330
Chemical Oceanography, 4th Edition
Betzer, P.R., et al., The ocean carbonate system: a reassessment of biogenic controls, Science, 226,
1074 (1984).
Brewer, P.G., Direct observation of the oceanic CO 2 increase, Geophys. Res. Lett., 5, 997–1000 (1978).
Broecker, W.S., and Peng, T.H., Tracers in the Sea, Eldigio Press, New York (1982).
Bustos, H., Morse, J.W., and Millero, F.J., The formation of whitings on the Little Bahama Banks, Mar.
Chem., 113, 1–8 (2009).
Byrne, R.H., Mecking, S., Feely, R.A., and Liu, X., Direct observations of basin- wide acidification of
the North Pacific Ocean, Geophys. Res. Lett., 37, L02601 (2010).
Caldeira, K., and Wickett, M.E., Oceanography: anthropogenic carbon and ocean pH, Nature, 425,
365 (2003).
Chen, C.-T.A., Decomposition of calcium carbonate and organic carbon in the deep oceans, Science,
201, 735 (1978).
Chen, C.-T.A., and Millero, F.J., Gradual increase of oceanic CO 2 , Nature, 277, 205–206 (1979).
Clayton, T.D., and Byrne, R.H., Spectrophotometric seawater pH measurements: total hydrogen ion
concentration scale calibration of m- cresol purple and at- sea results, Deep- Sea Res., 40, 2115 (1993).
Cloud, P.E., Carbonate precipitation and dissolution in the marine environment, Chapter 17, Chemical
Oceanography, Vol. 2, Riley, J.P., and Skirrow, G., Eds., Academic Press, New York, 127–158 (1965).
Coale, K.H., et al., Southern Ocean iron enrichment experiment: carbon cycling in high and low Si
waters, Science, 304, 408 (2004).
Delille, B. et al., Response of primary production and calcification to changes pf pCO 2 during experimental blooms of the coccolithophorid Emiliania hyxley, Globa. Biogeochem. Cycles, 19, GB2023,
doi:10.1029/2004GB002318 (2005).
Dickson, A.G., pH buffers for sea water media based on the total hydrogen ion concentration scale,
Deep- Sea Res., 40, 107 (1993).
Doney, S.C., et al., Ocean acidification, a critical emerging problem for the ocean science, Oceanography,
22, 16–25 (2009a).
Doney, S.C., et al., Ocean acidification, the other CO 2 problem, Annu. Rev. Mar. Sci, 1, 169–192 (2009b).
Feely, R.A., et al., In situ calcium carbonate dissolution in the Pacific Ocean, Global Biogeochem. Cycles,
16, 1144 (2002).
Feely, R.A., Sabine, C.L., Lee, K., Berelson, W., Kleypas, J., Fabry, V.J., and Millero, F.J., The impact of
anthropogenic CO 2 on the CaCO 3 system in the oceans, Science, 305, 362 (2004).
Feely, R.A., Sabine, C.L., Hernandez-Ayon, J.M., Ianson, D., and Hales, B., Evidence of upwelling of
corrosive”acidified” water onto the Continental Shelf, Science, 320, 1490–1492 (2008).
Feely, R.A., Sabine, C.L., Byrne, R.H., Millero, F.J., Dickson, A.G., Wanninkhof, R., Murata, A., Miller,
L.A., and Greeley, D., Decadal changes in the aragonite and calcite saturation state of the Pacific
Ocean, Global Biogeochem. Cycles, 26 (2012).
Friis, K., et al., On the temporal increase of anthropogenic CO 2 in the subpolar North Atlantic, DeepSea Res. Pt. I: Oceanogr. Res. Papers, 52, 681–698 (2005).
Friis, K., et al., Possible overestimation of shallow- depth calcium carbonate dissolution in the ocean,
Global Biogeochem. Cycles, 20, 1–11 (2006).
Friis, K., et al., Dissolution of calcium carbonate: observation and model result in the subpolar North
Atlantic, Biogeoscience 4, 205-207 (2007).
Gledhill, D.K., Wanninkhof, R., Millero, F.J., and Eakin, M., Ocean acidification of the greater
Caribbean region 1996–2006, J. Geophys. Res., 113, C10031 (2008).
González- Dávila, M., et al., Interannual variability of the upper ocean carbon cycle in the north- east
Atlantic Ocean, J. Geophys. Res. Lett., 34, L07608 (2007).
González- Dávila, M., et al., Oxidation of copper(I) in seawater at nanomolar levels, Mar. Chem.,
115(1–2), 118–124 (2009).
Gruber, N., et al., An improved method for detecting anthropogenic CO 2 in the oceans, Global
Biogeochem. Cycles, 10, 809 (1996).
Gruber, N. et al., Rapid progression of ocean acidification in the California current system, Science,
337, 220–223 (2012).
Chemical Oceanography, 4th Edition
Betzer, P.R., et al., The ocean carbonate system: a reassessment of biogenic controls, Science, 226,
1074 (1984).
Brewer, P.G., Direct observation of the oceanic CO 2 increase, Geophys. Res. Lett., 5, 997–1000 (1978).
Broecker, W.S., and Peng, T.H., Tracers in the Sea, Eldigio Press, New York (1982).
Bustos, H., Morse, J.W., and Millero, F.J., The formation of whitings on the Little Bahama Banks, Mar.
Chem., 113, 1–8 (2009).
Byrne, R.H., Mecking, S., Feely, R.A., and Liu, X., Direct observations of basin- wide acidification of
the North Pacific Ocean, Geophys. Res. Lett., 37, L02601 (2010).
Caldeira, K., and Wickett, M.E., Oceanography: anthropogenic carbon and ocean pH, Nature, 425,
365 (2003).
Chen, C.-T.A., Decomposition of calcium carbonate and organic carbon in the deep oceans, Science,
201, 735 (1978).
Chen, C.-T.A., and Millero, F.J., Gradual increase of oceanic CO 2 , Nature, 277, 205–206 (1979).
Clayton, T.D., and Byrne, R.H., Spectrophotometric seawater pH measurements: total hydrogen ion
concentration scale calibration of m- cresol purple and at- sea results, Deep- Sea Res., 40, 2115 (1993).
Cloud, P.E., Carbonate precipitation and dissolution in the marine environment, Chapter 17, Chemical
Oceanography, Vol. 2, Riley, J.P., and Skirrow, G., Eds., Academic Press, New York, 127–158 (1965).
Coale, K.H., et al., Southern Ocean iron enrichment experiment: carbon cycling in high and low Si
waters, Science, 304, 408 (2004).
Delille, B. et al., Response of primary production and calcification to changes pf pCO 2 during experimental blooms of the coccolithophorid Emiliania hyxley, Globa. Biogeochem. Cycles, 19, GB2023,
doi:10.1029/2004GB002318 (2005).
Dickson, A.G., pH buffers for sea water media based on the total hydrogen ion concentration scale,
Deep- Sea Res., 40, 107 (1993).
Doney, S.C., et al., Ocean acidification, a critical emerging problem for the ocean science, Oceanography,
22, 16–25 (2009a).
Doney, S.C., et al., Ocean acidification, the other CO 2 problem, Annu. Rev. Mar. Sci, 1, 169–192 (2009b).
Feely, R.A., et al., In situ calcium carbonate dissolution in the Pacific Ocean, Global Biogeochem. Cycles,
16, 1144 (2002).
Feely, R.A., Sabine, C.L., Lee, K., Berelson, W., Kleypas, J., Fabry, V.J., and Millero, F.J., The impact of
anthropogenic CO 2 on the CaCO 3 system in the oceans, Science, 305, 362 (2004).
Feely, R.A., Sabine, C.L., Hernandez-Ayon, J.M., Ianson, D., and Hales, B., Evidence of upwelling of
corrosive”acidified” water onto the Continental Shelf, Science, 320, 1490–1492 (2008).
Feely, R.A., Sabine, C.L., Byrne, R.H., Millero, F.J., Dickson, A.G., Wanninkhof, R., Murata, A., Miller,
L.A., and Greeley, D., Decadal changes in the aragonite and calcite saturation state of the Pacific
Ocean, Global Biogeochem. Cycles, 26 (2012).
Friis, K., et al., On the temporal increase of anthropogenic CO 2 in the subpolar North Atlantic, DeepSea Res. Pt. I: Oceanogr. Res. Papers, 52, 681–698 (2005).
Friis, K., et al., Possible overestimation of shallow- depth calcium carbonate dissolution in the ocean,
Global Biogeochem. Cycles, 20, 1–11 (2006).
Friis, K., et al., Dissolution of calcium carbonate: observation and model result in the subpolar North
Atlantic, Biogeoscience 4, 205-207 (2007).
Gledhill, D.K., Wanninkhof, R., Millero, F.J., and Eakin, M., Ocean acidification of the greater
Caribbean region 1996–2006, J. Geophys. Res., 113, C10031 (2008).
González- Dávila, M., et al., Interannual variability of the upper ocean carbon cycle in the north- east
Atlantic Ocean, J. Geophys. Res. Lett., 34, L07608 (2007).
González- Dávila, M., et al., Oxidation of copper(I) in seawater at nanomolar levels, Mar. Chem.,
115(1–2), 118–124 (2009).
Gruber, N., et al., An improved method for detecting anthropogenic CO 2 in the oceans, Global
Biogeochem. Cycles, 10, 809 (1996).
Gruber, N. et al., Rapid progression of ocean acidification in the California current system, Science,
337, 220–223 (2012).