Emily Sohn, Truthout
May 2009
Mercury concentrations have increased in the Pacific by 30 percent in the last 20 years, the study found. And if emissions continue to rise as expected, the scientists predict another 50 percent jump by 2050
Ocean fish can contain high levels of mercury, even though mercury levels
in the seawater around them are extraordinarily low. Now, scientists have an
explanation for what's going on.
A new study in the Pacific Ocean suggests that algae at the water's surface
absorb mercury from the atmosphere and then sink to mid-depths, where they
decompose and release methylmercury, a highly toxic form of the metal that
poisons both fish and the people who eat them.
Mercury concentrations have increased in the Pacific by 30 percent in the
last 20 years, the study found. And if emissions continue to rise as
expected, the scientists predict another 50 percent jump by 2050.
"We can now explain why large predatory fish in the open oceans have
methylmercury in the first place," said Dave Krabbenhoft, a geochemist with
the United States Geological Survey in Middleton, Wisc. "We don't have to
scratch our heads anymore."
Mercury is a byproduct of coal combustion, industrial waste and other human
activities. It is also a powerful neurotoxin that can cause developmental
problems in babies and heart disease in adults, among other health woes.
More than 90 percent of methylmercury that gets into people in the United
States comes from ocean fish and shellfish, especially tuna.
Yet, compared to lakes, oceans haven't been studied much when it comes to
mercury, and there hasn't been a clear explanation for how mercury gets from
the air into ocean fish. One reason is that ocean waters contain such low
amounts of methylmercury that scientists have struggled to collect reliable
samples.
Krabbenhoft and colleagues were the first to employ new, highly sensitive
techniques to get water samples at 16 sites in the Pacific Ocean, from
Alaska to Hawaii. At each site, the researchers analyzed samples every 100
meters (328 feet) or so, down to a depth of 1,000 meters.
When the team graphed their results, they saw that methylmercury levels were
highest at a depth where oxygen was being depleted the fastest. In this
zone, microbes are busy decomposing dead algae, which sink to a level where
water is dense enough to stop their descent.
That depth ranges from 300 meters (984 feet) to 800 meters (2,620 feet),
depending on the site. Tuna swim to those depths, Krabbenhoft added, but not
deeper.
"This is the first discovery of a specific depth in the ocean at any
particular spot where the maximum amount of methylmercury is produced," said
Krabbenhoft. "That's a really significant finding."
Previous theories proposed that oceanic mercury came either from volcanoes
that sit tens of thousands of meters below the surface, or from river
runoff.
Now, the most plausible theory for how mercury gets into fish in the middle
of the ocean, Krabbenhoft said, is that algae absorb mercury at the surface,
especially off the coast of Asia, where power plants burn lots of coal.
Then, circulation patterns carry the algae in a counter-clockwise pattern
across the Pacific to North America and back again. As the algae die, sink
and decompose along the way, they release methylmercury, which works its way
up the food chain into fish and the people who eat them.
Compared to previous research, the scientists reported an alarming rise in
ocean mercury levels in just the last two decades. Their results appeared in
the journal Global Biogeochemical Cycles.
"It was totally surprising that they were able to detect an increase in
mercury concentration in the Pacific Ocean," said Vincent St. Louis, a
biogeochemist at the University of Alberta. "That's a big body of water."
By clearly linking human-produced emissions with rising mercury levels in
fish, St. Louis added, the work might also help convince policy-makers that
there's a problem with allowing those emissions to rise unchecked.
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