File:Megalomoidea canadensis (fossil bivalve internal mold) (Lockport Dolomite, Middle Silurian; Martin-Marietta Quarry, Woodville, Ohio, USA).jpg

English: Megalomoidea canadensis (Hall, 1852) - fossil bivalve internal mold from the Silurian of Ohio, USA. (public display, Geology Department, Wittenberg University, Springfield, Ohio, USA)

This species was formerly known as Megalomus canadensis.

Bivalves are bilaterally symmetrical molluscs having two calcareous, asymmetrical shells (valves) - they include the clams, oysters, and scallops. In most bivalves, the two shells are mirror images of each other (the major exception is the oysters). They occur in marine, estuarine, and freshwater environments. Bivalves are also known as pelecypods and lamellibranchiates.

Bivalves are sessile, benthic organisms - they occur on or below substrates. Most of them are filter-feeders, using siphons to bring in water, filter the water for tiny particles of food, then expel the used water. The majority of bivalves are infaunal - they burrow into unlithified sediments. In hard substrate environments, some forms make borings, in which the bivalve lives. Some groups are hard substrate encrusters, using a mineral cement to attach to rocks, shells, or wood.

The fossil record of bivalves is Cambrian to Recent. They are especially common in the post-Paleozoic fossil record.

Shown above is an internal mold of a fossil bivalve, preserved in dolostone. These fossil clams are moderately common in certain intervals of the Silurian dolostone succession of Ohio. Quarrymen have nicknamed these fossils "beefhearts".

Classification: Animalia, Mollusca, Bivalvia, Heterodonta, Hippuritoida, Megalodontidae

Stratigraphy: Lockport Dolomite, upper Niagaran Series, (upper Wenlockian), upper Middle Silurian

Locality: Martin-Marietta Quarry, Woodville, northwestern Ohio, USA