Postindustrial enhancement of aragonite undersaturation in the upper tropical and subtropical Atlantic Ocean: The role of fossil fuel CO2

Sook Nye Chung, Geun Ha Park, Kitack Lee, Robert M. Key, Frank J Millero, Richard A. Feely, Christopher L. Sabine, Paul G. Falkowski

Research output: Contribution to journalArticle

14 Citations (Scopus)

Abstract

The dissolution of aragonite particles in the ocean primarily depends on the degree of undersaturation of seawater with respect to that mineral. Most of the upper Atlantic Ocean, particularly north of 30°S and at depths of less than 2000 m, is supersaturated with respect to aragonite, whereas much of the deep Atlantic is undersaturated. Here we report, for the first time, shallow layers of aragonite-undersaturated water between 20°S and 15°N in the eastern tropical Atlantic. These layers are centered at 800 m and are surrounded by aragonite-supersaturated water above and below. This feature most likely results from a combination of chemical and biological processes including the uptake of anthropogenic CO2 and the oxidation of organic matter falling from the highly productive overlying surface water. Reaction with protons resulting from these processes decreases the carbonate ion concentration and consequently the saturation state of the waters with respect to aragonite. The oceanic uptake of anthropogenic CO2 during the industrial era has caused a significant increase in the size of the undersaturated layers. Future expansion will likely occur laterally to the west and south, where the degree of supersaturation is low compared to waters to the north. This expansion of the undersaturated layers is a prime example of how human activity during the industrial era has altered the upper ocean chemistry by injecting fossil fuel CO2 into the ocean.

Original languageEnglish (US)
Pages (from-to)315-321
Number of pages7
JournalLimnology and Oceanography
Volume49
Issue number2
StatePublished - Mar 2004

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fossil fuels
aragonite
Atlantic Ocean
fossil fuel
ocean
oceans
water
upper ocean
supersaturation
chemical process
biological processes
protons
carbonates
surface water
chemistry
human activity
seawater
dissolution
organic matter
saturation

ASJC Scopus subject areas

  • Oceanography
  • Aquatic Science

Cite this

Chung, S. N., Park, G. H., Lee, K., Key, R. M., Millero, F. J., Feely, R. A., ... Falkowski, P. G. (2004). Postindustrial enhancement of aragonite undersaturation in the upper tropical and subtropical Atlantic Ocean: The role of fossil fuel CO2. Limnology and Oceanography, 49(2), 315-321.

Postindustrial enhancement of aragonite undersaturation in the upper tropical and subtropical Atlantic Ocean : The role of fossil fuel CO2. / Chung, Sook Nye; Park, Geun Ha; Lee, Kitack; Key, Robert M.; Millero, Frank J; Feely, Richard A.; Sabine, Christopher L.; Falkowski, Paul G.

In: Limnology and Oceanography, Vol. 49, No. 2, 03.2004, p. 315-321.

Research output: Contribution to journalArticle

Chung, SN, Park, GH, Lee, K, Key, RM, Millero, FJ, Feely, RA, Sabine, CL & Falkowski, PG 2004, 'Postindustrial enhancement of aragonite undersaturation in the upper tropical and subtropical Atlantic Ocean: The role of fossil fuel CO2', Limnology and Oceanography, vol. 49, no. 2, pp. 315-321.
Chung, Sook Nye ; Park, Geun Ha ; Lee, Kitack ; Key, Robert M. ; Millero, Frank J ; Feely, Richard A. ; Sabine, Christopher L. ; Falkowski, Paul G. / Postindustrial enhancement of aragonite undersaturation in the upper tropical and subtropical Atlantic Ocean : The role of fossil fuel CO2. In: Limnology and Oceanography. 2004 ; Vol. 49, No. 2. pp. 315-321.
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