File:Mollweide_Paleographic_Map_of_Earth,_510_Ma.png · Wikimedia Commons · See Wikimedia Commons
Also known as Cambrian Period, Cambrian System
The Cambrian ( ) is the first geological period of the Paleozoic Era and the Phanerozoic Eon. The Cambrian lasted 51.95 million years from the end of the preceding Ediacaran period 538.8 Ma (million years ago) to the beginning of the Ordovician Period 486.85 Ma.
The Cambrian is the earliest geological period of the Paleozoic Era, lasting about 52 million years from 538.8 to 486.85 million years ago. It marks the beginning of the Phanerozoic Eon, the time interval that encompasses all of Earth's history with visible life forms.
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The Cambrian ( ) is the first geological period of the Paleozoic Era and the Phanerozoic Eon. The Cambrian lasted 51.95 million years from the end of the preceding Ediacaran period 538.8 Ma (million years ago) to the beginning of the Ordovician Period 486.85 Ma.
Most of the continents were located in the southern hemisphere surrounded by the vast Panthalassa Ocean. The assembly of Gondwana during the Ediacaran and early Cambrian led to the development of new convergent plate boundaries and continental-margin arc magmatism along its margins that helped drive up global temperatures. Laurentia lay across the equator, separated from Gondwana by the opening Iapetus Ocean.
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Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).