Pongola Glaciation: Earth's Earliest Known Ice Age
The oldest known evidence of glaciers on Earth, showing that ice could form even under the faint young Sun of the Archean.
Era · Before c. 3000 BC
From the formation of Earth and the age of dinosaurs to the first cave art and monuments, before writing was invented.
The oldest known evidence of glaciers on Earth, showing that ice could form even under the faint young Sun of the Archean.
A proposed Neoarchean supercontinent whose existence is still debated; its suggested breakup after about 2.5 billion years ago is marked by large swarms of volcanic dykes.
Iron-rich sediments deposited in oxygen-poor oceans that now record the rise of oxygen and supply most of the world's iron ore.
Earth gained an oxygenated atmosphere, complex eukaryotic cells and multicellular life, ending with the first animals just before the Cambrian.
Repeated glaciations left tillites on several continents and coincided with the first lasting rise of atmospheric oxygen.
Free oxygen became a lasting part of Earth's atmosphere, transforming the chemistry of rocks, oceans and life.
Most of Earth's continental blocks joined into one landmass, which fragmented gradually between about 1.5 and 1.3 billion years ago.
Hundreds of centimetre-scale pyritised structures were found, sparking a continuing debate over whether they are early multicellular life.
An asteroid impact left a structure originally an estimated 250-300 km wide, now a UNESCO World Heritage Site.
A partnership between an archaeal host and a bacterium produced the complex cell, ancestor of all animals, plants, fungi and protists.
The first widely accepted Precambrian microfossils were described, opening the modern study of early life.
A giant impact created one of Earth's largest known impact structures and, indirectly, one of the world's richest nickel and copper ore districts.