Encrinus

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Encrinus
Temporal range: Late Silurian-Late Triassic, 428.2–215.6  Ma [1]
Encrinus liliiformis.JPG
Encrinus fossils on display at the Paläontologisches Museum München
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Echinodermata
Class: Crinoidea
Order: Encrinida
Family: Encrinidae
Genus: Encrinus
Andreae, 1764 [2]

Encrinus is an extinct genus of crinoids, and "one of the most famous". [3] It lived during the Late Silurian-Late Triassic, and its fossils have been found in Europe. [1]

Contents

History

Fossils of Encrinus went by several names in Germany before the establishment of modern paleontology. In Lower Saxony, they were called Sonnenräder ("sun wheels"), while in Thuringia and Hesse they were called Bonifatiuspfennige ("Saint Boniface's pennies"). In southwestern Germany, they went by Hexengeld ("witches' money"). The animal was correctly reconstructed for the first time in 1729, although various parts of the animal had been described before that. [4]

Encrinus was described in 1764 by Johann Gerhard Reinhard Andreae. It was assigned to the order Encrinida by Jack Sepkoski in 2002. [2]

Description

E. liliiformis with parts labeled, based on Douglas et al. 2009 Encrinus liliiformis with markup.jpg
E. liliiformis with parts labeled, based on Douglas et al. 2009

Encrinus possessed a large cup- [1] or crown-like structure at the top of its body, which has been described as resembling "an unopened tulip." [3] This "cup" could be between 1.5 inches (3.8 cm) and 2.25 inches (5.7 cm) long. The structure displayed "five-fold symmetry" and had a slightly concave base. It bore ten arms [1] (although in some species, such as E. carnallis, it bore 20), [5] which in turn bore many small branches (pinnules). When opened, the arms and pinnules formed a kind of "feeding fan", used to catch prey such as plankton. [1] "Microscopic interpinnular channels" suggest that Encrinus may have been an active filter feeder, creating its own currents by beating its cilia. It is known that the arms could shut tightly in life (most Encrinus fossils are found in this position), but it is difficult to estimate the greatest angle at which they could open. It is possible that specimens recorded as being widest open demonstrate the normal angle of opening in life. [3] A tegmen ("small leathery dome") covered the mouth and topped the cup. Any particles of food that the animal caught would be passed down the arms and below the tegmen via grooves, eventually leading to cilia, which in turn led to the mouth. When viewed from above, the stem was circular in shape. Large and small ossicles covered the stem, creating a pattern of frequent small ossicles sandwiched between the large ones. [1] The stem did not possess any cirri, and may have been held in place by roots of some sort. The breakage of the stem during the animal's life was a common occurrence, and it often survived long enough to form a new end on its shortened stem. [3] Being from the Middle Triassic, Encrinus is the last known from its group of crinoids, as most others died out during the Permian–Triassic extinction event. [1]

See also

Related Research Articles

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An echinoderm is any animal of the phylum Echinodermata, which includes starfish, brittle stars, sea urchins, sand dollars and sea cucumbers, as well as the sessile sea lilies or "stone lilies". While bilaterally symmetrical as larvae, as adults echinoderms are recognisable by their usually five-pointed radial symmetry, and are found on the sea bed at every ocean depth from the intertidal zone to the abyssal zone. The phylum contains about 7,600 living species, making it the second-largest group of deuterostomes after the chordates, as well as the largest marine-only phylum. The first definitive echinoderms appeared near the start of the Cambrian.

<span class="mw-page-title-main">Crinoid</span> Class of echinoderms

Crinoids are marine invertebrates that make up the class Crinoidea. Crinoids that remain attached to the sea floor by a stalk in their adult form are commonly called sea lilies, while the unstalked forms, called feather stars or comatulids, are members of the largest crinoid order, Comatulida. Crinoids are echinoderms in the phylum Echinodermata, which also includes the starfish, brittle stars, sea urchins and sea cucumbers. They live in both shallow water and in depths over 9,000 metres (30,000 ft).

<span class="mw-page-title-main">Entoprocta</span> Phylum of aquatic invertebrates

Entoprocta, or Kamptozoa, is a phylum of mostly sessile aquatic animals, ranging from 0.1 to 7 millimetres long. Mature individuals are goblet-shaped, on relatively long stalks. They have a "crown" of solid tentacles whose cilia generate water currents that draw food particles towards the mouth, and both the mouth and anus lie inside the "crown". The superficially similar Bryozoa (Ectoprocta) have the anus outside a "crown" of hollow tentacles. Most families of entoprocts are colonial, and all but 2 of the 150 species are marine. A few solitary species can move slowly.

<span class="mw-page-title-main">Articulata (Crinoidea)</span> Subclass of crinoids

Articulata are a subclass or superorder within the class Crinoidea, including all living crinoid species. They are commonly known as sea lilies or feather stars. The Articulata are differentiated from the extinct subclasses by their lack of an anal plate in the adult stage and the presence of an entoneural system. Articulata first appeared in the fossil record during the Triassic period although other, now extinct crinoid groups, originated in the Ordovician.

<i>Pentacrinites</i> Extinct genus of crinoids

Pentacrinites is an extinct genus of crinoids that lived from the Hettangian to the Bathonian 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 of Lyme Regis, Dorset, England. Pentacrinites can be recognized by the extensions all around the stem, which are long, unbranching, and of increasing length further down, the very small cup and 5 long freely branching arms.

<span class="mw-page-title-main">Brachiopod</span> Phylum of marine animals also known as lamp shells

Brachiopods, phylum Brachiopoda, are a phylum of trochozoan animals that have hard "valves" (shells) on the upper and lower surfaces, unlike the left and right arrangement in bivalve molluscs. Brachiopod valves are hinged at the rear end, while the front can be opened for feeding or closed for protection. Two major categories are traditionally recognized, articulate and inarticulate brachiopods. The word "articulate" is used to describe the tooth-and-groove structures of the valve-hinge which is present in the articulate group, and absent from the inarticulate group. This is the leading diagnostic skeletal feature, by which the two main groups can be readily distinguished as fossils. Articulate brachiopods have toothed hinges and simple, vertically oriented opening and closing muscles. Conversely, inarticulate brachiopods have weak, untoothed hinges and a more complex system of vertical and oblique (diagonal) muscles used to keep the two valves aligned. In many brachiopods, a stalk-like pedicle projects from an opening near the hinge of one of the valves, known as the pedicle or ventral valve. The pedicle, when present, keeps the animal anchored to the seabed but clear of sediment which would obstruct the opening.

<i>Antedon bifida</i> Species of crinoid

Antedon bifida is a species of crinoid in the family Antedonidae commonly known as the rosy feather star. It is found in north west Europe.

<span class="mw-page-title-main">Comatulida</span> Order of crinoids

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<i>Davidaster rubiginosus</i> Species of crinoid

Davidaster rubiginosus, the orange sea lily, is a species of crinoid in the family Comatulidae. At one time it was classified as Nemaster rubiginosa but the World Register of Marine Species has determined that the valid name is Davidaster rubiginosus. It is found on reefs in the tropical western Atlantic and the Caribbean Sea.

<i>Davidaster discoideus</i> Species of crinoid

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<i>Metacrinus rotundus</i> Species of crinoid

Metacrinus rotundus, the Japanese sea lily, is a species of stalked crinoid in the family Isselicrinidae. It is a species found off the west coast of Japan, near the edge of the continental shelf at a depth of around 100 to 150 metres deep. This is the shallowest-living species among the extant stalked crinoids.

<i>Antedon mediterranea</i> Species of crinoid

Antedon mediterranea is a species of stalkless crinoid in the family Antedonidae, commonly known as the Mediterranean feather star. It is found on the seabed at moderate depths in the Mediterranean Sea. It is a filter feeder and captures plankton with its long feathery arms.

<span class="mw-page-title-main">Bourgueticrinida</span> Extinct order of crinoids

Bourgueticrinida is an order of crinoids that typically live deep in the ocean. Members of this order are attached to the seabed by a slender stalk and are known as sea lilies. While other groups of crinoids flourished during the Permian, bourgueticrinids along with other extant orders did not appear until the Triassic, following a mass extinction event in which nearly all crinoids died out.

<i>Cenocrinus</i> Genus of crinoids

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<i>Ptilometra australis</i> Species of crinoid

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<i>Synapta maculata</i> Species of sea cucumber

Synapta maculata, the snake sea cucumber, is a species of sea cucumber in the family Synaptidae. It is found in shallow waters in the tropical Indo-Pacific Ocean. Sometimes growing as long as 3 m (10 ft), it is one of the longest sea cucumbers in the world.

<i>Promachocrinus kerguelensis</i> Species of crinoids

Promachocrinus kerguelensis is a species of free-swimming, stemless crinoids. It was the only member of its genus until several species were discovered in 2023. P. keruguelensis a coldwater crinoid which is found in the seas around Antarctica and surrounding island groups, including under the sea ice.

<i>Aporometra wilsoni</i> Species of crinoid

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<i>Notocrinus virilis</i> Species of crinoid

Notocrinus virilis is a marine invertebrate, a species of crinoid or feather star in the family Notocrinidae. It is found in deep water in the Southern Ocean around the coasts of Antarctica and adjacent islands. A sea snail sometimes parasitizes it.

<span class="mw-page-title-main">Flexibilia</span> Superorder of crinoids

Flexibilia is a superorder of specialized Paleozoic crinoids. They exhibited a conserved body plan and consistent suite of characteristics throughout their long history. Previously considered a subclass with unclear affinities, later investigation determined that flexibles are well-nested within Cladida, a broad group ancestral to living articulate crinoids. The Ordovician cladid Cupulocrinus acts as an intermediate form linking the generalized anatomy of other early cladids with the distinctive anatomy of flexibles, and several studies have considered it to be ancestral to the rest of the group. Although flexibles never reached the same abundance or diversity as many other crinoid groups, they remained a reliable component of crinoid faunas, particularly from the Silurian onwards. Flexible fossils are very rare in the Ordovician, but the Late Ordovician appears to have been an interval of rapid diversification for the group.

References

  1. 1 2 3 4 5 6 7 Palmer, Douglas; et al. (2009). Prehistoric Life: The Definitive Visual History of Life on Earth (first American ed.). New York: Dorling Kindersley. p. 205. ISBN   978-0-7566-5573-0.
  2. 1 2 "Encrinus". The Paleobiology Database . Retrieved March 21, 2012.
  3. 1 2 3 4 Jefferies, R. P. S. (1989). "The Arm Structure and Mode of Feeding of the Triassic Crinoid Encrinus liliiformis" (PDF). Palaeontology . 32 (3). The Palaeontological Association: 483–97. Retrieved March 25, 2012.[ permanent dead link ]
  4. Hess, Hans; Ausich, William I.; Brett, Carlton E.; Simms, Michael J. (1999). "Triassic Muschelkalk of Central Europe" (Google eBook). Fossil Crinoids (illustrated ed.). Cambridge University Press. pp. 164–7. ISBN   0-521-45024-1 . Retrieved March 23, 2012.
  5. Lehmann, Ulrich; Hillmer, Gero (1983). Fossil Invertebrates (Google eBook). Cambridge Earth Science Series. Cambridge University Press. p. 279. ISBN   0-521-27028-6 . Retrieved March 23, 2012.