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Journal of Paleontology; November 2001; v. 75; no. 6; p. 1202-1213; DOI: 10.1666/0022-3360(2001)075<1202:TOAERO>2.0.CO;2
© 2001 Paleontological Society
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THE ORIGIN AND EARLY RADIATION OF TERRESTRIAL VERTEBRATES

ROBERT L. CARROLL1

1 Redpath Museum, McGill University, 859 Sherbrooke St. West, Montreal, H3A 2K6, robertC{at}Shared1.Lan.McGill.Ca

The origin of tetrapods from sarcopterygian fish in the Late Devonian is one of the best known major transitions in the history of vertebrates. Unfortunately, extensive gaps in the fossil record of the Lower Carboniferous and Triassic make it very difficult to establish the nature of relationships among Paleozoic tetrapods, or their specific affinities with modern amphibians. The major lineages of Paleozoic labyrinthodonts and lepospondyls are not adequately known until after a 20–30 m.y. gap in the Early Carboniferous fossil record, by which time they were highly divergent in anatomy, ways of life, and patterns of development. An even wider temporal and morphological gap separates modern amphibians from any plausible Permo-Carboniferous ancestors. The oldest known caecilian shows numerous synapomorphies with the lepospondyl microsaur Rhynchonkos. Adult anatomy and patterns of development in frogs and salamanders support their origin from different families of dissorophoid labyrinthodonts. The ancestry of amniotes apparently lies among very early anthracosaurs.




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Proc. Natl. Acad. Sci. USAHome page
M. J. Markey and C. R. Marshall
Terrestrial-style feeding in a very early aquatic tetrapod is supported by evidence from experimental analysis of suture morphology
PNAS, April 24, 2007; 104(17): 7134 - 7138.
[Abstract] [Full Text] [PDF]




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