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

• 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.

• 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.

• 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.

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

• 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.

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

• 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.

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

• 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.

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

• 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.

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

• LoriciferaRelated: Reports of loriciferans from anoxic vent sediments raised questions about their habitat limits.

• Pacific–Antarctic RidgeRelated: Seawater circulates through newly formed crust along the ridge and can emerge at vents.

• São Miguel IslandRelated: Geothermal manifestations on São Miguel reveal heat circulating through volcanic rock.

• Southwest Indian RidgeRelated: Hydrothermal systems occur where seawater interacts with young, fractured ridge crust.

• Central Indian RidgeRelated: Ridge-related circulation can feed hydrothermal systems along its axis.

• Kiwa hirsutaRelated: The species was first found near vents, where chemical energy supports food webs.

• ThermoproteotaRelated: Vent systems provide hot, sulfur-rich habitats for some Thermoproteota.

• AquificotaRelated: Some Aquificota inhabit hot, chemically rich vent systems.

• Earliest known life formsRelated: Some oldest candidate biosignatures occur in hydrothermal deposits, where mineral processes can mimic biological patterns.