Phytoplankton not only constitutes the foundation of the food chain in the
oceans, it also fixes carbon through photosynthesis and
generates oxygen with the help of solar energy.
Ocean acidification is also predicted to reduce microbial production of nitrate from ammonium (Beman et al., 2011), which could have major consequences for oceanic primary production because a significant fraction of the nitrate used by phytoplankton is generated by nitrification at the ocean surface (Yool et al., 2
Ocean acidification is also predicted to reduce microbial production of nitrate from ammonium (Beman et al., 2011), which could have major consequences for oceanic primary production because a significant fraction of the nitrate used by
phytoplankton is
generated by nitrification at the
ocean surface (Yool et al., 2
ocean surface (Yool et al., 2007).
This indicates that replacing missing iron back into the
ocean could stimulate
phytoplankton based photosynthesis and
generate improvements to the
ocean ecosystem, while removing carbon dioxide from the atmosphere as it is consumed by photosynthesis.