Rapid Progression of Ocean Acidification in the California Current System

Author:

Gruber Nicolas1,Hauri Claudine1,Lachkar Zouhair1,Loher Damian1,Frölicher Thomas L.2,Plattner Gian-Kasper3

Affiliation:

1. Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich, Zürich, Switzerland.

2. Atmospheric and Oceanic Sciences Program, Princeton University, Princeton, NJ, USA.

3. Climate and Environmental Physics, University of Bern, Bern, Switzerland.

Abstract

Acidification Blues The increase in the concentration of atmospheric carbon dioxide threatens the health of the ocean's ecosystems because of the resulting acidification of the ocean and the decrease in its carbonate saturation state. Gruber et al. (p. 220 , published online 14 June) used a regional ocean model to project how the saturation state of aragonite, a form of calcium carbonate that is produced by many marine organisms, will change in the California Current System through the year 2050. The sea floor along many parts of the California coast is likely to become exposed to year-round aragonite undersaturation within the next 20 to 30 years, a situation that could severely reduce the range of habitats for marine shellfish.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference39 articles.

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2. W. S. Broecker Y.-H. Li T.-H. Peng in Impingement of Man on the Oceans D. W. Hood Ed. (Wiley New York 1971) pp. 287–324.

3. Effect of calcium carbonate saturation of seawater on coral calcification

4. Geochemical Consequences of Increased Atmospheric Carbon Dioxide on Coral Reefs

5. Reduced calcification of marine plankton in response to increased atmospheric CO2

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