| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2001Sci...293..847W |
| P356 | DOI | 10.1126/SCIENCE.1059251 |
| P698 | PubMed publication ID | 11486084 |
| P50 | author | Liang-Saw Wen | Q56811116 |
| P2093 | author name string | Wu J | |
| Boyle E | |||
| Sunda W | |||
| P433 | issue | 5531 | |
| P407 | language of work or name | English | Q1860 |
| P304 | page(s) | 847-849 | |
| P577 | publication date | 2001-08-01 | |
| P1433 | published in | Science | Q192864 |
| P1476 | title | Soluble and colloidal iron in the oligotrophic North Atlantic and North Pacific | |
| P478 | volume | 293 |
| Q57901532 | A comparative study of iron uptake mechanisms in marine microalgae: iron binding at the cell surface is a critical step |
| Q57201547 | A deterministic model for N2 fixation at stn. ALOHA in the subtropical North Pacific Ocean |
| Q58113865 | A modeling assessment of the interplay between aeolian iron fluxes and iron-binding ligands in controlling carbon dioxide fluctuations during Antarctic warm events |
| Q33220903 | Bacterial exopolysaccharides from extreme marine environments with special consideration of the southern ocean, sea ice, and deep-sea hydrothermal vents: a review. |
| Q56951410 | Chemical characterization of exopolysaccharides from Antarctic marine bacteria |
| Q34491245 | Combined analyses of the ITS loci and the corresponding 16S rRNA genes reveal high micro- and macrodiversity of SAR11 populations in the Red Sea. |
| Q37199235 | Combined uncertainty estimation for the determination of the dissolved iron amount content in seawater using flow injection with chemiluminescence detection |
| Q36780099 | Determination of size-dependent metal distribution in dissolved organic matter by SEC-UV/VIS-ICP-MS with special focus on changes in seawater. |
| Q37526215 | Different iron sources to study the physiology and biochemistry of iron metabolism in marine micro-algae |
| Q79509067 | Dissolved iron and its speciation in a shallow eutrophic lake and its inflowing rivers |
| Q59849763 | Dissolved iron in the Arctic Ocean: Important role of hydrothermal sources, shelf input and scavenging removal |
| Q34601290 | Distal transport of dissolved hydrothermal iron in the deep South Pacific Ocean |
| Q42592858 | Effects of incubation temperature on growth and production of exopolysaccharides by an antarctic sea ice bacterium grown in batch culture |
| Q37890246 | Emerging patterns of marine nitrogen fixation |
| Q51144654 | Exopolysaccharides from Marine and Marine Extremophilic Bacteria: Structures, Properties, Ecological Roles and Applications. |
| Q24273362 | Feedback Interactions between Trace Metal Nutrients and Phytoplankton in the Ocean |
| Q58411709 | Formation and Maintenance of the GEOTRACES Subsurface-Dissolved Iron Maxima in an Ocean Biogeochemistry Model |
| Q93189245 | Formation and stability of NOM-Mn(III) colloids in aquatic environments |
| Q38687143 | High particulate iron(II) content in glacially sourced dusts enhances productivity of a model diatom |
| Q58054880 | How well do global ocean biogeochemistry models simulate dissolved iron distributions? |
| Q54996941 | Humic substances may control dissolved iron distributions in the global ocean: Implications from numerical simulations |
| Q58074744 | Implications of the glacial CO2“iron hypothesis” for Quaternary climate change |
| Q47709087 | Iron Biogeochemistry in the High Latitude North Atlantic Ocean. |
| Q106636719 | Iron Distribution in the Subtropical North Atlantic: The Pivotal Role of Colloidal Iron |
| Q36756577 | Iron bioavailability to phytoplankton: an empirical approach |
| Q34508917 | Loose ligands and available iron in the ocean |
| Q58309972 | Marine diatom uptake of iron bound with natural colloids of different origins |
| Q58069116 | Modeling the speciation and biogeochemistry of iron at the Bermuda Atlantic Time-series Study site |
| Q36401464 | Molecular evidence of iron limitation and availability in the global diazotroph Trichodesmium |
| Q42931843 | Nonreductive iron uptake mechanism in the marine alveolate Chromera velia |
| Q35062591 | Persistence of deeply sourced iron in the Pacific Ocean |
| Q58309967 | Phase partitioning and solubility of iron in natural seawater controlled by dissolved organic matter |
| Q63952289 | Physical speciation of iron in the Atlantic sector of the Southern Ocean along a transect from the subtropical domain to the Weddell Sea Gyre |
| Q80028348 | Polysaccharide aggregation as a potential sink of marine dissolved organic carbon |
| Q106636807 | Processes governing the supply of iron to phytoplankton in stratified seas |
| Q95297770 | Reduced NOM triggered rapid Cr(VI) reduction and formation of NOM-Cr(III) colloids in anoxic environments |
| Q64007037 | Reduced effectiveness of terrestrial carbon sequestration due to an antagonistic response of ocean productivity |
| Q36691130 | Role of marine cyanobacteria in trace metal bioavailability in seawater |
| Q49958759 | Seasonal resource conditions favor a summertime increase in North Pacific diatom-diazotroph associations |
| Q90262573 | Selective collection of iron-rich dust particles by natural Trichodesmium colonies |
| Q90246038 | Shelf humic substances as carriers for basin-scale iron transport in the North Pacific |
| Q58392603 | The biogeochemical cycle of iron in the ocean |
| Q36041348 | The importance of kinetics and redox in the biogeochemical cycling of iron in the surface ocean. |
| Q38933969 | The integral role of iron in ocean biogeochemistry. |
| Q91045709 | The interplay between regeneration and scavenging fluxes drives ocean iron cycling |
| Q41564950 | The onset of widespread marine red beds and the evolution of ferruginous oceans |
| Q35786773 | The organic complexation of iron in the marine environment: a review |
| Q34162364 | The tomato fer gene encoding a bHLH protein controls iron-uptake responses in roots |
| Q58062319 | Trends in the solubility of iron in dust-dominated aerosols in the equatorial Atlantic trade winds: Importance of iron speciation and sources |
| Q58241322 | Western Pacific coastal sources of iron, manganese, and aluminum to the Equatorial Undercurrent |
| Q92923686 | Why microbes secrete molecules to modify their environment: the case of iron-chelating siderophores |
Search more.