about
Iron-Nutrient Interactions within PhytoplanktonTrace element and isotope deposition across the air–sea interface: progress and research needsOxygen depletion recorded in upper waters of the glacial Southern OceanOcean acidification in a geoengineering contextToxicity of atmospheric aerosols on marine phytoplanktonVolcanic ash fuels anomalous plankton bloom in subarctic northeast Pacific20th-Century doubling in dust archived in an Antarctic Peninsula ice core parallels climate change and desertification in South AmericaDeep carbon export from a Southern Ocean iron-fertilized diatom bloomCan land use intensification in the Mallee, Australia increase the supply of soluble iron to the Southern Ocean?Increased dust deposition in the Pacific Southern Ocean during glacial periods.The impact of iron limitation on the physiology of the Antarctic diatom Chaetoceros simplexBipolar correlation of volcanism with millennial climate changeIncreased productivity in the subantarctic ocean during Heinrich events.The Southern Ocean biogeochemical divide.Biological and physical controls in the Southern Ocean on past millennial-scale atmospheric CO2 changes.Influence of variable rates of neritic carbonate deposition on atmospheric carbon dioxide and pelagic sediments.Climate change: evidence of human causes and arguments for emissions reduction.The influence of Antarctic sea ice on glacial-interglacial CO2 variationsSouthern Ocean dust-climate coupling over the past four million years.Proterozoic ocean redox and biogeochemical stasis.Toxic diatoms and domoic acid in natural and iron enriched waters of the oceanic PacificRío tinto: a geochemical and mineralogical terrestrial analogue of Mars.Stable composition of the nano- and picoplankton community during the ocean iron fertilization experiment LOHAFEX.Distal transport of dissolved hydrothermal iron in the deep South Pacific OceanIroning out carbon export to the deep oceanCO2 and vitamin B12 interactions determine bioactive trace metal requirements of a subarctic Pacific diatomHigh iron requirement for growth, photosynthesis, and low-light acclimation in the coastal cyanobacterium Synechococcus bacillarisA long marine history of carbon cycle modulation by orbital-climatic changes.The Growth Response of Two Diatom Species to Atmospheric Dust from the Last Glacial Maximum.Evolution of South Atlantic density and chemical stratification across the last deglaciation.Photosynthetic maximum quantum yield increases are an essential component of the Southern Ocean phytoplankton response to iron.Iron bioavailability to phytoplankton: an empirical approach.Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation.High particulate iron(II) content in glacially sourced dusts enhances productivity of a model diatom.Deep-sea coral evidence for lower Southern Ocean surface nitrate concentrations during the last ice age.The integral role of iron in ocean biogeochemistry.Ocean acidification decreases the light-use efficiency in an Antarctic diatom under dynamic but not constant light.Biological response to physical processes in the Indian Ocean sector of the Southern Ocean: a case study in the coastal and oceanic waters.Constraints on soluble aerosol iron flux to the Southern Ocean at the Last Glacial Maximum.Recycled iron fuels new production in the eastern equatorial Pacific Ocean
P2860
Q28075533-F2525422-BBE8-4819-8A33-03181E9821F6Q28597231-09451D5E-AFFD-45F3-8BFD-BDB119355128Q28601161-F5EA6679-2C62-4C7A-802E-CA75A1FCA48BQ28728765-78A8FF51-9DE7-4E37-A0EB-191620B9E01BQ28755208-AAAD21D8-79AD-4D07-9E0C-31C8C84E0AB0Q29013633-41A088B3-6F21-4BFA-9E29-B130D7A117D6Q29038800-952BF098-6B9C-4633-890B-B4B536613101Q29395107-E69AB56D-F974-4FA5-8F70-15B6F4338672Q29959606-91D3EF00-5738-4077-8320-EB8703856373Q30741464-8589F59A-BDAE-4386-A8DD-0E9E89ECD5BAQ30797707-60DA4EC1-8E1C-47C1-81E0-5F8A3F5981B0Q30923534-E47EC9E0-5E47-44C0-BE17-F9D1A8314210Q30988452-2D723406-6077-40CD-BC1A-21880D29A6E2Q31045842-06C8322E-380F-4BDF-9895-A43CD9C72F8DQ31096702-8FEE872A-7AFC-48AA-92CF-EF736FD665C1Q33423812-5FB07B7A-DAB8-4120-9CE1-C3469D0E7D14Q33880882-79BAF5A4-EE13-4439-BD24-ABEC34A1CF95Q33895071-C2463BCF-0329-4EAA-87E2-67411D3F86EEQ33981153-71A885B2-1D3F-4183-9FC9-DC4D05BD3DDEQ34334288-704FE4C2-7BCB-4A63-BEEE-93B100A6AD2EQ34376029-78080833-1D8E-4EAC-8E4F-FDBB414FE6E9Q34390442-3B6ED91F-49B7-4034-98A9-5EAB7FBAEEB5Q34526847-4793034D-4C3A-4EFC-9BAE-404D8A326E5DQ34601290-F6E3EA06-108F-48D7-905C-C7F68A523544Q34985414-56BA1E65-5C78-48AC-AE30-F0604A83AC4EQ35135753-701C09DE-F1D4-4E1E-A0DE-8A4D0D98F121Q35753470-0A3C9366-C69F-48A3-BEAC-393B81F7353AQ36032759-630CE096-A9F0-485B-970F-73E14E11F33CQ36069278-ED768FEB-A0AE-42DD-80CC-E2CC23F2ECC7Q36498178-868CE0D1-D834-45C1-817A-FAD0B36B81CFQ36534345-A95B752E-139E-4776-9D9A-87A66527A126Q36756577-4793550D-D1E3-4D94-8836-ED006C82EEF2Q36770472-32394CF5-E8EF-4B95-B1B9-64787A6E8894Q38687143-718C582A-2DE0-4BD0-ACC6-61342D4936D9Q38905097-9A02C0E3-BDB2-4B91-AA4A-4A7A01DBC838Q38933969-3E6ED526-7C46-4A52-B26D-EDE4202E44F1Q39036060-40AD3142-65C9-46A6-B46C-D76C50912823Q39128251-C8C3A594-2A43-4732-8178-922B6FEAB3A7Q39185923-6B2001FF-8BED-4D1B-B3B6-161B8C15CB7AQ42565495-CC26FA05-A16D-4800-97C1-952AC98E3FC6
P2860
description
article
@en
im Februar 1990 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в лютому 1990
@uk
ലേഖനം
@ml
name
Glacial-interglacial CO2 change: The Iron Hypothesis
@en
Glacial-interglacial CO2 change: The Iron Hypothesis
@nl
type
label
Glacial-interglacial CO2 change: The Iron Hypothesis
@en
Glacial-interglacial CO2 change: The Iron Hypothesis
@nl
prefLabel
Glacial-interglacial CO2 change: The Iron Hypothesis
@en
Glacial-interglacial CO2 change: The Iron Hypothesis
@nl
P921
P356
P1433
P1476
Glacial-interglacial CO2 change: The Iron Hypothesis
@en
P2093
John H. Martin
P356
10.1029/PA005I001P00001
P577
1990-02-01T00:00:00Z