The Ordovician period is the second period of the Paleozoic Era, spanning approximately 41 million years from about 485.4 to 443.8 million years ago. It is named after the Celtic tribe of the Ordovices, and it is known for significant evolutionary events and environmental changes.
During the Ordovician period, the Earth's climate was relatively warm and stable. The presence of extensive shallow seas contributed to the diversification of marine life.
The Ordovician period saw a remarkable increase in the diversity of marine life. This period is often associated with the Great Ordovician Biodiversification Event (GOBE), during which many new species evolved.
The Ordovician period marked the first appearance of jawless fish, an important evolutionary development in the history of vertebrates. Additionally, this period witnessed the formation of the first coral reefs, which further contributed to the richness of marine ecosystems.
Though not as well-known as the mass extinctions of the later periods, the Ordovician period did experience some extinction events, particularly among marine organisms. Understanding the causes and effects of these events is an important aspect of studying this period.