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- W121474475 abstract "Next to water vapor, carbon dioxide is the most abundant greenhouse gas in the atmosphere. Over the last 150,000 years atmospheric CO{sub 2} levels have fluctuated between 180 and 290 ppmv. Within the last 150 years CO{sub 2} has increased exponentially from 275 to 360 ppmv. Prior to the industrial revolution, fluctuations in CO{sub 2} were a consequence of disequilibrium between global photosynthesis and respiration. Phytoplankton fix 40% of the carbon on the globe, yet account for less than 0.5% of the plant biomass. The geological record suggests that natural variations in atmospheric CO{sub 2} are inversely related to oceanic primary production. I will examine, within the context of plant molecular biology and biochemistry, various hypotheses which seek to explain the variability in phytoplankton production, including atmospheric inputs of iron to the surface ocean, increased nitrogen supply from the deep ocean, and temperature limitation." @default.
- W121474475 created "2016-06-24" @default.
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- W121474475 date "1990-05-01" @default.
- W121474475 modified "2023-09-25" @default.
- W121474475 title "Does phytoplankton photosynthesis influence the global climate" @default.
- W121474475 hasPublicationYear "1990" @default.
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