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  2. Hydrothermal vent - Wikipedia

    en.wikipedia.org/wiki/Hydrothermal_vent

    Hydrothermal vent fluids harbor temperatures (~40 to >400 °C) well above that of ocean floor seawater (~4 °C), meaning that hydrothermal fluid is less dense than the surrounding seawater and will rise through the water column due to buoyancy, forming a hydrothermal plume; therefore, the phase during which hydrothermal plumes rise through the ...

  3. Abiogenesis - Wikipedia

    en.wikipedia.org/wiki/Abiogenesis

    The deep sea or alkaline hydrothermal vent theory posits that life began at submarine hydrothermal vents. [ 231 ] [ 232 ] William Martin and Michael Russell have suggested that life evolved in structured iron monosulphide precipitates in a seepage site hydrothermal mound at a redox, pH, and temperature gradient between sulphide-rich ...

  4. Earliest known life forms - Wikipedia

    en.wikipedia.org/wiki/Earliest_known_life_forms

    Evidence of possibly the oldest forms of life on Earth has been found in hydrothermal vent precipitates. [1]The earliest known life forms on Earth may be as old as 4.1 billion years (or Ga) according to biologically fractionated graphite inside a single zircon grain in the Jack Hills range of Australia. [2]

  5. Riftia - Wikipedia

    en.wikipedia.org/wiki/Riftia

    Hydrothermal vent tubeworms get organic compounds from bacteria that live in their trophosome. In the middle part, the trunk or third body region, is full of vascularized solid tissue, and includes body wall, gonads, and the coelomic cavity. Here is located also the trophosome, spongy tissue where a billion symbiotic, thioautotrophic bacteria ...

  6. Eifuku - Wikipedia

    en.wikipedia.org/wiki/Eifuku

    Daikoku also features hydrothermal venting [8] and has been considered a twin cone with Eifuku. [9] Eifuku proper is composed of boulders, dykes and lava domes. [10] The occurrence of volcanic breccia, hydrothermal muds, sandstone and sulfides has been reported but without a clear attribution to either Eifuku or NW Eifuku. [11]

  7. Hydrothermal vents and seamounts of the Azores - Wikipedia

    en.wikipedia.org/wiki/Hydrothermal_vents_and...

    A relief map of the Azores Triple Fault region and southern bathymetric zone. The hydrothermal vents and seamounts of the Azores (Portuguese: fontes hidrotermais e montes submarinos dos Açores) are a series of Atlantic seamounts and hydrothermal vents that are part of the Mid-Atlantic Ridge system, giving rise to the archipelago and bathymetric region of the Azores.

  8. DSV Alvin - Wikipedia

    en.wikipedia.org/wiki/DSV_Alvin

    Emergency separation General layout. Alvin was designed as a replacement for bathyscaphes and other less maneuverable oceanographic vehicles. Its more nimble design was made possible in part by the development of syntactic foam, which is buoyant and yet strong enough to serve as a structural material at great depths.

  9. Guaymas Basin - Wikipedia

    en.wikipedia.org/wiki/Guaymas_Basin

    Hydrothermal vent diagram. Hydrothermal circulation, or the circulation of hot water, is a predominant feature of the Guaymas Basin. Hydrothermalism is mainly observed in the southern trough of the basin where hydrothermal vents make up a hydrothermal complex on the seafloor by creating mounds, chimney structures, and sediments. [7]