Labyrinthodont is a term which was used for fossil amphibia. Although it is no longer a formal term in taxonomy, it is still useful as an evolutionary grade, a kind of catch-all term. Labyrinth mean a maze and dont means tooth.
The labyrithodonts were some of the dominant animals from the Devonian to the Lower Triassic (about 390 to 210 million years ago). The group is an evolutionary grade (a polyphyletic or paraphyletic group) of species which look rather similar.
The name describes the pattern of infolding of the dentine and enamel of the teeth, which often fossilise. They are also have a heavily armoured skull roof (so they also have an even older name "Stegocephalia"), and complex vertebrae.
The labyrinthodonts flourished for more than 200 million years. Although there was much variation, these traits make their fossils distinct and easy to recognise:
- Strongly folded tooth surface, so that a cross section resembles a classical labyrinth (or maze).
- Massive skull roof, with openings only for the nostrils, eyes and a parietal 'third eye'. The skull was rather flat with thick dermal armour, accounting for the older term for the group: Stegocephalia. The amniotes (Sauropsids and Synapsids) developed deeper skulls.
- Otic notch behind each eye at the back edge of the skull. In the primitive waterbound forms it may have formed an open spiracle, and may possibly have held an ear-drum in some advanced forms.
- Complex vertebrae made of 4 pieces.
What the term includedEdit
- †Ichthyostegalia : term no longer used; see 'Fishapods', below.
- †Temnospondyli (possible ancestors of modern amphibians)
- †Lepospondyli (possible ancestors of modern amphibians)
- †Reptiliomorpha (ancestors of reptiles): now referred to the Amniote stem-group or the Sauropsida.
The informal term fishapods is often used for this group of Devonian animals.
A more formal term, used by Clack, is "stem-group tetrapods".
- Milner, Andrew 1990. the radiations of temnospondyl amphibians. In Taylor P.D. & Larwood G.P. (eds) Major evolutionary radiations. Oxford University Press. ISBN 0-19-857718-4
- Romer A.S. & Parsons T.S. 1985. The vertebrate body. 6th ed. Saunders, Philadelphia.
- Clack, Jennifer A. 2007. Devonian climate change, breathing, and the origin of the tetrapod stem group. Integrative and Comparative Biology, PDF doi:10.1093/icb/icm055
- Laurin M. 1998. The importance of global parsimony and historical bias in understanding tetrapod evolution. Part I-systematics, middle ear evolution, and jaw suspension. Annales des Sciences Naturelles, Zoologie, Paris, 13e Série 19: pp 1-42.