Oligobrachia | |
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Scientific classification ![]() | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Annelida |
Clade: | Pleistoannelida |
Clade: | Sedentaria |
Order: | Sabellida |
Family: | Siboglinidae |
Genus: | Oligobrachia Ivanov, 1957 |
Oligobrachia is a genus in the family Siboglinidae , [1] commonly known as beard worms. These beard worms are typically found at spreading centers, hydrothermal vents, and undersea volcanoes. [2] The Siboglinidae are annelids that can often be found buried in sediments.
Beard worms do not inhabit one specific part of the world's oceans but are distributed across ocean floors as long as the surrounding environmental conditions are suitable; these populations are referred to as metapopulations. [3] Most commonly, these organisms are found on the ocean floor, at depths ranging from approximately 25 meters to several hundred meters. [4]
Oligobrachia is typically associated with hydrothermal vents and methane seeps. A notable characteristic of this genus is the absence of a mouth and gut. Instead, these worms rely on symbiotic bacteria to provide them with energy necessary for survival.
The majority of Oligobrachia specimens observed have been found in the Arctic and other high-latitude regions of the world's oceans. [5]
Oligobrachia, like all genera within the Siboglinidae family, lack a mouth and gut. To compensate, this family has evolved a symbiotic relationship with bacteria. [6] These symbionts provide up to half of the DNA required by their tubeworm hosts.
Unlike vertical transmission, where DNA is passed directly from parent to offspring, these symbionts are shared among individuals within a generation through a process known as horizontal transmission. [7] This method of symbiont acquisition can be an evolutionary costly trait, as changing environmental conditions may impact the availability or functionality of these symbiotic bacteria. [8]
Even hydrothermal vents, which are hypothesized to be among the most stable environments on Earth, can undergo changes that alter the proportion of chemicals in the area. in the area. The genus Oligobrachia has evolved specialized cells that provide a habitat for the endosymbiotic bacteria on which the tube worm relies for survival.
Depending on the habitat where Oligobrachia resides—whether near a hydrothermal vent or an undersea volcano—the endosymbiotic bacteria oxidize methane, sulfide, or other dominant chemicals present in the water.
Studies have shown that Oligobrachia can select specific types of endosymbiotic bacteria that best suit their environmental conditions. These bacteria can be either thioautotrophic (utilizing sulfide as an energy source) or methanotrophic (utilizing methane as an energy source). [4]
Oligobrachia residing near undersea volcanoes are more likely to select thioautotrophic endosymbiotic bacteria, while those living near hydrothermal vents are more likely to select methanotrophic bacteria.
Some studies have explored hemoglobin production in beard worms. These studies have determined that the site of hemoglobin production is located in the peritoneal membrane of the posterior body. Although research on this process in tubeworms is limited, the findings consistently point to the peritoneal membrane as the site of hemoglobin synthesis. [9]
Among known deep sea organisms, tubeworms are some of the most extensively studied. Research on their nervous system has primarily focused on the central nervous system rather than the peripheral nervous system.
Studies have identified three main features of tubeworm sensory systems: epidermal solitary sensory cells, sensory spots, and structures presumed to be sensory organs. The lack of diversity observed in the nervous systems of the studied tubeworms may provide insights into the evolutionary origin of the genus Oligobrachia. [10]
Siboglinidae is one of the most extensively studied families of deep sea marine organisms. During the development of tubeworms, they form a structure known as the trophophore, a specialized part of the body that hosts their endosymbiotic bacteria.
It has been hypothesized that the trophophore develops in response to the needs of these bacteria, which rely on this feature of the tubeworm’s internal anatomy to perform metabolic processes that Siboglinidae cannot carry out on their own. As previously mentioned, Siboglinidae lack a mouth and gut, so the endosymbiotic bacteria perform these essential processes in exchange for a protected habitat. [11]
Studies on the development of Oligobrachia have also observed this species incubating embryos. [12]
Symbiosis is any type of a close and long-term biological interaction, between two organisms of different species. The two organisms, termed symbionts, can be either in a mutualistic, a commensalistic, or a parasitic relationship. In 1879, Heinrich Anton de Bary defined symbiosis as "the living together of unlike organisms".
Siboglinidae is a family of polychaete annelid worms whose members made up the former phyla Pogonophora and Vestimentifera. The family is composed of around 100 species of vermiform creatures which live in thin tubes buried in sediment (Pogonophora) or in tubes attached to hard substratum (Vestimentifera) at ocean depths ranging from 100 to 10,000 m. They can also be found in association with hydrothermal vents, methane seeps, sunken plant material, and whale carcasses.
Any worm that lives in a marine environment is considered a water worm. Marine worms are found in several different phyla, including the Platyhelminthes, Nematoda, Annelida, Chaetognatha, Hemichordata, and Phoronida. For a list of marine animals that have been called "sea worms", see sea worm.
Hydrothermal vents are fissures on the seabed from which geothermally heated water discharges. They are commonly found near volcanically active places, areas where tectonic plates are moving apart at mid-ocean ridges, ocean basins, and hotspots. The dispersal of hydrothermal fluids throughout the global ocean at active vent sites creates hydrothermal plumes. Hydrothermal deposits are rocks and mineral ore deposits formed by the action of hydrothermal vents.
A cold seep is an area of the ocean floor where seepage of fluids rich in hydrogen sulfide, methane, and other hydrocarbons occurs, often in the form of a brine pool. Cold does not mean that the temperature of the seepage is lower than that of the surrounding sea water; on the contrary, its temperature is often slightly higher. The "cold" is relative to the very warm conditions of a hydrothermal vent. Cold seeps constitute a biome supporting several endemic species.
Riftia pachyptila, commonly known as the giant tube worm and less commonly known as the giant beardworm, is a marine invertebrate in the phylum Annelida related to tube worms commonly found in the intertidal and pelagic zones. R. pachyptila lives on the floor of the Pacific Ocean near hydrothermal vents. The vents provide a natural ambient temperature in their environment ranging from 2 to 30 °C, and this organism can tolerate extremely high hydrogen sulfide levels. These worms can reach a length of 3 m, and their tubular bodies have a diameter of 4 cm (1.6 in).
Osedax is a genus of deep-sea siboglinid polychaetes, commonly called boneworms, zombie worms, or bone-eating worms. Osedax is Latin for "bone-eater". The name alludes to how the worms bore into the bones of whale carcasses to reach enclosed lipids, on which they rely for sustenance. They utilize specialized root tissues for bone-boring. It is possible that multiple species of Osedax reside in the same bone. Osedax worms are also known to feed on the collagen itself by making holes in the whale's skeletal structure. These holes can also serve as a form of protection from nearby predators.
Symbiotic bacteria are bacteria living in symbiosis with another organism or each other. For example, rhizobia living in root nodules of legumes provide nitrogen fixing activity for these plants.
Horizontal transmission is the transmission of organisms between biotic and/or abiotic members of an ecosystem that are not in a parent-progeny relationship. Because the evolutionary fate of the agent is not tied to reproductive success of the host, horizontal transmission tends to evolve virulence. It is therefore a critical concept for evolutionary medicine.
Lamellibrachia is a genus of tube worms related to the giant tube worm, Riftia pachyptila. They live at deep-sea cold seeps where hydrocarbons leak out of the seafloor, and are entirely reliant on internal, sulfide-oxidizing bacterial symbionts for their nutrition. The symbionts, gammaproteobacteria, require sulfide and inorganic carbon. The tube worms extract dissolved oxygen and hydrogen sulfide from the sea water with the crown of plumes. Species living near seeps can also obtain sulfide through their "roots", posterior extensions of their body and tube. Several sorts of hemoglobin are present in the blood and coelomic fluid to bind to the different components and transport them to the symbionts.
Colleen Marie Cavanaugh is an American academic microbiologist best known for her studies of hydrothermal vent ecosystems. As of 2002, she is the Edward C. Jeffrey Professor of Biology in the Department of Organismic and Evolutionary Biology at Harvard University and is affiliated with the Marine Biological Laboratory and the Woods Hole Oceanographic Institution. Cavanaugh was the first to propose that the deep-sea giant tube worm, Riftia pachyptila, obtains its food from bacteria living within its cells, an insight which she had as a graduate student at Harvard. Significantly, she made the connection that these chemoautotrophic bacteria were able to play this role through their use of chemosynthesis, the biological oxidation of inorganic compounds to synthesize organic matter from very simple carbon-containing molecules, thus allowing organisms such as the bacteria to exist in deep ocean without sunlight.
Lamellibrachia luymesi is a species of tube worms in the family Siboglinidae. It lives at deep-sea cold seeps where hydrocarbons are leaking out of the seafloor. It is entirely reliant on internal, sulfide-oxidizing bacterial symbionts for its nutrition. These are located in a centrally located "trophosome".
A trophosome is a highly vascularised organ found in some animals that houses symbiotic bacteria that provide food for their host. Trophosomes are contained by the coelom of tube worms and in the body of symbiotic flatworms of the genus Paracatenula.
Gigantopelta chessoia is a species of deep sea snail from hydrothermal vents, a marine gastropod mollusk in the family Peltospiridae.
Olavius algarvensis is a species of gutless oligochaete worm in the family Tubificidae which depends on symbiotic bacteria for its nutrition.
Microbial symbiosis in marine animals was not discovered until 1981. In the time following, symbiotic relationships between marine invertebrates and chemoautotrophic bacteria have been found in a variety of ecosystems, ranging from shallow coastal waters to deep-sea hydrothermal vents. Symbiosis is a way for marine organisms to find creative ways to survive in a very dynamic environment. They are different in relation to how dependent the organisms are on each other or how they are associated. It is also considered a selective force behind evolution in some scientific aspects. The symbiotic relationships of organisms has the ability to change behavior, morphology and metabolic pathways. With increased recognition and research, new terminology also arises, such as holobiont, which the relationship between a host and its symbionts as one grouping. Many scientists will look at the hologenome, which is the combined genetic information of the host and its symbionts. These terms are more commonly used to describe microbial symbionts.
Tevnia is a genus of giant tube worm in the family Siboglinidae, with only one species, Tevnia jerichonana, living in a unique deep-sea environment. These deep sea marine species survive in environments like hydrothermal vents. These vents give off gas and toxic chemicals with the addition of having superheated temperatures. The giant tube worm prefers environments such as these despite the harsh temperature and toxic sea water.
Armophorea is a class of ciliates in the subphylum Intramacronucleata. . It was first resolved in 2004 and comprises three orders: Metopida, Clevelandellida, and Armophorida. Previously members of this class were thought to be heterotrichs because of similarities in morphology, most notably a characteristic dense arrangement of cilia surrounding their oral structures. However, the development of genetic tools and subsequent incorporation of DNA sequence information has led to major revisions in the evolutionary relationships of many protists, including ciliates. Metopids, clevelandellids, and armophorids were grouped into this class based on similarities in their small subunit rRNA sequences, making them one of two so-called "riboclasses" of ciliates, however, recent analyses suggest that Armophorida may not be related to the other two orders.
Lamellibrachia satsuma is a vestimentiferan tube worm that was discovered near a hydrothermal vent in Kagoshima Bay, Kagoshima at the depth of only 82 m (269 ft) the shallowest depth record for a vestimentiferan. Its symbiotic sulfur oxidizer bacteria have been characterised as ε-Proteobacteria and γ-Proteobacteria. Subspecies have been later found associated with cold seeps at Hatsushima in Sagami Bay and at the Daini Tenryu Knoll in the Nankai Trough with specimens obtained at up to 1,170 m (3,840 ft) depth.
Frenulata, "beard worms", is a clade of Siboglinidae, "tube worms". They are one of four lineages with numerous species. They may be the most basal clade in the family. Despite being the first tube worms to be encountered and described, they remain the least studied group. This is because of their slender shape, they often get destroyed as a result of being caught as bycatch or poor preservation. They are found primarily in deep, muddy sediments, cold seeps, and anoxic firth sediments.