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"Organisms living within the deep sea have a variety of adaptations to survive in these conditions.\nOrganisms can survive in the deep sea through a number of feeding methods including scavenging, predation and filtration, with a number of organisms surviving by feeding on marine snow.\nExcept for the areas close to the hydrothermal vents, this energy comes from organic material drifting down from the photic zone. The sinking organic material is composed of algal particulates, detritus, and other forms of biological waste, which is collectively referred to as marine snow.\nInstead of relying on gas for their buoyancy, many deep-sea species have jelly-like flesh consisting mostly of glycosaminoglycans, which provides them with very low density.\nIt is also common among deep water squid to combine the gelatinous tissue with a flotation chamber filled with a coelomic fluid made up of the metabolic waste product ammonium chloride, which is lighter than the surrounding water.\nThe midwater fish have special adaptations to cope with these conditions—they are small, usually being under 25 centimetres (10 in); they have slow metabolisms and unspecialized diets, preferring to sit and wait for food rather than waste energy searching for it. They have elongated bodies with weak, watery muscles and skeletal structures. They often have extendable, hinged jaws with recurved teeth.\nBecause of the sparse distribution and lack of light, finding a partner with which to breed is difficult, and many organisms are hermaphroditic.\nBecause light is so scarce, fish often have larger than normal, tubular eyes with only rod cells. Their upward field of vision allows them to seek out the silhouette of possible prey.\nPrey fish however also have adaptations to cope with predation. These adaptations are mainly concerned with reduction of silhouettes, a form of camouflage. The two main methods by which this is achieved are reduction in the area of their shadow by lateral compression of the body, and counter illumination via bioluminescence. This is achieved by production of light from ventral photophores, which tend to produce such light intensity to render the underside of the fish of similar appearance to the background light.\nFor more sensitive vision in low light, some fish have a retroreflector behind the retina.\nFlashlight fish have this plus photophores, which combination they use to detect eyeshine in other fish.\nOrganisms in the deep sea are almost entirely reliant upon sinking living and dead organic matter which falls at approximately 100 meters per day.\nLarger food falls, such as whale carcasses, also occur and studies have shown that these may happen more often than currently believed. There are many scavengers that feed primarily or entirely upon large food falls.\nThere are a number of filter feeders that feed upon organic particles using tentacles, such as Freyella elegans.\nThere are a number of species that do not primarily rely upon dissolved organic matter for their food. These species and communities are found at hydrothermal vents at sea-floor spreading zones. One example is the symbiotic relationship between the tube worm Riftia and chemosynthetic bacteria. It is this chemosynthesis that supports the complex communities that can be found around hydrothermal vents.\nDeep-sea fish have different adaptations in their proteins, anatomical structures, and metabolic systems to survive in the Deep sea, where the inhabitants have to withstand great amount of hydrostatic pressure.\nThe deep-sea organisms must have the ability to maintain well-regulated metabolic system in the face of high pressures. In order to adjust for the extreme environment, these organisms have developed unique characteristics.\nSome Deep-sea fish developed pressure tolerance through the change in mechanism of their α-actin.\nIn some species that live in depths greater than 5 km (3.1 mi), C.armatus and C.yaquinae have specific substitutions on the active sites of α-Actin, which serves as the main component of muscle fiber. These specific substitutions, Q137K and V54A from C.armatus or I67P from C.yaquinae are predicted to have importance in pressure tolerance. Substitution in the active sites of actin result in significant changes in the salt bridge patterns of the protein, which allows for better stabilization in ATP binding and sub unit arrangement, confirmed by the free energy analysis and molecular dynamics simulation. It was found that deep sea fish have more salt bridges in their actins compared to fish inhabiting the upper zones of the sea.\nSpecific osmolytes were found to be abundant in deep sea fish under high hydrostatic pressure. For certain chondrichthyans, it was found that Trimethylamine N-oxide (TMAO) increased with depth, replacing other osmolytes and urea. Due to the ability of TMAO being able to protect proteins from high hydrostatic pressure destabilizing proteins, the osmolyte adjustment serves are an important adaptation for deep sea fish to withstand high hydrostatic pressure.\nDeep-sea organisms possess molecular adaptations to survive and thrive in the deep oceans. Mariana hadal snailfish developed modification in the Osteocalcin(burlap) gene, where premature termination of the gene was found. Osteocalcin gene regulates bone development and tissue mineralization, and the frameshift mutation seems to have resulted in the open skull and cartilage-based bone formation. Due to high hydrostatic pressure in the deep sea, closed skulls that organisms living on the surface develop cannot withstand the enforcing stress. Similarly, common bone developments seen in surface vertebrates cannot maintain their structural integrity under constant high pressure.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Deep_sea",
"Here is the extracted information about how deep-sea life survives:\n\n* **Reliance on Marine Snow for Food:** Deep-sea organisms rely heavily on marine snow (organic detritus falling from upper layers) as an energy source, as sunlight cannot reach them and there is a lack of primary producers.\n* **Adaptations to High Pressure:**\n * Deep-sea organisms have the same pressure within their bodies as is exerted on them from the outside, preventing them from being crushed.\n * They increase the proportion of unsaturated fatty acids in the lipids of their cell membranes to maintain fluidity, as high pressure reduces it.\n * Their metabolic processes are adapted to ultimately decrease the volume of the organism.\n * Deep-sea organisms contain gas-filled spaces (vacuoles), but because gas is compressed under high pressure, they can \"blow up\" if brought to the surface.\n * They have evolved changes in their protein structure and reaction criteria to withstand pressure, as high levels of external pressure affect metabolic processes and biochemical reactions.\n * Globular proteins of deep-sea fish are relatively rigid compared to surface fish, structurally strengthened by modification of bonds in their tertiary structure.\n * Their Na+/K+-ATPases (a lipoprotein enzyme important for osmoregulation) exhibit a much higher tolerance of hydrostatic pressure compared to shallow-water counterparts, explained by adaptations in the protein and lipid parts of the enzyme.\n * Ten orders, thirteen families, and about 200 known species have evolved a gelatinous layer below the skin or around the spine for buoyancy, low-cost growth, and to increase swimming efficiency by reducing drag.\n* **Sensory Adaptations (due to lack of light):**\n * Many organisms are blind and rely on other senses like sensitivities to changes in local pressure and smell.\n * Those that aren't blind have large and sensitive eyes (up to 100 times more sensitive than human eyes) to use bioluminescent light.\n * Some deep-sea fish have multiple Rhodopsin (Rh1) opsin genes (e.g., silver spinyfin has 38) to help them see in dim light.\n * Mesopelagic fish often have large eyes, with some deeper water fish having tubular eyes with large lenses and only rod cells that look upwards for binocular vision and sensitivity to small light signals.\n * Important sensory systems include the inner ear (responds to sound) and the lateral line (responds to changes in water pressure).\n * The olfactory system can be important, especially for males to find females by smell.\n* **Bioluminescence:**\n * More than 50% of deep-sea fish, shrimp, and squid are bioluminescent, producing light through the agitation of luciferin molecules in the presence of oxygen.\n * They often have photophores (light-producing glandular cells) which may contain lenses to intensify or lessen light.\n * Bioluminescence is used to search for food, attract prey (like the anglerfish's lure), claim territory, communicate and find a mate, and distract or temporarily blind predators.\n * In the mesopelagic zone, some organisms use counter-illumination (illuminating bellies to match ambient light) to camouflage themselves from predators below.\n* **Physical Adaptations for Buoyancy and Movement:**\n * Eggs and larvae often contain oil droplets in their plasma to maintain neutral buoyancy.\n * Deep-sea fish usually do not have gas-filled swim bladders due to high pressure; instead, they may use structures similar to hydrofoils for hydrodynamic lift.\n * The deeper a fish lives, the more jelly-like its flesh and the more minimal its bone structure.\n * They reduce tissue density through high fat content, reduction of skeletal weight (smaller size, thickness, mineral content), and water accumulation. This makes them slower and less agile but requires less energy to stay suspended.\n * Body shapes are generally better adapted for periodic bursts of swimming rather than constant swimming.\n* **Feeding Adaptations (due to scarce food):**\n * Some have long feelers to help locate prey or attract mates.\n * The deep-sea anglerfish has a bioluminescent, worm-like lure protruding from its face.\n * They must consume other fish of the same size or larger, so they have great sharp teeth, hinged jaws, disproportionately large mouths, and expandable bodies (e.g., gulper eel).\n * Bathypelagic fish have slow metabolisms and unspecialized diets, preferring to sit and wait for food rather than expend energy searching. They are almost all lie-in-wait predators.\n * They are not selective in their feeding habits and grab whatever comes close, using large mouths with sharp teeth and overlapping gill rakers to prevent small prey from escaping.\n* **Reproductive Adaptations:**\n * Some species depend on unique bioluminescent patterns for mate attraction.\n * Others are hermaphrodites to increase chances of reproduction when encounters are rare.\n * Female anglerfish release pheromones to attract tiny males. Some anglerfish males (e.g., Haplophryne mollis) bite onto a female, release an enzyme that fuses them, and their circulatory systems join, with the male atrophying into gonads.\n* **General Survival Characteristics:**\n * Many deep-sea fish are dark to blend in with their environment; red coloration also functions as camouflage as red light doesn't penetrate to deep-sea.\n * Bathypelagic fish have slow metabolisms, weak, watery muscles, and skeletal structures, and are slimy without scales.\n * Gills, kidneys, hearts, and swim bladders can be small or missing, a feature suggesting neoteny, which allows them to remain suspended with little energy expenditure.\n * Mesopelagic fish have muscular bodies, ossified bones, scales, well-developed gills, central nervous systems, and large hearts and kidneys.\n * Mesopelagic plankton feeders have small mouths with fine gill rakers, while piscivores have larger mouths and coarser gill rakers.\n * Some mesopelagic fish make daily vertical migrations (following zooplankton) to feed in shallower waters at night and return to depths for safety during the day, aided by a swim bladder.\n * They display considerable tolerances for temperature change, migrating through thermoclines.\n * Lack defensive spines.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Deep-sea_fish",
"The provided source material, \"Still Wakes the Deep,\" is a description of a psychological horror video game set on an oil rig. It does not contain information about how deep-sea life survives. The text focuses on the game's plot, gameplay, development, and reception, with the \"monsters\" in the game being mutated oil rig workers rather than natural deep-sea creatures.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Still_Wakes_the_Deep",
"The three main sources of energy and nutrients for deep sea communities are:\n\n* **Marine snow:** Particulate organic matter (POM) repackaged into larger particles that sink from the upper photic zone, providing food for opportunistic organisms on and in the bottom. This includes wood-boring bivalves feeding on plant remains.\n* **Occasional surface blooms:** Sudden access to nutrients near the surface leading to blooms of plankton, algae, or animals (like salps) that sink to the bottom without being consumed. These short bursts of nutrients are rapidly consumed by animals and microbes, with waste products becoming part of deep-sea sediments.\n* **Whale falls:** The death of a whale brings hundreds of tons of organic matter to the bottom, creating a community that progresses through three stages:\n * **Mobile scavenger stage:** Large, mobile deep-sea animals (amphipods, crabs, sleeper sharks, hagfish) scavenge the carcass.\n * **Opportunistic stage:** Organisms like *Osedax* (tube worms) colonize bones and surrounding sediments contaminated with organic matter.\n * **Sulfophilic stage:** Further decomposition of bones and seawater sulfate reduction create a sulphide-rich environment analogous to hydrothermal vents, attracting sulphur-loving creatures (polynoids, bivalves, gastropods).\n* **Chemosynthesis:**\n * **Hydrothermal vents:** Cold seawater circulates through cracks, heats up, dissolves minerals and sulfides, and then emanates from active sub-seafloor rifts. Chemosynthesis by bacteria provides energy and organic matter for the entire food web in these ecosystems. These bacteria can form mats on the seafloor, serving as food for other creatures, and are a key energy source.\n * **Cold seeps:** Areas on the ocean floor where hydrogen sulfide, methane, and other hydrocarbon-rich fluids seep, often forming brine pools. These provide energy to chemosynthetic extremophiles.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Deep-sea_community",
"Based on the provided text, there is no information about \"Adaptations of deep-sea organisms to high pressure.\"\n\nThe text mentions \"hydrostatic pressure\" once in the \"Lower temperature\" section, stating: \"In Arctic and Antarctic seas where there is a reduced vertical temperature gradient, there is also a reduced trend towards increased body size with depth, arguing against hydrostatic pressure being an important parameter.\" This suggests that hydrostatic pressure is *not* considered an important factor for deep-sea gigantism according to the text's explanations.\n\nThe text discusses other environmental factors like temperature, food scarcity, predation pressure, and dissolved oxygen levels, but does not detail adaptations *to high pressure* itself.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Deep-sea_gigantism",
"Many microorganisms in dark regions of the oceans use chemosynthesis to produce biomass from single-carbon molecules.\nIn most oceanic environments, energy for chemosynthesis derives from reactions in which substances such as hydrogen sulfide or ammonia are oxidized.\nLarge populations of animals can be supported by chemosynthetic secondary production at hydrothermal vents, methane clathrates, cold seeps, whale falls, and isolated cave water.\nGiant tube worms use bacteria in their trophosome to fix carbon dioxide (using hydrogen sulfide as their energy source) and produce sugars and amino acids.\nWinogradsky's suggestion was confirmed nearly 90 years later, when hydrothermal ocean vents were discovered in the 1970s.\nThe hot springs and strange creatures were discovered by Alvin, the world's first deep-sea submersible, in 1977 at the Galapagos Rift.\nAt about the same time, then-graduate student Colleen Cavanaugh proposed chemosynthetic bacteria that oxidize sulfides or elemental sulfur as a mechanism by which tube worms could survive near hydrothermal vents.\nCavanaugh later managed to confirm that this was indeed the method by which the worms could thrive, and is generally credited with the discovery of chemosynthesis.\nIn 2013, researchers reported their discovery of bacteria living in the rock of the oceanic crust below the thick layers of sediment, and apart from the hydrothermal vents that form along the edges of the tectonic plates.\nPreliminary findings are that these bacteria subsist on the hydrogen produced by chemical reduction of olivine by seawater circulating in the small veins that permeate the basalt that comprises oceanic crust.\nThe bacteria synthesize methane by combining hydrogen and carbon dioxide.\nChemosynthetic communities in different environments are important biological systems in terms of their ecology, evolution and biogeography, as well as their potential as indicators of the availability of permanent hydrocarbon- based energy sources.\nIn the process of chemosynthesis, bacteria produce organic matter where photosynthesis is impossible.\nIsolation of thermophilic sulfate-reducing bacteria Thermodesulfovibrio yellowstonii and other types of chemosynthetics provides prospects for further research.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Chemosynthesis",
"The following information about deep sea life at hydrothermal vents is extracted from the provided source:\n\n* Relative to the majority of the deep sea, the areas around hydrothermal vents are biologically more productive, often hosting complex communities fueled by the chemicals dissolved in the vent fluids.\n* Chemosynthetic bacteria and archaea found around hydrothermal vents form the base of the food chain, supporting diverse organisms including giant tube worms, clams, limpets, and shrimp.\n* Hydrothermal vents have been hypothesized to have been a significant factor to starting abiogenesis and the survival of primitive life. The conditions of these vents have been shown to support the synthesis of molecules important to life.\n* There are numerous species of extremophiles and other organisms currently living immediately around deep-sea vents, suggesting that this is indeed a possible scenario for the origin of life.\n* Life has traditionally been seen as driven by energy from the sun, but deep-sea organisms have no access to sunlight, so biological communities around hydrothermal vents must depend on nutrients found in the dusty chemical deposits and hydrothermal fluids in which they live.\n* Previously, benthic oceanographers assumed that vent organisms were dependent on marine snow, as deep-sea organisms are. Some hydrothermal vent organisms do consume this \"rain\", but with only such a system, life forms would be sparse.\n* Compared to the surrounding sea floor, however, hydrothermal vent zones have a density of organisms 10,000 to 100,000 times greater.\n* These organisms include yeti crabs, which have long hairy arms that they reach out over the vent to collect food with.\n* The hydrothermal vents are recognized as a type of chemosynthetic based ecosystems (CBE) where primary productivity is fuelled by chemical compounds as energy sources instead of light (chemoautotrophy).\n* Hydrothermal vent communities are able to sustain such vast amounts of life because vent organisms depend on chemosynthetic bacteria for food.\n* The water from the hydrothermal vent is rich in dissolved minerals and supports a large population of chemoautotrophic bacteria. These bacteria use sulfur compounds, particularly hydrogen sulfide, a chemical highly toxic to most known organisms, to produce organic material through the process of chemosynthesis.\n* The vents' impact on the living environment goes beyond the organisms that lives around them, as they act as a significant source of iron in the oceans, providing iron for the phytoplankton.\n* The oldest confirmed record of a \"modern\" biological community related with a vent is the Figueroa Sulfide, from the Early Jurassic of California.\n* The ecosystem so formed is reliant upon the continued existence of the hydrothermal vent field as the primary source of energy, which differs from most surface life on Earth, which is based on solar energy.\n* While it is often said that these communities exist independently of the sun, some of the organisms are actually dependent upon oxygen produced by photosynthetic organisms, while others are anaerobic.\n* The chemosynthetic bacteria grow into a thick mat which attracts other organisms, such as amphipods and copepods, which graze upon the bacteria directly.\n* Larger organisms, such as snails, shrimp, crabs, tube worms, fish (especially eelpout, cutthroat eel, Ophidiiformes and Symphurus thermophilus), and octopuses (notably Vulcanoctopus hydrothermalis), form a food chain of predator and prey relationships above the primary consumers.\n* The main families of organisms found around seafloor vents are annelids, pogonophorans, gastropods, and crustaceans, with large bivalves, vestimentiferan worms, and \"eyeless\" shrimp making up the bulk of nonmicrobial organisms.\n* Siboglinid tube worms, which may grow to over 2 m (6.6 ft) tall in the largest species, often form an important part of the community around a hydrothermal vent. They have no mouth or digestive tract, and like parasitic worms, absorb nutrients produced by the bacteria in their tissues.\n* About 285 billion bacteria are found per ounce of tubeworm tissue.\n* Tubeworms have red plumes which contain hemoglobin. Hemoglobin combines with hydrogen sulfide and transfers it to the bacteria living inside the worm. In return, the bacteria nourish the worm with carbon compounds.\n* Two of the species that inhabit a hydrothermal vent are *Tevnia jerichonana*, and *Riftia pachyptila*.\n* One discovered community, dubbed \"Eel City\", consists predominantly of the eel *Dysommina rugosa*. Though eels are not uncommon, invertebrates typically dominate hydrothermal vents.\n* In 1993, already more than 100 gastropod species were known to occur in hydrothermal vents.\n* Over 300 new species have been discovered at hydrothermal vents, many of them \"sister species\" to others found in geographically separated vent areas.\n* The examples of convergent evolution seen between distinct hydrothermal vents is seen as major support for the theory of natural selection and of evolution as a whole.\n* Although life is very sparse at these depths, black smokers are the centers of entire ecosystems. Sunlight is nonexistent, so many organisms, such as archaea and extremophiles, convert the heat, methane, and sulfur compounds provided by black smokers into energy through a process called chemosynthesis.\n* More complex life forms, such as clams and tubeworms, feed on these organisms.\n* The organisms at the base of the food chain also deposit minerals into the base of the black smoker, therefore completing the life cycle.\n* A species of phototrophic bacterium has been found living near a black smoker off the coast of Mexico at a depth of 2,500 m (8,200 ft). This is the first organism discovered in nature to exclusively use a light other than sunlight for photosynthesis.\n* New and unusual species are constantly being discovered in the neighborhood of black smokers.\n* The Pompeii worm *Alvinella pompejana*, which is capable of withstanding temperatures up to 80 °C (176 °F), was found in the 1980s.\n* A scaly-foot gastropod *Chrysomallon squamiferum* was found in 2001 during an expedition to the Indian Ocean's Kairei hydrothermal vent field. This gastropod uses iron sulfides (pyrite and greigite) for the structure of its dermal sclerites (hardened body parts), instead of calcium carbonate. This armor plating probably serves as a defense against the venomous radula (teeth) of predatory snails in that community.\n* In March 2017, researchers reported evidence of possibly the oldest forms of life on Earth. Putative fossilized microorganisms were discovered in hydrothermal vent precipitates in the Nuvvuagittuq Belt of Quebec, Canada, that may have lived as early as 4.280 billion years ago.\n* Hydrothermal vent ecosystems have enormous biomass and productivity, but this rests on the symbiotic relationships that have evolved at vents.\n* Deep-sea hydrothermal vent ecosystems differ from their shallow-water and terrestrial hydrothermal counterparts due to the symbiosis that occurs between macroinvertebrate hosts and chemoautotrophic microbial symbionts in the former.\n* Since sunlight does not reach deep-sea hydrothermal vents, organisms in deep-sea hydrothermal vents cannot obtain energy from the sun to perform photosynthesis. Instead, the microbial life found at hydrothermal vents is chemosynthetic; they fix carbon by using energy from chemicals such as sulfide, as opposed to light energy from the sun.\n* The symbiont converts inorganic molecules (H2S, CO2, O) to organic molecules that the host then uses as nutrition.\n* Scientists were astounded when they first found hydrothermal vents teeming with life in 1977. What was discovered was the ubiquitous symbiosis of chemoautotrophs living in (endosymbiosis) the vent animals' gills; the reason why multicellular life is capable to survive the toxicity of vent systems.\n* Scientists are studying how the microbial symbionts aid in sulfide detoxification (therefore allowing the host to survive the otherwise toxic conditions). Host-associated microbiomes are also important in host development, nutrition, defense against predators, and detoxification.\n* In return, the host provides the symbiont with chemicals required for chemosynthesis, such as carbon, sulfide, and oxygen.\n* In 1977, it was hypothesized that the chemoautotrophic bacteria at hydrothermal vents might be responsible for contributing to the diet of suspension-feeding bivalves.\n* In 1981, it was understood that giant tubeworm nutrition acquisition occurred as a result of chemoautotrophic bacterial endosymbionts.\n* Symbiotic relationships between chemoautotrophs and macrofauna invertebrate species were found to be ubiquitous. For instance, in 1983, clam gill tissue was confirmed to contain bacterial endosymbionts; in 1984 vent bathymodiolid mussels and vesicomyid clams were also found to carry endosymbionts.\n* Tubeworms have no mouth and no gut, but they do have a \"trophosome\", where they deal with nutrition and where their endosymbionts are found. They also have a bright red plume, which they use to uptake compounds such as O, H2S, and CO2, which feed the endosymbionts in their trophosome.\n* The tubeworms hemoglobin is capable of carrying oxygen without interference or inhibition from sulfide, due to zinc ions that bind the hydrogen sulfide, reducing tissue exposure to sulfide and providing bacteria with sulfide for chemoautotrophy.\n* Tubeworms can metabolize CO2 in two different ways, and can alternate between the two as needed.\n* In 1988, research confirmed thiotrophic (sulfide-oxidizing) bacteria in *Alviniconcha hessleri*, a large vent mollusk.\n* Mussels convert sulfide to thiosulfate before carrying it over to the symbionts to circumvent sulfide toxicity.\n* Motile organisms such as alvinocarid shrimp must track oxic (oxygen-rich) / anoxic (oxygen-poor) environments as they fluctuate.\n* Organisms living at the edge of hydrothermal vent fields, such as pectinid scallops, also carry endosymbionts in their gills, but their dependence on the microbial endosymbiont for nutrition is lessened.\n* Not all host animals have endosymbionts; some have episymbionts—symbionts living on the animal as opposed to inside the animal. Shrimp found at vents in the Mid-Atlantic Ridge were discovered to carry episymbionts in 1988. Other organisms like *Lepetodrilis fucensis* also carry episymbionts.\n* While some symbionts reduce sulfur compounds, others are known as \"methanotrophs\" and reduce carbon compounds, namely methane. Bathmodiolid mussels are an example of a host that contains methanotrophic endosymbionts; however, the latter mostly occur in cold seeps as opposed to hydrothermal vents.\n* While chemosynthesis allows organisms to live without sunlight in the immediate sense, they technically still rely on the sun for survival, since oxygen in the ocean is a byproduct of photosynthesis.\n* However, if the sun were to suddenly disappear and photosynthesis ceased to occur on our planet, life at the deep-sea hydrothermal vents could continue for millennia (until the oxygen was depleted).\n* Chemosynthetic ecosystems surrounding the Galápagos Rift submarine hydrothermal vents were first directly observed in 1977.\n* In 1979, a team of biologists led by J. Frederick Grassle returned to the Galápagos Rift to investigate the biological communities discovered two year earlier.\n* On Easter Sunday April 15, 1979, during a dive of Alvin to 2,600 meters, Roger Larson and Bruce Luyendyk found a hydrothermal vent field with a biological community similar to the Galápagos vents.\n* The unique depositing of metals and altered local chemistry in turn allow for conditions to support life of thermophiles and other organisms.\n* The highly saline character of the waters in the Red Sea hot brines was not hospitable to living organisms.\n* Conservation of hydrothermal vent ecosystems after mining would depend on the recolonization of chemosynthetic bacteria, and the continuation of hydrothermal vent fluid.\n* Studies on recolonization after volcanic destruction show it took 3–5 years for bacteria to recolonize, and around 10 years for megafauna to return. There was also a shift in species composition and the presence of immigrant species.\n* Research on deep sea shrimp has shown the potential for flood lights used on the sea floor to cause permanent retinal damage, warranting further research into the potential risk to other vent organisms.\n* A large percent of benthic organisms communicate using very low-frequency sounds; increasing ambient noise levels on the seafloor could potentially mask communication and alter behavioral patterns.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Hydrothermal_vent",
"From the provided source, the following information is relevant to \"Deep sea extremophiles\":\n\n* \"These support unique biomes based on chemotrophic microorganisms.\"\n* \"Much of the fluid trapped in sediments of the subducting slab returns to the surface at the oceanic trench, producing mud volcanoes and cold seeps. These support unique biomes based on chemotrophic microorganisms.\"\n* \"The fluids released at mud volcanoes and cold seeps are rich in methane and hydrogen sulfide, providing chemical energy for chemotrophic microorganisms that form the base of a unique trench biome.\"\n* \"Cold seep communities have been identified in the inner trench slopes of the western Pacific (especially Japan), South America, Barbados, the Mediterranean, Makran, and the Sunda trench.\"\n* \"These are found at depths as great as 6,000 meters (20,000 ft).\"\n* \"The genome of the extremophile Deinococcus from Challenger Deep has sequenced for its ecological insights and potential industrial uses.\"\n* \"Because trenches are the lowest points in the ocean floor, there is concern that plastic debris may accumulate in trenches and endanger the fragile trench biomes.\"\n\nBased on:\nhttps://en.wikipedia.org/wiki/Oceanic_trench",
"The provided text focuses exclusively on seahorses (genus Hippocampus), which are explicitly stated to be \"mainly found in shallow tropical and temperate salt water throughout the world.\"\n\nTherefore, this source does not contain relevant information about \"deep sea fish survival mechanisms.\"\n\nBased on:\nhttps://en.wikipedia.org/wiki/Seahorse",
"The provided text does not contain information about \"deep sea fish survival mechanisms.\" It focuses on deep sea mining, its types, locations, regulations, environmental impacts, and related economic and geopolitical aspects.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Deep_sea_mining",
"The provided source describes the television program \"Animal Face-Off\" and does not contain information about the challenges deep sea animals face.\n\nBased on:\nhttps://en.wikipedia.org/wiki/Animal_Face-Off"
]
}
}