Don’t believe in climate change? Talk to a clam digger. ‘Pray that the winds change soon.’
By Maria Dolan
18 February 2013 (Slate) – Behind the counter at Seattle’s Taylor Shellfish Market, a brawny guy with a goatee pries open kumamoto, virginica, and shigoku oysters as easily as other men pop beer cans. David Leck is a national oyster shucking champion who opened and plated a dozen of them in just over a minute (time is added for broken shells or mangled meat) at the 2012 Boston International Oyster Shucking Competition. You have to be quick, these days, to keep up with demand. The oysters here were grown nearby in Taylor’s hundred-year-old beds, but the current hunger for pedigreed mollusks on the half shell stretches to raw bars and markets across the country. A similar oyster craze swept the United States in the 1800s, when the bivalves were eaten with alacrity in New York, San Francisco, and anywhere else that could get them fresh. Development of a fancy new technology, canning, meant there was money in preserved oysters, too. Gold miners in Northern California celebrated their riches with an oyster omelet called hangtown fry. New Yorkers ate them on the street; late at night they ate them in “oyster cellars.” Walt Whitman had them for breakfast. That wave crashed. By the early 1900s, oysters were disappearing because of overharvesting and water pollution. Today’s revival is possible because oyster farms are better managed, and regulations have improved water quality. But a modern threat looms for ice-chilled fruits de mer platters, although it’s hard to tell with oyster juice on your chin. This time it’s a worldwide problem, affecting marine ecosystems everywhere. Ocean waters are turning corrosive, and it’s happening so quickly scientists say there may not be any oysters left to eat in coming decades. Ocean acidification, as scientists call this pickling of the seas, is, like climate change, a result of the enormous amount of carbon dioxide humans have pumped into the atmosphere. Oceans have absorbed about a quarter of that output, and ocean chemistry has changed as a result. Surface water pH has long been an alkaline 8.2, not far from the pH of baking soda, but it now averages about 8.1. That doesn’t look like much, but since pH is a logarithmic scale, that means a 30 percent increase in the acidity. By the end of this century, surface water pH could further lower to 7.8 or below. We don’t yet know who the ocean’s winners and losers will be in the more corrosive world. Jellyfish and some seagrasses may thrive under more acidic conditions. On the other hand, calcifiers—organisms that make calcium carbonate shells and skeletons, such as shellfish and corals—appear to be in trouble. In the United States, scientists have seen dissolving clam larvae in Maine, corroded oysters in Washington state’s hatcheries, and mussels with thinned shells off the Pacific Northwest coast. Taylor Shellfish first saw what this pH shift could do to its business in 2006, when the company noticed that two- and three-day-old oyster larvae in its hatcheries were dying. In itself, this wasn’t news. “Hatcheries have a lot of different variables,” says Bill Dewey, Taylor’s spokesperson. “There are a host of reasons your larvae can die.” But this time, none of the usual fixes—filtering out harmful bacteria, for instance—made a difference. By 2009, hatchery production was down 60 to 80 percent, and others in the region were reporting similar problems. Oyster larvae outside of hatcheries were dying, too. In Willapa Bay, an estuary off the southwest Washington coast where a quarter of the nation’s oysters are harvested, many growers rely on natural sets—free-spawning larvae that swim around until they attach themselves to oyster shells placed by growers. Those natural sets stopped producing, and the Willapa growers turned to the struggling hatcheries for oyster seed. The industry finally pulled out of its tailspin in 2010, when NOAA scientists determined that what was killing the oyster larvae was corrosive water that entered the hatchery at certain times of the year—usually in summer, and specifically on days when winds from the northwest caused upwelling of deeper water, which is more acidic than surface water. With federal money, hatcheries were able to install sophisticated pH monitors and CO2 monitors. When waters are becoming too corrosive, hatchery operators can now close off the seawater intake, and, Dewey says, “pray that the winds change soon.” [more]
