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Osteichthyes

Diverse clade of vertebrate animals

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Example of Osteichthyes: Queensland Lungfish and West Indian Ocean coelacanth (two Sarcopterygii), Iridescent shark and American black sturgeon (two Actinopterygii). File based on
Prehistoricplanes · CC BY-SA 4.0

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Through Biodiversity, Animal and Bone

The group is divided into two main clades, the ray-finned fish (Actinopterygii, which makes up the vast majority of extant fish) and the lobe-finned fish (Sarcopterygii, which gave rise to all land vertebrates). The oldest known fossils of bony fish are about 436 million years old from the early Silurian period, which are also transitional fossils showing a tooth pattern that is in between the tooth rows of sharks and true bony fishes. Despite the name, these early basal bony fish had not yet evolved ossification and their skeletons were still mostly cartilaginous, and the main distinguishing feature that set them apart from other fish clades were the development of foregut pouches that eventually evolved into the swim bladders and lungs, respectively.

Osteichthyes is broadly equivalent to Euteleostomi. In paleontology the terms are synonymous. In ichthyology the difference is that Euteleostomi presents a cladistic view which includes the terrestrial tetrapods that evolved from lobe-finned fish. Until recently, the view of most ichthyologists has been that Osteichthyes were paraphyletic and include only fishes. However, since 2013 widely cited ichthyology papers have been published with phylogenetic trees that treat the Osteichthyes as a clade including tetrapods.

Characteristics

Bony fish are characterized by a relatively stable pattern of cranial bones, rooted, medial insertion of mandibular muscle in the lower jaw. The head and pectoral girdles are covered with large dermal bones. The eyeball is supported by a scleral ring of four small bones, but this characteristic has been lost or modified in many modern species. The labyrinth in the inner ear contains large otoliths. The braincase, or neurocranium, is frequently divided into anterior and posterior sections divided by a fissure.

Early bony fish had simple respiratory diverticula (an outpouching on either side of the esophagus) which helped them breathe air in low-oxygen water as a form of supplementary enteral respiration. In ray-finned fish these have evolved into swim bladders, the changing sizes of which help to alter the body's specific density and buoyancy. In elpistostegalians, a crown group of lobe-finned fish that gave rise to the land-dwelling tetrapods, these respiratory diverticula became further specialized for obligated air breathing and evolved into the modern amphibian, reptilian, avian and mammalian lungs. Early bony fish did not have fin spines like most modern fish, but instead had the fleshy paddle-like fins similar to other non-bony clades of fish, although the lobe-finned fish evolved articulated appendicular skeletons within their paired fins, which gave rise to tetrapods' limbs. They also evolved a pair of opercula (gill covers), which can actively draw water across the gills so they can breathe without having to swim.

Bony fish do not have placoid scales like cartilaginous fish, but instead have scales that lie underneath the epidermis and do not penetrate it. The three categories of scales in Osteichthyes are cosmoid scales, ganoid scales, and teleost scales. Teleost scales are then divided into two subgroups which are cycloid scales and ctenoid scales. All of these scales have a base of bone that they all originate from; the main difference is that teleost scales have only one layer of bone. Ganoid scales have lamellar bone, and vascular bone that lies on top of the lamellar bone, then enamel that lies on top of both layers of bone. Cosmoid scales have the same two layers of bone that ganoid scales have except that they have dentin in between the enamel and vascular bone.

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