articleScienceJul 15, 2004Closed access

Impact of Anthropogenic CO 2 on the CaCO 3 System in the Oceans

NSF National Center for Atmospheric Research · University of Southern California · +4 more institutions

PubMed
Indexed incrossrefpubmed

Abstract

Rising atmospheric carbon dioxide (CO2) concentrations over the past two centuries have led to greater CO2 uptake by the oceans. This acidification process has changed the saturation state of the oceans with respect to calcium carbonate (CaCO3) particles. Here we estimate the in situ CaCO3 dissolution rates for the global oceans from total alkalinity and chlorofluorocarbon data, and we also discuss the future impacts of anthropogenic CO2 on CaCO3 shell-forming species. CaCO3 dissolution rates, ranging from 0.003 to 1.2 micromoles per kilogram per year, are observed beginning near the aragonite saturation horizon. The total water column CaCO3 dissolution rate for the global oceans is approximately 0.5 +/- 0.2…

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Authors

7

Topics & keywords

Keywords
  • Aragonite
  • Dissolution
  • Calcium carbonate
  • Alkalinity
  • Carbon dioxide
  • Saturation (graph theory)
  • Carbonate
  • Ocean acidification
UN Sustainable Development Goals
  • Life below water
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