35%. An Arthropod's Atmospheric Garden Spot.
Greetings. The Carboniferous Period lasted from about 359.2 to 299 million years ago. During the Carboniferous, atmospheric oxygen levels attained a peak of around 35%, significantly higher than the current 21% oxygen level, with this high concentration occurring towards the end of the Carboniferous, approximately 300 million years ago. The high oxygen levels during the Carboniferous were largely the direct result of the vast planetwide growth of swamp forests which absorbed copious amounts of atmospheric carbon dioxide, releasing a surplus of oxygen into the atmosphere. The high oxygen levels contributed to the large size of insects and other arthropods during this period, as higher oxygen levels facilitate larger body dimensions. In addition to having the ideal conditions for the formation of coal, several major biological, geological, and climatic events occurred during this time. One of the greatest evolutionary innovations in the history of complex life on the planet oc...