Ocean Acidification: Winners and Losers Among Marine Life

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by Carl Drews

What will happen to the Earth’s oceans as the level of dissolved CO 2 in the oceans increases? This post explores the likely consequences of this increase for plants and animals living in the oceans. We will not cover questions about the reality of climate change itself, nor the suggested causes of global warming (human-caused or natural).

The complexity of the earth system is such that nobody can be an expert on all aspects of the atmosphere, hydrosphere, and biosphere. Climate change involves many interrelated scientific disciplines. One of the great things about Panda’s Thumb is that it covers a wide range of scientific topics, and anyone can contribute their own expertise when their particular field comes up. I am sure that PT readers will correct me if I get something wrong here (and even if I don’t!).

Basic Chemistry. Charles Keeling began to measure the atmospheric level of carbon dioxide (CO2) at Hawaii’s Mauna Loa Observatory in 1958. The result of this research is the famous Keeling curve, which shows a time series of atmospheric CO2 that continues to the present day (Figure 1). The level of CO2 was about 290 parts per million (ppm) during 1800-1870, as calculated from ice cores.

DrewsFig1.jpg

Figure 1. Keeling curve of atmospheric carbon dioxide measured at Mauna Loa, Hawaii. Wikimedia Commons: Robert A. Rohde as user Dragons flight.

In climate science, many signals are often combined within a single time series. Figure 1 shows a sinusoidal annual cycle (the figure inset), superimposed over a steady decades-long increase from about 315 ppm to 385 ppm. The annual cycle reflects the earth’s seasons and land-based vegetation: terrestrial plants take up carbon dioxide during their growing season in spring and summer, and release it again during fall and winter. There is more land surface in the northern hemisphere (including Mauna Loa), so the contribution from the southern hemisphere does not balance that from the northern hemisphere. The overall curve is concave upwards, meaning that the overall increase of CO2 is accelerating.

Carbon dioxide can pass in either direction across an air-water interface. When a can of carbonated soda is placed in a refrigerator overnight, the CO2 dissolves into the soda water and reaches equilibrium. You can upset that equilibrium by shaking the can before you open it or by leaving the can in a hot car trunk on your way to a picnic.

The same equilibrium happens between the earth’s atmosphere and the oceans. If atmospheric CO2 is on the rise (and the Keeling curve shows that it is), then the level of oceanic carbon dioxide must also be rising. Note that I have stated the equilibrium relationship here without specifying which side is doing the forcing. If a quantity on one side of the interface changes, the other side must also be changing—maybe sooner, maybe later, but also changing in the same direction.

At first glance, this equilibrium might be considered a good thing for humans: The oceans will absorb all the excess carbon dioxide that we are releasing through our burning of fossil fuels. The oceans will suck it all up, and we don’t have to worry about greenhouse gases any more. The planet earth will fix the problem for us. Nice!

That’s what I thought too, until I attended a presentation by NCAR scientist Joan Kleypas at the Boulder Public Library on May 26, 2010. The title of her talk was Carbon Dioxide and the Ocean: The Acid Test of Climate Change. It took only five of her slides for the message to hit me, hard: Carbon dioxide makes water acidic, and acid dissolves sea-shells. Every marine organism that depends on shells might lose them, or not be able to build a shell in the first place. Ugh. That’s … like … really bad.

Marine chemistry. Acidity and alkalinity are measured in pH, which is a logarithmic scale. Before the Industrial Era, seawater had a pH of 8.2. The global average pH of ocean water at the surface is now 8.1. Ocean acidification is already happening; in fact, that change in pH represents the acidity changing by 26%. Since a pH of 7 is considered “neutral,” the current value of 8.1 means that surface ocean water is alkaline, or a base. “Ocean acidification” is defined to mean the pH of seawater decreasing over time, or moving toward the acidic end of the pH scale. Acidification does not mean that the pH of seawater necessarily moves across the 7.0 line into “acidic territory.”

When carbon dioxide dissolves in water, some of the molecules combine with water (Figure 2) to form carbonic acid:

CO2 + H2O ↔ H2CO3

This chemical reaction also reduces the number of carbonate ions: CO32-. The Woods Hole article Ocean acidification chemistry 101 sums it up this way:

The chemical changes in seawater resulting from increased atmospheric CO2 concentrations include increases in the concentrations of dissolved (or aqueous) carbon dioxide, hydrogen ions, and bicarbonate ions, and decreases in the carbonate ion concentration and pH.

DrewsFig2.jpg

Figure 2. The chemistry of ocean acidification. The arrows are shown in one direction to show the propagation of increasing atmospheric carbon dioxide into and through seawater. The net effect is to decrease the marine concentration of carbonate ions (shown in bold). Figure 2 is based on Introduction to Ocean Acidification Figure 2, at Woods Hole (2013).

Many marine organisms build their hard parts (shells, skeletons) out of dissolved calcium and carbonate ions, thereby forming calcium carbonate:

Ca2 + CO32- ↔ CaCO3

In the marine environment, carbonate ions are what “everyone wants because everyone needs,” to paraphrase Dr. Suess. They are an essential part of the process of shell formation. Remember that experiment you ran back in high school chemistry class? Where you placed a shell in vinegar and observed what happened? That’s the one. Acidic solutions break down calcium carbonate, or make it harder to form in the first place.

Impacts on marine life. First, let’s dispel some extreme scenarios:

  • Seawater will not turn into battery acid overnight.
  • Australia’s Great Barrier Reef will not melt away by this time next year. But - coral reefs will begin dissolving instead of accreting when atmospheric CO2 levels reach 560 ppm, perhaps by 2100.
  • Snails, clams, and other shelled mollusks will not become naked writhing blobs in one week.

Now that those canards are out of the way, we can be realistic. Figure 3 shows the historical change in ocean acidity up to the present time. The average pH of the ocean is likely to drop by an additional 0.3-0.4 by 2100, and this change represents an increase in acidity of 100-150 % since the Industrial Revolution [Woods Hole].

DrewsFig3.jpg

Figure 3. Change in ocean surface pH since the Industrial Revolution (1750). Wikimedia Commons: user Plumbago.

Calcifying organisms use aragonite, a form of calcium carbonate, to build their shells. Aragonite “saturation” refers to the concentration of aragonite available in seawater. Figure 4 shows the change in aragonite saturation since 1880. It’s all negative. Note that Australia’s Great Barrier Reef (on the eastern shore of Australia) is right in the middle of a red zone. That really gives me a sinking feeling.

DrewsFig4.jpg

Figure 4. Changes in marine saturation of aragonite, 1880-2012. “The more negative the change in aragonite saturation, the larger the decrease in aragonite available in the water, and the harder it is for marine creatures to produce their skeletons and shells. “ Wikimedia Commons: US Environmental Protection Agency, public domain.

Aragonite saturation depends on the ocean pH, but also on dissolved carbon and the water temperature. I think these additional factors explain why Figures 3 and 4 do not exactly correspond; if you have additional insight here, please contribute to the Comments section of this entry.

Winners and losers. Some marine organisms can tolerate a decrease in the pH of seawater, while others are more vulnerable. Crustaceans and copepods appear to be relatively tolerant of ocean acidification. The sensitive organisms are those that build shells and skeletons through calcification: the corals and shelled mollusks. Coral reefs are going to have a hard time.

Coral reefs are already stressed by a number of changes associated with climate change: ocean warming, sedimentation, and pollution. Ocean acidification adds another threat to their survival. Caitlin Martin (an undergraduate at the University of Southern California) states:

Numerous studies have been conducted to investigate the impact of increasing CO2 levels on corals, and they all arrive at the conclusion that high CO2 levels make it difficult for marine organisms to create their calcium carbonate shells. For example, a study in the Red Sea reef showed that, globally, when CO2 concentrations are at 560 ppm, corals will dissolve instead of accumulate calcium carbonate, resulting in massive die-offs (Pandolfi et al. 2011). In another study, the experiment exposed calcifying algae to four different temperatures and four different CO2 levels; the greater amounts of CO2 caused significant decline in photosynthetic efficiency, ability to accumulate calcium carbonate, and growth in all species (Sinutok 2011). The results also showed that after five weeks, in the 34 °C trial under all CO2 levels, all species died (Sinutok 2011). Therefore, increased oceanic CO2 levels have detrimental effects on coral reefs. Furthermore, linking increasing CO2 levels with climate change and global warming shows the cause of the processes that are affecting the health of coral reef ecosystems. As long as greenhouse gases continue to be emitted in large amounts, CO2 concentrations will increase in oceans and corals will continue to live in a chemically unhealthy ecosystem. If CO2 emissions continue at the rate they are emitted now, there will most certainly be reductions in the extent and diversity of coral reefs in the future (Wilkinson 1999). Caitlin Martin, 2013

Algae and seagrass may actually benefit from ocean acidification because they use CO2 and bicarbonate (HCO 3-) during photosynthesis. Creatures that eat seagrass, such as manatees and green sea turtles, may benefit from an increase in their available food source. However, the “winners” column is dependent on species and habitat. There will likely be significant shifts in the mix of species as a result of ocean acidification, and the new marine ecosystem may not be what humans want. The ocean food chain is composed of many interrelated species, and a drastic reduction in the numbers of one species may in turn cause a population crash in another [Woods Hole].

Conclusion. At a workshop in St. Petersburg, Florida in 2006, oceanographers recommended additional research to clarify the response of marine calcifiers to ocean acidification. However, they were confident enough to conclude:

“It is clear that seawater chemistry will change in coming decades and centuries in ways that will dramatically alter marine life,” says NCAR scientist Joan Kleypas, the report’s lead author.

“This is leading to the most dramatic changes in marine chemistry in at least the past 650,000 years,” says Richard Feely, one of the authors and an oceanographer at NOAA’s Pacific Marine Environmental Laboratory (PMEL) in Seattle.

“Decreased calcification in marine algae and animals is likely to impact marine food webs and has the potential to substantially alter the biodiversity and productivity of the ocean,” says Victoria Fabry (California State University, San Marcos), another of the report’s authors.

Further reading. Sea sickness: Report warns about carbon dioxide threats to marine life, UCAR Quarterly, Summer 2006, by David Hosansky.

Impacts of Ocean Acidification on Coral Reefs and Other Marine Calcifiers, by Joan Kleypas, Richard Feely, Victoria Fabry, Chris Langdon, Christopher Sabine, and Lisa Robbins, June 2006. Workshop report.

Frequently asked questions about ocean acidification at Woods Hole Oceanographic Institution.

The Effects of Climate Change on Coral Reef Health blog at Scientific American by Caitlin Martin, June 5, 2013.

Effects of Ocean Acidification on Corals at oceana.org.

Coral reefs may start dissolving when atmospheric CO2 doubles, by Jacob Silverman, Boaz Lazar, Long Cao, Ken Caldeira, & Jonathan Erez at the Department of Global Ecology, Stanford University.

Ocean Acidification Network.

Ocean Acidity at the United States Environmental Protection Agency.

10 Comments

As I understand it, ocean acidification will happen as long as the partial pressure of atmospheric CO2 is greater than the partial pressure of dissolved CO2 in the seas. The rate of acidification also depends very much on the amount of that difference: a bigger gap between atmospheric and oceanic CO2 partial pressures results in a greater rate of acidification.

A few mass extinction events in the fossil record are associated with powerful releases of CO2 into the atmosphere and changes in the ocean’s acidity. Perhaps the most drastic is “The Great Dying” at the Permian-Triassic boundary, which is timed coincidentally (as far as we can tell) with massive releases of CO2 from volcanic activity. There is evidence that the marine side of the extinction event, which is hard to overstate in terms of scale, was felt most strongly by creatures that depended on the ability to pull calcium carbonates out of the water to build shells and skeletons. It seems likely that ocean acidification was a major factor, which is corroborated by some geological features of the relevant strata.

What should raise eyebrows is that the current rate of increase in CO2 concentrations may be one or two orders of magnitude faster than what happened during The Great Dying. It’s pretty much unprecedented in the last 300 million years of the geological record.

Certainly corals and mollusks are important builders of calcified skeletons, but there are many more to be considered: forams and other microorganisms, echinoderms, barnacles and lobsters, red algae, sponges, and brachiopods, just off the top of my head. I also wonder if it will become more difficult to build calcium phosphate skeletons, with direct effects on vertebrates, among others. What do you know about that?

This acidification thing doesn’t hinge on a temperature increase, does it? Even if something else kept the temperature steady, the acid would still be there.

John Harshman said:

Certainly corals and mollusks are important builders of calcified skeletons, but there are many more to be considered: forams and other microorganisms, echinoderms, barnacles and lobsters, red algae, sponges, and brachiopods, just off the top of my head. I also wonder if it will become more difficult to build calcium phosphate skeletons, with direct effects on vertebrates, among others. What do you know about that?

I could not find a reliable statement about echinoderms in general. The purple sea urchin will be a winner, but other species may lose.

John Harshman said:

Certainly corals and mollusks are important builders of calcified skeletons, but there are many more to be considered: forams and other microorganisms, echinoderms, barnacles and lobsters, red algae, sponges, and brachiopods, just off the top of my head. I also wonder if it will become more difficult to build calcium phosphate skeletons, with direct effects on vertebrates, among others. What do you know about that?

I don’t know much, but here’s what I’ve already found on those topics.

The crustaceans seem fairly tolerant of gradual acidification (temperature changes might be a different story). Benthic foraminifera were one of the huge losers in the Paleocene-Eocene Thermal Maximum, another event associated with unusually high CO2 levels and probable ocean acidification. As the link shows, however, their fate was not shared by many other types of marine life at the time. But the PETM event also seems to have been going on at a much slower pace than today’s acidification.

Forams also suffered a big blow right after the thawing of the Last Glacial Maximum, about 18,000 years ago, which saw elevated CO2 levels and again a slower acidification than today’s. Even coccolithophores seem to have suffered at that time (unlike during the PETM event 3 million years ago where they actually seemed to thrive).

The problem isn’t just one of changing pH and temperatures, obviously, but how the whole network of living things reacts to those that ARE sensitive to these changes. There’s also the old and familiar problem of pollution and general degradation caused by our heavy use of the seas, and the direct threats posed by overfishing and indiscriminate harvesting practices. What’s pretty clear is that we do NOT need to be added warming and acidification on top of all those other things. The combination of stressors will certainly be worse than the effect of any one factor by itself. Even conditions that wouldn’t kill certain marine organisms outright can stress them enough to make them less resilient overall and cause a collapse.

I’ve got some experience with fishkeeping and aquariums. Whenever there’s news or a big debate about how we’re impacting the environment with our CO2 emissions, either on land or in the sea, I’m constantly finding useful lessons in that background. Keeping plants and animals alive in a tiny, enclosed space that has to be almost totally self-contained makes these issues more apparent and their effects more immediate. The careful balancing of pH, dissolved gases and minerals, and temperature are all necessary to let a tank or a pond thrive. More and more I’m coming to recognize the real educational value of pet keeping, and the importance of that responsibility for informing people about the issues we have to face in the public sphere as well as our own personal development. There are so many opportunities to learn about nature when you’re confronted with the task of replicating (even a tiny) part of it.

Henry J said:

This acidification thing doesn’t hinge on a temperature increase, does it? Even if something else kept the temperature steady, the acid would still be there.

As posed, the answer is No. The ocean acidification process described here does not depend on temperature. Henry J is correct. A bunch of extra H+ ions just show up (indirectly from atmospheric CO2) and move the ocean’s pH toward the acidic end of the scale.

However, temperature does affect the equilibrium point of CO2 between the air and the ocean. Here is a link:

Carbon dioxide in water equilibrium (PDF)

They say:

At room temperature, the solubility of carbon dioxide is about 90 cm3 of CO2 per 100 ml water (cl/cg = 0.8). Any water-soluble gas becomes more soluble as the temperature decreases, due to the thermodynamics of the reaction: GAS (l) GAS (g).

Cold water can hold more dissolved CO2, like the soda can in your fridge. According to that relationship, a warmer ocean will hold less carbon dioxide. In theory, I could heat up the ocean by 2° C with a bunch of nuclear reactors, force it to flush its CO2 back into the atmosphere, and stop the acidification. But I’m not a chemist. This sounds like a bad experiment to try full-scale.

Oceanographers use lab experiments, theoretical studies, and paleo records to determine the effects of ocean acidification on marine organisms and the overall ecology. Other sources of information are carbon dioxide seeps, which are natural volcanic sources of CO2 that bubble from the ocean floor and affect the chemistry of the surrounding ocean.

Carbon dioxide seeps in Papua New Guinea as a natural laboratory to investigate the effects of ocean acidification on coral reefs (Abstract only)

High risk of extinction of benthic foraminifera in this century due to ocean acidification “Carbon dioxide seeps serve as ‘windows into the future’ to study the ability of marine invertebrates to acclimatise to OA.”

Sneak Peek: Future of Coral Reefs in an Acidifying Ocean Great pictures! And a good readable article by Laetitia Plaisance: “Closer to the most intense vents where water is most acidic, corals have stopped growing altogether; they have been replaced by sand, rubble and algae beds.”

Minor nitpick- You say “Crustaceans and copepods appear to be relatively tolerant of ocean acidification”, but copepods are a kind of crustacean.

Mickey Mortimer said:

Minor nitpick- You say “Crustaceans and copepods appear to be relatively tolerant of ocean acidification”, but copepods are a kind of crustacean.

Right you are. Here is the extended version at Woods Hole:

Do crustaceans suffer from ocean acidification also?

The crustaceans seem fairly tolerant of gradual acidification

true, but not necessarily the things that they typically feed on.

I recall when I was an undergrad in the 80s at UC Santa Barbara, Barbara Prezlin and others had already shown significant decreases in primary productivity in areas where ocean acidification was increasing, even in the antarctic. This of course, becomes the limiting factor in krill populations, for example, much more so than whether acidification has an impact on the ability of krill to form exoskeletons.

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This page contains a single entry by Matt Young published on October 9, 2013 8:00 PM.

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