Staurinidia

From Wikipedia, the free encyclopedia

Phylum:Cnidaria
Class:Scyphozoa
Genus:Staurinidia
Fedonkin, 1985
Staurinidia
Temporal range: late Ediacaran
~557–552 Ma
3D Reconstruction of Staurinidia crucicula
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Cnidaria
Class: Scyphozoa
Order: incertae sedis
Genus: Staurinidia
Fedonkin, 1985
Species:
S. crucicula
Binomial name
Staurinidia crucicula
Fedonkin, 1985

Staurinidia is a genus of Ediacaran soft-bodied organism from the deposits of the Ust' Pinega Formation. It is a monotypic genus, containing only the single species Staurinidia crucicula.[1] The genus was first described in 1985 by Russian palaeontologist Mikhail A. Fedonkin. S. crucicula's four-fold symmetry is present as a result of four canals radiating from the middle of a small cavity in the middle of the body.[1] Other forms with four way symmetry, mainly medusoid forms, from the Ediacaran (Conomedusites, Persimedusites) comprise an essential chunk of the Ediacaran diversity of symmetry; their organisations are similar to, though smaller than, those of a modern-day scyphozoan cnidarian.[2]

See also

References

Related Articles

Wikiwand AI