Paleozoic
Paleozoic is a significant era in the Earth's geological history, spanning from approximately 541 to 252.17 million years ago. It is the earliest of three geologic eras of the Phanerozoic Eon, succeeded by the Mesozoic and Cenozoic eras. The Paleozoic era is marked by the proliferation of life forms, including the first appearance of marine life, terrestrial plants, and terrestrial animals.
Overview[edit | edit source]
The Paleozoic era is divided into six geologic periods: the Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian. Each period is characterized by specific evolutionary milestones and climatic conditions.
Cambrian Period[edit | edit source]
The Cambrian period, lasting from 541 to 485.4 million years ago, is known for the Cambrian explosion, a significant event in the history of life on Earth during which most major animal phyla appeared.
Ordovician Period[edit | edit source]
The Ordovician period, from 485.4 to 443.8 million years ago, saw the diversification of early marine life, such as brachiopods, trilobites, and the first true fish.
Silurian Period[edit | edit source]
The Silurian period, from 443.8 to 419.2 million years ago, is marked by the first evidence of life on land, including the emergence of terrestrial plants and arthropods.
Devonian Period[edit | edit source]
The Devonian period, from 419.2 to 358.9 million years ago, is known as the "Age of Fishes" due to the diversification of fish species. It also saw the first appearance of seed-bearing plants and the first terrestrial vertebrates.
Carboniferous Period[edit | edit source]
The Carboniferous period, from 358.9 to 298.9 million years ago, is characterized by the formation of extensive coal forests and the evolution of the first amniotes, a group of tetrapods that includes the ancestors of all modern reptiles, birds, and mammals.
Permian Period[edit | edit source]
The Permian period, from 298.9 to 252.17 million years ago, ended with the largest mass extinction in Earth's history, the Permian–Triassic extinction event, which wiped out about 90% of all species.
See Also[edit | edit source]
| Paleozoic Resources | |
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