Not exact matches
Both processes occur in regions of the
ocean that are naturally low in oxygen, or anoxic,
due to local lack of water circulation and intense phytoplankton
productivity overlying these regions.
Fertilizing the surface
ocean with iron increases biological
productivity, but the resulting carbon dioxide removal will be much less than expected
due to the increased
productivity of diatoms, which incorporate and remove the bioavailable iron.
There is another important angle to the
ocean productivity issue that you might consider — there is a very real danger that the satellites that provide climate - research quality observations of this kind will not be available in the near future
due to limited budgets and other priorities.
How would you improve the
productivity of coccolithophores — especially as an acidifying
ocean (
due to anthropogenic CO2 emisssions) in hibits their growth?