MineralogyGeologic RangeHabitatEcologyExamplesblastoids | lo-Mg calcite | Silurian - Permian | benthic marine | filter feeder | Pentremites | crinoids* | lo-Mg calcite | Ordovician - Recent | benthic marine | filter feeder | sea lillies | ![]() asteroids* lo-Mg calcite | Ordovician - Recent | benthic marine | various heterotrophe | star fish | ophiuroids* | lo-Mg calcite | Ordovician - Recent | benthic marine | various heterotrophe, usually deposit feeder | brittle stars | ![]() echinoids* lo-Mg calcite | Ordovician - Recent | benthic marine | various heterotrophe | sea biscuit, sea urchins, sand dollars | holothurians* | lo-Mg calcite | Ordovician - Recent | benthic marine | various heterotrophe | sea cucumbers | rhombiferans | lo-Mg calcite | Ordovician - Devonian | benthic marine | UNK, heterotrophic | diploporitans | lo-Mg calcite | Ordovician - Devonian | benthic marine | UNK, heterotrophic | eocrinoids | lo-Mg calcite | Cambrian - Silurian | benthic marine | UNK, heterotrophic | edrioasteroids | lo-Mg calcite | Cambrian - Pennsylvanian | benthic marine | UNK, heterotrophic | seat stars | |
* Extant taxa
Ranges of major echinoderm groups
Phylum Echinodermata
.....Superphylum Crinozoa
..........Class Crinoidea (Cambrian - Recent, 1005 genera)
..........Class Paracrinoidea (Ordovician - Silurian, 13-15 genera)
.....Subphylum Blastozoa
..........Class Blastoidea (Silurian - Permian, 95 genera)
..........Class Rhombifera (Ordovician - Devonian, 60 genera)
..........Class Diploporita (Ordovician - Devonian, 42 genera)
..........Class Eocrinoidea (Cambrian - Silurian, 30-32 genera)
..........Class Parablastoidea (Ordovician, 3 genera)
.....Subphylum Asterozoa
..........Class Asteroidea (Ordovician - Recent, 430 genera)
..........Class Ophiuroidea (Ordovician - Recent, 325 genera)
.....Subphylum Homalozoa
..........Class Stylophora (Cambrian - Devonian, 32 genera)
..........Class Homoiostelea (Cambrian - Devonian, 12-13 genera)
..........Class Homostelea (Cambrian, 3 genera)
..........Class Ctenocystoidea (Cambrian, 2 genera)
.....Subphylum Echinozoa
..........Class Echinoidea (Ordovician - Recent, 765 genera)
..........Class Holothuroidea (Ordovician - Recent, 200 genera)
..........Class Edrioasteroidea (Cambrian - Pennsylvanian, 35 genera)
..........Class Edrioblastoidea (Ordovician, 1 genus)
..........Class Helicoplacoidea (Cambrian, 3 genera)
..........Class Cyclocystoidea (Ordovician - Devonian, 8 genera)
![]() | Subphylum Crinozoa(Cambrian-Recent)Crinoids, which are commonly called "sea lilies", are benthonic passive filter-feeding echinoderms. Contrary to popular belief, they are not extinct - several hundred species of stalked and unstalked crinoids inhabit the modern world's oceans. The stalked forms inhabit the deep oceans, and thus are not regularly seen except by submersibles (a cheaper way to view crinoids is to rent the movie The Abyss - which correctly shows a sea floor inhabited by crinoids), while stalkless forms are commonly found in shallower depths (including the shallows of coral reefs). Crinoids have a compact calyx (body) with long, erect, mobile arms. The arms support smaller, feather-like structures called pinnules which form the filtration fan which crinoids use to feed. The food is transferred down the arms to the mouth by tube feet located on the pinnules and arms. The oral side of the calyx therefore faces the filtration fan, and the anus is also located on the oral side of the calyx - and thus also faces toward the filtration fan. The calyx is usually connected to the bottom via a stem composed of stacked, articulated plates called columnals. Stemmed forms frequently have a holdfast composed of small, polygonal plates, although some species wrapped their stem around other organisms, and thus didn't need a holdfast. |
(Cambrian - Permian)
Blastozoans are an extinct group of mostly stemmed echinoderms. They had delicate arm-like brachioles coming off their ambulacra, and a complex internal respiratory system which differentiates the blastozoan classes from other echinoderms. The morphology of the blastozoans has led some workers to suggest that the blastozoans lacked tube feet, and thus possibly a water vascular system - another feature which would differentiate them from all other echinoderms. However, this theory is still controversial.
Ranges of major blastozoan groups
(Ordovician-Recent)
Asterozoans express the classic pentameral symmetry of echinoderms. Each armin the living asterozoan contains a radial branch of the water vascular system, which supports numerous paired tube feet which extrude through the underside of each arm. These tube feet form the ambulacra and are located in the middle of each arm along a features called the ambulacral groove. In many echinoderms, this groove carries small captured food particles to the mouth of the organism, although in some types the feature has been altered to serve other functions. The mouth is located where the radiating ambulacra intersect. The side with the mouth in echinoderms is defined as the oral side. The side opposite is called the aboral side. Depending on the group, the oral side can point up or down (in asterozoans, it points down). The water vascular system maintains communication with the ambient sea water through a group of pores in the madreporite, which in asterozoans is located on the aboral side, and can be easy to spot in some species (it looks like a drain cover in a sink). Like most echinoderms, the skeleton of asterozoans is composed of numerous small calcite plates called ossicles which readily disarticulate upon the animal's death.
Ranges of major asterozoan groups
![]() | Subphylum Asterozoa
(Ordovician-Recent) |
![]() | Subphylum Asterozoa
(Ordovician-Recent) |
(Cambrian-Recent)
Echinozoans include the familiar sea urchins, sea biscuits, and sand dollars, as well as several obscure Paleozoic groups, and the unusual sea cucumbers. Except for sea cucumbers, echinozoans have a globose or discoidal test with 5 ambulacral regions. They lack free arms like those possessed by starfish and crinoids, and use spines and/or elongate tube feet for locomotion.
Ranges of major echinozoan groups
![]() | Subphylum Echinozoa
(Ordovician-Recent) |
Echinoderm References
Kier, P.M. 1974. Evolutionary trends in post-Paleozoic echinoids. Journal of Paleontology Memoir 5, 48.
Nichols, D. 1969. Echinoderms, 4th edition. Hutchinson and Co., London.
Smith, A. 1984. Echinoid palaeobiology. Special Topics in Palaeontology, Allen and Unwin, London.
Sprinkle, J. 1973. Morphology and evolution of blastozoan echinoderms. Harvard University Museum of Comparative Zoology Special Publication. Cambridge.
Sprinkle, J. and Kier, P.M. 1987. Phylum Echinodermata. in Boardman, R.S., Cheetham, A.H., and Rowell, A.J., (eds.). Fossil Invertebrates. Blackwell Scientific Publications. 713 pp.