of glacial deposits near the equator, posits that on several occasions the Earth was covered from pole to pole by a thick sheet of ice lasting for millions of years. These glaciations, far more severe than the usual Ice Ages, occurred from 750 to 580 million years ago, and in their aftermath, the oceans were rich in phosphorus, a nutrient that controls the abundance of life in the oceans, according to new research.