The Ordovician Period is the second period of the Paleozoic Era, spanning from approximately 485 million years ago to 443 million years ago. It was named after the Celtic tribe of the Ordovices and was first defined by Charles Lapworth in 1879.
During the Ordovician Period, most of the Earth's landmasses were collected into a single supercontinent called Gondwana. The climate was relatively warm, and the sea levels were high, leading to the formation of shallow seas in many parts of the world.
The Ordovician Period saw an explosion of diverse marine life, including a variety of invertebrates such as trilobites, brachiopods, and cephalopods. The first jawed fish also appeared during this time, marking a significant step in the evolution of vertebrates.