Related Experiment Video
Updated: Jun 6, 2026

07:59
Coral Reef Arks: An In Situ Mesocosm and Toolkit for Assembling Reef Communities
Published on: January 6, 2023
Ocean acidification: the other CO2 problem
Scott C Doney1, Victoria J Fabry, Richard A Feely
1Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA. sdoney@whoi.edu
Annual Review of Marine Science
|December 15, 2010
Summary
Ocean acidification, driven by rising carbon dioxide (CO2), alters seawater chemistry, impacting marine life. Research is needed to understand organism adaptation and ecosystem effects.
Area of Science:
- Marine Biology
- Oceanography
- Environmental Chemistry
Background:
- Rising atmospheric carbon dioxide (CO2) from human activities is increasing ocean acidity.
- Ocean acidification alters seawater chemistry, affecting marine ecosystems globally.
- The rate of ocean acidification is projected to accelerate this century.
Purpose of the Study:
- To document the effects of ocean acidification on marine organisms.
- To investigate the impact of changing seawater chemistry on biogeochemical cycles.
- To highlight research priorities concerning marine organism adaptation to CO2.
Main Methods:
- Analysis of field data on ocean acidification.
- Laboratory experiments on calcifying organisms under high-CO2 conditions.
- Review of existing research on ocean acidification impacts.
Main Results:
- Ocean acidification lowers calcium carbonate saturation states, affecting shell-forming organisms.
- Calcifying species show reduced calcification and growth rates in laboratory settings.
- Some photosynthetic organisms exhibit increased carbon fixation rates.
Conclusions:
- Ocean acidification poses significant risks to marine calcifiers and ecosystems.
- The capacity of marine organisms to adapt to increasing CO2 is largely unknown.
- Further research is crucial to predict and mitigate the effects of ocean acidification.
Related Concept Videos
The Carbon Cycle
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Carbon-dioxide Fixation
Carbon dioxide fixation in prokaryotes enables the assimilation of inorganic carbon into organic molecules, supporting biosynthetic pathways, sustaining ecosystems, and contributing to the global carbon cycle. It also has industrial applications in carbon capture and bioproduct synthesis. Autotrophic organisms rely on this process to utilize CO₂ as a carbon source in diverse environments.The Calvin CycleThe Calvin cycle is the most widespread carbon fixation mechanism, primarily used by...
The Sulfur Cycle
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
Diagnosing Acidosis and Alkalosis
Diagnosing acid-base imbalances involves systematically analyzing arterial blood samples, focusing on three key measurements: pH, bicarbonate (HCO3−) concentration, and carbon dioxide partial pressure (PCO2). This analysis follows a four-step process that helps identify the imbalance's underlying cause and nature.
First, the pH level is assessed to determine whether the blood pH is normal (7.35–7.45), low (acidosis), or high (alkalosis).
Next, the PCO2 and HCO3− values are examined to...
First, the pH level is assessed to determine whether the blood pH is normal (7.35–7.45), low (acidosis), or high (alkalosis).
Next, the PCO2 and HCO3− values are examined to...
Microbes and Climate Change
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
Factors Affecting Solubility
Compared with pure water, the solubility of an ionic compound is less in aqueous solutions containing a common ion (one also produced by dissolution of the ionic compound). This is an example of a phenomenon known as the common ion effect, which is a consequence of the law of mass action that may be explained using Le Chȃtelier’s principle. Consider the dissolution of silver iodide:

