In some cases, recognition of two species of the same genus can be problematic. In the examples shown here, however, the recognition is straightforward. The species are of a shallow-marine bivalve (clam) of Late Cretaceous age from the west coast of North America. These species lived as burrowers in subtidal shelfal depths.
|Pterotrigonia klamathonia, 4.5 cm length, Santa Ana Mountains,|
Turonian age, Orange County, southern California.
Pterotrigonia klamathonia (Anderson, 1958), which is of Turonian age, is characterized by its closely spaced radial ribs, 20 to 25 in number.
|Pterotrigonia evansana, 4.5 cm length, Campanian age,|
Simi Hills, Ventura County, southern California.
Pterotrigonia evansana (Meek, 1858) is geologically younger and is of Coniacian through Campanian age (see time table below). This species is characterized by its widely spaced radial ribs, commonly 10 or so in number.
Genus Pterotrigonia, which is the state fossil of Tennessee, is extinct. It belongs to the family Megatrigoniidae, whose geologic time range is latest Jurassic through the end of the Cretaceous. The family was very widespread in the world during the Cretaceous.