A unique group of exclusively marine animals with a peculiar body architecture. They are headless with a fivefold radial symmetry. The body wall contains the endoskeleton, made of numerous independent calcareous plates which frequently support spines. The plates may be tightly interlocked or loosely associated. The spines may protrude through the outer epithelium, and are often used for defense. The skeletal plates of the body wall, together with their associated muscles and connective tissue, form a tough and sometimes rigid test which encloses the large coelom. A unique water-vascular system is involved in locomotion, respiration, food gathering, and sensory perception. This shows outside the body as rows of fluid-filled tube feet in conspicuous double lines or ambulacra. Within the body wall lie the ducts and fluid reservoirs necessary to protract and retract the tube feet by hydrostatic pressure. The nervous system arises from the embryonic ectoderm and consists of a ring around the mouth with connecting nerve cords associated with each ambulacrum. There may also be diffuse nerve plexuses lying below the outer epithelium. The coelom houses the alimentary canal and associated organs and in most groups the reproductive organs.
The larvae are usually planktonic with a bilateral symmetry, but the adults are usually sedentary and benthic. They inhabit all seas and oceans, ranging from the shores to the ocean depths.
The phylum comprises about 6000 existing species and many fossils, providing a good fossil record. Echinoderms first appeared in the Early Cambrian and have been evolving over 600 million years. During this vast time several divergent patterns have arisen. The surviving groups show few resemblances to the original stock. The existing representatives fall into three subphyla: Crinozoa (class Crinoidea: sea lilies and feather stars); Asterozoa (class Asteroidea: starfishes, and class Ophiuroidea: brittle stars), and Echinozoa (class Echinoidea: sea urchins, sand dollars and heart urchins); and class Holothuroidea: sea cucumbers). The fourth subphylum, Homalozoa, has no living representatives. Following is the outline of classification for the phylum.
Phylum Echinodermata
Subphylum: Homalozoa
Class: Ctenocystoidea
Stylophora
Homostelea
Homoiostelea
Subphylum: Crinozoa
Class: Eocrinoidea
Crinoidea
Subclass: Inadunata
Camerata
Flexibilia
Articulata
Class: Rhombifera
Diploporita
Parablastoidea
Edrioblastoidea
Paracrinoidea
Coronoidea
Blastoidea
Subphylum: Echinozoa
Class: Helicoplacoidea
Camptostromatoidea
Edrioasteroidea
Echinoidea
Subclass: Perischoechinoidea
Order: Bothriocidaroida
Echinocystitoida
Subclass: Cidaroidea
Order: Cidaroida
Subclass: Euechinoidea
Superorder: Echinothuriacea
Order: Echinothurioida
Superorder: Diadematacea
Order: Diadematoida
Micropygoida
Pedinoida
Superorder: Echinacea
Order: Hemicidaroida
Salenioida
Phymosomatoida
Temnopleuroida
Echinoida
Superorder: Eognathostomata
Order: Pygasteroida
Holectypoida
Superorder: Neognathostomata
Order: Cassiduloida
Oligopygoida
Clypeasteroida
Neolampadoida
Superorder: Atelostomata
Order: Disasteroida
Holasteroida
Spatangoida
Class: Ophiocistioidea
Holothuroidea
Subphylum: Asterozoa
Class: Asteroidea
Order: Platyasterida
Trichasteropsida
Paxillosida
Notomyotida
Valvatida
Forcipulatida
Class: Ophiuroidea
Order: Stenurida
Oegophiurida
Phrynophiurida
Ophiurida
Echinoderms evolved very rapidly near the beginning of the Paleozoic Era, and Lower Cambrian deposits contain such divergent branches of the phylum as Homalozoa, Helicoplacoidea, Edrioasteroidea, and Eocrinoidea. These are primitive sorts of echinoderms. Cystoids, crinoids, and blastoids, as well as all recognized main groups of asterozoans and echinozoans (except holothurians), appear in Ordovician strata. During the Paleozoic, numerous well-marked evolutionary trends are discernible in nearly all echinoderm groups, including free-moving forms (especially echinoids) as well as crinozoans. Many small classes of echinoderms became extinct during the Paleozoic, and the surviving groups, especially the crinoids, lost many members at the great Late Permian mass extinction. All groups of modern echinoderms have their origin in early Paleozoic stocks, and the lines of their phylogeny are mostly indicated by the fossil record. Echinoids predominate in Mesozoic and Cenozoic echinoderms.