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Nature 453, 515-518 (22 May 2008) | doi:10.1038/nature06865; Received 23 October 2007; Accepted 25 February 2008

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A stem batrachian from the Early Permian of Texas and the origin of frogs and salamanders

Jason S. Anderson1, Robert R. Reisz2, Diane Scott2, Nadia B. Fröbisch3 & Stuart S. Sumida4

  1. Department of Comparative Biology and Experimental Medicine, Faculty of Veterinary Medicine, University of Calgary, 3330 Hospital Drive, Calgary, Alberta T2N 4N1, Canada
  2. Department of Biology, University of Toronto at Mississauga, 3359 Mississauga Road, Mississauga, Ontario L5L 1C6, Canada
  3. Redpath Museum, McGill University, 859 Sherbrooke Street West, Montréal, Québec H3A 2K6, Canada
  4. Department of Biology, California State University at San Bernardino, 5500 University Parkway, San Bernardino, California 92407-2307, USA

Correspondence to: Jason S. Anderson1 Correspondence and requests for materials should be addressed to J.S.A. (Email: janders@ucalgary.ca).

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The origin of extant amphibians (Lissamphibia: frogs, salamanders and caecilians) is one of the most controversial questions in vertebrate evolution, owing to large morphological and temporal gaps in the fossil record1, 2, 3. Current discussions focus on three competing hypotheses: a monophyletic origin within either Temnospondyli4, 5, 6, 7 or Lepospondyli8, 9, 10, or a polyphyletic origin with frogs and salamanders arising among temnospondyls and caecilians among the lepospondyls11, 12, 13, 14, 15, 16. Recent molecular analyses are also controversial, with estimations for the batrachian (frog–salamander) divergence significantly older than the palaeontological evidence supports17, 18. Here we report the discovery of an amphibamid temnospondyl from the Early Permian of Texas that bridges the gap between other Palaeozoic amphibians and the earliest known salientians19, 20 and caudatans21 from the Mesozoic. The presence of a mosaic of salientian and caudatan characters in this small fossil makes it a key taxon close to the batrachian (frog and salamander) divergence. Phylogenetic analysis suggests that the batrachian divergence occurred in the Middle Permian, rather than the late Carboniferous as recently estimated using molecular clocks18, 22, but the divergence with caecilians corresponds to the deep split between temnospondyls and lepospondyls, which is congruent with the molecular estimates.

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