Modeling the geochemical cycle of iron in the oceans and its impact on atmospheric CO2 concentrations
Open Access
- 1 September 1999
- journal article
- Published by American Geophysical Union (AGU) in Global Biogeochemical Cycles
- Vol. 13 (3) , 727-736
- https://doi.org/10.1029/1999gb900034
Abstract
No abstract availableKeywords
This publication has 53 references indexed in Scilit:
- What controls dissolved iron concentrations in the world ocean?Published by Elsevier ,1998
- What controls dissolved iron concentrations in the world ocean? Authors' closing commentsMarine Chemistry, 1997
- What controls dissolved iron concentrations in the world ocean? — a commentMarine Chemistry, 1997
- Control of dissolved iron concentrations in the world ocean, A commentMarine Chemistry, 1997
- What controls dissolved iron concentrations in the world ocean? — a commentMarine Chemistry, 1997
- Terrigenous Fe input and biogenic sedimentation in the glacial and interglacial equatorial Pacific OceanGlobal Biogeochemical Cycles, 1995
- Biogenic flux of Al to sediment in the central equatorial Pacific Ocean: Evidence for increased productivity during glacial periodsPaleoceanography and Paleoclimatology, 1993
- Three-dimensional simulations of the impact of Southern Ocean nutrient depletion on atmospheric CO2 and ocean chemistryLimnology and Oceanography, 1991
- Iron deficiency limits phytoplankton growth in Antarctic watersGlobal Biogeochemical Cycles, 1990
- The cause of the glacial to interglacial atmospheric CO2 change: A Polar Alkalinity HypothesisGlobal Biogeochemical Cycles, 1989