Osteichthyes are a
taxonomic superclass of
fish, also called bony fish that includes the
ray-finned fish (Actinopterygii)
and
lobe finned fish (Sarcopterygii).
The Osteichthyes are
paraphyletic with land vertebrates, in some classification
schemes the tetrapods et al are considered to be members of
the Osteichthyes for this reason.
Most bony-fish belong to the Actinopterygii, there are
only eight living species of lobe finned fish (Sarcopterygii)
including the
lungfish and
coelacanths. (Some species of lobe-finned fish have
jointed bones.)
They are traditionally treated as a class of vertebrates,
with subclasses Actinopterygii and Sarcopterygii, but some
newer schemes divide them into several separate classes.
The vast majority of fish are osteichthyes. Osteichthyes
are the most various group of vertebrates, consisting of
over 29,000 species, making them the largest class of
vertebrates in existence today.
Characteristics
Osteichthians are characterized by a relatively stable
pattern of cranial bones, rooted teeth, medial insertion of
mandibular muscle in lower jaw. The head and pectoral
girdles are covered with large dermal bones. The eyeball is
supported by a sclerotic 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
fissure. Osteichthyans have a lung or swim bladder. They do
not have fin spines, but instead support the fin with
lepidotrichia (bone fin rays). They also have an operculum, which helps them breathe without having to
swim.
Replacement bone
One of the best-known innovations of the osteichthians is
endochondral bone or "replacement" bone, i.e. bone ossified
internally, by replacement of cartilage, as well as
perichondrally, as "spongy bone." In the more general
vertebrates there are various types of calcified tissue:
dentine, enamel (or "enameloids") and bone, plus variants characterized by their ontogeny,
chemistry, form and location. But endochondral bone is
unique because it begins life as cartilage.
In more basal vertebrates, cartilaginous structures can
become superficially calcified. However, in osteichthians,
the circulatory system invades the cartilaginous matrix.
This permits the local
osteoblasts (bone-forming cells) to continue bone
formation within the cartilage and also recruits additional,
circulating osteoblasts. Other cells gradually eat away at
the surrounding cartilage. The net result is that the
cartilage is replaced from within by a somewhat irregular
vascularized network of bone. Structurally, the effect is to
create a relatively lightweight, flexible, "spongy" bone
interior, surrounded by an outline of dense, lamellar
periostial bone. Since this bone now surrounds other bone,
rather than cartilage, it is referred to as periostial
rather than perichondral. This is the unique endochondral
bone from which the osteichthians derived their name, as
well as many structural advantages. However useful
endochondral bone may be, it is also much heavier and less
flexible than cartilage. Thus, many modern osteichian
groups, including the extremely successful
teleosts, have evolved away from extensive use of
endochondral bone.
The dissection of a bony, or any other fish can prove
quite useful to study internal organs.
Examples
The
ocean sunfish is the most massive bony fish in the world
(but not the longest one; that honor goes to the oarfish).
Specimens of ocean sunfish have been observed up to 3.33 m
(11 ft) in length and weighing up to 2,300 kg (5,070 lb).
Other very large bony fish include the Atlantic blue marlin,
some specimens of which have been recorded as in excess of
820 kilograms (1,807.4 lb.), the black marlin, and some
sturgeon species.