Internal features
The general classification of the bivalves is typically based on shell structure and hinge and ligament organization. The internal anatomy is also a tool in classification, particularly the organs of the mantle cavity, the pattern of water movement through it, and the structure and functioning of the ctenidia and labial palps. Early anatomists established a correlation between shell and gill structure that is still often used as a basis for classification but which is now relegated to defining the evolutionary sequence from a deposit-feeding to a filter-feeding mode of life.
Nucula, from the subclass Protobranchia, reflects the primitive bivalve ancestor. Burrowing close to the sediment surface, Nucula is equivalve, anteriorly and posteriorly symmetrical, and isomyarian. The medial foot is wide. There are no mantle fusions ventrally, and the aerating water current passes through the mantle cavity from front to back, a feature not typical of most modern bivalves. The structure of the small gills, located posteriorly, is interpreted as being similar to the earliest mollusks—hence the name protobranch, or “first gills.” The paired gills, separated by a central axis, are suspended from the mantle roof. Individual short gill filaments extend outward from either side of the axis, and cilia on their surfaces create an upward respiratory water current that passes from the mantle cavity below the gill (the infrabranchial, or inhalant, chamber) to that area above it (the suprabranchial, or exhalant, chamber). The anus and the urogenital pores also open into the exhalant chamber so that all waste products exit the animal in the exhalant stream. The paired labial palps in the mantle cavity are used in feeding. The outer palp on each side bears a long, extensible proboscis with a ciliated groove that collects organic material, which is then sorted by the inner pair and outer pair of palps. Certain particles are transferred to the mouth by the ciliary currents of the inner pair of palps, while the remaining particles are sent by the outer palps into the mantle cavity as a mucus-bound mass known as pseudofeces, which are ejected by periodic contractions of the adductor muscles.
An important event in the evolution of the modern bivalve from the more primitive form illustrated above was the reorientation of the anterior inhalant stream to the posterior below the exhalant stream so that water both enters and exits the mantle cavity posteriorly. For burrowing bivalves, such a body organization allows deep burrowing in a vertical (head down) orientation, and thus escape from the sediment surface. These changes generally are associated with changes in the method of feeding and, as a consequence, the selective fusion of left and right mantle margins to exclude sediment from the mantle cavity.
The burrowing Spisula illustrates these changes. It, like Nucula, is equivalve and anteriorly and posteriorly symmetrical (isomyarian). The mantle margin is fused ventrally, allowing the foot to extend through an anterior pedal gape. The posterior inhalant and exhalant orifices are formed into tentacle-fringed siphons. The gills are here positioned on either side of the visceral mass. Gill filaments are greatly elongated and folded (forming the shape of a W) to increase their surface area. The central axis of the W joins it to the body, and the outermost arms unite with the visceral body on one side and the mantle on the other. A complex arrangement of cilia on the apex of each filament constituting the gill lamellae draws a water current through the gill, which provides oxygen, but more importantly now sieves food from this current and transfers such material along tracts in the gill axes or their ventral margins (bound in mucus) toward the labial palps. The palps process this food and eliminate the pseudofeces as in Nucula.
The modified gill is called a ctenidium, and its structure is best explained by the term lamellibranch. The lamellibranch structure may be further qualified as filibranch, pseudolamellibranch, or eulamellibranch. In filibranchs the filaments are only weakly united by cilia, and often the ctenidium retains some inherent sorting mechanism. Collection and sorting of potential food has not yet been definitively ascribed to gills and labial palps, respectively. In the pseudolamellibranch ctenidium, filaments and lamellae are more securely united, and an inherent sorting mechanism still exists in some. In many, however, the filaments are vertically aggregated into folds, or plicae, that greatly increase the total surface area. In the eulamellibranch ctenidium the filaments and lamellae are closely united, the selection function is lost, and gill structure varies widely. Most modern bivalves are suspension feeders, and particles suspended in the water column are drawn in through the incurrent siphon by the action of the gill cillia in all but a few species.
In the deep seas, modification of the lamellibranch ctenidium has allowed the adoption of carnivory. The predatory bivalves of the subclass Anomalodesmata have an incurrent siphon that can be everted rapidly to form a capacious hood beneath which small crustaceans are trapped and brought into the mantle cavity. The eversion of the siphon is assisted by a horizontal septum across the mantle cavity, which is derived from the mantle and the greatly reduced ctenidium. This is the septibranch ctenidium.
The release from a burrowing mode of life has been facilitated by the retention of a larval structure (the byssus) into adult life. The byssus, secreted by a gland in the foot, secures the animal to a hard surface in preparation for burrowing. Its retention and enlargement in the adult has provided a secure means of attachment to the open surfaces of rocks in the intertidal, estuarine, and fresh waters.
In the triangular mussels (Mytilidae) of such habitats the anterior is reduced, and the body and organs of the mantle cavity are contained in the expanded posterior regions of the shell. The reduction of the anterior adductor muscle is matched by a reduction in the size of the anterior pedal retractor muscles (and enlargement of the posterior equivalents). Since such muscles are less concerned with locomotion and more with pulling the shell down against the substrate, they are more correctly redefined as byssal retractors. The ctenidia and palps fulfil the same role as they do in burrowing lamellibranch bivalves, but, because of the triangular cross section of the shell, they come to lie largely underneath the visceral mass instead of beside it.
Further reduction of the anterior adductor, leading to its eventual loss, creates what is called the monomyarian condition. In bivalves with such a configuration, the anterior shell and mantle are confined to a small area; the foot, where present, is always greatly reduced and positioned anteriorly. The visceral mass and organs of the mantle cavity are arranged around the central posterior adductor muscle, and there is extreme reduction or loss of the anterior pedal/byssal retractor muscles. Shell valves may be so compressed that the space between them, as in Placuna, the windowpane oyster, is very narrow. Alternatively, as in oysters and scallops, one valve is cup-shaped, with the other fitting against it like a lid. In such a case, the body occupies the former valve, the left in oysters and generally the right in all others, such as the scallops. In these bivalves the bilateral symmetry of the shell and mantle is replaced by a radial symmetry from the midpoint of the hinge line. In these bivalves, too, the adductor muscle is more clearly demarcated into “quick” (striated) and “slow” (smooth) components for rapid and sustained adduction respectively. The capacity for work of the greatly enlarged quick component of the scallop muscle permits rapid adduction that facilitates swimming by directing jets of water out of the mantle cavity to each side of the hinge line characterized by shell auricles.
The shell
The bivalve shell is made of calcium carbonate embedded in an organic matrix secreted by the mantle. The periostracum, the outermost organic layer, is secreted by the inner surface of the outer mantle fold at the mantle margin. It is a substrate upon which calcium carbonate can be deposited by the outer surface of the outer mantle fold. The number of calcareous layers in the shell (in addition to the periostracum), the composition of those layers (aragonite or aragonite and calcite), and the arrangement of these deposits (e.g., in sheets, or foliate) is characteristic for different groups of bivalves. Middorsally an elastic ligament creates the opening thrust that operates against the closing action of the adductor muscles. The ligament typically develops either externally (parivincular) or internally (alivincular) but comprises outer lamellar, and inner fibrous, layers secreted by the mantle crest. The ligament type is generally characteristic of each bivalve group. The hinge plate with ligament also possesses interlocking teeth to enforce valve alignment and locking, when closed, to prevent shear. Many variations in teeth structure occur.
The mantle and musculature
The mantle lobes secrete the shell valves; the mantle crest secretes the ligament and hinge teeth. Growth takes place at the margins, although increases in thickness take place everywhere. The mantle is withdrawn between the shell valves by mantle retractor muscles; their point of attachment to the shell being called the pallial line.
The musculature comprises two (dimyarian) primitively equal (isomyarian) adductor muscles; the anterior and the posterior. The anterior of these may be reduced (anisomyarian; heteromyarian) or lost (monomyarian). Only very rarely is the posterior lost and the anterior retained.
Internal to the adductors are paired anterior and posterior pedal retractor muscles. Where the anterior adductor muscle is reduced, so are the anterior pedal retractors. In highly active burrowers, paired anterior pedal protractors and pedal elevator muscles occur—for example, the family Trigonioidea.
In byssally attached bivalves, pedal retractors are reduced and byssal retractors serve to pull the animal down in closer opposition to the rock surface. In oysters, commensurate with the extreme reduction of the foot, pedal retractors are lost. This is also the case in swimming scallops.
The nervous system and organs of sensation
The nervous system is simple and the head is completely absent, reflecting the sedentary habit. In primitive bivalves (e.g., Palaeotaxodonta) there are four pairs of ganglia—cerebral, pleural, pedal, and visceral. In all other bivalves the cerebral and pleural ganglia are fused into two cerebropleural ganglia, located above and on either side of the esophagus. The pedal ganglia are in the base of the foot, and the visceral ganglia are located under the posterior adductor muscle. Nerve fibres arising from the cerebropleural ganglia extend to the pedal and visceral ganglia. In some bivalves with long siphons, there are accessory siphonal ganglia, and in many swimming bivalves the visceral ganglia are much enlarged, presumably to coordinate complex swimming actions.
Again reflecting the sedentary life, sensory functions are largely taken over by the posterior mantle margins and typically comprise tentacles developed from the middle mantle folds that are mechanoreceptors and chemoreceptors. Scallops (family Pectinidae) have complex eyes with a lens and retina. In other bivalves, eyes are simple ciliated cups, although some variation is possible. In the predatory deepwater septibranchs the inhalant siphon, which captures food, is surrounded by tentacles that have vibration-sensitive papillae for detecting the movements of prey.
Situated close to the pedal ganglia but with direct connections to the cerebropleural ganglia are a pair of statocysts, which comprise a capsule of ciliated sense cells. In the lumen is either a single statolith or numerous crystalline statoconia. Their points of contact with the surrounding cilia yield information about the animal’s orientation. Additionally, most bivalves with or without eyes have light-sensitive cells that respond to shadows. Below the posterior adductor muscle an osphradium has been identified in some bivalves that may monitor water flow and quality.
The digestive system and nutrition
The bivalve digestive system comprises a complex stomach and associated structures but an otherwise simple intestine. The various types of stomach have been used to erect an alternative classification. Digestion typically takes place in two phases: extracellular in the stomach and intracellular in the digestive diverticula, opening laterally from the stomach wall. Transport of food particles is effected by cilia, creating an array of tracts and sorting areas within the stomach. The principal organ of extracellular digestion is the crystalline style. It is rotated in its sac by cilia; the head, projecting into the stomach, grinds against a part of the stomach wall lined by a chitinous gastric shield. As it rotates, it dissolves, releasing enzymes and initiating primary extracellular digestion of the mucus-bound food. Products of this process are passed in a fluid suspension into large embayments and thence into the digestive diverticula, where intracellular digestion takes place. Waste material is consolidated in the midgut and rectum and expelled as firm fecal pellets from an anus opening into the exhalant stream. Feeding and digestion are highly coordinated, typically regulated by tidal and diurnal cycles.
The excretory system
Blood is forced through the walls of the heart into the pericardium. From there it passes into the kidneys where wastes are removed, producing urine. The paired kidneys (nephridia) are looped with an opening into the pericardium and another into the suprabranchial chamber. The kidneys may be united. Bivalves also possess pericardial glands lining either the auricles of the heart or the pericardium; they serve as an additional ultrafiltration device.