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Plants consume atmospheric carbon dioxide (CO
2
) during photosynthesis. Oceanic phytoplankton account for almost half of all photosynthesis on Earth. CO
2
is a major contributor to global warming. How could these facts tie together to change global temperature?
In 1990, scientist
John Martin claimed that iron supplies in the Southern Ocean
(also known as the Antarctic Ocean) limit the growth of phytoplankton
tiny, plantlike organisms, including certain algae,
that live in aquatic ecosystems. Martin suggested that higher
iron levels would encourage more phytoplankton to grow in
the ocean. The phytoplankton would remove greater quantities
of CO 2 from the atmosphere
during photosynthesis, therefore contributing to a reduction
of global warming.
A group of scientists conducted an experiment called SOIREE (Southern Ocean iron release experiment) to test Martin's theory. As part of the experiment, the scientists "fertilized" an area of the Southern Ocean with an iron compound. As predicted, an increase occurred in both the phytoplankton levels and rates of photosynthesis near the ocean surface. The scope of the experiment was not sufficient to determine if carbon was drawn to the deep ocean, a process that would be necessary in order to cause a reduction in the atmospheric CO
2
.
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