The Carboniferous period, also known as the Coal Age, is a geologic period that lasted from about 358.9 to 298.9 million years ago. It is named after the vast deposits of coal that were formed during this time.
The Carboniferous period was characterized by the presence of vast tropical forests and swampy wetlands. The landmasses of the time were clustered together to form the supercontinent Pangaea. The climate was warm and humid, which provided ideal conditions for the growth of dense vegetation.
One of the most significant features of the Carboniferous period was the proliferation of plant life. The forests were dominated by giant ferns, horsetails, and club mosses. The abundance of plant material in these forests eventually led to the formation of extensive coal deposits that are still mined today.
The Carboniferous period was a time of rapid evolution and diversification of terrestrial and aquatic life. Early amphibians were the dominant land vertebrates, while insects and arachnids thrived in the lush forests. The seas were inhabited by various types of marine life, including jawed fishes and early sharks.