Iron persistence in a distal hydrothermal plume supported by dissolved-particulate exchange
暂无分享,去创建一个
C. German | R. Sherrell | J. Fitzsimmons | C. Hoffman | C. Marsay | S. John | S. Nicholas | B. Toner
[1] E. Galbraith,et al. How well do global ocean biogeochemistry models simulate dissolved iron distributions? , 2016 .
[2] E. Boyle,et al. Dissolved iron and iron isotopes in the southeastern Pacific Ocean , 2015 .
[3] J. Adkins,et al. Fractionation of iron isotopes during leaching of natural particles by acidic and circumneutral leaches and development of an optimal leach for marine particulate iron isotopes , 2015 .
[4] S. John,et al. The cycling of iron, zinc and cadmium in the North East Pacific Ocean – Insights from stable isotopes , 2015 .
[5] C. Völker,et al. Modeling organic iron-binding ligands in a three-dimensional biogeochemical ocean model , 2015 .
[6] William J. Jenkins,et al. Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean , 2015, Nature.
[7] E. Boyle,et al. Partitioning of dissolved iron and iron isotopes into soluble and colloidal phases along the GA03 GEOTRACES North Atlantic Transect , 2015 .
[8] P. Lam,et al. Size-fractionated major particle composition and concentrations from the US GEOTRACES North Atlantic Zonal Transect , 2015 .
[9] E. Boyle,et al. Distal transport of dissolved hydrothermal iron in the deep South Pacific Ocean , 2014, Proceedings of the National Academy of Sciences.
[10] E. Boyle,et al. Assessment and comparison of Anopore and cross flow filtration methods for the determination of dissolved iron size fractionation into soluble and colloidal phases in seawater , 2014 .
[11] D. Connelly,et al. The importance of shallow hydrothermal island arc systems in ocean biogeochemistry , 2014 .
[12] A. Findlay,et al. Nanoparticulate pyrite and other nanoparticles are a widespread component of hydrothermal vent black smoker emissions , 2014 .
[13] J. Adkins,et al. A new method for precise determination of iron, zinc and cadmium stable isotope ratios in seawater by double-spike mass spectrometry. , 2013, Analytica chimica acta.
[14] D. Connelly,et al. The stabilisation and transportation of dissolved iron from high temperature hydrothermal vent systems , 2013 .
[15] B. Baker,et al. The microbiology of deep-sea hydrothermal vent plumes: ecological and biogeographic linkages to seafloor and water column habitats , 2013, Front. Microbiol..
[16] V. Faure. Deep circulation in the Eastern South Pacific Ocean , 2012 .
[17] M. Saito,et al. Basin‐scale inputs of cobalt, iron, and manganese from the Benguela‐Angola front to the South Atlantic Ocean , 2012 .
[18] W. Sunda. Feedback Interactions between Trace Metal Nutrients and Phytoplankton in the Ocean , 2012, Front. Microbio..
[19] K. Bruland,et al. Rapid and noncontaminating sampling system for trace elements in global ocean surveys , 2012 .
[20] R. Sherrell,et al. Sampling for particulate trace element determination using water sampling bottles: methodology and comparison to in situ pumps , 2012 .
[21] P. Laan,et al. Dissolved iron in the Arctic Ocean: Important role of hydrothermal sources, shelf input and scavenging removal , 2012 .
[22] K. Buck,et al. The Organic Complexation of Iron in the Marine Environment: A Review , 2012, Front. Microbio..
[23] C. German,et al. Size fractionation of trace metals in the Edmond hydrothermal plume, Central Indian Ocean , 2012 .
[24] P. Laan,et al. Dissolved iron in the Southern Ocean (Atlantic sector) , 2011 .
[25] Christopher R. German,et al. Dissolved and particulate organic carbon in hydrothermal plumes from the East Pacific Rise, 9°50'N , 2011 .
[26] M. Yücel,et al. Hydrothermal vents as a kinetically stable source of iron-sulphide-bearing nanoparticles to the ocean , 2011 .
[27] F. Lacan,et al. Iron isotopes in the seawater of the equatorial Pacific Ocean: New constraints for the oceanic iron cycle , 2011 .
[28] A. Koschinsky,et al. Metal flux from hydrothermal vents increased by organic complexation , 2011 .
[29] M. Wells,et al. Dissolved iron anomaly in the deep tropical-subtropical Pacific: Evidence for long-range transport of hydrothermal iron , 2011 .
[30] A. Anbar,et al. Fe isotope fractionation during equilibration of Fe-organic complexes. , 2010, Environmental science & technology.
[31] D. Garbe‐Schönberg,et al. Iron isotope fractionation in a buoyant hydrothermal plume, 5°S Mid-Atlantic Ridge , 2009 .
[32] B. Toner. Preservation of iron(II) by carbon-rich matrices in a hydrothermal plume , 2009 .
[33] J. Baker,et al. Equilibrium Fe isotope fractionation between inorganic aqueous Fe(III) and the siderophore complex, Fe(III)-desferrioxamine B , 2008 .
[34] Richard A. Krishfield,et al. Particulate organic carbon fluxes to the ocean interior and factors controlling the biological pump: A synthesis of global sediment trap programs since 1983 , 2008 .
[35] C. German,et al. The distribution and stabilisation of dissolved Fe in deep-sea hydrothermal plumes , 2007 .
[36] O. Rouxel,et al. Mass spectrometry and natural variations of iron isotopes. , 2006, Mass spectrometry reviews.
[37] David L. Kirchman,et al. The oceanic gel phase: a bridge in the DOM-POM continuum , 2004 .
[38] E. Boyle,et al. Modeling the global ocean iron cycle , 2004 .
[39] A. Koschinsky,et al. Uptake of elements from seawater by ferromanganese crusts: solid-phase associations and seawater speciation , 2003 .
[40] E. Anderson,et al. Interferometer-controlled scanning transmission X-ray microscopes at the Advanced Light Source. , 2003, Journal of synchrotron radiation.
[41] R. Sherrell,et al. Dissolved and particulate Fe in a hydrothermal plume at 9°45′N, East Pacific Rise:: Slow Fe (II) oxidation kinetics in Pacific plumes , 2000 .
[42] J. Lupton. Hydrothermal helium plumes in the Pacific Ocean , 1998 .
[43] E. Baker,et al. Hydrothermal plume particles and dissolved phosphate over the superfast-spreading southern East Pacific Rise , 1996 .
[44] J. Cowen,et al. Reactive trace metals in the stratified central North Pacific , 1994 .
[45] S. Riser,et al. A Nonconservative β-Spiral Determination of the Deep Circulation in the Eastern South Pacific , 1993 .
[46] M. Wells,et al. Marine submicron particles , 1992 .
[47] C. German,et al. Hydrothermal scavenging at the Mid-Atlantic Ridge: Modification of trace element dissolved fluxes , 1991 .
[48] R. Feely,et al. Scavenging rates of dissolved manganese in a hydrothermal vent plume , 1990 .
[49] E. Baker,et al. Bacterial scavenging of Mn and Fe in a mid- to far-field hydrothermal particle plume , 1986, Nature.
[50] D. E. Fisher,et al. Aluminum‐poor ferromanganoan sediments on active oceanic ridges , 1969 .
[51] Edward D. Goldberg,et al. Marine Geochemistry 1. Chemical Scavengers of the Sea , 1954, The Journal of Geology.
[52] C. Lamborg,et al. The oceanographic toolbox for the collection of sinking and suspended marine particles , 2015 .
[53] Karl K. Turekian,et al. Treatise on geochemistry , 2014 .
[54] C. German. 8.7 – Hydrothermal Processes , 2014 .
[55] J. Nishioka,et al. Evidence of an extensive spread of hydrothermal dissolved iron in the Indian Ocean , 2013 .
[56] K. Nealson,et al. Occurrence and Mechanisms of Microbial Oxidation of Manganese , 1988 .