Acasta Gneiss: Canada's 4-Billion-Year-Old Rock Formation
The Acasta Gneiss became the oldest securely dated intact rock on Earth, showing that evolved crust existed by about 4 billion years ago.
Region
The Acasta Gneiss became the oldest securely dated intact rock on Earth, showing that evolved crust existed by about 4 billion years ago.
One of the oldest well-preserved sequences of volcanic and sedimentary rock on Earth, central to debates over the earliest traces of life.
A Canadian rock belt whose age and possible microfossils remain among the most debated claims for Earth's earliest life.
Repeated glaciations left tillites on several continents and coincided with the first lasting rise of atmospheric oxygen.
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.
The fossil red alga provided the oldest widely accepted evidence of sexual reproduction, complex multicellularity and a eukaryote belonging to a living group.
Rock surfaces at Mistaken Point preserve some of the oldest known communities of large, complex organisms, recognised as a UNESCO World Heritage Site in 2016.
Pikaia is now regarded as an early stem-group chordate, a distant relative of vertebrates rather than their direct ancestor.
Found in 1909, the Burgess Shale became the most famous record of Cambrian soft-bodied animals and transformed scientific understanding of early animal evolution.
The Iapetus Ocean closed and Laurentia, Baltica and Avalonia fused into the continent of Laurussia, raising a long mountain belt.
Dunkleosteus became one of the best-known early vertebrate predators; it and all other placoderms died out by the end of the Devonian.