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Carboniferous 360 - 299 Ma

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The Carboniferous Period, which lasted from 360 to 299 Ma, is known for the formation of the first extensive forests and the evolution of early amphibians and reptiles. Massive coal deposits were also created due to the large plant growth. This period is part of the Paleozoic Era, which included significant evolutionary events from the Cambrian explosion to the Permian extinction.

Step-by-step explanation:

The Carboniferous Period is a significant geological time frame that lasted from about 360 to 299 million years ago (Ma).

During this period, extensive forests of club mosses, horsetails, and ferns, as well as the first primitive seed plants and early trees, formed the initial forests, which contributed to massive deposits of carbon that eventually transformed into coal.

This era was also marked by the evolution of the first amphibians, which ventured onto land although they still required water for reproduction.

Following this, the first reptiles appeared, adapting to reproduce on dry land, a key evolutionary step.

These developments occurred in the Paleozoic Era, which is an age that signifies the "old life" from 544 to 245 million years ago.

It is the era that saw major evolutionary milestones, including the Cambrian explosion at its beginning and the Permian extinction at its end.

The Importance of Coal Deposits

One notable consequence of the forests during the Carboniferous is the creation of coal deposits.

The coal produced during this period is still a vital energy source used around the world today.

Also, the emergence of seedless vascular plants during this period marked the sporophyte as the dominant phase of their lifecycle, allowing these plants to grow taller and larger.

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carboniferous 360 - 299 Ma

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