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From the following article:

Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms

James C. Orr, Victoria J. Fabry, Olivier Aumont, Laurent Bopp, Scott C. Doney, Richard A. Feely, Anand Gnanadesikan, Nicolas Gruber, Akio Ishida, Fortunat Joos, Robert M. Key, Keith Lindsay, Ernst Maier-Reimer, Richard Matear, Patrick Monfray, Anne Mouchet, Raymond G. Najjar, Gian-Kasper Plattner, Keith B. Rodgers, Christopher L. Sabine, Jorge L. Sarmiento, Reiner Schlitzer, Richard D. Slater, Ian J. Totterdell, Marie-France Weirig, Yasuhiro Yamanaka & Andrew Yool

Nature 437, 681-686(29 September 2005)

doi:10.1038/nature04095

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Figure 1

Increasing atmospheric CO2 and decreasing surface ocean pH and [CO32-].

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Figure 2

The aragonite saturation state in the year 2100 as indicated by Delta[CO32-]A.

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Figure 3

Climate-induced changes in surface [CO32-].

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Figure 4

Key surface carbonate chemistry variables as a function of pCO2.

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Figure 5

Average surface [CO32-] in the Southern Ocean under various scenarios.

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Figure 6

Shell dissolution in a live pteropod.

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