Eras
Ordovician
or-duh-VISH-ee-un
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The Ordovician is the second period of the Paleozoic Era, following the Cambrian and preceding the Silurian, spanning roughly 486.85 to 443.1 million years ago. Marine life diversified enormously during the Great Ordovician Biodiversification Event, but the period closed with the Ordovician-Silurian extinction, the second-largest mass extinction in Earth history.
Facts
Start (Million Years Ago)Standard boundary age from the ICS International Chronostratigraphic Chart; not independently re-dated by this atlas. End (Million Years Ago)Standard boundary age from the ICS International Chronostratigraphic Chart; not independently re-dated by this atlas. Key EventThe Ordovician-Silurian extinction events at the period's close eliminated about 49 percent of marine genera, with brachiopods, bryozoans, trilobites, conodonts and graptolites especially hard hit. 1 Cross-Tradition Connections
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