For decades, air pollution drifting from East Asia out over the world’s largest ocean has kicked off a chain reaction that contributed to oxygen levels falling in tropical waters thousands of miles away, new research shows.
“There’s a growing awareness that oxygen levels in the ocean may be changing over time,” says Taka Ito, an associate professor at Georgia Institute of Technology. “One reason for that is the warming environment—warm water holds less gas. But in the tropical Pacific, the oxygen level has been falling at a much faster rate than the temperature change can explain.”
In the report, the researchers describe how air pollution from industrial activities had raised levels of iron and nitrogen—key nutrients for marine life—in the ocean off the coast of East Asia. Ocean currents then carried the nutrients to tropical regions, where they were consumed by photosynthesizing phytoplankton.
But while the tropical phytoplankton may have released more oxygen into the atmosphere, their consumption of the excess nutrients had a negative effect on the dissolved oxygen levels deeper in the ocean.
“If you have more active photosynthesis at the surface, it produces more organic matter, and some of that sinks down,” Ito says. “And as it sinks down, there’s bacteria that consume that organic matter. Like us breathing in oxygen and exhaling CO2, the bacteria consume oxygen in the subsurface ocean, and there is a tendency to deplete more oxygen.”
That process plays out in all across the Pacific, but the effects are most pronounced in tropical areas, where dissolved oxygen is already low.
Declining since the 1970s
Athanasios Nenes, a professor at Georgia Tech who worked with Ito on the study, says the research is the first to describe just how far reaching the impact of human industrial activity can be.
“The scientific community always thought that the impact of air pollution is felt in the vicinity of where it deposits,” says Nenes. “This study shows that the iron can circulate across the ocean and affect ecosystems thousands of kilometers away.”
While evidence had been mounting that global climate change may have an impact on future oxygen levels, Ito and Nenes were spurred to search for an explanation for why oxygen levels in the tropics had been declining since the 1970s.
To understand how the process worked, the researchers developed a model that combines atmospheric chemistry, biogeochemical cycles, and ocean circulation. Their model maps out how polluted, iron-rich dust that settles over the Northern Pacific gets carried by ocean currents east toward North America, down the coast and then back west along the equator.
In their model, the researchers accounted for other factors that can also impact oxygen levels, such as water temperature and ocean current variability.
Whether due to warming sea waters or an increase in iron pollution, the implications of growing oxygen-minimum zones are far reaching for marine life.
“Many living organisms depend on oxygen that is dissolved in seawater,” Ito says. “So if it gets low enough, it can cause problems, and it might change habitats for marine organisms.”
Not easily replaced
Occasionally, waters from low oxygen areas swell to the coastal waters, killing or displacing populations of fish, crabs and many other organisms. Those “hypoxic events” may become more frequent as the oxygen-minimum zones grow, he adds.
The increasing phytoplankton activity is a double-edged sword, according to Ito.
“Phytoplankton is an essential part of the living ocean,” he says. “It serves as the base of food chain and absorbs atmospheric carbon dioxide. But if the pollution continues to supply excess nutrients, the process of the decomposition depletes oxygen from the deeper waters, and this deep oxygen is not easily replaced.”
The study also expands on the understanding of dust as a transporter of pollution, Nenes says.
“Dust has always attracted of a lot of interest because of its impact on the health of people,” Nenes says. “This is really the first study showing that dust can have a huge impact on the health of the oceans in ways that we’ve never understood before. It just raises the need to understand what we’re doing to marine ecosystems that feed populations worldwide.”
The study, published in Nature Geoscience, was sponsored by the National Science Foundation, a Georgia Power Faculty Scholar Chair and a Cullen-Peck Faculty Fellowship.
Source: Georgia Tech
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