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Page 1: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 2: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 3: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 4: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 5: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 6: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 7: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 8: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 9: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 10: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 11: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 12: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 13: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 14: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 15: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,
Page 16: University of Otago, University of Otago, New Zealand · Aragonite saturation state (Q) 1850 a High-co, I Gap. SCOR Parts of the Arctic are already corrosive to shells of marine organisms,

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