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- W1989343721 abstract "Abstract. Rising atmospheric CO2 is acidifying the surface ocean, a process which is expected to greatly influence the chemistry and biology of the future ocean. Following the development of iron-replete phytoplankton blooms in a coastal mesocosm experiment at 350, 700, and 1050 μatm pCO2, we observed significant increases in dissolved iron concentrations, Fe(II) concentrations, and Fe(II) half-life times during and after the peak of blooms in response to CO2 enrichment, suggesting increased iron bioavailability. If applicable to the open ocean this may provide a negative feedback mechanism to the rising atmospheric CO2 by stimulating marine primary production." @default.
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- W1989343721 date "2009-07-09" @default.
- W1989343721 modified "2023-09-27" @default.
- W1989343721 title "Ocean acidification affects iron speciation in seawater" @default.
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- W1989343721 doi "https://doi.org/10.5194/bgd-6-6781-2009" @default.
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