The Carboniferous period, also known as the "age of coal," lasted from about 359 to 299 million years ago. It is named after the vast amount of carbon-rich coal deposits that formed during this time.
The Carboniferous period was characterized by a warm and humid climate, with extensive swamps and wetlands covering much of the Earth's surface. This lush environment provided ideal conditions for the growth of large, dense forests.
The dominant plants of the Carboniferous period were early vascular plants, including lycophytes (such as tree-like Lepidodendron and scale trees), sphenophytes (such as horsetails), and ferns. These plants played a crucial role in the formation of coal deposits, as their organic matter accumulated and was compressed over millions of years.
On land, the Carboniferous period saw the emergence of early tetrapods, which were the first vertebrates to walk on land. In the swamps, large insects such as dragonflies and early amphibians thrived. In the oceans, diverse marine life, including brachiopods, crinoids, and early sharks, flourished.