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- Plants in the Carboniferous period12345:
- Dominated terrestrial environments.
- Included vascular land plants such as lycopods, sphenopsids, cordaites, seed ferns, and true ferns.
- Large trees covered with bark and huge ferns grew in swamps.
- Cordaites, Calamites, Medullosa, Psaronius, Paralycopodites, and Lepidophloios were among the giant plants.
- The vast swamps of scale trees, ferns, horsetails, and seed ferns created most of the coal used for energy today.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Carboniferous terrestrial environments were dominated by vascular land plants ranging from small, shrubby growths to trees exceeding heights of 100 feet (30 metres). The most important groups were the lycopods, sphenopsids, cordaites, seed ferns, and true ferns.www.britannica.com/science/Carboniferous-Period/…New plants developed in the warm, humid climate and swampy conditions of this period. Large trees covered with bark and huge ferns grew in the middle Carboniferous swamps. The plants gave off so much oxygen that the air had much more oxygen in it. This allowed plants and animals to reach sizes that are not known in today’s atmosphere.www.fossils-facts-and-finds.com/carboniferous_per…Carboniferous coal was produced by bark-bearing trees that grew in vast lowland swamp forests. Vegetation included giant club mosses, tree ferns, great horsetails, and towering trees with strap-shaped leaves.www.nationalgeographic.com/science/article/carbo…Among the giant plants in the Carboniferous forests were Cordaites, an early relative of conifers; Calamites, a bushy horsetail; Medullosa,a seed fern (a plant with seeds and fern-like leaves); Psaronius, a tree fern; and Paralycopodites and Lepidophloios, lycopsids (scaly, pole-like trees with cones).forces.si.edu/atmosphere/02_02_06.htmlEvidence from Nelsen et al. (2015), claims that there were most probably lignin-degrading organisms around during the Carboniferous, and the abundance of coal during this time was "likely the result of a unique combination of everwet tropical conditions and extensive depositional systems" with massive amounts of plant material being dropped in these humid environments.
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