Planorbulinoidea
Superfamily of single-celled organisms
From Wikipedia, the free encyclopedia
Planorbulinoidea is a superfamily of rotalliid foraminifera that has been extant since the Early Cretaceous (Berriasian), characterized by trochospiral tests, at least in early stage but which later may become uncoiled. The test wall is of perforate hyaline calcite, commonly optically radial in structure, with crystallographic c-axes perpendicular to the surface. The apertural face may be imperforate; the aperture interiomarginal and extraumbilical-umbilical to nearly equatorial in coiled forms, subterminal in uncoiled forms.
| Planorbulinoidea Temporal range: Early Cretaceous - recent | |
|---|---|
| |
| Planulina limbata | |
Scientific classification  | |
| Domain: | Eukaryota |
| Supergroup: | Rhizaria |
| Phylum: | Foraminifera |
| Class: | Globothalamea |
| Order: | Rotaliida |
| Superfamily: | Planorbulinoidea Schwager, 1877 |
| Families[1] | |
|
Bisacciidae | |
| Synonyms[1] | |
|
Planorbulinacea Schwager, 1877 | |
The Planorbulinoidea unite six families which are distinguished primarily by their morphological differences.