Geochemistry of hydrothermal fluids from the ultramafic-hosted Logatchev hydrothermal field, 15°N on the Mid-Atlantic Ridge: Temporal and spatial investigation
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Differentiating biotic from abiotic methane genesis in hydrothermally active planetary surfacesHydrogen is an energy source for hydrothermal vent symbiosesA serpentinite-hosted ecosystem in the Southern Mariana ForearcMicrobial community structure of hydrothermal deposits from geochemically different vent fields along the Mid-Atlantic Ridge.Endemic hydrothermal vent species identified in the open ocean seed bank.Acquisition of epibiotic bacteria along the life cycle of the hydrothermal shrimp Rimicaris exoculata.Bacterial sulfur cycling shapes microbial communities in surface sediments of an ultramafic hydrothermal vent field.Feasible metabolisms in high pH springs of the PhilippinesExpression patterns of mRNAs for methanotrophy and thiotrophy in symbionts of the hydrothermal vent mussel Bathymodiolus puteoserpentis.Pathways for abiotic organic synthesis at submarine hydrothermal fieldsOrganic analysis of peridotite rocks from the Ashadze and Logatchev hydrothermal sites.Confinement Effects on Carbon Dioxide Methanation: A Novel Mechanism for Abiotic Methane Formation.Niche partitioning of diverse sulfur-oxidizing bacteria at hydrothermal vents.Heterotrophic Proteobacteria in the vicinity of diffuse hydrothermal venting.Linking geology, fluid chemistry, and microbial activity of basalt- and ultramafic-hosted deep-sea hydrothermal vent environmentsAlteration at the ultramafic-hosted Logatchev hydrothermal field: Constraints from trace element and Sr-O isotope dataDetachment 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 AtlanticMicroseismicity of the Mid-Atlantic Ridge at 7°S-8°15′S and at the Logatchev Massif oceanic core complex at 14°40′N-14°50′NSerpentinites act as sponges for fluid-mobile elements in abyssal and subduction zone environmentsPetrology and Trace Element Budgets of High-pressure Peridotites Indicate Subduction Dehydration of Serpentinized Mantle (Cima di Gagnone, Central Alps, Switzerland)Phase equilibria controls on the chemistry of vent fluids from hydrothermal systems on slow spreading ridges: Reactivity of plagioclase and olivine solid solutions and the pH-silica connection
P2860
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P2860
Geochemistry of hydrothermal fluids from the ultramafic-hosted Logatchev hydrothermal field, 15°N on the Mid-Atlantic Ridge: Temporal and spatial investigation
description
wetenschappelijk artikel
@nl
наукова стаття, опублікована в липні 2007
@uk
name
Geochemistry of hydrothermal f ...... oral and spatial investigation
@en
Geochemistry of hydrothermal f ...... oral and spatial investigation
@nl
type
label
Geochemistry of hydrothermal f ...... oral and spatial investigation
@en
Geochemistry of hydrothermal f ...... oral and spatial investigation
@nl
prefLabel
Geochemistry of hydrothermal f ...... oral and spatial investigation
@en
Geochemistry of hydrothermal f ...... oral and spatial investigation
@nl
P2093
P1433
P1476
Geochemistry of hydrothermal f ...... oral and spatial investigation
@en
P2093
Katja Schmidt
Leandro M. de Carvalho
Richard Seifert
P356
10.1016/J.CHEMGEO.2007.01.023
P577
2007-07-01T00:00:00Z
P819
2007ChGeo.242....1S