Sarcopterygii (; )—sometimes considered synonymous with Crossopterygii ()—is a clade (traditionally a class or subclass) of vertebrate which includes a group of bony fish commonly referred to as lobe-finned fish. These vertebrates are characterised by prominent muscular (lobes) within their fish fin, which are supported by articulated appendicular skeletons. This is in contrast to the other clade of bony fish, the Actinopterygii, which have only skin-covered lepidotrichia supporting the fins.
The , a mostly terrestrial clade of vertebrates, are now recognized as having evolved from sarcopterygian ancestors and are most closely related to . Their paired pectoral fins and evolved into limbs, and their lung bud eventually evolved into air-breathing . Cladistics, this would make the tetrapods a subgroup within Sarcopterygii and thus sarcopterygians themselves. As a result, the phrase "lobe-finned fish" normally refers to not the entire clade but only aquatic animal members that are not tetrapods, i.e. a paraphyletic group.
Non-tetrapod sarcopterygians were once the dominant predators of freshwater ecosystems during the Carboniferous and Permian periods, but suffered significant decline after the Permian–Triassic extinction event. The only known extant non-tetrapod sarcopterygians are the two species of and six species of .
Most species of lobe-finned fishes are extinct. The largest known lobe-finned fish was Rhizodus from the Carboniferous period of Scotland which may have exceeded 7 meters in length. Among the two groups of living species, the and the , the largest species is the West Indian Ocean coelacanth, reaching in length and weighing up . The largest lungfish is the marbled lungfish which can reach 2 m (6.6 ft) in length and weigh up to .
The extensive fossil record and numerous morphological and molecular studies have shown that lungfish and some fossil lobe-finned fish ("rhipidistians") are more closely related to tetrapods than they are to coelacanths; as a result tetrapods are nested within Sarcopterygii.
Multiple Linnean classifications have been proposed with the explicit intent to incorporate Sarcopterygii as a monophyletic taxon instead of maintaining its traditional paraphyletic definition.
Other classifications do not use Sarcopterygii as a ranked taxon but still nonetheless still reject traditional paraphyletic assemblages. In the scheme below, sarcopterygian groups are marked in bold letters.
In the Early Devonian (416–397 Ma), the sarcopterygians, or lobe-finned fishes, split into two main lineages: the and the . Coelacanths never left the oceans and their heyday was the late Devonian and Carboniferous, from 385 to 299 Ma, as they were more common during those periods than in any other period in the Phanerozoic.
Actinistians, a group within the lobe-finned fish, have been around for almost 380 million years. Over time, researchers have identified 121 species spread across 47 genera. Some species are well-documented in their evolutionary placement, while others are harder to track. The greatest boom in actinistian diversity happened during the Early Triassic, just after the Great Dying.
Coelacanths of the genus Latimeria still live today in the open oceans and retained many primordial features of ancient sarcopterygians, earning them a reputation as living fossils.
The rhipidistians, whose ancestors probably lived in the oceans near river mouths and estuaries, left the marine world and migrated into freshwater habitats. They then split into two major groups: the lungfish and the , and both of them evolved their swim bladders into air-breathing lungs. Lungfish radiated into their greatest diversity during the Triassic period; today, fewer than a dozen genera remain, having evolved the first proto-lungs and proto-limbs, adapting to living outside a submerged water environment by the middle Devonian (397–385 Ma). The tetrapodomorphs, on the other hand, evolved into the fully-limbed and later the fully terrestrial during the Late Devonian, when the Late Devonian Extinction bottlenecked and selected against the more aquatically adapted groups among . The surviving tetrapods then underwent adaptive radiation on dry land and become the dominant terrestrial animals during the Carboniferous and the Permian periods.
Non-tetrapod sarcopterygians continued until towards the end of Paleozoic era, suffering heavy losses during the Permian–Triassic extinction event (251 Ma).
Classification
Ahlberg (1991)
Nelson et al. (2016)
Betancur-Rodrigues et al. (2017)
Tedersoo (2017)
Taxonomy
Evolution
Hypotheses for means of pre-adaptation
History through to the end-Permian extinction
Phylogeny
See also
Footnotes
|
|