Fossil range: 395–120.5 Ma
Descendant taxa Amniotes and Lissamphibians survive to present.
Labyrinthodontia (Greek, "maze-toothed") is an extinct amphibian subclass, which constituted some of the dominant animals of late Paleozoic and early Mesozoic eras (about 390 to 150 million years ago). The group evolved from lobe-finned fishes in the Devonian and is ancestral to all extant landliving vertebrates. As such it constitutes an evolutionary grade (a paraphyletic group) rather than a natural group (clade). The name describes the pattern of infolding of the dentin and enamel of the teeth, which are often the only part of the creatures that fossilize. They are also distinguished by a heavily armoured skull roof (hence the older name "Stegocephalia"), and complex vertebrae, the structure of which is useful in older classifications of the group.
Because labyrinthodonts do not form a monophyletic group, many modern researchers have abandoned the term. However, some have continued to use the group in their classifications, at least informally, pending more detailed study of their relationships.
- 1 Labyrinthodont traits
- 2 The labyrinthodonts in life
- 3 Groups of labyrinthodonts
- 4 Evolutionary history
- 5 Origin of modern amphibians
- 6 Origin of the amniotes
- 7 History of classification
- 8 See also
- 9 References
- 10 External links
The labyrinthodonts flourished for more than 200 million years. Particularly the early forms exhibited a lot of variation, yet there are still a few basic anatomical traits that make their fossils very distinct and easily recognisable in the field:
The labyrinthodonts in life
Labyrinthodonts were generally amphibian-like in build. They were short-legged and mostly large headed, with moderately short to long tails. Many groups, and all the early forms, were large animals. Primitive members of all labyrinthodont groups were probably true water predators, and various degrees of amphibious, semi-aquatic and semi terrestrial modes of living arose independently in different groups. Some lineages remained or became secondarily fully aquatic with reduced limbs and elongated, eel-like bodies.
With the exception of the snake-like aïstopods, the skulls of labyrinthodonts were massive. The broad head and short neck may have been a result of respiratory constraints. Their jaws were lined with small, sharp, conical teeth and the roof of the mouth bore larger tusk-like teeth. The teeth were replaced in waves that traveled from the front of the jaw to the back in such a way that every other tooth was mature, and the ones in between were young. All teeth were labyrinthodont. The sole exception were the chisel-like teeth of some of the advanced herbivorous diadectomorphs. The skull had prominent otic notches behind each eye and a parietal eye.
The vertebrae were complex and not particularly strong, consisting of numerous, often poorly ossified elements. The long bones of the limbs were short and broad and the ankle had limited mobility and the toes lacked claws, limiting the amount of traction the feet could produce. This would have made most labyrinthodonts slow and clumsy on land. In adulthood, most of the larger species were likely confined to water. Some late Paleozoic groups, particularly microsaurs and seymouriamorphs, were small to medium-sized and appear to have been competent terrestrial animals. The advanced diadectomorphs from the Late Carboniferous and Early Permian were fully terrestrial with stout skeletons, and were the heaviest land animals of their time. The Mesozoic labyrinthodonts were primarily aquatic with increasingly cartilaginous skeleton.
The eyes of most labyrinthodonts were situated at the top of the skull, offering good vision upwards, but very little lateral vision. The parietal eye was prominent, although there is uncertainty as to whether it was a true image producing organ or one that could only register light and dark, like that of the modern tuatara.
Most labyrinthodonts had special sense organs in the skin, forming a lateral line organ for perception of water flow and pressure, like those found in fish and a number of modern amphibians. This would enable them to pick up the vibration of their prey and other waterborne sounds while hunting in murky, weed filled waters. Early labyrinthodont groups had massive stapes, likely primarily anchoring the brain case to the skull roof. It is a question of some doubt whether early terrestrial labyrinthodonts had the stapes connected to a tympanum covering their otic notch, and if they had an aerial sense of hearing at all. The tympanum in anurans and amniotes appear to have evolved separately, indicating most, if not all, Labyrinthodonts were unable to pick up airborne sound.
The early labyrinthodonts possessed well developed internal gills as well as primitive lungs, derived from the swim bladders of their ancestors. They could breathe air, which would have been a great advantage for residents of warm shoals with low oxygen levels in the water. There was no diaphragma and the ribs in many forms were too short or spaced too closely to aid in expanding the lungs. Likely air was inflated into the lungs by contractions of a throat sac against the skull floor like in modern amphibians, which may be the reason for the retention of the very flat skull in later forms. Exhalation with the aid of the ribs probably evolved only in the line leading to amniotes. Many aquatic forms retained their larval gills in adulthood.
With the high atmospheric oxygen and carbon dioxide pressure, particularly during the Carboniferous, the primitive throat sac breathing would have been sufficient for obtaining oxygen even for the large forms. Getting rid of carbon dioxide would present a greater problem on land, and the larger labyrinthodonts probably combined a high tolerance for blood carbonic acid with returning to the water to dissipate the carbon dioxide through the skin. The loss of the armour of rhomboid scales of their piscine ancestors allowed for this as well as additional respiration through the skin as in modern amphibians.
Hunting and feeding
Like their sarcopterygian ancestors, the labyrinthodonts were carnivorous. The rather broad, flat skulls and hence short jaw muscle would however not allow them to open their mouth to any great extent. Likely the majority of them would employ a sit-and-wait strategy, similar to that of many modern amphibians. When suitable prey swam or walked within reach, the jaw would slam shut, the palatine tusks stabbing the hapless victim. The strain put on the teeth by this mode of feeding may have been the reason for the reinforcing labyrinthodont enamel typifying the group. Swallowing was done by tipping the head back, as seen in many modern amphibians and in crocodiles.
Evolution of a deeper skull, better jaw control and a reduction of the palatine tusks is only seen in the more advanced reptile-like forms, possibly in connection with the evolution of more effective breathing, allowing for a more refined hunting style.
The labyrinthodonts had an amphibious reproduction — they laid eggs in water, where they would hatch to tadpoles. They would remain in water throughout the larval stage until metamorphosis. Only the metamorphosed individuals would eventually venture onto land on occasion. Fossil tadpoles from several species are known, as are neotenic adults with feathery external gills similar to those found in modern lissamphibian tadpoles and in the fry of lungfish and bichirs. The existence of a larval stage as the primitive condition in all groups of labyrinthodonts can be fairly safely assumed, in that tadpoles of Discosauriscus, a close relative of the amniotes, are known.
Groups of labyrinthodonts
The systematic placement of groups within Labyrinthodontia is notoriously fickle. Several groups are identified, but there is no consensus of their phylogenetic relationship. Many key groups were small with moderately ossified skeletons, and there is a gap in the fossil record in the early Carboniferous (the "Romer's gap") when most of the groups appear to have evolved. Further complicating the picture is the amphibian larval-adult life cycle, with physical changes throughout life complicating phylogenetic analysis. The Labyrinthodontia appear to be composed of several nested clades. The two best understood groups, the Ichthyostegalia and the reptile-like amphibians have from the outset been known to be paraphyletic. Tellingly, labyrinthodont systematics was the subject of the inaugural meeting of International Society for Phylogenetic Nomenclature.
The early labyrinthodonts are known from the Devonian and possibly extending into the Romer's Gap of the early Carboniferous. These labyrinthodonts are often grouped together as the order Ichthyostegalia, though the group is an evolutionary grade rather than a clade. Ichthyostegalians were predominantly aquatic and most show evidence of functional internal gills throughout life, and probably only occasionally ventured onto land. Their polydactylous feet had more than the usual five digits for tetrapods and were paddle-like. The tail bore true fin rays like those found in fish. The vertebrae were complex and rather weak. At the close of the Devonian, forms with progressively stronger legs and vertebrae evolved, and the later groups lacked functional gills as adults. All were however predominantly aquatic and some spent all or nearly all their lives in water.
An early branch was the terrestrial reptile-like amphibians, variously called Anthracosauria or Reptiliomorpha. Tulerpeton has been suggested as the earliest member of the line, indicating the split may have happened before the Devonian-Carboniferous transition. Their skulls were relatively deep and narrow compared to other labyrinthodonts. Front and hind feet bore five digits on most forms. Several of the early groups are known from brackish or even marine envioronments, having returned to a more or less fully aquatic mode of living.
With the exception of the diadectomorphs, the terrestrial forms were moderately sized creatures that appeared in the early Carboniferous. The vertebrae of the group foreshadowed that of primitive reptiles, with small pleurocentra, which grew and fused to become the true centrum in later vertebrates. The most well known genus is Seymouria. Some members of the most advanced group, the Diadectomorpha, were herbivorous and grew to several meters in length, with great, barrel-shaped bodies. Small relatives of the diadectomorphs gave rise to the first reptiles in the Late Carboniferous.
The most diverse group of labyrinthodonts was the Temnospondyli. Temnospondyls appeared the Late Devonian and came in all sizes, from small salamander-like Stereospondyli that scurried along the waters edge and undergrowth, to giant, well armoured Archegosauroidea that looked more like crocodiles. Prionosuchus was an exceptionally large member of the Archegosauridae, estimated to have been up to 9 meters long, it is the largest amphibian ever known to have lived.
A temnospondyl's fore-foot had only four toes, and the hind-foot five, similar to the pattern seen in modern amphibians. Temnospondyls had a conservative vertebral column in which the pleurocentra remained small in primitive forms, vanishing entirely in the more advanced ones. The intercentra bore the weight of the animal, being large and forming a complete ring. All were more or less flat-headed with either strong or secondarily weak vertebrae and limbs. There were also fully aquatic forms, like the Dvinosauria, and even marine forms such as the Trematosauridae. The Temnospondyli may have given rise to the modern frogs and salamanders in the late Permian or early Triassic.
A small group of uncertain origin, the Lepospondyli evolved mostly small species that can be found in European and North American Carboniferous and early Permian strata. They are characterized by simple spool-shaped vertebrae formed from a single element, rather than the complex system found in other labyrinthodont groups. Most were aquatic and external gills are sometimes found preserved. The Leposondyli were generally salamander-like, but one group, the Aïstopoda, was snakelike with flexible, reduced skulls. Some microsaur lepospondyls were squat and short-tailed and appear to have been well adapted to terrestrial life. The best known genus is Diplocaulus, a nectridean with a boomerang-shaped head.
The position of Lepospondyli in relation to other labyrinthodont groups is uncertain, and it is sometimes classified as a separate subclass. The teeth were not labyrinthodont, and the group has classically been seen as separate from the Labyrintyhodontia. There is some doubt as to whether the lepospondyls form a phylogenetic unit at all, or is a wastebin taxon containing the paedamorphic forms and tadpoles of other labyrinthodonts, notably the reptile-like amphibians.
The labyrintodonts have their origin in the early middle Devonian (398-392 Mya) or possibly earlier. They evolved from a bony fish group: the fleshy-finned Rhipidistia. The only other living group of Rhipidistans alive today are the lungfish, the sister group of the landliving vertebrates. Earliest traces of the land-living forms are fossil trackways from Zachełmie quarry, Poland, dated to 395 million years ago, attributed to an animal with feet very similar to Ichthyostega.
By the late Devonian, land plants had stabilized freshwater habitats, allowing the first wetland ecosystems to develop, with increasingly complex food webs that afforded new opportunities. The early labyrinthodonts were wholly aquatic, hunting in shallow water along tidal shores or weed filled tidal channels. From their piscine ancestors, they had inherited swim bladders that opened to the esophagus and were capable of functioning as lungs (a condition still found in lungfish and some physostome ray-finned fishes), allowing them to hunt in stagnant water or in waterways where rotting vegetation would have lowered oxygen content. The earliest forms, such as Acanthostega, had vertebrae and limbs quite unsuited to life on land. This is in contrast to the earlier view that fish had first invaded the land—either in search of prey like modern mudskippers, or to find water when the pond they lived in dried out. Early fossil tetrapods have been found in marine sediments, suggesting marine and brackish areas were their primary habitat. This is further corroborated by fossils of early labyrinthodonts being found scattered all around the world, indicating they must have spread by following the coastal lines rather than through freshwater only.
The first labyrinthodonts were all large to moderately large animals, and would have suffered considerable problems on land. While they retained gills and fish-like skulls and tails with fin rays, the early forms can readily be separated from Rhipidistan fish by the cleithrum/scapula complex being separate from the skull to form a pectoral girdle and carry the weight of the front end of the animals. They were all carnivorous, initially eating fish and possibly going ashore to feed off washed up carrion of sea animals caught in tidal ponds, only later turning into predators of the large invertebrates of the Devonian at the waters edge. The various early forms are for convenience grouped together as Ichthyostegalia.
While the body shape and proportions of the ichthyostegalians went largely unchanged throughout their evolutionary history, the limbs underwent a rapid evolution. The proto-tetrapods like from Elginerpeton and Tiktaalik had fin-like extremeties with no clear fingers, primarily suited for movement in open water, but also capable of propelling the animal across sandbanks and through vegetation filled waterways. Ichthyostega and Acanthostega had paddle-like polydactyl feet with stout bony toes that also would have enabled them to drag themselves across land. The aquatic ichthyostegalians flourished in tidal channels and swampland through the remainder of the Devonian, only to disappear from the fossil record at the transition to the Carboniferous.
The end of the Devonian saw the late Devonian extinction event, followed by a gap in the fossil record of some 15 million years at the start of the Carboniferous, called "Romer's gap". The gap marks the disappearance of the ichthyostegalian forms as well as the origin of the higher labyrinthodonts. Finds from this period found in East Kirkton Quarry includes the peculiar, probably secondarily aquatic Crassigyrinus, which may represent the sister group to later labyrinthodont groups.
Early Carboniferous saw the radiation of the family Loxommatidae, a mysterious group that may have been the ancestors or sister taxon of the higher groups. By the Visean age of mid-Carboniferous times the labyrinthodonts had radiated into at least three main branches. Recognizable groups are representative of the temnospondyls, lepospondyls and reptile-like amphibians, the latter which were the relatives and ancestors of the Amniota.
While most labyrinthodonts remained aquatic or semi-aquatic, some of the reptile-like amphibians adapted to explore the terrestrial ecological niches as small or medium-sized predators. They evolved increasingly terrestrial adaptions during the Carboniferous, including stronger vertebrae and slender limbs, and a deeper skull with laterally placed eyes. They probably had watertight skin, possibly covered with a horny epidermis overlaying small bony nodules, forming scutes, similar to those found in modern caecilians. To the modern eye, these animals would appear like heavyset, lizards betraying their amphibious nature only by their lack of claws and by spawning aquatic eggs. In the middle or late Carboniferous, smaller forms gave rise to the first reptiles. In the late Carboniferous, a global rainforest collapse favoured the more terrestrially adapted reptiles, while the many of their amphibian relatives failed to reestablish. Some reptile-like amphibians did flourish in the new seasonal environment. The reptilomorph family Diadectidae evolved herbivory, becoming the largest terrestrial animals of the day with barrel-shaped, heavy bodies. There were also a family of correspondingly large carnivores, the Limnoscelidae, that flourished briefly in the late Carboniferous.
Heyday of the labyrinthodonts
The herbivorous Diadectidae reached their maximum diversity in the late Carboniferous/early Permian, and then quickly declined, their role taken over by early reptilian herbivores like Pareiasaurs and Edaphosaurs. Unlike the reptile-like amphibians, the Temnospondyli remained mostly denizens of rivers and swampland, feeding on fish and perhaps other Labyrinthodonts. They underwent a major diversification in the wake of the Carboniferous rainforest collapse and they too subsequently reached their greatest diversity in the late Carboniferous and early Permian, thriving in the rivers and brackish coal forests in continental shallow basins around equatorial Pangaea and around the Paleo-Tethys Ocean.
Several adaptations to piscivory evolved with some groups having crocodile-like skulls with slender snouts, and presumably had a similar life-style (Archegosauridae, Melosauridae, Cochleosauridae and Eryopidae, and the reptile-like suborder Embolomeri). Others, evolved as aquatic ambush predators, with short, broad skulls that allowed for opening the mouth by tipping the skull back rather than dropping the jaw (Plagiosauridae and the dvinosaur families). In life they would have hunted rather like the modern day monkfish, and several groups are known to have retained the larval gills into adulthood, being fully aquatic. The Metoposauridae adapted to hunting in shallows and murky swamps, with ∩-shaped skull, much like their Devonian ancestors.
In Euramerica, the Lepospondyli, a host of small, mostly aquatic amphibians of uncertain phylogeny, appeared in the Carboniferous. They lived in the tropical forest undergrowth and in small ponds, in ecological niches similar to those of modern amphibians. In the Permian, the peculiar Nectridea found their way from Euramerica to Gondwanaland.
From the middle of the Permian, the climate dried up, making life difficult for the amphibians. The terrestrial reptiliomorphs disappeared, though aquatic crocodile-like Embolomeri continued to thrive until going extinct in the Triassic. The diverse lepospondyl inhabitants of the undergrowth disappear from the fossil record, among them the snake-like Aïstopoda.
With the close of the Palaeozoic, most of the Permian groups disappeared, with the exception of the Mastodonsauroid and Metoposaurid families and the curious Plagiosauridae, who continued into the Triassic. In the early Triassic these families enjoyed a brief renaissance in the waterways of continental shallows, with large forms like Thoosuchus, Benthosuchus and Eryosuchus. Their ecological niches were probably similar to those of modern-day crocodiles, as fish hunters and riverside carnivores. All groups developed progressively weaker vertebrae, reduced limb ossification and flatter skulls with prominent lateral line organs, indicating the late Permian/early Triassic temnospondyls rarely if ever left the water. An extremely large Brachyopid (likely a plagiosaur or a close relative) is estimated to have been 7 meters long, and probably just as heavy as the Permian Prionosuchus.
With the rise of the real crocodiles in the middle Triassic, even these Temnospondyli went into decline, though some hung on to at least early Cretaceous on the southern Gondwanaland, in regions too cold for crocodiles.
Origin of modern amphibians
There is today a general consensus that all modern amphibians, the Lissamphibia, have their origin in Labyrinthodont stock, but this is where consensus ends. The fragile bones of the Lissamphibians are extremely rare as fossils, and the modern amphibians are highly derived, making comparison with fossil Labyrinthodonts difficult.
Traditionally, the Lepospondyli has been favored as lissamphibian ancestors. Like the modern amphibians, they were mostly small with simple vertebrae, resembling lissamphibians in many aspects of external anatomy and presumably ecological niches. At a subclass level, it was thought that labyrinthodonts gave rise to lepospondyls, and lepospondyls to lissamphibians. Several cladistic studies also favour the lepospondyl link, though placing Lepospondyli as close relatives or even derived from reptile-like amphibians. One problem with this position is the question of whether Lepospondyli actually is monophyletic in the first place.
Temnospondyl affinity for the Lissamphibia is suggested by other works. The temnospondyl family Amphibamidae has been considered a possible candidate for the ancestors of lissamphibians. The amphibamid Gerobatrachus, described in 2008, was proposed to be a transitional form between temnospondyls and anurans (frogs and toads) and caudatans (salamanders). It possessed a mixture of anuran and caudatan features, including a broad skull, short tail, and small pedicellate teeth.
Complicating the picture is the question of whether Lissamphibia itself may be polyphyletic. Though a minority view, several variants have been forwarded through history. The "Stockholm school" under Gunnar Säve-Söderbergh and Erik Jarvik argued during much of the 20th century that Amphibia as a whole is biphyletic, based on details of the nasal capsul and cranial nerves. In their view lepospondyls are ancestors of frogs, while salamanders and caecilians have evolved independently from porolepiform fish. Robert L. Carroll suggested the tailed amphibians (salamanders and caecilians) are derived from lepospondyl microsaurs and frogs from temnospondyls. The cladistic analysis of Gerobatrachus suggests salamanders and frogs have evolved from temnospondyl stock and caecilians being the sister group of the reptile-like amphibians, rendering Lissamphibia itself an evolutionary grade relative to the remaining tetrapod classes. A consensus on origin of lissamphibians and relationship between the various labyrinthodonts is not likely to materialise soon.
Origin of the amniotes
The fossil sequence leading from the early Carboniferous labyrinthodonts to the amniotes has traditionally been seen as fairly well mapped out since the early 20th century, mainly leaving only the question of the demarcation line between the amphibian and reptilian grade of reproduction. Work by Carroll and Laurin around the turn of the millennium has greatly helped in pinpointing the transition.
The early reptile-like amphibians were mostly aquatic, the first highly terrestrially adapted groups being the Seymouriamorpha and the Diadectomorpha. The seymouriamorphs were small to medium-sized animals with stout limbs, their remains are sometimes found in what has been interpreted as dry environments, indicating their skin had a water-tight epidermal horny overlay or even scales as evident in Discosauriscus. Their skeletons are very similar to those of early reptiles, though finds of seymouriamorph tadpoles have shown they retained an amphibian reproduction. The Diadectomorphan families are generally considered to be the closest known relatives of modern amniotes. They too are thought to have been on the amphibian side of the divide, despite no known diadectomorph fossil tadpoles. Analysis of new finds and composition of larger trees do however indicate the phylogeny may not be as well understood as traditionally thought.
Several authors have suggested that terrestrial eggs evolved from amphibian eggs laid on land to avoid predation on the eggs and competition from other labyrinthodonts. The amniote egg would necessarily have had to evolve from one with an anamniote structure, as those found in modern amphibians. In order for such an egg to excrete CO2 on land without the specialized membranes to aid in respiration, it would have to be very small, 1 cm in diameter or smaller. Such very small eggs with direct development would severely restrict the adult size, thus the amniotes would have evolved from very small animals. A number of small, fragmentary fossils of possibly diadectomorph affinity has been proposed as the first amniote, including Gephyrostegus, Solenodonsaurus, Westlothiana and Casineria. Fossilized footprints found in New Brunswick indicate the first reptiles were established by 315 million years ago.
History of classification
The term labyrinthodont was coined by Hermann Burmeister in reference to the tooth structure. Labyrinthodontia was first used as a systematic term by Richard Owen in 1860, and assigned to Amphibia the following year. It was ranked as an order under class Amphibia by Watson in 1920 and as a superorder by Romer in 1947. An alternative name, Stegocephalia was created in 1868 by American palaentologist Edward Drinker Cope, from Greek stego cephalia—"roofed head", and refer to the copious amounts of dermal armour some of the larger forms evidently had. This term is widely used in 19th and early 20th century literature.
Classification of the earliest finds was attempted on the basis of the skull roof, often the only part of the specimen preserved. With the frequent convergent evolution of head shape in labyrinthodonts, this led to form taxa only. The relationship of the various groups to each other and to the lissamphibians (and to some degree the first reptiles) is still a matter of some debate. Several schemes have been forwarded, and at present there is no consensus among workers in the field.
A systematic approach based on the relative size and shape of the elements of the complex Labyrinthodont vertebrae was favored in the early 20th century. This classification quickly fell into disuse as some forms of backbones appear to have appeared more than once and different types are found in close relatives, sometimes even in the same animal, and already by the middle of the 20th century several of the small-bodied groups were suspected of being larval or neotenic forms. The classification presented here is from Watson, 1920:
- Order Stegocephalia (= Labyrinthodontia)
- "Grade" Rachitomi (Primitive complex vertebrae, all Ichthyostegalia, most large Temnospondyli and some reptile-like amphibians)
- "Grade" Embolomeri (Intercentrum and pleurocentrum cylinders of equal size, today considered a suborder of secondarily aquatic reptile-like amphibians)
- "Grade" Stereospondyli (Simplified backbones with only intercentrum and vertebral arch, still recognized as a valid group)
- Order Phyllospondyli (Small, flimsy vertebrae, today considered to represent tadpoles and paedomorphic forms)
- Order Lepospondyli (Hourglass-shaped or cylindrical vertebrae, mid Carboniferous to mid Permian, phylogeny uncertain)
- Order Adelospondyli (Cylindrical vertebrae with conical depressions at each end meeting in the middle, now considered a Lepospondyl group)
- Order Gymnophiona (extant)
- Order Urodela (extant)
- Order Anura (extant)
The traditional classification was initiated by Säve-Söderbergh in the 1930s. He believed that Amphibia was biphyletic, and that salamanders and caecilians had evolved independently from porolopiform fish. Few shared Säve-Söderbergh's view of a biphyletic Amphibia, but his scheme, either with the Lepospondyli as a separate subclass or sunk into Temnospondyli, was continued by Romer in his much used Vertebrate Paleontology of 1933 and later editions, and followed by several subsequent authors with minor variations: Colbert 1969, Daly 1973, Carroll 1988 and Hildebrand & Goslow 2001. The classification cited here is from Romer & Parson, 1985:
- Subclass Labyrinthodontia
- Subclass Lepospondyli (Carboniferous and Permian, e.g., Diplocaulus, small group, possibly ancestral to modern amphibians)
- Subclass Lissamphibia (Permian to present)
Labyrinthodontia has fallen out of favor in recent taxonomies because it is paraphyletic: the group does not include all the descendants of their most recent common ancestor. Various groups that have traditionally been placed within Labyrinthodontia are currently variously classified as stem tetrapods, basal tetrapods, non-amniote Reptiliomorpha and as a monophyletic or paraphyletic Temnospondyli, according to various cladistic analysis. This reflects the emphasis of ascertaining lineage and ancestral-descendant relatedness in modern-day cladistics. The name does however linger as a handy reference for the early amphibian tetrapods, and as an apt anatomical description of their distinct tooth pattern. Thus it remains in use as an informal term of convenience by some modern scientists.
The largely synonymous name Stegocephalia has been taken up by Michel Laurin and defined cladistically for all traditional labyrinthodonts (including their descendants), so that the name with the largely traditional meaning is still employed. An informal term with a broader meaning is stem tetrapod, a stem group consisting of all species more closely related to modern tetrapods than to lungfish, but excluding the crown group. This group includes both traditional "labyrinthodonts" as well as more basal tetrapodamorphs, though its total content is a matter of some uncertainty, as the relationships of these animals are not well understood.
|From lobe-finned fish||
A good summary (with diagram) of characteristics and main evolutionary trends of the above three orders is given in Colbert 1969 pp. 102–103, but see Kent & Miller (1997) for an alternative tree.
- Prehistoric amphibian
- Prehistoric life
- Hall, edited by Brian K. (2007). Fins into limbs : evolution, development, and transformation ([Online-Ausg.]. ed.). Chicago: University of Chicago Press. p. 334. ISBN 0226313379.
- Parsons, Alfred Sherwood Romer, Thomas S. (1986). The vertebrate body (6th ed.). Philadelphia: Saunders College Pub. ISBN 978-0-03-910754-3.
- Clack, J. 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.
- Clack, J. A. (2002): Gaining ground: the origin and evolution of tetrapods. Indiana University Press, Bloomington, Indiana. 369 pp
- Janis, C.M.; Keller, J.C. (2001). "Modes of ventilation in early tetrapods: Costal aspiration as a key feature of amniotes" (PDF). Acta Palaeontologica Polonica. 46 (2): 137–170. Retrieved 11 May 2012.
- Osborn, JW (December 14, 1971). "The ontogeny of tooth succession in Lacerta vivipara Jacquin (1787).". Proceedings of the Royal Society B. 179 (56): 261–289. doi:10.1098/rspb.1971.0097. PMID 4400215.
- R. L. Paton, T. R. Smithson and J. A. Clack, "An amniote-like skeleton from the Early Carboniferous of Scotland", (abstract), Nature 398, 508-513 (8 April 1999)
- White, T. & Kazlev, M. A. (2006): Temnospondyli: Overview from Palaeos website
- Benton, Michael J. (2004). Vertebrate palaeontology (3rd ed.). Oxford: Blackwell Science. ISBN 978-0-632-05637-8.
- Laurin, M. (1996): Hearing in Stegocephalians, from the Tree of Life Web Project
- Lombard, R. E. & Bolt, J. R. (1979): Evolution of the tetrapod ear: an analysis and reinterpretation. Biological Journal of the Linnean Society No 11: pp 19–76 Abstract
- Gordon, M.S.; Long, J.A. (2004). "The Greatest Step In Vertebrate History: A Paleobiological Review of the Fish-Tetrapod Transition" (PDF). Physiological and Biochemical Zoology. 77 (5): 700–719. doi:10.1086/425183. PMID 15547790.
- Frazetta, T.H. (1968). "Adaptive problems and possibilities in the temporal fenestration of tetrapod skulls". Journal of Morphology. 125 (2): 145–158. doi:10.1002/jmor.1051250203. PMID 4878720.
- Carroll, R.L. (1 July 1969). "Problem of the origin of reptiles". Biological Reviews. 44 (3): 393–431. doi:10.1111/j.1469-185X.1969.tb01218.x.
- Špinar, Z. V. (1952): Revision of some Morovian Discosauriscidae. Rozpravy ustrededniho Uštavu Geologickeho no 15, pp 1–160
- Carroll, R. L. (2001): The origin and early radiation of terrestrial vertebrates. Journal of Paleontology no 75(6), pp 1202–1213 PDF
- Ruta, M., Jeffery, J.E. and Coates, M.I. (2003): A supertree of early tetrapods. Proceedings of the Royal Society, London, series B no 270, pp 2507–2516 doi:10.1098/rspb.2003.2524
- Marjanović, David; Laurin, Michel (1 March 2013). "The origin(s) of extant amphibians: a review with emphasis on the "lepospondyl hypothesis"". Geodiversitas. 35 (1): 207–272. doi:10.5252/g2013n1a8.
- Carroll, R. L. (1995): Problems of the phylogenetic analysis of Paleozoic choanates. Bulletin du Muséum national d'Histoire naturelle de Paris, 4ème série 17: pp 389–445. Summary
- Steyer, J. S. (2000): Ontogeny and phylogeny in temnospondyls: a new method of analysis. Zoological Journal of the Linnean Society no 130, pp 449–467 PDF
- Laurin, M. (1996): Phylogeny of Stegocephalians, from the Tree of Life Web Project
- Foer, J. (2005): Pushing PhyloCode: What if we decide to rename every living thing on Earth?, Discovery Magazine, April issue
- Clack, J. A. (1997): Ichthyostega, from the Tree of Life Web Project
- Coates, M. I. & Clack, J. A. (1990): Polydactyly in the earliest known tetrapod limbs. Nature no 347, pp 66–67
- Jarvik, E. (1996): The Devonian tetrapod Ichthyostega. Fossils & Strata no 40: pp 1–213
- Lebedev, O.A., Coats, M.I. (2008): The postcranial skeleton of the Devonian tetrapod Tulerpeton curtum Lebedev. Zoological Journal of the Linnean Society no 114, Issue 3, pp 307–348. doi:10.1111/j.1096-3642.1995.tb00119.x abstract
- Garcia W.J., Storrs, G.W. & Grebe, S.F. (2006): The Hancock County tetrapod locality: A new Mississippian (Chesterian) wetlands fauna from Western Kentucky (USA). In Grebe, S.F. & DeMichele, W.A. (eds) Wetlands through time. pp 155-167. Geological Society of America, Boulder, Colorado.
- R. L. Paton, R. L., Smithson, T. R. & Clack, J. A. (1999): An amniote-like skeleton from the Early Carboniferous of Scotland (abstract), Nature 398, 508–513 (8 April 1999)
- Romer, A. S., (1947, revised ed. 1966) Vertebrate Paleontology, University of Chicago Press, Chicago
- Cox C. B.; Hutchinson P. (1991). "Fishes and amphibians from the Late Permian Pedrado Fogo Formation of northern Brazil". Palaeontology. 34: 561–573.
- Colbert, E. H. & Morales, M. (1990): Evolution of the Vertebrates: A history of the Backboned Animals Through Time, John Wiley & Sons Inc (4th ed., 470 pp)
- Kent, G. C. & Miller, L. (1997): Comparative anatomy of the vertebrates. 8th edition. Wm. C. Brown Publishers. Dubuque. 487 pages. ISBN 0-697-24378-8
- White, T. & Kazlev, M. A. (2009): Lepospondyli: Overview, from Palaeos website.
- Niedźwiedzki (2010). "Tetrapod trackways from the early Middle Devonian period of Poland". Nature. 463 (7277): 43–48. doi:10.1038/nature08623. PMID 20054388.
- Uppsala University (2010, January 8). Fossil footprints give land vertebrates a much longer history. ScienceDaily. Retrieved January 8, 2010, from http://www.sciencedaily.com /releases/2010/01/100107114420.htm
- Beerbower, J. R., Boy, J. A., DiMichele, W. A., Gastaldo, R. A., Hook, R. & Hotton, N., Illustrations by Phillips, T. L., Scheckler, S. E., & Shear, W. A. (1992): Paleozoic terrestrial ecosystems. In: Behrensmeyer, A. K., Damuth, J. D., DiMichele, W. A., Potts, R., Sues, H. D. & Wing, S. L. (eds.) Terrestrial Ecosystems through Time, pp. 205–235. Chicago: Univ. Chicago Press summary from "Devonian Times"
- Milner, A. R. (1993): Amphibian-grade Tetrapoda. In The Fossil Record vol 2, (ed. Benton, M. J.) Chapman & Hall, London, pp 665–679
- Clack, J. A. (2006): Baphetidae, from the Tree of Life Web Project
- Sahney, S., Benton, M.J. & Falcon-Lang, H.J. (2010). "Rainforest collapse triggered Pennsylvanian tetrapod diversification in Euramerica" (PDF). Geology. 38 (12): 1079–1082. doi:10.1130/G31182.1.
- Jenkins, F. A., Jr., Shubin, N. H., Gatesy, S. M., Warren, A. (2008): Gerrothorax pulcherrimus from the Upper Triassic Fleming Fjord Formation of East Greenland and a reassessment of head lifting in temnospondyl feeding. Journal of Vertebrate Paleontology No 28 (4): pp 935–950. News article with animation of skull
- Steyer, J. S.; Damiani, R. (2005). "A giant brachyopoid temnospondyl from the Upper Triassic or Lower Jurassic of Lesotho". Bulletin de la Societe Geologique de France. 176 (3): 243–248. doi:10.2113/176.3.243.
- Warren & al. (1991): An Early Cretaceous labyrinthodont. Alcheringa: An Australasian Journal of Palaeontology, Volume 15, Issue 4, pp 327–332 Article from Informaworld
- Panchen, A.L. (1967): Amphibia, In Harland, W.B., Holland, C.H., House, M.R., Hughes, N.F., Reynolds, A.B., Rudwick, M.j.S., Satterthwaite, G.E., Tarlo, L.B.H. & Willey, E.C. (eds.): The Fossil Record, Geological Society, London, Special Publications, vol 2, chapter 27: pp 685-694; doi:10.1144/GSL.SP.1967.002.01.46 extract
- Laurin, M. & Reisz, R. R. (1997): A new perspective on tetrapod phylogeny. In Sumida, S. & Martin, K. (eds.) Amniotes Origins: Completing the Transition to Land, pp 9–59. London: Academic Press.
- Anderson, J. S. (2001): The phylogenetic trunk: maximal inclusion of taxa with missing data in an analysis of the Lepospondyli (Vertebrata, Tetrapoda). Systematic Biology No 50, pp 170–193 Article as PDF
- Vallin G. & Laurin, M. (2004): Cranial morphology and affinities of Microbrachis, and a reappraisal of the phylogeny and lifestyle of the first amphibians. Journal of Vertebrate Paleontology No 24: pp 56–72 Article as PDF
- Panchen, A. L. & Smithson, T. R. (1988): The relationships of the earliest tetrapods. In Benton, M. J. (ed.) The Phylogeny and Classification of the Tetrapods, Volume 1: Amphibians, Reptiles, Birds, pp 1–32. Oxford: Clarendon Press.
- Trueb, L. & Cloutier, R. (1991): A phylogenetic investigation of the inter- and intrarelationships of the Lissamphibia (Amphibia: Temnospondyli). In: Schultze, H-P & Trueb, L. (eds.) Origins of the higher groups of tetrapods—Controversy and Consensus, pp 223–313. Comstock Publishing Associates, Ithaca
- Ahlberg, PE.; Milner, A. R. (1994). "The origin and early diversification of tetrapods". Nature. 368 (6471): 507–514. Bibcode:1994Natur.368..507A. doi:10.1038/368507a0.
- Sigurdsen, T.; Green, D.M. (2011). "The origin of modern amphibians: a re-evaluation". Zoological Journal of the Linnean Society. 162 (2): 457–469. doi:10.1111/j.1096-3642.2010.00683.x.
- Anderson, J. S.; Reisz, R. R.; Scott, D.; Fröbisch, N. B.; Sumida, S. S. (2008). "A stem batrachian from the Early Permian of Texas and the origin of frogs and salamanders". Nature. 453 (7194): 515–518. doi:10.1038/nature06865. PMID 18497824.
- Säve-Söderbergh G. (1934). "Some points of view concerning the evolution of the vertebrates and the classification of this group". Arkiv för Zoologi. 26A: 1–20.
- Carroll, R. L.; Holme, R. (1980). "The skull and jaw musculature as guides to the ancestry of salamanders". Zoological Journal of the Linnean Society. 68: 1–40. doi:10.1111/j.1096-3642.1980.tb01916.x.
- Carroll R.L. (1991): The origin of reptiles. In: Schultze H.-P., Trueb L., (ed) Origins of the higher groups of tetrapods — controversy and consensus. Ithaca: Cornell University Press, pp 331-353.
- Laurin, M. (2004). "The Evolution of Body Size, Cope's Rule and the Origin of Amniotes". Systematic Biology. 53 (4): 594–622. doi:10.1080/10635150490445706.
- Klembara J. & Meszáros, S. (1992): New finds of Discosauriscus austriacus (Makowsky 1876) from the Lower Permian of Boskovice furrow (Czecho-Slovakia). Geologica Carpathica No 43: pp 305-312
- Laurin, M. and Rize R.R. (1999): A new study of Solenodonsaurus janenschi, and a reconsideration of amniote origins and stegocephalian evolution. Canadian Journal of Earth Science, no 36 (8): pp 1239–1255 (1999) doi:10.1139/cjes-36-8-1239
- Romer, A. S. (1957). "Origin of the amniote egg". The Scientific Monthly. 85: 57–63.
- Carroll, R. L. (1970). "Quantitative aspects of the amphibian-reptilian transition". Forma et. Functio. 3: 165–178.
- Margaret C. Brough; J. Brough (June 1, 1967). "The Genus Gephyrostegus". Philosophical Transactions of the Royal Society B. 252 (776): 147–165. doi:10.1098/rstb.1967.0006. JSTOR 2416682.
- Smithson, T.R.; Rolfe, W.D.I. (1990). "Westlothiana gen. nov. :naming the earliest known reptile". Scottish Journal of Geology. 26: 137–138. doi:10.1144/sjg26020137.
- Falcon-Lang, H.J.; Benton, M.J.; Stimson, M. (2007). "Ecology of early reptiles inferred from Lower Pennsylvanian trackways". Journal of the Geological Society. 164 (6): 1113–1118. doi:10.1144/0016-76492007-015.
- Burmeister, H. (1850): Die Labyrinthodonten aus dem Saarbrücker Steinkohlengebirge, Dritte Abtheilung: der Geschichte der Deutschen Labyrinthodonten Archegosaurus. Berlin: G. Reimer, 74 pp.
- Owen, R. (1861): Palaeontology, or a Systematic Summary of Extinct Animals and their Geological Relations. Adam and Charles Black, Edinburgh, pages 1–463
- Watson, D. M. S. (1 January 1920). "The Structure, Evolution and Origin of the Amphibia. The "Orders' Rachitomi and Stereospondyli" (PDF). Philosophical Transactions of the Royal Society B. 209 (360-371): 1–73. doi:10.1098/rstb.1920.0001.
- A. S. Romer (1947): Review of the Labyrinthodontia. Bulletin of the Museum of Comparative Zoology no 99 (1): pp 1–368, cited in The Paleobiology Database: Labyrinthodontia, Amphibia - Apsidospondyli 
- Cope E. D. 1868. Synopsis of the extinct Batrachia of North America. Proceedings of The Academy of Natural Sciences of Philadelphia: pp 208–221
- Case, E. C. (1946). "A Census of the determinable Genera of Stegocephalia". Transactions of the American Philosophical Society. 35 (4): 325–420. doi:10.2307/1005567.
- Colbert, E. H., (1969), Evolution of the Vertebrates, John Wiley & Sons Inc (2nd ed.)
- Daly, E. (1973): A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology no 47(3): pages 562–589
- Carroll, R. L. (1988), Vertebrate Paleontology and Evolution, WH Freeman & Co.
- Hildebrand, M. & G. E. Goslow, Jr. Principal ill. Viola Hildebrand. (2001). Analysis of vertebrate structure. New York: Wiley. p. 429. ISBN 0-471-29505-1.
- Buell, Donald R. Prothero ; with original illustrations by Carl (2007). Evolution : what the fossils say and why it matters. New York: Columbia University Press. p. 224. ISBN 0231139624.
- Carroll, R. L. (1997): Patterns and Processes of Vertebrate Evolution. Cambridge University Press, Cambridge. 464 pages
|Wikimedia Commons has media related to