Hydrothermal vent
A hydrothermal vent is an opening in the seabed of the Earth by which geothermal energy escapes. Sea water enters, becomes very hot, and rises. The hottest ones carry many black chemicals and are called black smokers. Scientists have found fewer white smokers. Heat escapes from underground in many places. If they are on land, they are usually hot springs, geysers, or fumaroles. Many archaea and bacteria live near hydrothermal vents. They support giant tube worms, clams and shrimp, and many other eukaryotes. The earliest known life forms are thought to have lived near such vents.[1]
Biological communities
Deep sea organisms have no access to sunlight, so they must depend on nutrients in the chemical deposits and hydrothermal fluids in which they live. Despite this, hydrothermal vent zones have more than 10,000 to 100,000 times as much life as the rest of the seafloor.
Hydrothermal vent communities are able to sustain such vast amounts of life because vent organisms depend on chemosynthetic bacteria for food, as opposed to the photosynthetic plants other ecosystems use. These bacteria use sulfur compounds, particularly hydrogen sulfide, a chemical highly toxic to most other organisms, to produce organic material through the process of chemosynthesis.
The chemosynthetic bacteria grow into a thick mat which attracts other organisms such as amphipods and copepods which graze upon the bacteria directly. Larger organisms such as snails, shrimp, crabs, giant tube worms, fish, and octopus form a food chain of predator and prey relationships above the primary consumers.
The main groups of organisms around seafloor vents are worms, gastropods, and crustaceans, with large bivalves, and 'eyeless' shrimp making up the bulk of non-microbial organisms.
Tube worms form an important part of the community around a hydrothermal vent. They absorb nutrients directly into their tissues. There are approximately 285 billion bacteria per ounce of tubeworm tissue.
Tubeworms have red plumes which contain haemoglobin. Haemoglobin combines hydrogen sulfide and transfers it to the bacteria living inside the worm. In return the bacteria nourish the worm with carbon compounds.
Other examples of the unique fauna who inhabit this ecosystem are the gastropod Crysomallon squamiferum, a species of snail with a foot reinforced by scales made of iron and organic materials, and the 'Pompeii Worm' Alvinella pompejana, which is capable of withstanding temperatures up to 80°C (176°F).
Over 300 new species have been discovered at hydrothermal vents,[2] many of them "sister species" to others in geographically separated vent areas. It has been proposed that before the North American plate overrode the Mid-Atlantic Ridge, there was a single biogeographic vent region found in the eastern Pacific.[3] The subsequent barrier to travel began the evolutionary divergence of species in different locations. The examples of convergent evolution seen between distinct hydrothermal vents is seen as major support for the theory of natural selection and evolution as a whole.
Scientists have found bacteria that use photosynthesis in a black smoker off the coast of Mexico at a depth of 2,500 m (8,200 ft). No sunlight penetrates that far into the waters. Instead, the bacteria, part of the Chlorobiaceae family, uses the faint glow from the black smoker. This is the first organism discovered in nature to exclusively use a light other than sunlight for photosynthesis.[4]
Hydrothermal Vent Media
NOAA video on hydrothermal vents
In this phase diagram, the green dotted line illustrates the anomalous behavior of water. The dotted green line marks the melting point and the blue line the boiling point, showing how they vary with pressure; the solid green line shows the typical melting point behavior for other substances.
The black smoker "Candelabra" in the Logatchev hydrothermal field on the Mid-Atlantic Ridge at a water depth of 3,300 m (10,800 ft)
Sound recording from a black smoker
Carbon dioxide bubbles are emitted from white smokers at the Champagne vent site in Eifuku.
White smokers at Champagne Vent, Eifuku, Japan
Diagram of biogeochemical processes within a hydrothermal vent system
Living community at hydrothermal seeps on the Mid-Ocean Ridge at a water depth of 3,030 m (9,940 ft)
References
- ↑ Dodd, Matthew S.; Papineau, Dominic; Grenne, Tor; slack, John F.; Rittner, Martin; Pirajno, Franco; O'Neil, Jonathan; Little, Crispin T. S. (2 March 2017). "Evidence for early life in Earth's oldest hydrothermal vent precipitates". Nature. 543 (7643): 60–64. Bibcode:2017Natur.543...60D. doi:10.1038/nature21377. PMID 28252057. S2CID 2420384. Archived from the original on 16 February 2019. Retrieved 17 December 2018.
{{cite journal}}: CS1 maint: bot: original URL status unknown (link) - ↑ Botos, Sonia. "Life on a hydrothermal vent".
- ↑ Van Dover, Cindy Lee. "Hot Topics: Biogeography of deep-sea hydrothermal vent faunas".
- ↑ Beatty J.T.; et al. (2005). "An obligately photosynthetic bacterial anaerobe from a deep-sea hydrothermal vent". PNAS. 102 (26): 9306–10. Bibcode:2005PNAS..102.9306B. doi:10.1073/pnas.0503674102. PMC 1166624. PMID 15967984.