Columbia (Nuna) Supercontinent: Assembly and Breakup
Most of Earth's continental blocks joined into one landmass, which fragmented gradually between about 1.5 and 1.3 billion years ago.
Region
Most of Earth's continental blocks joined into one landmass, which fragmented gradually between about 1.5 and 1.3 billion years ago.
A partnership between an archaeal host and a bacterium produced the complex cell, ancestor of all animals, plants, fungi and protists.
Climate, ocean chemistry and oxygen levels stayed relatively stable for roughly a billion years while eukaryotes diversified only slowly, before the upheavals of the Neoproterozoic.
Most of Earth's continental crust was joined in one landmass, whose breakup opened new oceans and may have helped trigger the Cryogenian Snowball Earth glaciations.
Two long glaciations, the Sturtian and the Marinoan, covered much or all of the oceans in ice before greenhouse warming ended them, setting the stage for the Ediacaran Period.
The first assemblages of large, multicellular organisms appeared in the oceans, including some of the earliest animals, before most forms vanished near the start of the Cambrian.
Gondwana assembled by about 500 million years ago, joined Pangaea, and broke apart from about 180 million years ago into today's southern continents.
Life spread from the sea onto land and diversified enormously before the era ended with the largest mass extinction in Earth's history.
Within some 20 to 30 million years, most major animal body plans, including arthropods, molluscs and chordates, appeared in the fossil record.
Trilobites diversified into more than 20,000 known species before dying out in the Permian–Triassic extinction about 252 million years ago.
Recognised in 1985 as a single animal rather than several, Anomalocaris became the best-known member of the radiodonts, early relatives of the arthropods.
Marine diversity rose several-fold and the brachiopod-crinoid-bryozoan ecosystems that dominated Paleozoic seas were established.