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Hydrothermal Vent Fluids (Seafloor)
2014Hydrothermal vent fluid (seafloor): a hot (up to >400 C) aqueous solution discharging at the seafloor that typically originates from the reaction of seawater with oceanic crust under hightemperature high-pressure conditions, leading to enrichments in dissolved components such as metals and gases.
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Hydrothermal Vent Animals: Distribution and Biology
Science, 1985Hydrothermal vent communities characterized by large clams, mussels, and vestimentiferan worms thrive on chemosynthetic microbial production. There are similarities in the animal distributions at vent communities from 20°S to 46°N on the Mid-Ocean Ridge in the Pacific Ocean and at cold sulfide seeps in the Gulf of Mexico.
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Geological indexes of hydrothermal venting
Journal of Geophysical Research: Solid Earth, 1996Hydrothermal venting occurs on mid‐ocean ridge axes with a diverse array of morphological, structural, and petrological characteristics. Consequently, it is not clear if certain geological environments are more conducive than others to hydrothermal activity.
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Structure of Hydrothermal Vent Communities
2016Deep-sea hydrothermal vent communities are characterized by complicated taxonomic, trophic, and spatial structure. Different animals consume chemosynthetic bacterial production to a variable extent and by different ways. Different animal groups demonstrate variable degree of adaptations to the extreme environment of hydrothermal vent systems. According
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Exploring habitability with artificial hydrothermal vents
Nature Reviews Earth & Environment, 2021Arlaine M Sanchez
exaly

