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Siboglinidae

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Siboglinidae

Siboglinidae
Riftia pachyptila
Scientific classification
Kingdom: Animalia
Subkingdom: Eumetazoa
Phylum: Annelida
Class: Polychaeta
Subclass: Palpata
Order: Canalipalpata
Family: Siboglinidae
Caullery, 1914
Genera

See text.

Siboglinidae, also known as the beard worms, is a family of polychaete annelid worms whose members made up the former phyla Pogonophora (the giant tube worms) and Vestimentifera.[1][2] They are composed of about 100 species of vermiform creatures and live in thin tubes buried in sediments at ocean depths from 100 to 10,000 m. They can also be found in association with hydrothermal vents, methane seeps, with sunken plant material or whale carcasses.

The first specimen was dredged from the waters of what is now Indonesia in 1900. These specimens were given to French zoologist Maurice Caullery, who studied them for nearly 50 years.

Anatomy

Most siboglinids are less than 1 millimetre (0.04 in) in diameter but 10–75 centimetres (3.9–29.5 in) in length. They inhabit tubular structures composed of chitin and fixed to the bottom. The tubes are often clustered together in large colonies.[3]

The body is divided into four regions. The anterior end is called the cephalic lobe, which bears from 1 to over 200 thin branchial ciliated tentacles, each bearing tiny side branches known as pinnules. Behind this is a glandular forepart, which helps to secrete the tube. The main part of the body is the trunk, which is greatly elongated and bears various annuli, papillae, and ciliary tracts. Posterior to the trunk is the short metamerically segmented opisthosoma, bearing external paired chaetae, which apparently help to anchor the animal to the base of its tube.[3]

The body cavity has a separate compartment in each of the first three regions of the body, and extends into the tentacles. The opisthoma has a coelomic chamber in each of its 5 to 23 segments, separated by septa. The worms have a complex closed circulatory system and a well-developed nervous system, but as adults, siboglinids completely lack a mouth, gut and anus.[4]

Siboglinids are dioecious, with one gonad on each side of the trunk, within the body cavity. The fertilised eggs develop within the tubes, and hatch to produce small ciliated worm-like larvae.[3]

Evolution

The family Siboglinidae has been difficult to place in an evolutionary context.[5] By examining genetic differences between annelids there is now a scientific consensus that Siboglinidae is a family within the order Polychaeta.[6] The fossil record along with molecular clocks suggests the family has Mesozoic (250 mya - 66 mya) or Cenozoic (66 mya - recent) origins.[5] Examination of molecular work aligning five genes has made clear that there are four distinct clades within Siboglinidae.[7][8][9] The clades are vestimentiferans, Sclerolinum, frenulates, and Osedax.[8] These clades represent the four tracks evolution has followed within Siboglinidae.[8] Vestimentiferans live in vent and seep habitats.[8] Sclerolinum is a monogeneric clade living on organic-rich remains.[5] Frenulates live in organic-rich sediment habitats.[10] Osedax is a monogeneric clade specialized in living on whale bones, although recently there has been evidence of them living on fish bones as well.[11]

Vestimentiferans

Like other tube worms, vestimentiferans are marine and [4] A more recent study of three species of tubeworms including Riftia pachyptila demonstrated that the bacteria actually infect juvenile worms through their skin. Their body is divided into four regions; the obturaculum, vestimentum, trunk, and opisthosome.

Discovery of the hydrothermal vents in the eastern Pacific Ocean was quickly followed by the discovery and description of new vestimentiferan tubeworm species. These tubeworms are one of the most dominant organisms associated with the hydrothermal vents in the Pacific Ocean. Tubeworms anchor themselves to the substratum of the hydrocarbon seep by roots located at the basal portion of their bodies.[12] Intact tubeworm roots have proven very difficult to obtain for study because they are extremely delicate, and often break off when a tubeworm is removed from hypothermal vent regions. It is unsure how long the roots of the tube worms can grow to, but root have been recovered longer than 30 m in length. A single aggregation of tubeworms can contain thousands of individuals, and the roots produced by each tubeworm can become tangled with the roots of neighbouring tubeworms.[13] These mats of roots are known as “ropes”, and travel down the tubes of dead tubeworms, and run through holes in rocks. The diameter and wall thickness of the tubeworm roots do not appear to change with distance from the trunk portion of the tubeworms body. Like the trunk portion of the body, the roots of the Vestimentiferans tubeworms are composed of chitin crystallites, which support and protect the tubeworm from predation and environmental stresses. The Vestimenifera tubeworms build the external chitin structure themselves by secreting chitin from specialized glands located in their body walls.

Genera in the family Siboglinidae

References

  1. ^ Shigeaki Kojima, Tetsuo Hashimoto, Masami Hasegawa, Shigenori Murata, Suguru Ohta, Humitake Seki and Norihiro Okada (July 1993). "Close phylogenetic relationship between vestimentifera (tube worms) and annelida revealed by the amino acid sequence of elongation factor-lα". Journal of Molecular Evolution 37 (1): 66–70.  
  2. ^ a b c d Rouse G.W. (2001). "A cladistic analysis of Siboglinidae Caullery, 1914 (Polychaeta, Annelida): formerly the phyla Pogonophora and Vestimentifera". Zoological Journal of the Linnean Society 132 (1): 55–80.  
  3. ^ a b c Barnes, Robert D. (1982). Invertebrate Zoology. Philadelphia, PA: Holt-Saunders International. pp. 862–863.  
  4. ^ a b  
  5. ^ a b c d Hilário, Ana; Capa, María; Dahlgren, Thomas G.; Halanych, Kenneth M.; Little, Crispin T. S.; Thornhill, Daniel J.; Verna, Caroline; Glover, Adrian G. (2011). Laudet, Vincent, ed. "New Perspectives on the Ecology and Evolution of Siboglinid Tubeworms". PLoS ONE 6 (2): e16309.  
  6. ^ Struck, T. H., Schult, N., Kusen, T., Hickman, E., Bleidorn, C., McHugh, D., and Halanych, K. M. (2007). "Annelid phylogeny and the status of Sipuncula and Echiura". BMC Evol Biol 7: 57.  
  7. ^ Black, M. B., K. M. Halanych, P. A. Y. Maas, W. R. Hoeh, J. Hashimoto, D. Desbruyeres, R. A. Lutz et al. (1997). "Molecular systematics of vestimentiferan tubeworms from hydrothermal vents and cold-water seeps". Marine Biology 130 (2): 141–149.  
  8. ^ a b c d Glover, A. G., B. Kallstrom, C. R. Smith, and T. G. Dahlgren (2005). "World-wide whale worms? A new species of Osedax from the shallow north Atlantic". Proceedings of the Royal Society B-Biological Sciences 272 (1581): 2587–2592.  
  9. ^ Vrijenhoek, R. C., S. B. Johnson, and G. W. Rouse (2009). "A remarkable diversity of bone-eating worms (Osedax; Siboglinidae; Annelida)". BMC Biol 7: 74.  
  10. ^ Rodrigues, C. F., Hilario, A., Cunha, M. R., Weightman, A. J., and Webster, G. (2011). "Microbial diversity in Frenulata (Siboglinidae, Polychaeta) species from mud volcanoes in the Gulf of Cadiz (NE Atlantic)". Antonie Van Leeuwenhoek 100: 83–98.  
  11. ^ Rouse, G. W., Goffredi, S. K., Johnson, S. B., and Vrijenhoek, R. C. (2011). "Not whale-fall specialists, Osedax worms also consume fishbones". Biology Letters 7 (5): 736–739.  
  12. ^ Halanych, K., Maas, P., Hoeh, W., Hashimoto, J., Desbruyeres, D., Lutz, R., and Vrijenhoek, R. (1997). "Molecular systematics of vestimentiferan tubeworms from hydrothermal vents and cold-water seeps". Marine Biology 130 (2): 141.  
  13. ^ Julian, D., Gaill, F., Wood, E., Arp, A., and Fisher, C (1999). "Roots as a site of hydrogen sulphide uptake in the hydrocarbon seep vestimetiferan Lamellibrachia sp". The Journal of experimental biology 202 (Pt 17): 2245–57.  
  14. ^ Ana Hilário and Marina R. Cunha, On some frenulate species (Annelida: Polychaeta: Siboglinidae) from mud volcanoes in the Gulf of Cadiz (NE Atlantic)
  15. ^ Southward et al, Vestimentiferans (Pogonophora) in the PaciŽ c and Indian Oceans: a new genus from Lihir Island (Papua New Guinea) and the Java Trench, with the Ž rst report of Arcovestia ivanovi from the North Fiji Basin, J. Nat. Hist. 36: 1179-1197 (2002)
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