Linked from

The 65 pages that link to Hydrothermal vent, each with the reason it gives.

• Benthic zoneBroader topic: Vent communities depend on chemosynthesis in an otherwise dark benthic setting.

• Mid-ocean ridgeRelated: Seawater circulates through fresh ridge crust and exits at vents like black smokers.

• Mid-Atlantic RidgeRelated: Seawater invades the fresh crust at the ridge axis, driving black smoker systems.

• Origin of lifeRelated: Vent minerals and chemical gradients offer a setting for reactions proposed in origin-of-life models.

• Marine biodiversityBroader topic: Vent communities show how specialized life thrives without sunlight.

• Primary productionBroader topic: Chemosynthetic communities there produce organic matter without sunlight.

• Marine ecosystemBroader topic: Vent communities rely on chemosynthesis rather than sunlight as their primary energy source.

• Banded iron formationRelated: Hydrothermal activity supplied dissolved iron to some ancient marine basins.

• Deep-sea miningRelated: Vent ecosystems can be affected when nearby massive sulfide deposits are mined.

• AbiogenesisRelated: Vents provide gradients and minerals that may have powered early chemical reactions.

• EuropaRelated: Such vents could supply chemical energy if they exist on Europa’s rocky seafloor.

• GemstoneRelated: Hydrothermal fluids can form gem-bearing veins and deposits.

• SerpentinizationRelated: Seawater circulating through serpentinized rocks feeds some vent systems.

• Transform faultRelated: Transform walls expose deep mantle rocks whose alteration fuels vent ecosystems.

• Deep-sea explorationRelated: Vent discovery revealed thriving deep-sea ecosystems powered by chemical energy.

• Hydrothermal circulationBroader topic: Vents are surface expressions of focused hydrothermal flow.

• ChemosynthesisRelated: Vent fluids provide reduced chemicals that microbes use to power carbon fixation.

• EnceladusRelated: Cassini detected plume chemicals consistent with hydrothermal reactions on the ocean floor.

• Lake BaikalRelated: Hydrothermal activity occurs in parts of Baikal’s rift basin.

• Deep-sea ecologyBroader topic: Vents create localized habitats powered by chemical energy.

• Prebiotic chemistryRelated: Vent gradients and mineral surfaces provide possible settings for reactions that build and concentrate organic molecules.

• Deep seaBroader topic: Vents support dense communities powered by chemical energy rather than sunlight.

• Marine biologyBroader topic: Vent communities revealed ecosystems sustained without sunlight.

• Sulfur cycleBroader topic: Vents release reduced sulfur compounds that fuel distinctive microbial food webs.

• East Pacific RiseRelated: Seawater circulates through newly formed crust and returns through vents.

• Last universal common ancestorRelated: Some hypotheses place LUCA or its precursors in chemically energized vent environments.

• SeawaterBroader topic: Vent fluids add dissolved minerals and compounds to deep seawater.

• SulfideRelated: Vent fluids carry sulfide and precipitate metal sulfide deposits.

• Abyssal zoneBroader topic: Vents create unusual deep-sea habitats powered by chemical energy.

• Benthic ecologyBroader topic: Vent communities rely on chemosynthesis rather than sunlight-driven food reaching the seabed.

• Chemical evolutionRelated: Vent gradients and mineral surfaces are proposed settings for prebiotic reactions.

• Ocean drillingRelated: Drilling near vents investigates fluid pathways and subsurface microbial habitats.

• Deep-sea biodiversityBroader topic: Vent communities show how deep-sea life can thrive without sunlight-derived food.

• Life (biology)Related: Vent environments supply chemical gradients proposed as energy sources for early life.

• Marine geologyBroader topic: These sites reveal how seawater circulates through and alters oceanic crust.

• Marine habitatBroader topic: Chemosynthetic microbes support communities without relying on sunlight as their primary energy source.

• Nuvvuagittuq Greenstone BeltRelated: Some proposed Nuvvuagittuq microfossils resemble structures associated with ancient vent environments.

• AutotrophRelated: Chemosynthetic autotrophs support food webs around many vents without sunlight.

• Bathyal zoneCompared with: Vents are often associated with mid-ocean ridges, unlike the continental-slope setting typical of bathyal habitats.

• Deception IslandRelated: Geothermal activity warms parts of the island’s beaches and coastal waters.

• Deep-sea benthosBroader topic: Vent fields host distinctive benthic communities powered by chemosynthesis.

• Dresser FormationRelated: The formation preserves deposits associated with ancient seafloor hydrothermal activity.

• Juan de Fuca RidgeRelated: Circulating seawater carries heat from magma beneath the ridge to vent fields.

• Lōʻihi SeamountRelated: Vent fields on the volcano support unusual deep-sea ecosystems.

• Submarine volcanoRelated: Submarine volcanic heat drives many vents and their chemical plumes.

• Volcanic outgassingRelated: Hydrothermal circulation can transport interior gases to the surface without an eruption.

• FumaroleCompared with: Unlike many fumaroles, hydrothermal vents commonly discharge liquid water as well as gas.

• Lost City Hydrothermal FieldNarrower topic: Lost City is a hydrothermal system with a chemistry and heat source unlike typical volcanic vents.

• Marine benthic zoneBroader topic: Vent ecosystems show how benthic food webs can thrive without sunlight.

• PaleoarcheanRelated: Vent systems could have supplied chemical energy and minerals to Paleoarchean marine environments.