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Fundamental changes in seawater
chemistry are occurring throughout Earth’s oceans. Since the beginning of the
industrial revolution, the release of carbon dioxide (CO2) from
industrial and agricultural activities has increased the amount of CO2
in the atmosphere. Ocean acidification is the term given to the chemical
changes in the ocean as a result of carbon dioxide emissions.
Oceanographic measurements worldwide indicate that the pH of seawater is decreasing—that is, the ocean is becoming more acidic. This is due to the fact that seawater absorbs CO2 from the atmosphere, and the concentration of CO2 in the atmosphere has been steadily rising owing primarily to the burning of coal, oil and gas for transportation, heating, electricity generation, and other industrial activities. The amount of CO2 produced by human activities is small compared to that released naturally through biological and geological processes, but it is large enough that forests, grasslands, and aquatic plant communities can’t absorb it all, so every year the amount in the atmosphere rises. The rate of atmospheric CO2 accumulation has steadily increased in recent decades, reaching a record high of 31.6 gt in 2011 (IEA 2012).
In addition to the CO2 from natural sources that it absorbs, the ocean absorbs approximately 30% of the CO2 emitted into the atmosphere by humans (Sabine et al. 2004). Consequently, seawater worldwide is becoming more acidic.
The average pH of ocean surface water has decreased from a calculated value of 8.2 in 1750 to a measured value of approximately 8.1 today. Although it seems small, since the pH scale is logarithmic, this decline actually represents 30% greater acidity overall. It is important to note that the ocean is not ‘acid’, its pH is greater than 7 and will in all likelihood remain so. However, it is becoming more acidic, and this acidification will have profound biological effects.
How Was It Measured?
Acidification layer models the difference in global distribution changes in the
aragonite saturation state (Ωarag) between pre-industrial (~1870) and modern times (2000-2009) as a proxy
for ocean acidification due to human influences. Aragonite is the most common form of calcium
carbonate (CaCO3), used by corals, mollusks and other sea
life to form shells. In seawater,
calcium carbonate must remain in equilibrium with the concentration of calcium
ions and carbonate ions as can be
seen in the following equation:
Ca2+ + CO32- ↔ CaCO3
Too many calcium ions or carbonate ions force the equation to the right, making calcium carbonate. Too few calcium ions or carbonate ions force it to the left, dissolving calcium carbonate to restore the chemical equilibrium.
The saturation state, symbolized as Ω, is a function of the concentrations of those three components in seawater, defined as:
( [Ca2+] × [CO32-] ) / [CaCO3] = Ω
When Ω = 1, CaCO3 remains stable: a calcium carbonate structure such as a shell or reef skeleton doesn’t dissolve or grow. When Ω < 1, calcium carbonate structures dissolve. When Ω > 1, calcium carbonate precipitates out of solution or adds to existing calcium carbonate structures. Note that calcifier species make shells easily when Ω ≥ 1. They can also make shells when Ω < 1, but the lower the saturation state, the more energy they must expend until a point is reached where they do not have enough energy to replace shell structure that is dissolving and they probably cannot survive.
All pressures have different affects on different goals. For each goal, the affect of each pressure is weighted 'low' (1), 'medium' (2) or 'high' (3). The actual data-derived value of the pressure is then multiplied by the weight assigned to it for that goal. That process is repeated for each pressure-goal combination. The sum of those values divided by 3 (the (the maximum pressure-goal value) expresses the total affect of that pressure on the goal.
Ocean Acidification has low effect (weight=1) on Natural Products (Coral, Sponges, and Shells), Carbon Storage (Seagrasses), Coastal Protection (Corals and Seagrasses), Livelihoods and Economies (Aquarium Trade), Sense of Place (Iconic Species), and Biodiversity (Habitats-Seagrasses and Corals, and Species).
What Are the Impacts?
of CO2 in the ocean causes acidification, slows or prevents the
formation of shells, coral reefs and other structures composed of calcium carbonate (CaCO3), and weakens or dissolves previously
HUMAN HEALTH IMPACT
ocean acidification compromises the growth and structural integrity of coral
reefs and their ability to provide shoreline protection, food, and other health
500 million people worldwide depend on reefs for shoreline protection, food and income (Wilkinson 2008).
affects the larval development of certain commercial fish and shellfish. Fisheries may experience declines due to
low survival rates and the inhibited development of marine calcifier species.
A 10-25% decrease in US mollusk harvest from the 2007 rate would result in a loss of US $75-187 million per year and a net loss of US $1.7-10 billion through the mid-century (Cooley and Doney 2009a).
Get More Information
The Ocean Acidification Network
This international symposium gathers scientists from around the world to address the impacts of ocean acidification and to discuss policy and management options.
United Nations Division for Sustainable Development
Ocean Acidification: A Hidden Risk for Sustainable Development
Ocean Acidification - The Untold Story: a report on the impacts of ocean acidification upon marine life.
Acid Test: The Global Challenge of Ocean Acidification
Created to raise awareness about the problems associated with ocean acidification.
Connell, S.D., & Russell, B.D.
(2010). The direct effects of increasing CO2 and temperature on non-calcifying
organisms: Increasing the potential for phase shifts in kelp forests. Proceedings of the Royal Society B, 277(1686),
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Anticipating ocean acidification’s economic consequences for commercial
fisheries. Environmental Research
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Fabry, V.J., Seibel, B.A., Feely, R.A.,
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