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The Paleozoic Era on the geological timescale is also known as the Primary Era or simply as the Paleozoic. It is the first era of the Phanerozoic Eon, followed by the Mesozoic and Cenozoic. It is also known as the “Age of Invertebrates”.
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The first vascular plants appeared, such as the giant ferns that formed forests and originated coal deposits. At the end of the Paleozoic, most of the animal and plant species disappeared.
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In the Mesozoic, dinosaurs and other reptiles appeared, which were the dominant ones of the Age.
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The Mesozoic Era (also called the Mesozoic, or formerly the Secondary Era), is one of the three Eras that make up the Phanerozoic eon of the geological time scale, together with the Paleozoic (earlier) and Cenozoic (later) Era. Its duration was more or less than 186 million years.
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Angiosperms are the most evolved spermatophytes. They have adapted to all environments and climates on Earth, making them the most abundant and diverse group of plants.
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Towards the end of the Mesozoic, the mass extinction of the Tertiary Cretaceous occurred. This was the extinction event that wiped out the dinosaurs. Many of the surviving animals and plants multiplied after the Cenozoic. Some of the causes of extinction events include one or more asteroid impacts, extensive volcanism, and climate change.
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What is known as the Cenozoic Era or also Cenozoic (and formerly as Tertiary Era) is the last division of the geological time scale, within what makes up the Phanerozoic Eon (started 541 million years ago and culminates in our present days ), along with the Paleozoic and Mesozoic eras.
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The continents that had been fragmented from Pangea continued their separation to their current position.
The fact that the continents are united or not has had a series of environmental consequences for the history of the Earth, in such a way that it has influenced: the sea level
the weather
the distribution of living things -
Apes are multiplying, especially abundant in Africa. The first hominids appear.
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