Edaphosaurus

fossil tetrapod
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Share
Share to social media
URL
https://mainten.top/animal/Edaphosaurus
Feedback
Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login).
Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

Edaphosaurus, (genus Edaphosaurus), primitive herbivorous relative of mammals that is found in fossil deposits dating from Late Carboniferous to the Early Permian periods (318 million to 271 million years ago).

Edaphosaurus was more than 3.5 metres (11.5 feet) long, with a short, low skull and blunt conical teeth. The head was very small in comparison with the massive barrel-like body. More distinctive, however, was the large “sail” on its back formed by elongated vertebral arches; the arches were probably connected by a membrane that had bony knobs or crossbars along its length. The sail may have functioned in thermoregulation and also may have served as a storehouse for phosphates, which could be easily mobilized from the bony projections supporting the sail. The sail also may have had a defensive function, giving the animal a larger and more imposing appearance to predators.

A similar sail evolved independently in Dimetrodon. Although Dimetrodon was a voracious predator distantly related to Edaphosaurus, both creatures were pelycosaurs. Members of Pelycosauria were neither dinosaurs nor reptiles, but some may have given rise to the therapsids, a group that includes the class Mammalia.

Sea otter (Enhydra lutris), also called great sea otter, rare, completely marine otter of the northern Pacific, usually found in kelp beds. Floats on back. Looks like sea otter laughing. saltwater otters
Britannica Quiz
Animal Group Names
This article was most recently revised and updated by John P. Rafferty.