What controls dissolved iron concentrations in the world ocean? Authors' closing comments
- 31 July 1997
- journal article
- editorial
- Published by Elsevier in Marine Chemistry
- Vol. 57 (3-4) , 181-186
- https://doi.org/10.1016/s0304-4203(97)00047-9
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific OceanNature, 1996
- Iron stimulation of Antarctic bacteriaNature, 1996
- Controls on iron(III) hydroxide solubility in seawater: The influence of pH and natural organic chelatorsLimnology and Oceanography, 1996
- 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 methodMarine Chemistry, 1995
- Testing the iron hypothesis in ecosystems of the equatorial Pacific OceanNature, 1994
- Atmospheric transport of iron and its deposition in the oceanLimnology and Oceanography, 1991
- Temporal variability of lead in the western North AtlanticJournal of Geophysical Research: Oceans, 1986
- Vertical concentration profiles of lead in the Central Pacific at 15°N and 20°SEarth and Planetary Science Letters, 1983
- Distribution of thorium isotopes between dissolved and particulate forms in the deep seaJournal of Geophysical Research: Oceans, 1982
- Growth rate influence on the chemical composition of phytoplankton in oceanic watersNature, 1979