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June 11, 2008

Global warming’s twin, ocean acidification, is here

The impacts of CO2 emissions on the marine realm have surfaced in Pacific waters.

Since the Industrial Revolution, oceans have absorbed an estimated 525 billion metric tons of human-generated CO2 and become 30% more acidic. This acidification is decreasing the amount of carbonate available for marine organisms such as plankton and corals to construct calcium carbonate shells and skeletons. The effects have remained virtually invisible thus far, but now, in a study published online May 22 in Science (DOI 10.1126/science.1155676), researchers report detecting acidified surface water along the west coast of North America.

The pteropod <em>Limacina helicina</em>, or planktonic sea snail, is one creature at risk from ocean acidification. It is an important food source for Pacific salmon, cod, and herring.
RUSS HOPCROFT, UAF/NOAA
The pteropod Limacina helicina, or planktonic sea snail, is one creature at risk from ocean acidification. It is an important food source for Pacific salmon, cod, and herring.

Deep ocean waters normally are more acidic and have higher CO2 levels than shallow waters because decomposing organic matter sinks and makes deep water acidic, and deep water contains CO2 absorbed when the water last circulated to the surface. Seasonal upwelling propels this deep water onto continental shelves. During the spring of 2007, Richard Feely of the National Oceanic and Atmospheric Administration’s Pacific Marine Environmental Laboratory and colleagues sampled waters along 13 survey lines extending from British Columbia (Canada) to Baja California (Mexico). The water was more acidic than expected close to shore and near the surface, and the entire water column was undersaturated in carbonate down to 50 meters in places, which would make it difficult for marine organisms to form calcium carbonate shells. According to the researchers’ calculations, the conditions would not have occurred without the continually rising levels of anthropogenic CO2 added to these waters.

As the ocean continues to absorb CO2, global seawater circulation patterns will bring increasingly acidic waters to shallower depths. Under current carbon emissions trends, carbonate levels could plunge by as much as 50% by 2100, Feely says. In studies mimicking future ocean acidification conditions, researchers have found a range of harmful impacts, from the dissolution of plankton and bivalve shells to depressed metabolism in mollusks and invertebrates. “Acidified water disrupts multiple physiological processes,” explains Jim Barry of the Monterey Bay Aquarium Research Institute. “For coral reefs and other calcifying animals, the effects may be large, but we don’t know yet what the long-term impacts will be on all marine ecosystems.” —NOREEN PARKS

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