Since 1800, one third of anthropogenic CO2 emissions has been absorbed by the oceans, corresponding to an annual uptake of one ton of CO2 per person. This massive absorption has allowed to partly mitigate climate change but it has also caused a major disruption to the chemistry of seawater. Indeed, this absorbed CO2 causes an acidification of the oceans and, at the current rate of emissions, it is estimated that their pH will fall by 0.4 units between now and 2100. This corresponds to a 3-fold increase of the mean acidity of the oceans, which is unprecedented during the past 20 million years. The LOV team, led by Jean-Pierre Gattuso, studied the impact of such a reduction in pH on calcifying organisms. Pteropods (pelagic marine mollusks) and deep-water corals, both playing essential roles in their respective ecosystems, live in areas that will be among the first to be affected by ocean acidification.
The pteropod Limacina helicina thus has an important part to play in the food chain and functioning of the Arctic marine ecosystem. Its calcium carbonate shell provides vital protection. However, the LOV study has shown that the shell of this mollusk develops at a rate that is 30% slower when it is kept in seawater with the characteristics anticipated in 2100. An even more marked reduction (50%) has been measured in the cold-water coral Lophelia pertusa. While tropical coral reefs are built by a large number of species, coral communities in cold waters are constructed by one or two species but provide shelter for many others. A reduction in the growth of reef-building corals due to ocean acidification may therefore threaten the very existence of these biological structures.
These first results raise major concerns about the future of pteropods, deep-water corals and the organisms that depend on them for nutrition or habitat. Research programs such as EPOCA(1), coordinated by CNRS, are planning new studies on other marine organisms and ecosystems. They are carrying out long-term experiments to study the combined impact of ocean acidification and other parameters that will also be modified during the decades to come, such as temperature and nutrient concentrations.
Ocean acidification can only be controlled by limiting future atmospheric levels of CO2. Negotiations aimed at reducing greenhouse gas emissions (COP 15) are under way and should be finalized in Copenhagen next December. These negotiations must take account not only of increased temperature but also of the acidic nature of CO2 which, once absorbed by the oceans, will have potentially dramatic effects on numerous marine organisms and ecosystems.
© S. Comeau, LOV
The Arctic pteropod (pelagic sea mollusk) Limacina helicina (Spitzberg).
© C. Maier, LOV
The deep-water coral Lophelia pertusa (150 m off the Hebrides Islands in the North Atlantic).
(1) The EU FP7 large-scale integrating project EPOCA (European Project on OCean Acidification) was launched in May 2008 with the overall goal to fill the numerous gaps in our understanding of ocean acidification and its consequences. The EPOCA consortium brings together more than 100 researchers from 27 institutes and 9 European countries. The research of this four-year long project is partly funded by the European Commission.
Project web site: View web site
Previous press release: View web site
Impact of ocean acidification on a key Arctic pelagic mollusc (Limacina helicina).
Comeau S., Gorsky G., Jeffree R., Teyssié J. L., Gattuso J.-P.
Published in September in Biogeosciences
Calcification of the cold-water coral Lophelia pertusa under ambient and reduced pH.
Maier C., Hegeman J., Weinbauer M. G., Gattuso J.-P.
Published in August in Biogeosciences