422
Chemical Oceanography, 4th Edition
Platt, T., and Sathyendranath, S., Oceanic primary production: estimation by remote sensing at local
and regional scales, Science, 241, 1613 (1988).
Rodhe, H., Standard correlations between pelagic photosynthesis and light, in Primary Productivity
in Aquatic Environments, Goldman et al., Eds., University of California Press, Berkeley and Los
Angeles, CA, 464 pp. (1966).
Ryther, J., and Yentsch, C., The estimation of phytoplankton production in the ocean from chlorophyll and light data, Limnol. Oceanogr., 2, 281 (1957).
Strickland, J.D.H., Production of organic matter in the primary stages of the marine food chain,
Chapter 12, Chemical Oceanography, Vol. 1, Riley, J.P., and Skirrow, G., Eds., Academic Press,
New York, 478–610 (1965).
Strickland, J.D.H., and Parson, T.R.S., A practical handbook of sea water analysis, Fish Res. D. Can.
Bull., 167, 311 pp. (1968).
Talling, J.F., The incidence of vertical mixing, and some biological and chemical consequences in
tropical African Lakes, Verhandlungen der Internationale Vereinigung fur Limonologie, 17, 998–1012
(1969).
iron limitation
Bakker, D.C.E., Watson, A.J., and Law, C.S., Southern Ocean iron enrichment promotes inorganic
carbon drawdown, Deep- Sea Res. II, 48, 2483 (2001).
Banse, K., Does iron really limit phytoplankton production in the offshore subarctic Pacific? Limnol.
Oceanogr., 35, 772 (1990).
Boyd, P.W., et al., A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron
fertilization, Nature, 407, 695 (2000).
Bozec, Y., et al., The CO 2 system in a Redfield context during an iron enrichment experiment in the
Southern Ocean, Mar. Chem., 95, 89–105 (2004).
Brand, L., Minimum iron requirements of marine phytoplankton and the implications for the biogeochemical control of new production, Limnol. Oceanogr., 36, 1756 (1991).
Chavez, F., The iron hypothesis: ecosystem test in Equatorial Pacific waters, Nature, 371, 123 (1994).
Chisholm, S.W., and Morel, F.M.M., What controls phytoplankton production in nutrient rich areas
of the open sea? Limnol. Oceanogr., 36, 1507 (1991).
Coale, K.H., et al., The IronExII mesoscale experiment produces massive phytoplankton bloom in the
equatorial Pacific, Nature, 383, 495 (1996).
Coale, K.H., et al., Southern Ocean iron enrichment experiment: carbon cycling in high- and low- Si
waters, Science, 304, 408 (2004).
Cooper, D.J., Watson, A., and Nightingale, P., Large decrease in ocean surface CO 2 fugacity in
response to in situ iron fertilization, Nature, 381, 511 (1996).
Greene, R., Geider, R., and Falkowski, P., Effect of iron limitation on photosynthesis in a marine diatom, Limnol. Oceanogr., 36, 1772 (1991).
Hiscock, W., and Millero, F.J., Nutrient and carbon parameters during the Southern Ocean Iron
Experiment (SOFeX), Deep- Sea Res. I, 52, 2086–2108 (2005).
Hudson, R.J.M., and Morel, F.F.M., Iron transport in marine phytoplankton: kinetics of cellular and
medium coordination reaction, Limnol. Oceanogr., 35, 1002 (1990).
Kolber, K., et al., Iron limitation of phytoplankton photosynthesis in the Equatorial Pacific Ocean,
Nature, 371, 145 (1994).
Ledwell, J., Watson, A., and Law, C., Evidence for slow mixing across the pycnocline from an openocean tracer- release experiment, Nature, 364, 701 (1993).
Martin, J.H., Glacial–interglacial CO 2 change: the iron hypothesis, Paleoceanography, 5, 1 (1990).
Martin, J.H., Iron as a limiting factor in oceanic productivity in Primary Productivity and Biogeochemical
Cycles in the Sea, Falkowski, P.G., and Woodhead, A., Eds., Plenum, New York, 123–137 (1992).
Martin, J.H., and Fitzwater, S.E., Iron deficiency limits phytoplankton growth in the northeast Pacific
subarctic, Nature, 331, 341 (1989).
Chemical Oceanography, 4th Edition
Platt, T., and Sathyendranath, S., Oceanic primary production: estimation by remote sensing at local
and regional scales, Science, 241, 1613 (1988).
Rodhe, H., Standard correlations between pelagic photosynthesis and light, in Primary Productivity
in Aquatic Environments, Goldman et al., Eds., University of California Press, Berkeley and Los
Angeles, CA, 464 pp. (1966).
Ryther, J., and Yentsch, C., The estimation of phytoplankton production in the ocean from chlorophyll and light data, Limnol. Oceanogr., 2, 281 (1957).
Strickland, J.D.H., Production of organic matter in the primary stages of the marine food chain,
Chapter 12, Chemical Oceanography, Vol. 1, Riley, J.P., and Skirrow, G., Eds., Academic Press,
New York, 478–610 (1965).
Strickland, J.D.H., and Parson, T.R.S., A practical handbook of sea water analysis, Fish Res. D. Can.
Bull., 167, 311 pp. (1968).
Talling, J.F., The incidence of vertical mixing, and some biological and chemical consequences in
tropical African Lakes, Verhandlungen der Internationale Vereinigung fur Limonologie, 17, 998–1012
(1969).
iron limitation
Bakker, D.C.E., Watson, A.J., and Law, C.S., Southern Ocean iron enrichment promotes inorganic
carbon drawdown, Deep- Sea Res. II, 48, 2483 (2001).
Banse, K., Does iron really limit phytoplankton production in the offshore subarctic Pacific? Limnol.
Oceanogr., 35, 772 (1990).
Boyd, P.W., et al., A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron
fertilization, Nature, 407, 695 (2000).
Bozec, Y., et al., The CO 2 system in a Redfield context during an iron enrichment experiment in the
Southern Ocean, Mar. Chem., 95, 89–105 (2004).
Brand, L., Minimum iron requirements of marine phytoplankton and the implications for the biogeochemical control of new production, Limnol. Oceanogr., 36, 1756 (1991).
Chavez, F., The iron hypothesis: ecosystem test in Equatorial Pacific waters, Nature, 371, 123 (1994).
Chisholm, S.W., and Morel, F.M.M., What controls phytoplankton production in nutrient rich areas
of the open sea? Limnol. Oceanogr., 36, 1507 (1991).
Coale, K.H., et al., The IronExII mesoscale experiment produces massive phytoplankton bloom in the
equatorial Pacific, Nature, 383, 495 (1996).
Coale, K.H., et al., Southern Ocean iron enrichment experiment: carbon cycling in high- and low- Si
waters, Science, 304, 408 (2004).
Cooper, D.J., Watson, A., and Nightingale, P., Large decrease in ocean surface CO 2 fugacity in
response to in situ iron fertilization, Nature, 381, 511 (1996).
Greene, R., Geider, R., and Falkowski, P., Effect of iron limitation on photosynthesis in a marine diatom, Limnol. Oceanogr., 36, 1772 (1991).
Hiscock, W., and Millero, F.J., Nutrient and carbon parameters during the Southern Ocean Iron
Experiment (SOFeX), Deep- Sea Res. I, 52, 2086–2108 (2005).
Hudson, R.J.M., and Morel, F.F.M., Iron transport in marine phytoplankton: kinetics of cellular and
medium coordination reaction, Limnol. Oceanogr., 35, 1002 (1990).
Kolber, K., et al., Iron limitation of phytoplankton photosynthesis in the Equatorial Pacific Ocean,
Nature, 371, 145 (1994).
Ledwell, J., Watson, A., and Law, C., Evidence for slow mixing across the pycnocline from an openocean tracer- release experiment, Nature, 364, 701 (1993).
Martin, J.H., Glacial–interglacial CO 2 change: the iron hypothesis, Paleoceanography, 5, 1 (1990).
Martin, J.H., Iron as a limiting factor in oceanic productivity in Primary Productivity and Biogeochemical
Cycles in the Sea, Falkowski, P.G., and Woodhead, A., Eds., Plenum, New York, 123–137 (1992).
Martin, J.H., and Fitzwater, S.E., Iron deficiency limits phytoplankton growth in the northeast Pacific
subarctic, Nature, 331, 341 (1989).