Cirratulidae

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Cirratulidae
Cirratulus cirratus.jpg
Cirratulus cirratus
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Annelida
Clade: Pleistoannelida
Subclass: Sedentaria
Order: Terebellida
Family: Cirratulidae
Carus, 1863
Genera [1]

See text

Cirratulidae is a family of marine polychaete worms. Members of the family are found worldwide, mostly living in mud or rock crevices. [2] Most are deposit feeders, but some graze on algae or are suspension feeders. [1] Although subject to multiple revisions over time, cirratulids are among the few polychaete clades with a verified fossil record.

Contents

Description

Cirratulids vary in size from one to twenty centimetres long. They are mostly burrowers in soft sediments but some live in rock crevices. The head is conical or wedge-shaped and has no antennae. The body is generally cylindrical, tapering at both ends. Cirratulids are characterised by a large number of simple elongate filaments along the body. Some of these occur as an anterior cluster of tentacles, grooved for deposit-feeding, but the majority, the branchiae, are found one pair per segment, and do not have grooves. The chaetae (bristles) are simple capillaries, usually with hooks, and emerge directly from the body wall. There are no anal cirri (slender sensory appendages). The worm is usually buried with only the writhing branchial filaments visible. [2] [3] Some cirratulids can build tubes of calcium carbonate [4] . A study by Guido et al. (2024) [5] reported cirratulid aggregates as the first known example in the animal kingdom of the so called double-phased biomineralization process.

When alive, the body, branchiae and tentacular filaments are often red, orange or yellow, though species of Dodecaceria are dark green or black. Terebellidae and other worm families may superficially look similar to cirratulids with a mass of filaments. However, in terebellids, the filaments arise from the mouth or are restricted to the anterior three segments, whereas cirratulid branchiae occur throughout the body, one pair per segment. [6]

Taxonomy

The genera are poorly defined and Blake undertook a partial revision in 1996. He divided them into three groups, the multi-tentaculate genera such as Cirratulus and Cirriformia, the bi-tentaculate soft-substrate genera such as Caulleriella, Chaetozone, Tharyx and the bi-tentaculate hard substrate genera such as Dodecaceria. [7]

There is considerable confusion as to the phylogenetic relationships in the family and Blake suggests that many species with global distributions will be found to represent species complexes within which some species are presently undescribed. [7]

Fossil record

The earliest cirratulid on record, Dodecaceria cretacea (Voigt, 1971), later reclassified as the ichnofossil Caulostrepsis cretacea, was responsible for leaving boring traces on Late Cretaceous coral reefs. [8] There's no known Paleocene record, but from the Eocene onwards, reports of cirratulid bioconstructions in South Africa and the Americas are relatively frequent. Two species within Diplochaetetes, D. longitubus (Weissermel, 1913) [9] and D. longitubus vermicularis (Weissermel, 1926) [10] , are known from Namibian sites. The species D. mexicanus (Wilson, 1986) was reported in Oligocene to Miocene fossiliferous sites across multiple locations in the pacific coasts of the Americas, from Mexico [11] to Peru [12] . Recent cirratulid bioconstructions found in the same areas are attributed to the genus Dodecaceria. [13]

Several authors, such as Reish (1952) [14] , Fischer et al. (1989 [15] , 2000 [13] ) and Guido et al. (2024) [5] have reported many similarities between Dodecaceria and Diplochaetetes bioconstructions, but whether the two genera should be considered synonyms or not remains unresolved.

Genera

Related Research Articles

<span class="mw-page-title-main">Polychaete</span> Class of annelid worms

Polychaeta is a paraphyletic class of generally marine annelid worms, commonly called bristle worms or polychaetes. Each body segment has a pair of fleshy protrusions called parapodia that bear many bristles, called chaetae, which are made of chitin. More than 10,000 species are described in this class. Common representatives include the lugworm and the sandworm or clam worm Alitta.

<span class="mw-page-title-main">Chaeta</span> Chitinous bristle found on annelid worms

A chaeta or cheta is a chitinous bristle or seta found on annelid worms, although the term is also frequently used to describe similar structures in other invertebrates such as arthropods. Polychaete annelids are named for their chaetae. In Polychaeta, chaetae are found as bundles on the parapodia, paired appendages on the side of the body. The chaetae are epidermal, extracellular structures, and clearly visible in most polychaetes. They are probably the best-studied structures in these animals. Segments bearing chaetae are called chaetigers.

<span class="mw-page-title-main">Eunicidae</span> Family of annelids

Eunicidae is a family of marine polychaetes. The family comprises marine annelids distributed in diverse benthic habitats across Oceania, Europe, South America, North America, Asia and Africa. The Eunicid anatomy typically consists of a pair of appendages near the mouth (mandibles) and complex sets of muscular structures on the head (maxillae) in an eversible pharynx. One of the most conspicuous of the eunicids is the giant, dark-purple, iridescent "Bobbit worm", a bristle worm found at low tide under boulders on southern Australian shores. Its robust, muscular body can be as long as 2 m. Eunicidae jaws are known from as far back as Ordovician sediments. Cultural tradition surrounds Palola worm reproductive cycles in the South Pacific Islands. Eunicidae are economically valuable as bait in both recreational and commercial fishing. Commercial bait-farming of Eunicidae can have adverse ecological impacts. Bait-farming can deplete worm and associated fauna population numbers, damage local intertidal environments and introduce alien species to local aquatic ecosystems.

<i>Spirobranchus giganteus</i> Species of marine tube worm

Spirobranchus giganteus, commonly known as the Christmas tree worm, is a tube-building polychaete worm belonging to the family Serpulidae.

<span class="mw-page-title-main">Serpulidae</span> Family of annelids

The Serpulidae are a family of sessile, tube-building annelid worms in the class Polychaeta. The members of this family differ from other sabellid tube worms in that they have a specialized operculum that blocks the entrance of their tubes when they withdraw into the tubes. In addition, serpulids secrete tubes of calcium carbonate. Serpulids are the most important biomineralizers among annelids. About 300 species in the family Serpulidae are known, all but one of which live in saline waters. The earliest serpulids are known from the Permian.

<span class="mw-page-title-main">Sabellidae</span> Family of annelid worms

Sabellidae, or feather duster worms, are a family of marine polychaete tube worms characterized by protruding feathery branchiae. Sabellids build tubes out of a tough, parchment-like exudate, strengthened with sand and bits of shell. Unlike the other sabellids, the genus Glomerula secretes a tube of calcium carbonate instead. Sabellidae can be found in subtidal habitats around the world. Their oldest fossils are known from the Early Jurassic.

<span class="mw-page-title-main">Terebellida</span> Order of annelid worms

Terebellida make up an order of the Polychaeta class, commonly referred to as "bristle worms". Together with the Sabellida, the Spionida and some enigmatic families of unclear taxonomic relationship, they make up the subclass Canalipalpata, one of the three main clades of polychaetes. Like most polychaetes, almost all members of the Terebellida are marine organisms. Most are small, sessile detritivores which live in small tubes they build from mud or similar substrate, or burrow in the sand. Their central nervous system displays characteristic apomorphies.

<i>Hesionidae</i> Family of annelids

Hesionidae are a family of phyllodocid "bristle worms". They are marine organisms. Most are found on the continental shelf; Hesiocaeca methanicola is found on methane ice, where it feeds on bacterial biofilms.

<i>Serpula</i> Genus of annelid worms

Serpula is a genus of sessile, marine annelid tube worms that belongs to the family Serpulidae. Serpulid worms are very similar to tube worms of the closely related sabellid family, except that the former possess a cartilaginous operculum that occludes the entrance to their protective tube after the animal has withdrawn into it. The most distinctive feature of worms of the genus Serpula is their colorful fan-shaped "crown". The crown, used by these animals for respiration and alimentation, is the structure that is most commonly seen by scuba divers and other casual observers.

<span class="mw-page-title-main">Arenicolidae</span> Family of annelids

Arenicolidae is a family of marine polychaete worms. They are commonly known as lugworms and the little coils of sand they produce are commonly seen on the beach. Arenicolids are found worldwide, mostly living in burrows in sandy substrates. Most are detritivores but some graze on algae.

<span class="mw-page-title-main">Biomineralising polychaete</span> Polychaetes that produce minerals

Biomineralising polychaetes are polychaetes that produce minerals to harden or stiffen their own tissues (biomineralize).

<i>Dodecaceria</i> Genus of annelid worms

Dodecaceria is a genus of marine polychaete worms in the family Cirratulidae. It's also one of the very few polychaete genera with a verified fossil record.

<i>Cirriformia</i> Genus of annelid worms

Cirriformia is a genus of marine polychaete worms in the family Cirratulidae.

<span class="mw-page-title-main">Chrysopetalidae</span> Family of annelids

Chrysopetalidae is a family of polychaete worms. The body is short or elongated, with few or numerous segments. All segments bear on their dorsal side a fan or a transverse row of paleae. The cephalic lobe has tentacles and eyes and the buccal segment has two or four tentacular cirri on each side. The parapodia are uniramous or biramous, with dorsal cirri upon all segments. The ventral bristles are compound.

<i>Aphelochaeta</i> Genus of annelids

Aphelochaeta is a genus of bitentaculate cirratulidan, or two-tentacled marine worms.

<span class="mw-page-title-main">Melinninae</span> Subfamily of annelid worms

Melinninae are a subfamily of the Ampharetidae, belonging to the Terebellida.

Austropolaria is a genus of marine annelids in the family Polynoidae. The genus includes a single species, Austropolaria magnicirrata, which is known only from the Amundsen Sea in the Southern Ocean, at depths of 1000 to 1500m.

Ysideria is a genus of marine polychaete worms belonging to the family Polynoidae, the scale worms. Ysideria contains a single species, Ysideria hastata which is known from the North Pacific Ocean off the coast of California at depths of about 50–60 m.

<span class="mw-page-title-main">Pleistoannelida</span> Clade of annelid worms

Pleistoannelida is a group of annelid worms that comprises the vast majority of the diversity in phylum Annelida. Discovered through phylogenetic analyses, it is the largest clade of annelids, comprised by the last common ancestor of the highly diverse sister groups Errantia and Sedentaria and all the descendants of that ancestor. Most groups in the Clade find their ancestors within the Cambrian explosion when Annelid diversity expanded dramatically. The Pleistoannelida clade covers a variety of traits. However, the evolution of simple to complex eyes, developed papillae for burrowing, and for some specialized radioles for feeding can be seen universally across every species. New findings have discovered the range of Annelid diversity have led to uncertainty if groups with developed ancestral traits should remain within the clade. Furthermore There's been a lack of recently discovered Annelid traits being used in the categorization of groups within the clade, leading to many hypothesis on how to do so and which should remain within the clade. Currently three smaller clades that were originally a part of the groups Errantia and Sedentaria have been proven to fall outside while still being connected to the basal groups.

<span class="mw-page-title-main">Olga Hartman</span> American invertebrate zoologist (1900–1974)

Olga Hartman was an American invertebrate zoologist and polychaetologist. She was a student of S. F. Light at the University of California, Berkeley, and later a staff researcher at the Allan Hancock Foundation and professor of biology at the University of Southern California. Active from the 1930s to the 1970s, Hartman specialized in Polychaeta, a class of marine annelid worms, and was known for her work as a cataloger and as a polychaete systematist. She is considered one of the top three most prolific authors in her field, having described 473 polychaete species during her lifetime.

References

  1. 1 2 World Register of Marine Species
  2. 1 2 Marine Species Identification Portal
  3. Cirratulidae
  4. Vinn, O. (2009). "The ultrastructure of calcareous cirratulid (Polychaeta, Annelida) tubes" (PDF). Estonian Journal of Earth Sciences. 58 (2): 153–156. doi: 10.3176/earth.2009.2.06 . Retrieved 2012-09-16.
  5. 1 2 Guido A, D'Amico F, DeVries TJ, Kočí T, Collareta A, Bosio G, Sanfilippo R (2024). "Double-phased controlled and influenced biomineralization in marine invertebrates: The example of Miocene to recent reef-building polychaete cirratulids from southern Peru". Palaeogeography, Palaeoclimatology, Palaeoecology. 639: 112060. doi:10.1016/j.palaeo.2024.112060.
  6. Polychaetes:Cirratulidae Archived 2011-09-29 at the Wayback Machine
  7. 1 2 Blake, J.A. (1996). Family Cirratulidae Ryckholdt, 1851. pp. 263-384 in Blake, J.A., Hilbig, B. & Scott, P.H. (eds) The Annelida. Part 3 Polychaeta: Orbiniidae to Cossuridae. Vol. 6. Taxonomic Atlas of the Benthic Fauna of the Santa Maria Basin and western Santa Barbara Channel. Santa Barbara Museum of Natural History : Santa Barbara, California
  8. Voigt E (1971). "Fremdskulpturen an Steinkernen von Polychaeten-Bohrgängen aus der Maastrichter Tuffkreide". Paläontologische Zeitschrift. 45(3-4): 144–153. doi:10.1007/BF02989572.
  9. Weissermel W (1913). "Uber tertiäre Versteinerungen von den Bogenfelser Diamantfeldern II. Tabulaten und Hydrozoen". Beiträge zur geologischen Erforschung der deutschen Schutzgebiete. 5: 84–111.
  10. Weissermel W (1926). "Neues uber Tabulaten, Hydrozoen und eine Hexakoralle aus dem Tertiar der Bogenfelser Diamantenfelder". Die Diamantenwuste Sudwest-Afrikas. (ed Kaiser, H.). 2: 88–106.
  11. Wilson EC (1986). "The first tertiary sclerosponge from the Americas". Palaeontology. 29(3): 577–583.
  12. Kočí T, Bosio G, Collareta A, Sanfilippo R, Ekrt B, Urbina M, Malinverno E (2021). "First report on the cirratulid (Annelida, Polychaeta) reefs from the Miocene Chilcatay and Pisco Formations (East Pisco Basin, Peru)". Journal of South American Earth Sciences. 107: 103042. doi:10.1016/j.jsames.2020.103042.
  13. 1 2 Fischer R, Pernet B, Reitner, J (2000). "Organomineralization of cirratulid annelid tubes-fossil and recent examples". Facies. 42: 35–49. doi:10.1007/BF02562565.
  14. Reish DJ (1952). "Discussion of the colonial tube-building polychaetous annelid Dodecaceria fistulicola Ehlers". Bulletin of the Southern California Academy of Sciences. 51: 103–107. doi:10.3160/0038-3872-51.3.103.
  15. Fischer R, Galli Oliver C, Reitner J (1989). "Skeletal structure, growth, and paleoecology of the patch reef-buildingpolychaete worm Diplochaetetes mexicanus wilson, 1986 from the oligocene of baja california (Mexico)". Geobios. 22(6): 761–775. doi:10.1016/S0016-6995(89)80071-3.