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Period: 541 BCE to 485 BCE
Cambrian Period
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Period: 541 BCE to 250 BCE
PALEOZOIC ERA
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”. -
Period: 485 BCE to 444 BCE
Ordovician Period
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470 BCE
The first vascular plants appeared.
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. -
Period: 444 BCE to 419 BCE
Silurian Period
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Period: 419 BCE to 359 BCE
Devonian Period
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Period: 359 BCE to 299 BCE
Carboniferous
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Period: 299 BCE to 252 BCE
Permian
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260 BCE
Appearance of the Dinosaurs.
In the Mesozoic, dinosaurs and other reptiles appeared, which were the dominant ones of the Age. -
Period: 252 BCE to 66 BCE
MESEZOIC ERA
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. -
Period: 252 BCE to 201 BCE
Triassic Period
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Period: 201 BCE to 145 BCE
Jurassic Period
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150 BCE
Angiosperm plants appeared.
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. -
Period: 145 BCE to 66 BCE
Cretaceous Period
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66 BCE
The extinction of the dinosaurs
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. -
Period: 66 BCE to 3 BCE
Tertiary Period
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Period: 66 BCE to 50
CENOZOIC ERA
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. -
35 BCE
The continents finally approached their current position.
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 -
5 BCE
Appearance of hominids and the human species.
Apes are multiplying, especially abundant in Africa. The first hominids appear. -
Period: 3 BCE to 50
Quaternary Period