div class=trans-pagebuttonPage 1button div class=trans-image amp-img class=trans-thumb alt=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 src=https:reader033fdocumentsnetreader033viewer2022053110607fccd5fb116940424cce8dhtml5thumbnails1jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 2button div class=trans-image amp-img class=trans-thumb alt=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 src=https:reader033fdocumentsnetreader033viewer2022053110607fccd5fb116940424cce8dhtml5thumbnails2jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 3button div class=trans-image amp-img class=trans-thumb alt=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 src=https:reader033fdocumentsnetreader033viewer2022053110607fccd5fb116940424cce8dhtml5thumbnails3jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 4button div class=trans-image amp-img class=trans-thumb alt=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 src=https:reader033fdocumentsnetreader033viewer2022053110607fccd5fb116940424cce8dhtml5thumbnails4jpg width=142 height=106 layout=responsive amp-img divdivdiv class=trans-pagebuttonPage 5button div class=trans-image amp-img class=trans-thumb alt=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...