The Ordovician Period is the second period of the Paleozoic Era, spanning from about 485 to 443 million years ago. It is named after the Celtic tribe of the Ordovices in Wales.
The key events of the Ordovician Period include the diversification of life, formation of continents, and climate change.
The diversification of marine life during the Ordovician led to the rise of early fish and the proliferation of invertebrate species, contributing to the overall biodiversity of the planet.
The Ordovician experienced dramatic climate fluctuations, including periods of glaciation, which influenced the evolution and distribution of life on Earth.
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