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deep-sea vent

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deep-sea vent

Hydrothermal (hot-water) vent formed on the ocean floor when seawater circulates through hot volcanic rocks, often located where new oceanic crust is being formed. Vents also occur on submarine volcanoes. In either case, the hot solution emerging into cold seawater precipitates mineral deposits that are rich in iron, copper, zinc, and other metals. Outflow of these heated waters probably accounts for 20% of the Earth's heat loss. Exotic biological communities are now known to exist around the vents; these ecosystems are totally independent of energy from the Sun, depending not on photosynthesis but rather on chemosynthesis by sulfur-fixing bacteria.



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The largest worm, Riftia pachyptila, from deep-sea vents, doesn't move.
Four short commentaries describe deep-sea vent mining, research employing Venezuelan bivalves, acid-enhanced harmful algal blooms, and the use of sediment as a methods for managing eutrophic lagoons.
Here we briefly summarize our new findings regarding geographical subdivision within and among Lepetodrilus MOTUs and compare them with published information on other deep-sea vent taxa.
 
 
 
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