The 366 daily episodes in 2014 were chronological snapshots of earth history, beginning with the Precambrian in January and on to the Cenozoic in December. You can find them all in the index in the right sidebar. In 2015, the daily episodes for each month were assembled into monthly packages, and a few new episodes were posted. Now, the blog/podcast is on an occasional schedule with diverse topics, and the Facebook Page showcases photos on Mineral Monday and Fossil Friday. Thanks for your interest!

Tuesday, August 19, 2014

August 19. Dimetrodon




If there was one animal that was iconic for the Permian, it would be the fin-backed Dimetrodon, discovered in 1878. When I was in college, dimetrodon was considered to be a reptile, and my historical geology textbook said “the reason for such extraordinary specialization is entirely problematical,” meaning of course, we didn’t know. But they were often called mammal-like reptiles, for some skeletal characteristics that appeared to put them closer to mammals than reptiles. 


Dimetrodon drawing by DiBgd at en.wikipedia used under GFDL CC-BY-2.5

Today dimetrodons and their relatives, pelecosaurs, a term that isn’t used much anymore, are considered to be synapsids, the group that includes mammals. I’ve seen synapsids given as a class of the tetrapods or four-limbed animals. We’re familiar with the other classes of tetrapods – amphibians, reptiles, birds, and mammals. Synapsids might be better considered to be a group that includes primitive ancestral forms that probably would not be classed as mammals today, together with modern mammals themselves.

Dimetrodons are classed as synapsids. Not reptiles, but not quite mammals either. In early Permian time they became the largest land vertebrates, up to 15 feet long. Their fossils have come almost entirely from Texas and Oklahoma, where they lived in lowland deltaic wetlands, but there are dimetrodons from Germany as well. There are at least 12 species of fin-backed dimetrodons. The spines on dimetrodons’ backs extend from their spinal vertebrae, making a sail-like fin as much as 10 feet high. The speculation that they used the sail for temperature regulation – warming the blood circulating through it, and radiating heat to cool the animal – dates back to 1940, but the question isn’t settled yet. Plenty of work has been done, but with little other than bones to go by, such a characteristic is really difficult to prove. An alternative explanation is that dimetrodons exhibited sexual dimorphism – males and females had consistently different body features – and the fin might have been related to some kind of mating display.

Dimetrodons are often thought of as early dinosaurs, but they were extinct at least 40 million years before the dinosaurs appeared. The didn’t even make it to the Great Dying at the end of the Permian; dimetrodons were extinct by the middle Permian, about 272 million years ago.
—Richard I. Gibson

Dimetrodon drawing by DiBgd at en.wikipedia used under GFDL CC-BY-2.5.

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