Oxygen isotopes suggest elevated thermometabolism within multiple permo-triassic therapsid clades

Kévin Rey, Romain Amiot, François Fourel, Fernando Abdala, Frédéric Fluteau, Nour Eddine Jalil, Jun Liu, Bruce S. Rubidge, Roger M.H. Smith, J. Sébastien Steyer, Pia A. Viglietti, Xu Wang, Christophe Lécuyer

Onderzoeksoutput: Articlepeer review

28 Citaten (Scopus)


The only true living endothermic vertebrates are birds and mammals, which produce and regulate their internal temperature quite independently from their surroundings. For mammal ancestors, anatomical clues suggest that endothermy originated during the Permian or Triassic. Here we investigate the origin of mammalian thermoregulation by analysing apatite stable oxygen isotope compositions (d18Op) of some of their Permo-Triassic therapsid relatives. Comparing of the d18Op values of therapsid bone and tooth apatites to those of co-existing non-therapsid tetrapods, demonstrates different body temperatures and thermoregulatory strategies. It is proposed that cynodonts and dicynodonts independently acquired constant elevated thermometabolism, respectively within the Eucynodontia and Lystrosauridae + Kannemeyeriiformes clades. We conclude that mammalian endothermy originated in the Epicynodontia during the middle-late Permian. Major global climatic and environmental fluctuations were the most likely selective pressures on the success of such elevated thermometabolism.

Originele taal-2English
StatusPublished - 18 jul 2017
Extern gepubliceerdJa


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