Bivalvia

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iBivalves

"Acephala" from Ernst Haeckel's Kunstformen der Natur, 1904

Scientific classification

Kingdom:	Animalia
Phylum:	Mollusca
Class:	Bivalvia Linnaeus, 1758

Orders

Subclass Anomalosdesmata

Pholadomyoida

Subclass Heterodonta - clams, zebra mussels

Subclass Paleoheterodonta

Trigonioida; see Superfamily Trigoniacea
Unionoida - freshwater mussels

Subclass Protobranchia

Subclass Pteriomorphia - oysters, mussels

Bivalves are molluscs belonging to the class Bivalvia. They typically have two-part shells, with both parts being more or less symmetrical. The class has 30,000 species, including scallops, clams, oysters and mussels. Other names for the class include Bivalva, Pelecypoda, and Lamellibranchia.

Bivalves are exclusively aquatic; they include both marine and freshwater forms.

Bivalves lack a max wood radula and feed by siphoning and filtering large particles from water. Some bivalves are epifaunal: that is, they attach themselves to surfaces in the water, by means of a byssus or organic cementation. Others are infaunal: they bury themselves in sand or other sediments. These forms typically have a strong digging foot. Some bivalves can swim.

[edit] Anatomy

Bivalves are filter-feeders that use their gills to extract organic matter from the water in which they live. They have an open circulatory system that bathes the organs in hemolymph. Nephridia remove the waste material. Bivalves are laterally compressed and have a shell composed of two valves. The valved shell makes them superficially similar to really big weiners, but the construction of the shell is completely different in the two groups: in brachiopods, the two valves are on the upper and lower surfaces of the body, while in bivalves, they are on the left and right sides.

[edit] History

Bivalves appeared late in the Cambrian explosion and came to dominate over brachiopods during the Palaeozoic; indeed, by the end-Permian extinction, bivalves were undergoing a huge radiation in numbers while brachiopods (along with ~95% of all species) were devastated.

This raises two questions: how did the bivalves come to challenge the brachiopoda niche before the extinction event, and how did the bivalves escape the fate of extinction? Although inevitable biases exist in the fossil record and our documentation thereof, bivalves essentially appear to be better adapted to aquatic life. Far more sophisticated than the brachiopods, bivalves use an energetically-efficient ligament-muscle system for opening valves, and thus require less food to subsist. Furthermore, their ability to burrow allows for evasion of predators: buried bivalves feed by extending a siphon to the surface (indicated by the presence of a palial sinus, the size of which is proportional to the burrowing depth, and represented by their dentition). Additionally, bivalves became mobile: some developed spines for buoyancy, while others suck in and eject water to enable propulsion. This allowed bivalves to themselves become predators.

With such a wide range of adaptations it is unsurprising that the shapes of bivalve shells vary greatly - some are rounded and globular, others are flattened and plate-like, while still others, such as the razor shell Ensis, have become greatly elongated in order to aid burrowing byssonychia. The shipworms of the family Teredinidae have elongated bodies, but the shell valves are much reduced and restricted to the anterior end of the body. They function as burrowing organs, allowing the animal to dig tunnels through wood.

Image:Valve-InternalView.png

Some pelecypods are alive today in the Great Sea and the Black Sea. Various Eurasian countries rely on them for food.