ocean acidification

Ocean acidification has been called the evil twin of global warming. Carbon dioxide emitted into the atmosphere is absorbed by ocean water, forming acid in the process. As a result, the acidity of the ocean has increased measurably in recent decades. More acidic oceans could have severe consequences for marine animals and plants, the ecosystems they build, and the economies they drive.

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Applying lessons from overfishing to climate change

Photo courtesy of Mark Kasianowicz, Massachusetts State House Photographer.

A wood carving of a cod fish has hung in the Massachusetts' State House since 1747. The state's iconic fish has been decimated by overfishing and now faces increasing pressures from climate change.

New England’s fisheries stand at a cross-roads. With the strict fishing limits that went into effect for the 2010 fishing year (which ends in just over a month), fisheries regulators believe we have reached an historic milestone: the end of overfishing in U.S. waters. Or, more accurately, the beginning of sustainable fishing. Reaching this point has been financially painful for New England fishermen (and yes, many would consider that to be a gross understatement). But catch limits are expected to rise in coming years as historically overfished populations begin to recover, leading some in the industry to say that fisheries have reached their lowest point and things are starting to look up.

But here’s the catch (no pun intended). A few years ago, Michael Fogarty of the New England Fisheries Science Center in Woods Hole told me that he expected climate change to overtake overfishing as the primary pressure on fish populations within a decade. Indeed, the impacts of climate change on marine life – including commercially important fish species – are becoming increasingly apparent.

Scientists with the New England Fisheries Science Center in Woods Hole have documented dozens of species of fish and shellfish gradually shifting northward and into deeper offshore waters in response to warming waters.

William Cheung of the University of East Anglia predicts that the poleward movement could be as rapid as two and a half miles per year, and his computer models match up well with what scientists are seeing on the ground (or in the water). That means that the waters around Cape Cod could could be too warm for the region’s iconic namesake within decades.

Then there are the changes in water chemistry that come with rising levels of carbon dioxide – decreasing amounts of oxygen, increasing acidity. Although the idea is still open for debate, many scientists expect the combination of warming and shifting chemistry to cause precipitous declines in the abundance of the microscopic plants at the base of the food chain. Limited food plus inhospitable water conditions are a recipe for one thing – smaller fish. Cheung says we’ll likely see the maximum size of fish cut almost in half by 2050 and predicts a 30% drop in the tonnage of New England fish harvests.

While climate change and overfishing are fundamentally different processes, they present some of the same challenges for fishermen – namely, reducing both the size and number of fish. As a result, many of the strategies for coping with the two problems could be similar. Last week, I mentioned innovative projects around New England aimed at raising profit margins for fishermen catching fewer fish. But there’s another important component: diversification.

Catching smaller amounts of lots of different fish is one way fishermen can catch enough fish to stay afloat financially without putting undue pressure on any one species. But that assumes there’s a market for all those different fish. And that requires willing retailers and informed consumers – people who know how to cook and enjoy herring and redfish, as well as cod and haddock. There’s a growing interest in sustainable seafood, in all its varied possible forms, so there’s reason to be optimistic on this front.

Of course, to blithely say that fishermen can handle climate change and overfishing the same way ignores a fundamental difference. Catch limits and diversification are actually direct solutions to the problem of overfishing. In the case of climate change, the same measures are merely means of adapting to the completely external problem of climate change. The only way to solve the problem is limit greenhouse gas emissions, and that’s not something fishermen can do by themselves.

Postcard from a changing sea

U.S. Geological Survey

There is evidence that changes in ocean acidity linked to rising carbon dioxide levels is already impacting health and survival of scallops and other shellfish.

As you may recall, ocean acidification is the phenomenon in which carbon dioxide from the atmosphere dissolves in the surface waters of the ocean, producing carbonic acid that (in sufficient quantities) shifts the pH balance of the ocean toward acidity and impairs the ability of animals like oysters and corals to extract the calcium carbonate they need to build their skeletons or shells. In the past 200 years, the ocean has absorbed nearly a third of carbon dioxide emissions, resulting in a 30% increase in ocean acidity. There’s evidence that ocean acidification is already impacting the health and survival of bay scallops (like that little guy in the photo) and other shellfish.

In an effort to raise awareness about the problem of ocean acidification – and their research on the topic – scientists with the U.S. Geological Survey are trying something a little out of the ordinary: they’re making postcards. This particular one caught my eye, not because it was breathtakingly exotic. Exactly the opposite. A scallop nestled in eelgrass is a scene you might find any number of places around Cape Cod. It’s a reminder that ocean acidification isn’t just happening to remote coral reefs; it’s happening right here and now.

The staying power of plastic

There’s a lot of uncertainty about what the ocean will look like in fifty or a hundred years. Will fishing drive large fish extinct? Will rising water temperatures decimate the microscopic marine plants upon which all life on Earth depends? Will ocean acidification caused by the absorption of increasing atmospheric carbon dioxide bring corals and shellfish to their knees?

Harry – a resident of Saco, Maine, who collects plastic debris from his local beach and blogs about it at The Flotsam Diaries – says one thing is certain: there will still be plastic. In a rather extreme demonstration of the effects of acidity, Harry put clam shells in one bucket with vinegar and put plastic debris in another. After a week, the clam shells had completely dissolved. Not so for the plastic, as the video shows.

The ocean isn’t going to turn to vinegar, or anything remotely close. So it’s not a terribly realistic picture of what will happen to shellfish. But it’s a vivid reminder of the staying power of plastic.

Ocean acidification on your iPhone

flickr/marcopapale

Are you the type that has all ten of Climate Central’s top-rated climate science apps for iPhone? Then check this out: CO2calc, a new user-friendly software package for Windows, Mac … or iPhone. You enter basic water chemistry data – pH, salinity, temperature – and it calculates local carbon dioxide levels in the water and atmosphere. It’s not flashy. To be honest, it’s a pretty bare bones interface intended as a serious research tool for scientists. So it’s not for everybody. Still cool, though.

(Ocean) Science Friday

Last Friday, NPR’s Science Friday broadcast live from the Our Changing Oceans conference hosted by the National Council for Science and the Environment. It was two straight hours of ocean science. As you might imagine, I was in listening heaven. In case you missed it (or want to hear it again):

Ocean acidification, part I: carbon dioxide

As carbon dioxide accumulates in the atmosphere, so too in the ocean. The result is a complex web of chemical reactions that, collectively, have come to be known as ocean acidification. Often called “global warming’s evil twin” or “the other carbon dioxide problem”, ocean acidification has risen to widespread notice, if not fame, in the past five years. What follows is the first in a three-part exploration of the diverse chemical and ecological impacts of rising carbon dioxide in the ocean.

Part I: Carbonation

Carbon dioxide is highly soluble in water (kind of like salt or sugar), so carbon dioxide levels in the ocean rise in proportion to increases in atmospheric carbon dioxide. In the past two centuries, it is estimated that the ocean has absorbed somewhere between a third and half of all man-made carbon dioxide emissions. That’s on top of naturally-produced carbon dioxide (from animals breathing, plants dying, forest fires, volcanoes) that the ocean normally absorbs as part of the global carbon cycle. Call it ocean carbonation.

Carbon dioxide is not inherently evil. In fact, it is necessary for life on Earth. All plants – from microscopic marine phytoplankton to towering Redwood trees – produce the sugars they need to grow and the oxygen so crucial to life on Earth using the energy of the sun and (drumroll, please) carbon dioxide. In addition, some marine microbes “fix” carbon dioxide into biological building blocks using chemical energy – a process known as chemosynthesis.

In theory, rising levels of carbon dioxide could act like a fertilizer for such organisms. That, in turn, could spur growth throughout the oceanic food web and, ultimately, trap more carbon dioxide in the deep ocean – Mother Ocean’s way of balancing out the increasingly tilted carbon equation.  It’s a lovely and reassuring idea. But, in reality, it’s not at all clear that will happen. That’s because phytoplankton growth in the ocean tends to be limited by nutrients other than carbon dioxide, especially iron. So adding all the carbon dioxide in the world might not lead to more phytoplankton. And ocean acidification may actually exacerbate iron limitation (we’ll get to that in part 3), further limiting – not boosting – phytoplankton populations.

Then, of course, there are all those animals in the ocean, most of them essentially breathing water. For them, excess carbon dioxide can be a serious health problem – in medical terms, hypercapnia. Just as in the ocean, elevated levels of carbon dioxide in the body of a fish or worm cause acid-base imbalance (fish acidification?); restoring that balance is energy-intensive (impossible for some species) and can cause secondary chemical imbalances. Hypercapnia can also dramatically slow down metabolism and reduce the oxygen-carrying capacity of blood. Coping with elevated carbon dioxide levels for short periods of time is a natural part of life for many marine animals. But permanent alterations in environmental and bodily chemistry – even subtle ones – pose potentially serious repercussions for growth, reproduction, even survival.

In part two of my ocean acidification series, I’ll tackle acidification itself – why, how much, and what it means.

Ocean acidification: no small change

Oceana’s CEO Andrew Sharpless has something to say about ocean acidification:

The sea’s pH can vary from place to place. But just a few hundred years ago, it was typically about 8.2. Today, due to all the carbon dioxide we’ve spewed into the atmosphere, it is about 8.1.

It may seem that such a small change wouldn’t create a big problem, and that ocean ecosystems will cope just fine. The sad reality is that ocean acidification is a bigger problem than the number suggests. One reason is that, due to the way pH scales work, a 0.1 drop in pH is actually a 26 percent increase in acidity. Another is that this acidification has occurred with “startling” rapidity, scientists say – perhaps 100 times faster than anything Earth’s sea life has experienced in millions of years…

flickr/jakmi

The test, or shell, of the 'foram' Elphidium.

Already, ocean scientists are seeing just the kind of corrosive effects you would expect from acidification. Last year, for instance, one team reported in the prestigious journal Science that coral growth along Australia’s Great Barrier Reef had declined by 14 percent since 1990 – a “severe and sudden decline” unseen in centuries. Other studies have found that the shells of some “forams” – tiny creatures that are a key part of the marine food chain – are 30 percent lighter today than they were in the past…

But things could get worse. Thanks to some irrefutable laws of physics and math, researchers have calculated that ocean pH will fall to about 7.8 by the end of the century, if we don’t act soon to curb our carbon dioxide emissions. That is a four-tenths pH drop from pre-industrial levels – or a whopping 150 percent increase in acidity. Our seas haven’t been that acidic in tens of millions of years.

Sharpless walks a fine line between exposing harsh realities and ranting (okay, maybe he crosses the line once or twice), but his message is clear: ocean acidification is no small change.

Ocean acidification may limit phytoplankton

Spike Walker, Wellcome Images

Diatom frustules - shells - seen under a polarizing light microscope. Diatoms may be responsible for half of all phytoplankton productivity.

If it’s not one thing, it’s another. Serious questions have been raised about the claim that warming seas have caused a precipitous decline in global phytoplankton abundance. But another study, this one published in Science, says that ocean acidification – the direct chemical result of carbon dioxide dissolving in ocean waters, sometimes called global warming’s evil twin – may threaten phytoplankton populations. Here’s the skinny.

WHAT WE KNOW

As atmospheric carbon dioxide dissolves in the ocean, water and carbon dioxide react to form carbonic acid. One major impact of this reaction is that it limits the amount of calcium bicarbonate available for organisms like oysters, corals, and phytoplankton to build their shells or skeletons (yes, some phytoplankton have shells). Increasing amounts of carbonic acid also shift the pH of the ocean toward greater acidity, and that, according to the new study, can reduce the availability of iron – a nutrient crucial to phytoplankton growth that is already limiting in many parts of the ocean.

HOW WE KNOW IT

The researchers grew four species of phytoplankton – Thalassiosira weissflogii (coastal), Thalassiosira oceanica (open ocean), Phaeodactylum tricornutum, and Emiliana huxleyi – in the lab, varying the pH and the amount and type of iron present. In every case, as the pH dropped (acidity increased) the planktors (that’s what you call individual plankton) took in less and less iron. That result, alone, could be explained one of two ways – a chemical change in the availability of iron, or a physiological change in the planktors’ ability to take in the iron. But the researchers also looked at what happened when pH was held steady and iron levels varied. Again, the result was unanimous – all of the planktors were able to take up more iron if given more iron, even under the most acidic conditions. That suggests that the effect of ocean acidification is to limit the availability of iron, not the physiological ability of plankton to get the iron.

The researchers point out that most iron in the ocean isn’t floating around on its own, it’s bound to organic molecules – long chains of carbon, hydrogen, oxygen, and nitrogen. In the lab, the researchers ran their experiments using a few different organic molecules that bind iron, called chelators. Changing the chelator dramatically changed the end result, completely erasing the effect of acidity on iron availability in some cases.

WHAT WE DON’T KNOW

Whether this will bear out in the real world – where there are a lot of different organic molecules floating around – is an open question. The researchers did try running their experiments with some ocean water samples; the results were undramatic, showing a very slight trend toward decreasing iron uptake that was only statistically significant at pH levels equivalent to carbon dioxide levels two and a half times the current level.

There’s also the fact that other climate change-related processes could counteract the impact of pH on iron availability. For example, most of the iron in the ocean comes from dust and climate change may increase the amount of dust that falls on the ocean.

WHAT IT MEANS

“We’re just at the beginning of research on ocean acidification,” said François Morel of Princeton University, the senior investigator in the team. “This is the first study published of its kind that looks at the uptake of a critical nutrient.”

It’s certainly an important area to consider, says Ken Buesseler of Woods Hole Oceanographic Institution: “The concept of changes to ocean productivity and ecosystems due to acidification is a very important one to consider. If half of the photosynthesis on the planet is in the ocean and if you reduce that because of acidification, that is a big deal.”

But at this point, that’s still a big IF.

Discovery of the year: ocean acidification is happening NOW

The greatest threat facing the ocean, namely rising levels of carbon dioxide in the atmosphere, actually poses two distinct threats – warming and acidification. Each will get its day in the “Discovery of the Year” spotlight. Today, it’s ocean acidification’s turn.

As you may recall, ocean acidification is the phenomenon in which carbon dioxide from the atmosphere dissolves in the surface waters of the ocean, producing carbonic acid that (in sufficient quantities) shifts the pH balance of the ocean toward acidity and impairs the ability of animals like oysters and corals to extract the calcium carbonate they need to build their skeletons or shells. In the past 200 years, the ocean has absorbed nearly a third of carbon dioxide emissions, resulting in a 30% increase in ocean acidity.

Stony Brook University

The impacts of ocean acidification - slowed growth and thinner shells - are strikingly visible in a side-by-side comparison of quahogs raised in water simulating past (250ppm), present (390ppm) and future (750ppm and 1500ppm) levels of atmospheric carbon dioxide.

Scientists have generally considered the impacts of ocean acidification to be a problem of the (near) future. But in September 2010, two marine scientists from Stony Brook University – Stephanie Talmage and Christopher Gobler – published a paper in the Proceedings of the National Academy of Sciences that forced a revision of that thinking, suggesting that ocean acidification may already be (and have been for some time) taking a toll on shellfish.

WHAT WE KNOW (and HOW WE KNOW IT)

Talmage and Gobler reared quahogs (Mercenaria mercenaria) and bay scallops (Argopecten irradia) under conditions simulating past, present, and likely future carbon dioxide levels. Not surprisingly (because numerous previous studies have documented similar findings), the shellfish of the future had severe shell defects, higher death rates, and slower growth than their modern-CO2 counterparts. What was less expected was the observation that modern conditions produced shellfish with thinner shells, slower growth, and death rates almost double those of shellfish grown in pre-industrial water conditions.

WHAT IT MEANS

Talmage and Gobler conclude that ocean acidification “may [already] be inhibiting the development and survival of larval shellfish and contributing to global declines of some bivalve populations.” In fact, since shellfish grown in the laboratory are granted a relatively luxurious life with abundant food and no predators or competitors, the authors say their data represent conservative estimates of the impacts of acidification. In the wild, slow-growing, thin-shelled animals would likely be vulnerable to any number of untimely ends – predation, over-crowding, incidental crushing. Stressed animals may also be more susceptible to diseases, like those that have ravaged east coast oyster populations in recent decades.

WHAT WE DON’T KNOW

With ocean acidity reaching levels not seen in over twenty million years, perhaps the biggest question on many scientists’ minds is whether evolutionary adaptation will be able to keep pace with rising acidity.

Top stories of the year: #3 – ocean acidification

flickr/greenkayak73

Ocean acidification - the result of increasing quantities of carbon dioxide dissolving in the ocean - threatens oysters and other organisms with calcium-based shells. A memo from the EPA makes clear that the problem is subject to the Clean Water Act.

#3. EPA policy for addressing ocean acidification through the Clean Water Act

Carbon dioxide emissions don’t just build up in the atmosphere; nearly a third of atmospheric carbon dioxide gets absorbed by the ocean. As carbon dioxide dissolves in water, it produces carbonic acid. On a grand enough scale, this process can shift the pH balance of the ocean. Indeed, as a whole, the ocean is approximately 30% more acidic than it was two hundred years ago. This phenomenon is called ocean acidification. It is a problem which has the potential to decimate organisms with calcium-based shells (corals, oysters) and rearrange oceanic food webs. But, until recently (say, the past five years), the problem went largely unrecognized; even ocean scientists did not fully grasp our ability to alter the fundamental chemistry of the vast ocean.

In mid-November, the Environmental Protection Agency published a memo that put ocean acidification on the federal regulatory map. The memo elucidated the Agency’s stance that changes in the acidity of coastal waters caused (or presumed to be caused) by rising atmospheric carbon dioxide levels could be listed under the Clean Water Act. Continue reading