sameAs
The discovery of new deep-sea hydrothermal vent communities in the southern ocean and implications for biogeography.Geochemistry, faunal composition and trophic structure in reducing sediments on the southwest South Georgia margin.Talc-dominated seafloor deposits reveal a new class of hydrothermal system.A chemosynthetic weed: the tubeworm Sclerolinum contortum is a bipolar, cosmopolitan speciesFunctional diversity of bacteria in a ferruginous hydrothermal sediment.Biogeochemical controls on microbial diversity in seafloor sulphidic sediments.Geochemical and visual indicators of hydrothermal fluid flow through a sediment-hosted volcanic ridge in the Central Bransfield Basin (Antarctica)Impact of volcanic ash on anammox communities in deep sea sediments.Distinct iron isotopic signatures and supply from marine sediment dissolution.Hydrothermal impacts on trace element and isotope ocean biogeochemistrySouthern Ocean deep-water carbon export enhanced by natural iron fertilization.Dedication: Professor Henry (Harry) Elderfield FRS (1943-2016).Lipidomics of Thalassiosira pseudonana Under Phosphorus Stress Reveal Underlying Phospholipid Substitution Dynamics and Novel Diglycosylceramide Substitutes.Non steady state diagenesis in hydrothermal systems records oceanic variability over the last 800ka in the South East PacificGenesis of ferromanganese crusts from the TAG hydrothermal fieldBrent Spar or Broken Spur?Lead behaviour at the TAG hydrothermal vent field, 26°N, Mid-Atlantic Ridge
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P50
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