Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean.
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Tracking the spatiotemporal variations of statistically independent components involving enrichment of rare-earth elements in deep-sea sedimentsIron Transformation Pathways and Redox Micro-Environments in Seafloor Sulfide-Mineral Deposits: Spatially Resolved Fe XAS and δ(57/54)Fe ObservationsSiderophore-based microbial adaptations to iron scarcity across the eastern Pacific OceanThe Irony of Iron - Biogenic Iron Oxides as an Iron Source to the Ocean.Co-registered Geochemistry and Metatranscriptomics Reveal Unexpected Distributions of Microbial Activity within a Hydrothermal Vent Field.Potential Mechanisms for Microbial Energy Acquisition in Oxic Deep-Sea SedimentsBiogeochemistry: Iron's voyage from the abyss.Could It Be Snowing Microbes on Enceladus? Assessing Conditions in Its Plume and Implications for Future Missions.Hidden diversity revealed by genome-resolved metagenomics of iron-oxidizing microbial mats from Lō'ihi Seamount, Hawai'i.The integral role of iron in ocean biogeochemistry.Biogeography of bacteriophages at four hydrothermal vent sites in the Antarctic based on g23 sequence diversity.Bringing microbial diversity into focus: high-resolution analysis of iron mats from the Lō'ihi Seamount.Community Structure of Lithotrophically-Driven Hydrothermal Microbial Mats from the Mariana Arc and Back-ArcMicrobial analysis of Zetaproteobacteria and co-colonizers of iron mats in the Troll Wall Vent Field, Arctic Mid-Ocean Ridge.Hydrothermal impacts on trace element and isotope ocean biogeochemistryQuantifying He fluxes from the mantle using multi-tracer data assimilation.Impact of hydrothermalism on the ocean iron cycle.Diagnosing oceanic nutrient deficiency.Developing a test-bed for robust research governance of geoengineering: the contribution of ocean iron biogeochemistry.Physiological and ecological implications of an iron- or hydrogen-oxidizing member of the Zetaproteobacteria, Ghiorsea bivora, gen. nov., sp. nov.Iron Biogeochemistry in the High Latitude North Atlantic Ocean.Microbial ecology: Here, there and everywhere.Geoelectrochemical CO production: Implications for the autotrophic origin of life.The Role of External Inputs and Internal Cycling in Shaping the Global Ocean Cobalt Distribution: Insights From the First Cobalt Biogeochemical Model.Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP).Aerosol trace metal leaching and impacts on marine microorganisms.ConclusionsSimulating natural carbon sequestration in the Southern Ocean: on uncertainties associated with eddy parameterizations and iron depositionHydrothermal Vents and Methane Seeps: Rethinking the Sphere of InfluenceVoltammetric Investigation of Hydrothermal Iron SpeciationHow well do global ocean biogeochemistry models simulate dissolved iron distributions?On the Role of Dust-Deposited Lithogenic Particles for Iron Cycling in the Tropical and Subtropical AtlanticCombined Effects of Atmospheric and Seafloor Iron Fluxes to the Glacial OceanIron sources and pathways into the Pacific Equatorial Undercurrent
P2860
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P2860
Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean.
description
2015 nî lūn-bûn
@nan
2015年の論文
@ja
2015年論文
@yue
2015年論文
@zh-hant
2015年論文
@zh-hk
2015年論文
@zh-mo
2015年論文
@zh-tw
2015年论文
@wuu
2015年论文
@zh
2015年论文
@zh-cn
name
Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean.
@en
type
label
Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean.
@en
prefLabel
Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean.
@en
P2093
P2860
P356
P1433
P1476
Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean.
@en
P2093
Bettina M Sohst
Christopher R German
James W Moffett
Joseph A Resing
William J Jenkins
P2860
P2888
P304
P356
10.1038/NATURE14577
P407
P577
2015-07-01T00:00:00Z
P6179
1049569885