The main conversation around climate change focuses primarily on one thing: how much carbon is in the air – and by extension how to reduce it. However, what is less talked about, but which can become incredibly important, is how much carbon there is in our oceans. There is 50 times more carbon in the ocean than in the atmosphere. Some climate scientists believe that if we could just slightly increase the amount of carbon the ocean can absorb from the atmosphere, we could avoid some of the worst effects of climate change.
It may seem unusual when you first hear it, but think about it a little longer. The ocean covers approximately 70 percent of the Earth’s surface, and it naturally absorbs carbon dioxide – and effectively dissolves it. Phytoplankton in the ocean use this carbon dioxide and sunlight to drive photosynthesis just like land-based plants. Oxygen is produced by this process – phytoplankton are actually responsible for about 50 percent of the oxygen in our atmosphere.
Some climate scientists have suggested that if we could just increase the amount of phytoplankton in the ocean, we could pull more carbon out of the atmosphere. A well-known way to produce a phytoplankton bloom is to introduce iron, an essential nutrient for the plankton community, to the water. Many parts of the ocean are low in iron, so even a relatively small addition of iron could theoretically produce a lot of phytoplankton and thus remove a lot of carbon dioxide from the atmosphere.
How to arm our dying oceans against climate change
“Give me half a tanker of iron and I’ll give you an ice age,” wrote John Martin, an oceanographer at Moss Landing Marine Laboratories, in 1988. Back then, most people were just getting to know the idea. climate change as we know it now. But that’s also around the time people started thinking about how iron fertilization could affect phytoplankton growth and in turn change atmospheric carbon levels.
Although climate scientists have spent a lot of time discussing this strategy among themselves, there has not been a concerted effort to explore it further and take it seriously. Ken Buesseler, a marine radiochemist at the Woods Hole Oceanographic Institution, is a researcher who has researched iron fertilization in the ocean. He and his team looked at whether introducing iron could “change the carbon flow to the deep ocean” and found that there was a significant carbon sequestering effect.
Buesseler told The Daily Beast that his research was done almost 20 years ago, and it hasn’t been much since.
“What happened 20 years ago is we started going around and we would spread out a chemical form of iron and look for that phytoplankton – the plant response – and it actually showed very clearly that if you improve the iron, you can create more uptake of carbon dioxide,” Buesseler said. “The difference between now and 20 years ago is that I think the climate crisis is so much more apparent to the public.”
A phytoplankton bloom off the coast of Iceland, seen from space.
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