The fate of added iron during a mesoscale fertilisation experiment in the Southern Ocean

Deep-Sea Research Part II: Topical Studies in Oceanography

Volumn 48, Issue 11-12, 2001, Pages 2703-2743

  Bowie, Andrew R ^a,b,g   Maldonado, Maria T ^d   Frew, Russell D ^e   Croot, Peter L ^f   Achterberg, Eric P ^c   Mantoura, R Fauzi C ^g   Worsfold, Paul J ^c   Law, Cliff S ^g   Boyd, Philip W ^e  

^a UNIVERSITY OF PLYMOUTH   (United Kingdom)

^b UNIVERSITY OF MAINE   (United States)

^c McGill University ^*

^d MCGILL UNIVERSITY   (Canada)

^e UNIVERSITY OF OTAGO   (New Zealand)

^f ROYAL NETHERLANDS INSTITUTE FOR SEA RESEARCH   (Netherlands)

^g PLYMOUTH MARINE LABORATORY   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

BACTERIA; BIOMASS; CHLOROPHYLL; GROWTH KINETICS; IRON; SURFACE WATERS;

HIGH NUTRIENT LOW CHLOROPHYLL(HNLC);

OCEANOGRAPHY;

BIOGEOCHEMICAL CYCLE; IRON; NUTRIENT ENRICHMENT; POLAR REGION;

SOUTHERN OCEAN;

ALGAE; BACILLARIOPHYTA; BACTERIA (MICROORGANISMS); CELLULAR ORGANISMS; MASTIGOPHORA (FLAGELLATES);

EID: 0034960827     PISSN: 09670645     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0967-0645(01)00015-7     Document Type: Article

References (107)

1. The stirring of an iron-fertilised phytoplankton bloom
2. Changes of carbon dioxide in surface waters during spring in the Southern Ocean
3. Southern Ocean iron enrichment promotes inorganic carbon drawdown
4. Low seasonality of low concentrations of surface chlorophyll in the Subantarctic water ring: Underwater irradiance, iron, or grazing?
5. Role of protozoan grazing in relieving iron limitation of phytoplankton
6. Size classes and major taxanomic groups of phytoplankton at two locations in the Subarctic Ocean in May and August
7. Determination of sub-nanomolar levels of iron in seawater using flow injection with chemiluminescence detection
8. Iron-mediated changes in phytoplankton photosynthetic competence during SOIREE
9. Phytoplankton dynamics in the NE Subarctic Pacific
10. Role of iron, light, and silicate in controlling algal biomass in subantarctic waters SE of New Zealand
11. The Southern Ocean Iron RElease Experiment (SOIREE) - Introduction and overview
12. Mesoscale iron fertilisation elevates phytoplankton stocks in the polar Southern Ocean
13. On-line voltammetric monitoring of dissolved Cu and Ni in the Gulf of Cadiz, South-west Spain
14. Sampling and analytical methods for the determination of copper, cadmium, zinc and nickel at the nanogram per litre level in seawater
15. Metal enrichment experiments in the Weddell-Scotia Seas - Effects of iron and manganese on various plankton communities
16. Differential response of Equatorial Pacific phytoplankton to iron fertilisation
17. Does iron fertilisation lead to rapid carbon export in the Southern Ocean?
18. Metabolic consequences of iron deficiency in heterotrophic marine protozoa
19. Control of community growth and export production by upwelled iron in the Equatorial Pacific Ocean
20. Iron limitation of phytoplankton growth affects nutrient drawdown ratios in the Southern Ocean
21. A massive phytoplankton bloom induced by an ecosystem-scale iron fertilisation experiment in the Equatorial Pacific Ocean
22. IronEx-I, an in situ iron-enrichment experiment: Experimental design, implementation and results
23. Trace-metal determinations in estuarine waters by electrothermal atomic-absorption spectrometry after extraction of dithiocarbamate complexes into freon
24. Aerosol concentrations over the last climatic cycle (160Kyr) from an Antarctic ice core
25. On iron limitation of the Southern Ocean - Experimental observations in the Weddell and Scotia Seas
26. Importance of iron for plankton blooms and carbon dioxide drawdown in the Southern Ocean
27. Low dissolved Fe and the absence of diatom blooms in remote Pacific waters of the Southern Ocean
28. Atmospheric transport of iron and its deposition in the ocean
29. Iron in ice cores from Law Dome, East Antarctica: Implications for past deposition of aerosol iron
30. Nutrient and trace-metal geochemistry of an in situ iron-induced Southern Ocean bloom
31. Phytoplankton processes. Part 1: Community structure during the Southern Ocean Iron RElease Experiment (SOIREE)
32. Phytoplankton process. Part 2: Rates of primary production and factors controlling algal growth during the Southern Ocean Iron RElease Experiment (SOIREE)
33. Complex lessons of iron uptake
34. The role of iron in phytoplankton photosynthesis, and the potential for iron-limitation of primary productivity in the sea
35. Determination of complexation of iron(III) with natural organic complexing ligands in seawater using cathodic stripping voltammetry
36. The behaviour of iron and other trace elements during the IronEx-I and PlumEx experiments in the Equatorial Pacific
37. On the conditions for the production of plankton in the sea
38. The importance of siderophores in iron nutrition of heterotrophic marine bacteria
39. The impact of in situ Fe fertilisation on the microbial food web in the Southern Ocean
40. Response of the marine diatom Thalassiosira weissflogii to iron stress
41. Distinguishing between extra and intracellular iron in marine phytoplankton
42. Grazer-mediated regeneration and assimilation of Fe, Zn and Mn from planktonic prey
43. Iron and regenerated production - Evidence for biological iron recycling in two marine environments
44. Competition among marine phytoplankton for different chelated iron species
45. Atmospheric iron input to the oceans
46. Iron photochemistry in seawater from the Equatorial Pacific
47. What controls dissolved iron concentrations in the world ocean?
48. Microbial ferrous wheel
49. Controls on iron(III) hydroxide solubility in seawater - The influence of pH and natural organic chelators
50. Increased biological productivity and export production in the glacial Southern Ocean
51. Modelling phytoplankton blooms and carbon export production in the Southern Ocean: Dominant controls by light and iron in the Atlantic sector in austral spring 1992
52. The contrasting biogeochemistry of iron and manganese in the Pacific Ocean
53. Automated vacuum analysis of sulphur hexafluoride in seawater -Derivation of the atmospheric trend (1970-1993) and potential as a transient tracer
54. Sulphur hexafluoride as a tracer of biogeochemical and physical processes in an open-ocean iron fertilisation experiment
55. Mixing of a tracer in the pycnocline
56. Relationships between biovolume and biomass of naturally derived marine bacterioplankton
57. 2 concentrations
58. Dust sources and deposition during the last glacial maximum and current climate: A comparison of model results with paleodata from ice cores and marine sediments
59. Influence of N substrate on Fe requirements of marine centric diatoms
60. Utilisation of iron bound to strong organic ligands by plankton communities in the Subarctic Pacific Ocean
61. Iron uptake and physiological response of phytoplankton during a mesoscale Southern Ocean iron enrichment
62. Iron acquisition by photosynthetic marine phytoplankton from ingested bacteria
63. 2 change: The iron hypothesis
64. Testing the iron hypothesis in ecosystems of the Equatorial Pacific Ocean
65. Iron deficiency limits phytoplankton growth in the North-east Pacific Subarctic
66. Iron deficiency limits phytoplankton growth in Antarctic waters
67. North-east Pacific iron distributions in relation to phytoplankton productivity
68. Iron in Antarctic waters
69. VERTEX: Phytoplankton/iron studies in the Gulf of Alaska
70. 2 in seawater
71. The oxidation kinetics of Fe(II) in seawater
72. Limitation of productivity by trace-metals in the sea
73. Measurements of air-sea gas transfer during an open-ocean algal bloom
74. Is Southern Ocean organic carbon and biogenic silica export enhanced by iron-stimulated increases in biological production? Sediment trap results from SOIREE
75. Climate and atmospheric history of the past 420, 000 years from the Vostok ice core, Antarctica
76. Iron distributions in surface waters of the South Atlantic
77. Biological cycling of iron in the ocean
78. Predictions of Mn and Fe use efficiencies of phototrophic growth as a function of light availability for growth and of C assimilation pathway
79. Complexation of iron(III) by natural organic ligands in the central North Pacific as determined by a new competitive ligand equilibration adsorptive cathodic stripping voltammetric method
80. The role of organic complexation on ambient iron chemistry in the Equatorial Pacific Ocean and the response of a mesoscale iron addition experiment
81. The role of iron nutrition in photosynthesis and nitrogen assimilation in Scenedesmus quadricauda (Chlorophyceae)
82. 234Th
83. Simulated response of the ocean carbon cycle to anthropogenic climate warming
84. Assimilation of Fe and carbon by marine copepods from Fe-limited and Fe-replete diatom prey
85. Regulation of algal blooms in Antarctic shelf waters by the release of iron from melting sea ice
86. Limitation of algal growth by iron deficiency in the Australian Subantarctic region
87. The distribution of Fe in the Australian sector of the Southern Ocean
88. Distributions of phytoplankton blooms in the Southern Ocean
89. Iron uptake and growth limitation in oceanic and coastal phytoplankton
90. Iron-mediated effects on nitrate reductase in marine phytoplankton
91. Iron stress in the Pacific region of the Southern Ocean: Evidence from enrichment bioassays
92. Marine bacteria and biogeochemical cycling of iron in the oceans
93. The role of heterotrophic bacteria in iron-limited ocean ecosystems
94. Circulation and seasonal evolution of polar waters south of Australia: Implications for iron fertilisation of the Southern Ocean
95. Iron enrichment experiments in the Southern Ocean: Physiological responses of plankton communities
96. Relationships between cell-volume and the carbon and nitrogen content of marine photosynthetic nanoplankton
97. The effect of in situ iron addition on the sinking rates and export flux of Southern Ocean diatoms
98. 2
99. Annual primary production and export flux in the Southern Ocean from sediment trap data
100. Mesozooplankton community composition, feeding, and export production during SOIREE
101. The dissolution of atmospheric iron in surface seawater of the open-ocean