Crinoid

Crinoids are marine animals that make up the class Crinoidea, one of the classes of the phylum Echinodermata, which also includes the starfish, brittle stars, sea urchins and sea cucumbers.[3] Those crinoids which, in their adult form, are attached to the sea bottom by a stalk are commonly called sea lilies, while the unstalked forms are called feather stars or comatulids, being members of the largest crinoid order, Comatulida.

Adult crinoids are characterised by having the mouth located on the upper surface. This is surrounded by feeding arms, and is linked to a U-shaped gut, with the anus being located on the oral disc near the mouth. Although the basic echinoderm pattern of fivefold symmetry can be recognised, in most crinoids the five arms are subdivided into ten or more. These have feathery pinnules and are spread wide to gather planktonic particles from the water. At some stage in their life, most crinoids have a stem used to attach themselves to the substrate, but many live attached only as juveniles and become free-swimming as adults.

There are only about 600 living species of crinoid,[4] but the class was much more abundant and diverse in the past. Some thick limestone beds dating to the mid- to late-Paleozoic era are almost entirely made up of disarticulated crinoid fragments.

Crinoids
Temporal range: Darriwilian–recent[1]
Crinoid on the reef of Batu Moncho Island
Crinoid on the reef of Batu Moncho Island, Indonesia
Scientific classification
Kingdom: Animalia
Phylum: Echinodermata
Subphylum: Crinozoa
Class: Crinoidea
Miller, 1821[2]
Subclasses

Articulata (540 species)
†Flexibilia
Camerata
†Disparida

Etymology

The name "Crinoidea" comes from the Greek word κρίνος, "a lily", with the suffix –oid meaning "like".[5][6] They live in both shallow water[7] and in depths as great as 9,000 meters (30,000 ft).[8] Those crinoids which in their adult form are attached to the sea bottom by a stalk are commonly called sea lilies.[9] The unstalked forms are called feather stars[10] or comatulids, being members of the largest crinoid order, Comatulida.[11]

Morphology

Crinoid anatomy
Anatomy of a stalked crinoid

The basic body form of a crinoid is a stem (not present in adult feather stars) and a crown consisting of a cup-like central body known as the theca, and a set of five rays or arms, usually branched and feathery. The mouth and anus are both located on the upper side of the theca, making the dorsal (upper) surface the oral surface, unlike in the other echinoderm groups such as the sea urchins, starfish and brittle stars where the mouth is on the underside.[12] The numerous calcareous plates make up the bulk of the crinoid, with only a small percentage of soft tissue. These ossicles fossilise well and there are beds of limestone dating from the Lower Carboniferous around Clitheroe, England, formed almost exclusively from a diverse fauna of crinoid fossils.[13]

Haeckel Crinoidea
Stalked crinoid drawn by Ernst Haeckel

The stem of sea lilies is composed of a column of highly porous ossicles which are connected by ligamentary tissue. It attaches to the substrate with a flattened holdfast or with whorls of jointed, root-like structures known as cirri. Further cirri may occur higher up the stem. In crinoids that attach to hard surfaces, the cirri may be robust and curved, resembling birds' feet, but when crinoids live on soft sediment, the cirri may be slender and rod-like. Juvenile feather stars have a stem, but this is later lost, with many species retaining a few cirri at the base of the crown. The majority of living crinoids are free-swimming and have only a vestigial stalk. In those deep-sea species that still retain a stalk, it may reach up to 1 m (3 ft) in length (although usually much smaller), and fossil species are known with 20 m (66 ft) stems.[14]

The theca is pentamerous (has five-part symmetry) and is homologous with the body or disc of other echinoderms. The base of the theca is formed from a cup-shaped set of ossicles (bony plates), the calyx, while the upper surface is formed by the weakly-calcified tegmen, a mebranous disc. The tegmen is divided into five "ambulacral areas", including a deep groove from which the tube feet project, and five "interambulacral areas" between them. The mouth is near the centre or on the margin of the tegmen, and ambulacral grooves lead from the base of the arms to the mouth. The anus is also located on the tegmen, often on a small elevated cone, in an interambulacral area. The theca is relatively small and contains the crinoid's digestive organs.[14]

The arms are supported by a series of articulating ossicles similar to those in the stalk. Primitively, crinoids had only five arms, but in most modern forms these are divided into two at ossicle II, giving ten arms in total. In most living species, especially the free-swimming feather stars, the arms branch several more times, producing up to two hundred branches in total. Being jointed, the arms can curl up. They are lined, on either side alternately, by smaller jointed appendages known as "pinnules" which give them their feather-like appearance. Both arms and pinnules have tube feet along the margins of the ambulacral grooves. The tube feet come in groups of three of different size; they have no suction pads and are used to hold and manipulate food particles. The grooves are equipped with cilia which facilitate feeding by moving the organic particles along the arm and into the mouth.[14]

Crinoide vraie

Stem, theca and arms of a "true" (stalked) crinoid (family Isselicrinidae)

Comasteridae - Oxycomanthus bennetti-001

Oxycomanthus bennetti (comatulid)

Lamprometra palmata hgsus03

Tegmen of a Lamprometra palmata. The mouth is located at the center of the 5 feeding grooves, and the anus at the top of the column.

Elegant feather star9

Close-up on the cirri that allow comatulids to walk and attach themselves

Myzostoma fuscomaculatum at Percys Hole detail

Close-up on the pinnules of a Tropiometra carinata (with parasites Myzostoma fuscomaculatum)

Biology

Feeding

Podia of a red feather star
Two arms with pinnules and tube feet outstretched

Crinoids are passive suspension feeders, filtering plankton and small particles of detritus from the sea water flowing past them with their feather-like arms. The arms are raised to form a fan-shape which is held perpendicular to the current. Mobile crinoids move to perch on rocks, coral heads or other eminences to maximise their feeding opportunities. The food particles are caught by the primary (longest) tube feet, which are fully extended and held erect from the pinnules, forming a food-trapping mesh, while the secondary and tertiary tube feet are involved in manipulating anything encountered.[14]

The tube feet are covered with sticky mucus that traps any particles which come in contact. Once they have caught a particle of food, the tube feet flick it into the ambulacral groove, where the cilia propel the mucus and food particles towards the mouth. Lappets at the side of the groove help keep the mucus stream in place. The total length of the food-trapping surface may be very large; the 56 arms of a Japanese sea lily with 24 cm (9 in) arms, have a total length of 80 m (260 ft) including the pinnules. Generally speaking, crinoids living in environments with relatively little plankton have longer and more highly branched arms than those living in food-rich environments.[14]

The mouth descends into a short oesophagus. There is no true stomach, so the oesophagus connects directly to the intestine, which runs in a single loop right around the inside of the calyx. The intestine often includes numerous diverticulae, some of which may be long or branched. The end of the intestine opens into a short muscular rectum. This ascends towards the anus, which projects from a small conical protuberance at the edge of the tegmen. Faecal matter is formed into large, mucous-cemented pellets which fall onto the tegmen and thence the substrate.[14]

Predation

Specimens of the sea urchin Calocidaris micans found in the vicinity of the crinoid Endoxocrinus parrae, have been shown to contain large quantities of stem portions in their guts. These consist of articulated ossicles with soft tissue, whereas the local sediment contained only disarticulated ossicles without soft tissue. This makes it highly likely that these sea urchins are predators of the crinoids, and that the crinoids flee, offering part of their stem in the process.[15]

Various crinoid fossils hint at possible prehistoric predators. Coprolites of both fish and cephalopods have been found containing ossicles of various crinoids, such as the pelagic crinoid Saccocoma, from the Jurassic lagerstatten Solnhofen,[16] while damaged crinoid stems with bite marks matching the toothplates of coccosteid placoderms have been found in Late Devonian Poland.[17] The calyxes of several Devonian to Carboniferous-aged crinoids have the shells of a snail, Platyceras, intimately associated with them.[18] Some have the snail situated over the anus, suggesting that Platyceras was a coprophagous commensal, while others have the animal directly situated over a borehole, suggesting a more pernicious relationship.[19]

Water vascular system

Like other echinoderms, crinoids possess a water vascular system that maintains hydraulic pressure in the tube feet. This is not connected to external sea water via a madreporite, as in other echinoderms, but only connected through a large numbers of pores to the coelom (body cavity). The main fluid reservoir is the muscular-walled ring canal which is connected to the coelom by stone canals lined with calcareous material. The coelom is divided into a number of interconnecting spaces by mesenteries. It surrounds the viscera in the disc and has branches within the stalk and arms, with smaller branches extending into the pinnules. It is the contraction of the ring canal that extends the tube feet. Three narrow branches of the coelom enter each arm, two on the oral side and one aborally, and pinnules. The action of cilia cause there to be a slow flow of fluid (1mm per second) in these canals, outward in the oral branches and inward in the aboral ones, and this is the main means of transport of nutrients and waste products. There is no heart and separate circulatory system but at the base of the disc there is a large blood vessel known as the axial organ, containing some slender blind-ended tubes of unknown function, which extends into the stalk.[14]

These various fluid-filled spaces, in addition to transporting nutrients around the body, also function as both a respiratory and an excretory system. Oxygen is absorbed primarily through the tube feet, which are the most thin-walled parts of the body, with further gas exchange taking place over the large surface area of the arms. There are no specialised organs for excretion while waste is collected by phagocytic coelomocytes.[14]

Nervous system

The crinoid nervous system is divided into three parts, with numerous connections between them. The oral or uppermost portion is the only one homologous with the nervous systems of other echinoderms. It consists of a central nerve ring surrounding the mouth, and radial nerves branching into the arms and is sensory in function. Below this lies an intermediate nerve ring, giving off radial nerves supplying the arms and pinnules. These nerves are motor in nature, and control the musculature of the tube feet. The third portion of the nervous system lies aborally, and is responsible for the flexing and movement actions of the arms, pinnules and cirri. This is centred on a mass of neural tissue near the base of the calyx, and provides a single nerve to each arm and a number of nerves to the stalk.[14]

Reproduction and life cycle

Crinoids are not capable of clonal reproduction as are some starfish and brittle stars, but are capable of regenerating lost body parts. Arms torn off by predators or damaged by adverse environmental conditions can regrow, and even the visceral mass can regenerate over the course of a few weeks. This regeneration may be vital in surviving attacks by predatory fish.[14]

Crinoids are dioecious, with individuals being either male or female. In most species, the gonads are located in the pinnules but in a few, they are located in the arms. Not all the pinnules are reproductive, just those closest to the crown. The gametes are produced in genital canals enclosed in genital coeloms. The pinnules eventually rupture to release the sperm and eggs into the surrounding sea water. In certain genera, such as Antedon, the fertilised eggs are cemented to the arms with secretions from epidermal glands; in others, especially cold water species from Antarctica, the eggs are brooded in specialised sacs on the arms or pinnules.[14]

The fertilised eggs hatch to release free-swimming vitellaria larvae. The bilaterally symmetrical larva is barrel-shaped with rings of cilia running round the body, and a tuft of sensory hairs at the upper pole. While both feeding (planktotrophic) and non-feeding (lecithotrophic) larvae exist among the four other extant echinoderm classes, all present day crinoids appear to be descendants from a surviving clade that went through a bottleneck after the Permian extinction, at that time losing the feeding larval stage.[20] The larva's free-swimming period lasts for only a few days before it settles on the bottom and attaches itself to the underlying surface using an adhesive gland on its underside. The larva then undergoes an extended period of metamorphoses into a stalked juvenile, becoming radially symmetric in the process. Even the free-swimming feather stars go through this stage, with the adult eventually breaking away from the stalk.[14]

Locomotion

Crinoid and comatule
A stalked crinoid (white) and a comatulid (red) in deep sea, showing the differences between these two sister groups

Most modern crinoids, i.e., the feather stars, are free-moving and lack a stem as adults. Examples of fossil crinoids that have been interpreted as free-swimming include Marsupitsa, Saccocoma and Uintacrinus.[21] In general, crinoids move to new locations by crawling, using the cirri as legs. Such a movement may be induced in relation to a change in current direction, the need to climb to an elevated perch to feed, or because of an agonistic behaviour by an encountered individual.[22] Crinoids can also swim. They do this by co-ordinated, repeated sequential movements of the arms in three groups. At first the direction of travel is upwards but soon becomes horizontal, travelling at about 7 cm (2.8 in) per second with the oral surface in front. Swimming usually takes place as short bursts of activity lasting up to half a minute, and in the comatulid Florometra serratissima at least, only takes place after mechanical stimulation or as an escape response evoked by a predator.[22]

In 2005, a stalked crinoid was recorded pulling itself along the sea floor off the Grand Bahama Island. While it has been known that stalked crinoids could move, before this recording the fastest motion known for a stalked crinoid was 0.6 metres (2 feet) per hour. The 2005 recording showed one of these moving across the seabed at the much faster rate of 4 to 5 cm (1.6 to 2.0 in) per second (144 to 180 metres per hour).[23]

Evolution

Origins

Agaricocrinus americanus Carboniferous Indiana
Agaricocrinus americanus, a fossil crinoid from the Carboniferous of Indiana
JurassicCrinoidsIsrael
Middle Jurassic (Callovian) Apiocrinites crinoid pluricolumnals from the Matmor Formation in southern Israel

If one ignores the enigmatic Echmatocrinus of the Burgess Shale, the earliest known unequivocal crinoid groups date back to the Ordovician. There are two competing hypotheses pertaining to the origin of the group: the traditional viewpoint holds that crinoids evolved from within the blastozoans (the eocrinoids and their derived descendants, the blastoids and the cystoids), whereas the most popular alternative suggests that the crinoids split early from among the edrioasteroids.[24] The debate is difficult to settle, in part because all three candidate ancestors share many characteristics, including radial symmetry, calcareous plates, and stalked or direct attachment to the substrate.[24]

Diversity

Echinoderms with mineralized skeletons entered the fossil record in the early Cambrian (540 mya), and during the next 100 million years, the crinoids and blastoids (also stalked filter-feeders) were dominant.[25] At that time, the Echinodermata included twenty taxa of class rank, only five of which survived the mass extinction events that followed. The long and varied geological history of the crinoids demonstrates how well the echinoderms had adapted to filter-feeding.[3]

The crinoids underwent two periods of abrupt adaptive radiation, the first during the Ordovician (485 to 444 mya), and the other during the early Triassic (around 230 mya).[26] This Triassic radiation resulted in forms possessing flexible arms becoming widespread; motility, predominantly a response to predation pressure, also became far more prevalent than sessility.[27] This radiation occurred somewhat earlier than the Mesozoic marine revolution, possibly because it was mainly prompted by increases in benthic predation, specifically of echinoids.[28] There then followed a selective mass extinction at the end of the Permian period, during which all blastoids and most crinoids became extinct.[26] After the end-Permian extinction, crinoids never regained the morphological diversity and dominant position they enjoyed in the Paleozoic; they employed a different suite of ecological strategies open to them from those that had proven so successful in the Paleozoic.[26]

Fossils

Some fossil crinoids, such as Pentacrinites, seem to have lived attached to floating driftwood and complete colonies are often found. Sometimes this driftwood would become waterlogged and sink to the bottom, taking the attached crinoids with it. The stem of Pentacrinites can be several metres long. Modern relatives of Pentacrinites live in gentle currents attached to rocks by the end of their stem. The largest fossil crinoid on record had a stem 40 m (130 ft) in length.[29]

In 2012, three geologists reported they had isolated complex organic molecules from 340-million-year-old (Mississippian) fossils of multiple species of crinoids. Identified as "resembl[ing ...] aromatic or polyaromatic quinones", these are the oldest molecules to be definitively associated with particular individual fossils, as they are believed to have been sealed inside ossicle pores by precipitated calcite during the fossilization process.[30]

Taxonomy

Colorful crinoids at shallow waters of Gili Lawa Laut
Colorful crinoids in shallow waters in Indonesia
Multiple crinoids occupying the reef of Nusa Kode Island
Multiple crinoids on a reef in Indonesia

Crinoidea has been accepted as a distinct clade of echinoderms since the definition of the group by Miller in 1821.[31] According to the World Register of Marine Species, Articulata, the only extant subclass of Crinoidea, includes the following families:-[32]

  • order Comatulida Clark, 1908
    • super-family Antedonoidea Norman, 1865
      • family Antedonidae Norman, 1865
      • family Pentametrocrinidae AH Clark, 1908
      • family Zenometridae AH Clark, 1909
    • super-family Atelecrinoidea Bather, 1899
      • family Atelecrinidae Bather, 1899
    • super-family Comatuloidea Fleming, 1828
    • super-family Himerometroidea AH Clark, 1908
      • family Colobometridae AH Clark, 1909
      • family Eudiocrinidae AH Clark, 1907
      • family Himerometridae AH Clark, 1907
      • family Mariametridae AH Clark, 1909
      • family Zygometridae AH Clark, 1908
    • super-family Notocrinoidea Mortensen, 1918
    • super-family Paracomatuloidea Hess, 1951
    • super-family Tropiometroidea AH Clark, 1908
      • family Asterometridae Gislén, 1924
      • family Calometridae AH Clark, 1911
      • family Charitometridae AH Clark, 1909
      • family Ptilometridae AH Clark, 1914
      • family Thalassometridae AH Clark, 1908
      • family Tropiometridae AH Clark, 1908
    • Comatulida incertae sedis
      • family Atopocrinidae Messing, 2011 (in Hess & Messing, 2011)
      • family Bathycrinidae Bather, 1899
      • family Bourgueticrinidae Loriol, 1882
      • family Guillecrinidae Mironov & Sorokina, 1998
      • family Phrynocrinidae AH Clark, 1907
      • family Septocrinidae Mironov, 2000
  • order Cyrtocrinida
    • Sub-order Cyrtocrinina
      • family Sclerocrinidae Jaekel, 1918
    • Sub-order Holopodina
      • family Eudesicrinidae Bather, 1899
      • family Holopodidae Zittel, 1879
  • order Encrinida †
  • order Hyocrinida
    • family Hyocrinidae Carpenter, 1884
  • order Isocrinida
    • Sub-order Isocrinina
    • Sub-order Pentacrinitina †
      • family Pentacrinitidae Gray, 1842
  • order Millericrinida

Phylogeny

The phylogeny, geologic history, and classification of the Crinoidea was discussed by Wright et al. (2017).[33] These authors presented new phylogeny-based and rank-based classifications based on results of recent phylogenetic analyses.[31][34][35][36] Their rank-based classification of crinoid higher taxa (down to Order), not fully resolved and with numerous groups incertae sedis (of uncertain placement), is illustrated in the cladogram.

Crinoidea

† Protocrinoidea (incertae sedis)

† Camerata
† Eucamerata

† Diplobathrida

Monobathrida Actinocrinus indiana 330m.jpg

Pentacrinoidea
Inadunata
Disparida

Eustenocrinida

Maennilicrinida

Tetragonocrinida

Calceocrinida

‘Homocrinida’ (incertae sedis)

‘Myelodactyla’ (incertae sedis)

‘Pisocrinoidea’ (incertae sedis)

Cladida
Porocrinoidea

Porocrinida

Hybocrinida

Flexibilia

Taxocrinida

Sagenocrinida

Eucladida
Cyathoformes

‘Cyathocrinida’ (incertae sedis)

‘Dendrocrinida’ (incertae sedis)

‘Poteriocrinida’ (incertae sedis)

† ‘Ampelocrinida’ (incertae sedis)

Articulata

Holocrinida

† Encrinida Encrinus liliiformis

Millericrinida Seirocrinus subsingularis, view 2, Jurassic, Hlzmaden Black Shale Formation, Holzmaden, Germany

Uintacrinida

Roveacrinida

Cyrtocrinida Holopus

Hyocrinida Calamocrinus diomedæ (Plate XXVIII) BHL4232451

Isocrinida Neocrinus decorus

Comatulida Comasteridae - Oxycomanthus bennetti-003

In culture

Fossilised crinoid columnal segments extracted from limestone quarried on Lindisfarne, or found washed up along the foreshore, were threaded into necklaces or rosaries, and became known as St. Cuthbert's beads in the Middle Ages.[37] Similarly, in the Midwestern United States, fossilized segments of the columns of crinoids are sometimes known as Indian beads.[38] Crinoids are the state fossil of Missouri.[39]

Fossil crinoids

Fossile-seelilie

Fossil from Germany showing the stem, calyx, and arms with pinnules

Crinoids iowa 330m

330 million year old crinoid fossils from Iowa

OrdCrinoidHoldfasts

Crinoid holdfasts and bryozoans on an Upper Ordovician cobble from northern Kentucky

Seirocrinus subangularis (fossil Crinoid)

Seirocrinus subangularis from the Early Jurassic Posidonia Shale at Holzmaden, Germany

Isocrinus nicoleti Encrinite Mt Carmel

Crinoid columnals (Isocrinus nicoleti) from the Middle Jurassic Carmel Formation at Mount Carmel Junction, Utah

CrinoidHoldfastRoots

Root-like crinoid holdfast from the Upper Ordovician, southern Ohio

Crinoid internal mold lumen

Internal mold of crinoid stem lumen (and external mold of stem) from Lower Carboniferous, Ohio

Seirocrinus subsingularis, view 2, Jurassic, Hlzmaden Black Shale Formation, Holzmaden, Germany

Fossils of Seirocrinus subsingularis from the Jurassic Holzmaden Black Shale Formation, Germany

References

  1. ^ Zamora, Samuel; Rahman, Imran A.; Ausich, William I. (2015). "Palaeogeographic implications of a new iocrinid crinoid (Disparida) from the Ordovician (Darriwillian) of Morocco". Proceedings of the Royal Society B: Biological Sciences. 3: e1450. doi:10.7717/peerj.1450. PMC 4675106. PMID 26664800.
  2. ^ Hansson, Hans (2012). "Crinoidea". WoRMS. World Register of Marine Species. Retrieved 2013-01-30.
  3. ^ a b Ruppert, Edward E.; Fox, Richard, S.; Barnes, Robert D. (2004). Invertebrate Zoology, 7th edition. Cengage Learning. pp. 917–918. ISBN 978-81-315-0104-7.
  4. ^ "Animal Diversity Web: Crinoidea". University of Michigan Museum of Zoology. Retrieved 26 August 2012.
  5. ^ Webster's New Universal Unabridged Dictionary. 2nd ed. 1979.
  6. ^ "crinoid". Online Etymology Dictionary.
  7. ^ Zmarzly, D.L. (1985). "The Shallow-Water Crinoid Fauna of Kwajalein Atoll, Marshall Islands: Ecological Observations, Interatoll Comparisons, and Zoogeographic Affinities". Pacific Science. 39: 340–358.
  8. ^ Oji, T.; Ogawa, Y.; Hunter, A. W. & Kitazawa, K. (2009). "Discovery of Dense Aggregations of Stalked Crinoids in Izu-Ogasawara Trench, Japan". Zoological Science. 26 (6): 406–408. doi:10.2108/zsj.26.406. PMID 19583499.
  9. ^ "Sea lily". Encyclopædia Britannica. Retrieved 14 March 2011.
  10. ^ "Feather star". Encyclopædia Britannica. Retrieved 14 March 2011.
  11. ^ Ausich, William I.; Messing, Charles G. "Crinoidea". Tree of Life. Retrieved 14 March 2011.
  12. ^ O'Hara, Timothy; Byrne, Maria (2017). Australian Echinoderms: Biology, Ecology and Evolution. Csiro Publishing. pp. 171–180. ISBN 978-1-4863-0763-0.
  13. ^ Hess, Hans; Brett, Carlton E.; Ausich, William I.; Simms, Michael J. (2002). Fossil Crinoids. Cambridge University Press. pp. 3–5, 45–46. ISBN 978-0-521-52440-7.
  14. ^ a b c d e f g h i j k l Ruppert, Edward E.; Fox, Richard, S.; Barnes, Robert D. (2004). Invertebrate Zoology, 7th edition. Cengage Learning. pp. 917–927. ISBN 978-81-315-0104-7.
  15. ^ Baumiller, Tomasz K.; Mooi, Rich; Messing, Charles G. (2008). "Urchins in the meadow: Paleobiological and evolutionary implications of cidaroid predation on crinoids". Paleobiology. 34 (1): 22–34. doi:10.1666/07031.1. JSTOR 20445573.
  16. ^ Hess, Hans (2003). "Upper Jurassic Solnhofen Plattenkalk of Bavaria, German". In Brett, Carlton E.; Ausich, William I.; Simms, Michael J. (eds.). Fossil Crinoids. Cambridge University Press. pp. 216–24. ISBN 978-0-521-52440-7.
  17. ^ Gorzelak, Przemys Law; Rakowicz, Lukasz; Salamon, Mariusz A.; Szrek, Piotr (2011). "Inferred placoderm bite marks on Devonian crinoids from Poland". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 259: 105–12. doi:10.1127/0077-7749/2010/0111.
  18. ^ Brett, Carlton E.; Walker, Sally E. (2002). "Predators and predation in Paleozoic marine environments" (PDF). Paleontological Society Papers. 8: 93–118. doi:10.1017/S1089332600001078. Archived from the original (PDF) on 2012-08-13. Retrieved 2014-04-06.
  19. ^ Gahn, Forest J.; Baumiller, Tomasz K. (2003). "Infestation of Middle Devonian (Givetian) camerate crinoids by platyceratid gastropods and its implications for the nature of their biotic interaction" (PDF). Lethaia. 36 (2): 71–82. doi:10.1080/00241160310003072. hdl:2027.42/75509.
  20. ^ Raff, R A; Byrne, M (2006). "The active evolutionary lives of echinoderm larvae". Heredity. 97 (3): 244–52. doi:10.1038/sj.hdy.6800866. PMID 16850040.
  21. ^ "About Crinoids". FossilEra. Retrieved 15 March 2019.
  22. ^ a b Shaw, G.D.; Fontaine, A.R. (2011). "The locomotion of the comatulid Florometra serratissima (Echinodermata: Crinoidea) and its adaptive significance". Canadian Journal of Zoology. 68 (5): 942–950. doi:10.1139/z90-135.
  23. ^ Baumiller, Tomasz K.; Messing, Charles G. (6 October 2005). "Crawling In Stalked Crinoids: In Situ Observations, Functional Morphology, and Implications for Paleozoic Taxa". Geological Society of America Abstracts with Programs. 37. p. 62.
  24. ^ a b Guensburg, Thomas E.; Mooi, Rich; Sprinkle, James; David, Bruno; Lefebvre, Bertrand (2010). "Pelmatozoan arms from the mid-Cambrian of Australia: Bridging the gap between brachioles and brachials? Comment: There is no bridge". Lethaia. 43 (3): 432–40. doi:10.1111/j.1502-3931.2010.00220.x.
  25. ^ Waggoner, Ben (16 January 1995). "Echinodermata: Fossil Record". Introduction to the Echinodermata. Museum of Paleontology: University of California at Berkeley. Retrieved 30 March 2019.
  26. ^ a b c Foote, Mike (1999). "Morphological diversity in the evolutionary radiation of Paleozoic and post-Paleozoic crinoids". Paleobiology. 25 (sp1): 1–116. doi:10.1666/0094-8373(1999)25[1:MDITER]2.0.CO;2. ISSN 0094-8373. JSTOR 2666042.
  27. ^ Baumiller, Tomasz K. (2008). "Crinoid Ecological Morphology". Annual Review of Earth and Planetary Sciences. 36: 221–249. Bibcode:2008AREPS..36..221B. doi:10.1146/annurev.earth.36.031207.124116.
  28. ^ Baumiller, T. K.; Salamon, M. A.; Gorzelak, P.; Mooi, R.; Messing, C. G.; Gahn, F. J. (2010). "Post-Paleozoic crinoid radiation in response to benthic predation preceded the Mesozoic marine revolution". Proceedings of the National Academy of Sciences. 107 (13): 5893–6. Bibcode:2010PNAS..107.5893B. doi:10.1073/pnas.0914199107. JSTOR 25665085. PMC 2851891. PMID 20231453. INIST:22572914.
  29. ^ Ponsonby, David; Dussart, George (2005). The Anatomy of the Sea. Vancouver: Raincoast Books. p. 129. ISBN 978-0-8118-4633-2.
  30. ^ O'Malley, C. E.; Ausich, W. I.; Chin, Y.-P. (2013). "Isolation and characterization of the earliest taxon-specific organic molecules (Mississippian, Crinoidea)". Geology. 41 (3): 347. Bibcode:2013Geo....41..347O. doi:10.1130/G33792.1. Lay summaryPhys.org (Feb 19, 2013). Note that the first sentence of the phys.org article contradicts the paper itself, which reviews several isolations of molecules from particular fossils over the past decade.
  31. ^ a b Ausich, William I.; Kammer, Thomas W.; Rhenberg, Elizabeth C.; Wright, David F. (2015). "Early phylogeny of crinoids within the pelmatozoan clade". Palaeontology. 58 (6): 937–952. doi:10.1111/pala.12204.
  32. ^ Messing, Charles (2007). "Articulata". WoRMS. World Register of Marine Species. Retrieved 31 March 2019.
  33. ^ Wright, David F.; Ausich, William I.; Cole, Selina R.; Peter, Mark E.; Rhenberg, Elizabeth C. (2017). "Phylogenetic taxonomy and classification of the Crinoidea (Echinodermata)". Journal of Paleontology. in press (4): 829–846. doi:10.1017/jpa.2016.142.
  34. ^ Wright, David F. (2017). "Bayesian estimation of fossil phylogenies and the evolution of early to middle Paleozoic crinoids (Echinodermata)". Journal of Paleontology. in press (4): 799–814. doi:10.1017/jpa.2016.141.
  35. ^ Cole, Selina R. (2017). "Phylogeny and morphologic evolution of the Ordovician Camerata (Class Crinoidea, Phylum Echinodermata)". Journal of Paleontology. in press (4): 815–828. doi:10.1017/jpa.2016.137.
  36. ^ Rouse, Greg W.; Jermiin, Lars S.; Wilson, Nerida G.; Eeckhaut, Igor; Lanterbecq, Deborah; Oji, Tatsuo; Young, Craig M.; Browning, Teena; Cisternas, Paula; Helgen, Lauren E.; Stuckey, Michelle; Messing, Charles G. (2013). "Fixed, free, and fixed: the fickle phylogeny of extant Crinoidea (Echinodermata) and their Permian-Triassic origin". Molecular Phylogenetics and Evolution. 66 (6): 161–181. doi:10.1016/j.ympev.2012.09.018. PMID 23063883.
  37. ^ Lane, N. Gary; Ausich, William I. (2001). "The Legend of St Cuthbert's Beads: A Palaeontological and Geological Perspective". Folklore. 112 (1): 65–73. JSTOR 1260865.
  38. ^ "Identifying Unknown Fossils (by their shape)". Kentucky Geological Survey / University of Kentucky. Retrieved 21 June 2009.
  39. ^ "Missouri's State Fossil". Office of the Secretary of State, Missouri. Retrieved 31 March 2019.

External links

  • Media related to Crinoidea at Wikimedia Commons
  • Data related to Crinoid at Wikispecies
Agaricocrinus americanus

Agaricocrinus americanus, the mushroom crinoid, is a species of extinct crinoid, known only from its fossils, which are found in the U.S. states of Indiana, Tennessee and Kentucky. They date back to the Lower Mississippian, about 345 million years ago.

Allogalathea elegans

Allogalathea elegans (known as the feather star squat lobster, crinoid squat lobster or elegant squat lobster) is a species of squat lobster that is sometimes kept in marine aquariums.

Brassfield Formation

The Brassfield Formation, named by A.F. Foerste in 1906, is a limestone and dolomite formation exposed in Arkansas, Ohio, Kentucky, Indiana, Tennessee and West Virginia in the United States. It is Early Silurian (Aeronian, Llandoverian) in age and well known for its abundant echinoderms, corals and stromatoporoids. In Ohio, where the unit has escaped dolomitization, the Brassfield is an encrinite biosparite with numerous crinoid species.

Camerata (Crinoidea)

The Camerata or camerate crinoids are an extinct subclass of Paleozoic stalked crinoids. They originated during the Early Ordovician, reached their maximum diversity during the Mississippian and became extinct during the Permian–Triassic extinction event.Anatomically, they are distinguished by:

fused junctions between the plates of the cup

brachial plates incorporated into the cup

tegmen forming a rigid roof over the mouth

no less than ten and sometimes a very large number of free arms, often pinnulate

Cirrus (biology)

In biology, a cirrus SIRR-əs, plural cirri, SIRR-eye, (from the Latin cirrus meaning a curl-like tuft or fringe) is a long, thin structure in an animal similar to a tentacle but generally lacking the tentacle's strength, flexibility, thickness, and sensitivity.

In the sheep liver fluke, for example, the cirrus is the worm's muscular penis and when not in use is retained within a cirrus sac or pouch near the animal's head. The same structure exists in the various Taenia species of tapeworm. In the clam worms, however, the cirrus is the tentacular process or growth on each of the feet (parpodia), either the dorsal cirrus or the ventral cirrus, and has nothing to do with reproduction.Among the ribbonworms, the caudal cirrus is a small thread-like growth at the posterior end of the worm. Among the bristleworms, a cirrus is a tentacular growth near the head or notopodium containing sense organs and may be either dorsal, ventral, or lamellar. Among feather stars or barnacles, a cirrus is a long slender gripping or feeding appendage.In sea lilies, the cirri are the thin strands that line the animal's stalk. Among the tube blennies, a cirrus is a long growth extending from above the eye (a supraorbital cirrus) or extending below the neck-region (a nuchal cirrus). In a nautilus, each of the animal's tentacles is composed of a thin flexible cirrus and the corresponding hardened and protective cirrus sheath into which the cirri may be withdrawn.

Comatulida

Comatulida is an order of crinoids. Members of this order are known as feather stars and mostly do not have a stalk as adults. The oral surface with the mouth is facing upwards and is surrounded by five, often divided rays with feathery pinnules. Comatulids live on the seabed and on reefs in tropical and temperate waters.

Cyathocrinites

Cyathocrinites is an extinct genus of crinoids that lived from the Early Silurian to the Late Permian in Europe and North America.

Dimerocrinites

Dimerocrinites is an extinct genus of crinoids that lived from the Silurian to the Early Devonian of Australia and North America.

Encrinus

Encrinus is an extinct genus of crinoids, and "one of the most famous". It lived during the Middle Triassic, and its fossils have been found in Europe.

Eretmocrinus

Eretmocrinus is an extinct genus of crinoids.

Eucalyptocrinites

Eucalyptocrinites is an extinct genus of crinoid that lived from the Silurian to the Middle Devonian. Its remains have been found in Asia, Australia, Europe, and North America.

Glyptocrinus

Glyptocrinus is an extinct genus of sea lily that lived from the Middle Ordovician to the Early Silurian (471.8 - 436.0 Ma). Its remains have been found in North America.

Iocrinus

Iocrinus is an extinct genus of crinoid (sea lilies and feather stars). It is an early form of crinoid, from the Ordovician rock of North America, England, and Gilwern Hill, Powys in Wales.

List of crinoid genera

This list of crinoid genera is an attempt to create a comprehensive listing of all genera that have ever been considered to be crinoids, excluding purely vernacular terms. The list includes all commonly accepted genera, but also genera that are now considered invalid, doubtful (nomina dubia), or were not formally published (nomina nuda), as well as junior synonyms of more established names, and genera that are no longer considered crinoids.

Marsupiocrinus

Marsupiocrinus is an extinct genus of crinoids that lived from the Silurian to the Early Devonian in North America.

Pentacrinites

Pentacrinites is an extinct genus of crinoids that lived from the Middle Triassic to the Eocene of Asia, Europe, North America, and New Zealand. Their stems are pentagonal to star-shaped in cross-section and are the most commonly preserved parts. Pentacrinites are commonly found in the Pentacrinites Bed of the Early Jurassic (Lower Lias) of Lyme Regis, Dorset, England. Pentacrinites can be recognized by the extensions (or cirri) all around the stem, which are long, unbranching, and of increasing length further down, the very small cup and 5 long freely branching arms.

Platycrinites

Platycrinites are an extinct genus of Paleozoic stalked crinoids belonging to the family Platycrinitidae.These stationary upper-level epifaunal suspension feeders lived during the Devonian, Permian and the Carboniferous periods, from 376.1 to 259.0 Ma.

Taxocrinus

Taxocrinus is an extinct genus of crinoids.

Uintacrinus

Uintacrinus ("crinoid from the Uinta Mountains") is an extinct genus of crinoids from the Cretaceous of Kansas. It was unusual among crinoids because it had no stalk, and probably floated above the seafloor. It lived in the Western Interior Seaway. This crinoid was a colonial animal with ten long arms each that it used to capture prey.

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