30,000 years of hydrothermal activity at the lost city vent field. - Wikidata - wikimedia - TriplyDB

30,000 years of hydrothermal activity at the lost city vent field.

30,000 years of hydrothermal activity at the lost city vent field.

http://www.wikidata.org/entity/Q34217129

about

Archaea and bacteria with surprising microdiversity show shifts in dominance over 1,000-year time scales in hydrothermal chimneys On the origin of biochemistry at an alkaline hydrothermal vent Methane- and sulfur-metabolizing microbial communities dominate the Lost City hydrothermal field ecosystem Fluid mixing and the deep biosphere of a fossil Lost City-type hydrothermal system at the Iberia Margin Fossil evidence for serpentinization fluids fueling chemosynthetic assemblages Early evolution without a tree of life Microbial ecology of the dark ocean above, at, and below the seafloor.Bio-inspired CO2 conversion by iron sulfide catalysts under sustainable conditions.Comparison of intact polar lipid with microbial community composition of vent deposits of the Rainbow and Lucky Strike hydrothermal fields.Abiogenic hydrocarbon production at lost city hydrothermal field.Record of archaeal activity at the serpentinite-hosted Lost City Hydrothermal Field.Feasible metabolisms in high pH springs of the Philippines Physiological differentiation within a single-species biofilm fueled by serpentinization.Serpentinite and the dawn of life.Prospects for the study of evolution in the deep biosphere.Dispersal of thermophilic Desulfotomaculum endospores into Baltic Sea sediments over thousands of years The evolution of organic matter in space.Effect of water activity on rates of serpentinization of olivine Early Microbial Evolution: The Age of Anaerobes.Deeply-sourced formate fuels sulfate reducers but not methanogens at Lost City hydrothermal field.Prebiotic Synthesis of Glycine from Ethanolamine in Simulated Archean Alkaline Hydrothermal Vents.On the differing growth mechanisms of black-smoker and Lost City-type hydrothermal vents Off-axis symbiosis found: Characterization and biogeography of bacterial symbionts of Bathymodiolus mussels from Lost City hydrothermal vents Tectonic structure, evolution, and the nature of oceanic core complexes and their detachment fault zones (13°20′N and 13°30′N, Mid Atlantic Ridge)A New View on the Petrogenesis of the Oman Ophiolite Chromitites from Microanalyses of Chromite-hosted Inclusions Detachment fault control on hydrothermal circulation systems: Interpreting the subsurface beneath the TAG hydrothermal field using the isotopic and geological evolution of oceanic core complexes in the Atlantic Drilling constraints on lithospheric accretion and evolution at Atlantis Massif, Mid-Atlantic Ridge 30°N Serpentinization and associated hydrogen and methane fluxes at slow spreading ridges IODP Expedition 304 & 305 Characterize the Lithology, Structure, and Alteration of an Oceanic Core Complex Seawater-peridotite interactions: First insights from ODP Leg 209, MAR 15°N Controls of faulting and reaction kinetics on serpentinization and double Benioff zones Geochemical character of serpentinites associated with high- to ultrahigh-pressure metamorphic rocks in the Alps, Cuba, and the Himalayas: Recycling of elements in subduction zones The internal structure of an oceanic core complex: An integrated analysis of oriented borehole imagery from IODP Hole U1309D (Atlantis Massif)Geodiversity of hydrothermal processes along the Mid-Atlantic Ridge and ultramafic-hosted mineralization: A new type of oceanic Cu-Zn-Co-Au volcanogenic massive sulfide deposit Trace-element geochemistry of transform-fault serpentinite in high-pressure subduction mélanges (eastern Cuba): implications for subduction initiation A 19 to 17 Ma amagmatic extension event at the Mid-Atlantic Ridge: Ultramafic mylonites from the Vema Lithospheric Section A Field and Chemical Study of Serpentinization—Stonyford, California: Chemical Flux and Mass Balance

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30,000 years of hydrothermal activity at the lost city vent field.

http://www.wikidata.org/entity/Q34217129

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2003 nî lūn-bûn

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2003年の論文

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Stefano M. Bernasconi

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