Tetrapod

Tetrapods (Greek tetrapoda = four feet) are vertebrate tetrapodomorph land animals. The basic tetrapod plan is four legs and feet. This kind of locomotion is quadrupedal. Amphibians, reptiles, dinosaurs, birds, and mammals are all tetrapods. Even though snakes do not have limbs, they are tetrapods because they evolved from animals with four limbs.

The earliest tetrapods evolved from the Sarcopterygii, or lobe-finned fish, into air-breathing amphibians, perhaps in the Upper Devonian period. This means the transition took place in fish, before the land was the main habitat. This is typical of transitional fossils undergoing mosaic evolution.

Evolution

Fishapods 
Clear fossil tetrapod tracks from the mid-Devonian predate previous tetrapod records by 18 million years. These tracks are from the Middle Devonian of Poland, dated to nearly 400 million years ago. The footprints were made in the mud of a tropical lagoon, and no animal of that time could have made the tracks except a tetrapod. The find strongly suggests that the animals were fish, not amphibia, when the transition to limbs occurred. The term fishapod is becoming used. They would have been derived from lobe-finned fish (Sarcopterygii), but of a genus whose body fossil has not yet been found. The Polish team suggest the fish > tetrapod transition might have taken place as early as the Lower Devonian.

The earliest tetrapods lived entirely in water. They could not live on land. Earlier, it was believed that fish had first moved onto land – either looking for food (like modern mudskippers) or to find water when the pond they lived in dried out. It was believed that they later evolved legs, lungs, and other body parts to live better on land.

Nine genera of Devonian tetrapods have been described. These earliest tetrapods were not terrestrial. They lived in swampy habitats like shallow wetlands, coastal lagoons, brackish river deltas, and even shallow marine sediments. There is much to suggest that these are the kind of environments in which the tetrapods evolved. Also, because fossils of early tetrapods are found widely in the Old Red Sandstone continent, they must have spread by following the coastal lines. This means they could not have lived only in freshwater.

Still, they may have spent brief periods out of water and would have used their legs to paw their way through the mud. The earliest confirmed terrestrial forms are known from the early Carboniferous deposits, some 20 million years later.

Tetrapods adapted to terrestrial environments over time and spent longer periods away from the water. They also spent more of their juvenile stage on land before returning to the water for the rest of their life. It is also possible that the adults started to spend some time on land  to bask in the sun, close to the water's edge. The first true tetrapods that were adapted to moving on land were small. Only later did they increase in size.

Romer's gap 
Between the lobe-finned fish tetrapods and the first amphibia and amniotes in the Middle Carboniferous lies a gap of 30 million years, with few satisfactory tetrapod fossils. This, noted in the early 1950s by Alfred Romer, is Romer's gap. Some new fossils were found in the 1990s, such as Pederpes, right in the middle of the Romer Gap. The gap still hides details of the transition from fish to tetrapod, but not so much as before.

So far, only two fossil sites from the Tournasian (earliest Carboniferous) are known. One is Horton Bluff Formation at Blue Beach, Nova Scotia. Much of this material has not yet been scientifically described.

The only other place a Tournasian tetrapod was found is near Dumbarton in the West of Scotland. The articulated (connected) skeleton of Pederpes was found there. Now comes news of new finds from this formation in five places in the Scottish Borders. The paper describes  five new Tournaisian tetrapods, with information about their habitat. 
"Our analysis shows that the Tournaisian included a rich and diverse assemblage of taxa, which included close relatives of some Devonian forms on the tetrapod stem and basal members of the amphibian stem".

The authors say 
"Although an extinction event at the end of the Devonian saw the demise of many archaic fish groups, our studies provide new perspectives on the recovery and diversification of surviving groups that went on to found the basis of modern vertebrate diversity".

Apparently, the split between the amphibians and the amniotes came soon after the extinction event as the tetrapods began to recover. "This accords with most molecular dates for the split, which place it at an average of 355  my ago, a date only 4 myr after the end-Devonian".

The cleidoic egg 
Whereas amphibia lay their eggs in water, all other tetrapods (the amniotes) lay cleidoic eggs. These eggs are like private little ponds, protecting and nourishing the embryo until it grows into a hatchling. This was a key evolutionary 'invention', which allowed the amniotes to invade the land. Once the amniotes were truly land animals, there followed a huge adaptive radiation. This was one of the most significant advances in vertebrate evolution.

Stem tetrapods 
Stem tetrapods are difficult to classify because they lack some or all of the key characteristics of the standard groups.
Land-dwelling stem tetrapods
Descendants of fishapods which at first lived an amphibious life-style. The amniotes and later amphibia are their descendants. Features: able to support their body on land for long periods; had five fingers and toes (pentadactyl limb) in contrast to their fishapod ancestors. Have not yet developed the characteristic features of the main tetrapod groups.
Stem tetrapods evolved into:
Amphibia > present-day Lissamphibia
Amniota
Sauropsida > present-day reptiles and birds
Synapsida > present-day mammals

Early fossils of stem tetraopds 
 Pederpes, an early Mississippian tetrapod, 359–345 million years ago (mya).
 Westlothiana, from 350mya, either an early amniote or a sister group to the amniotes
 Casineria, from 340 mya, a basal amniote.
 Protoclepsydrops, from the middle Pennsylvanian, 314 mya, probable earliest synapsid
 Hylonomus, from 312 mya, early anapsid sauropsid
 Paleothyris, 312–304 mya, another early anapsid sauropsid
 Archaeothyris, from 306 mya, an early synapsid
 Petrolacosaurus, from 302 mya, the first diapsid sauropsid

The tetrapod clade 
The tetrapod clade separated from fish in the Devonian. The amniotes were the earliest to lay cleidoic eggs. The Synapsids (> mammals) and the Sauropsids (> reptiles) are sister clades, and in particular, reptiles did not give rise to mammals.

Simple example cladogram.    Warm-bloodedness evolved somewhere in thesynapsid–mammal transition. ?  Warm-bloodedness must also have evolved at one of these points – an example of convergent evolution.

Living tetrapods 

There are three main groups of living ("crown group") tetrapods. Each group also includes many extinct groups:

Amphibia  frogs and toads, newts and salamanders, and caecilians
Sauropsida  birds and modern reptiles
Synapsida  mammals

Snakes and other legless reptiles are tetrapods because they are evolved from ancestors who had four limbs. This is also true for caecilians and aquatic mammals.

Classification 
[[Image:Pederpes22small.jpg|thumb|200px|Pederpes finneyae]]

A partial taxonomy of the tetrapods:
 Phylum Chordata
 Class Sarcopterygii
 Subclass Tetrapodomorpha
 Eusthenopteron
 Panderichthys
 Tiktaalik
 Superclass Tetrapoda
 Pederpes
 Whatcheeria
 Class Amphibia  
 (Subclass Labyrinthodontia)
 Subclass Lepospondyli
 Subclass Temnospondyli
 Subclass Lissamphibia  frogs, salamanders
 Class Amniota
 Class Sauropsida  Reptiles
 Class Aves  Birds
 Class Synapsida  Mammal-like reptiles
 Class Mammalia  Mammals

Related pages 
Tetrapodomorpha: a cladistic account of the group

References

Other websites 

"Tetrapod"? What is a tetrapod? 
Tetrapod cladograms  - similar to genealogical family trees
Tetrapod environments of the Upper Devonian