267
References
Hart, T.J., 1934. On the phytoplankton of the southwest Atlantic and the Bellinghausen Sea, 1929-31.
Discovery Reports VIII.
Hein, J.R., Yeh, H.-W. and Alexander, E., 1979. Origin
of iron rich montmorillonite from the manganese
nodule belt of the north equatorial Pacific. Clays
and Clay Mineralogy, 27: 185-194.
Hunter, K.A., 1983. On the estuarine mixing of dissolved substances in relation to colloid stability and
surface properties. Geochimica Cosmochimica Acta,
47: 467-473.
Hüttel, M., Ziebis, W., Forster, S. and Luther, G.W. III,
1998. Advective transport affecting metal and
nutrient distributions and interfacial fluxes in
permeable sediments. Geochimica Cosmochimica
Acta, 62: 613-631.
Hyacinthe, C., and Van Cappellen, P., 2004. An
authigenic iron phosphate phase in estuarine
sediments: composition, formation and chemical
reactivity. Marine Chemistry, 91: 227-251.
Jensen, H.S., Mortensen, B.P., Andersen, F.Ø.,
Rasmussen, E. and Jensen, A., 1995. Phosphorus
cycling in a coastal marine sediment, Aarhus Bay,
Denmark. Limnology and Oceanography, 40: 908917.
Johnson, K.S., Coale, K.H., Elrod, V.A. and Tindale,
N.W., 1994. Iron photochemistry in seawater from
the equatorial Pacific. Marine Chemistry, 46: 319334.
Johnson, K.S., Gordon, R.M. and Coale, K.H., 1997.
What controls dissolved iron concentrations in the
world ocean? Marine Chemistry, 57: 137-161.
Johnson, C.M., Beard, B.L., Roden, E.E., Newman,
D.K., and Nealson, K.H., 2004. Isotopic constraints
on biogeochemical cycling of Fe. In: Geochemistry
of non-traditional stable isotopes, Eds: Johnson,
C.M., Beard, B.L., and Albarède, F., Reviews in
Mineralogy & Geochemistry, 55: 359-408.
Jørgensen, B.B., 1977. Bacterial sulfate reduction within
reduced microniches of oxidized marine sediments.
Marine Biology, 41: 7-17.
Kester, D.R. and Pytkowicz, R.M., 1967. Determination
of apparent dissociation constants of phosphoric
acid in sea water. Limnology and Oceanography, 12:
243-252.
Kostka, J.E. and Luther, G.W. III, 1994. Partitioning
and speciation of solid phase iron in saltmarsh
sediments. Geochimica Cosmochimica Acta, 58:
1701-1710.
Kostka, J.E. and Nealson, K.H., 1995. Dissolution and
reduction of magnetite by bacteria. Environmental
Science and Technology, 29: 2535-2540.
Kostka, J.E., Stucki, J.W., Nealson, K.H. and Wu, J.,
1996. Reduction of structural Fe(III) in smectite by
a pure culture of Shewanella putrefaciens Strain MR1. Clays and Clay Minerals, 44: 522-529.
König, I., Drodt, M., Suess, E., Trautwein, A.X., 1997.
Iron reduction through the tan-green color
transition in deep-sea sediments. Geochimica
Cosmochimica Acta, 61: 1679-1683
Krauskopf, K.B., 1956. Factors controlling the
concentration of thirteen trace metals in seawater.
Geochimica Cosmochimica Acta, 12: 331-334.
Krom, M.D., Berner, R.A., 1980. Adsorption of
phosphate in anoxic marine sediments. Limnology
and Oceanography, 25: 797-806.
Kuma, K., Nishioka, J., Matsunaga, K., 1994. Controls
of iron(III) hydroxide solubility in seawater: The
influence of pH and natural organic chelators.
Limnology and Oceanography, 41: 396-407.
Lear, P.R. and Stucki, J.W., 1989. Effects of iron
oxidation state on the specific surface area of
nontronite. Clays and Clay Minerals, 37: 547-552.
Leventhal, J. and Taylor, C., 1990. Comparison of
methods to determine the degree of pyritisation.
Geochimica Cosmochimica Acta, 54: 2621-2625.
Lord, C.J. III., 1980. The chemistry and cycling of iron,
manganese, and sulfur in salt marsh sediments. Ph.D.
thesis, University Delaware, 177 pp.
Lovley, D.R., 1987. Organic matter mineralization with
the
reduction
of
ferric
iron:
A
review.
Geomicrobiology Journal, 5: 375-399.
Lovley, D.R. and Phillips, E.J.P., 1988. Novel mode of
microbial energy metabolism: Organic carbon
oxidition coupled to dissimilatory reduction of iron
and manganese. Applied and Environmental
Microbiology, 54: 1472-1480
Lovley, D.R., 1991. Dissimilatory Fe(III) and Mn(IV)
reduction. Microbiological Reviews 55: 259-287.
Lovley, D.R., 1997. Microbial Fe(III) reduction in
subsurface environments. FEMS Microbiological
Reviews, 20: 305-313.
Lovley, D.R., Coates, J.D., Saffarini, D. and Lonergan,
D.J., 1997. Diversity of dissimilatory Fe(III)reducing bacteria. In: Winkelman, G. and Carrano,
C.J. (eds) Iron and Related Transition Metals in
Microbial
Metabolism,
Harwood
Academic
Publishers, Switzerland, pp. 187-215.
Lyle, M., 1983, The brown-green color transition in
marine sediments: A marker of the Fe(III)-Fe(II)
redox boundary. Limnology and Oceanography, 28:
1026-1033.
Mackenzie, F.T. and Garrels, R.M., 1966, Chemical mass
balance between rivers and oceans. American Journal
of Science, 264: 507-525.
Martin, J.H., Gordon, R.M., Fitzwater, S.E., Broenkow,
W.W., 1989. VERTEX: phytoplankton/iron studies
in the Gulf of Alaska. Deep-Sea Research, 36: 649680.
Martin, J.H., 1990. Glacial-interglacial CO 2 change: The
iron hypothesis. Paleoceanography, 5: 1-13.
Martin, J.H., Gordon, R.M. and Fitzwater, S.E.,
1991. The case for iron. In: Chisholm, S.W. and
Morel, F.M.M. (eds). What controls phytoplankton production in nutrient-rich areas of the
open sea?, ASLO Symposium, Lake San Marcos,
California, Feb. 22-24, 1991, Allen Press, Lawr e n c e .
Martin, J.H., Coale, K.H., Johnson, K.S. and Fitzwater,
S.E., 1994. Testing the iron hypothesis in
ecosystems of the equatorial Pacific Ocean. Nature,
371: 123-129.
References
Hart, T.J., 1934. On the phytoplankton of the southwest Atlantic and the Bellinghausen Sea, 1929-31.
Discovery Reports VIII.
Hein, J.R., Yeh, H.-W. and Alexander, E., 1979. Origin
of iron rich montmorillonite from the manganese
nodule belt of the north equatorial Pacific. Clays
and Clay Mineralogy, 27: 185-194.
Hunter, K.A., 1983. On the estuarine mixing of dissolved substances in relation to colloid stability and
surface properties. Geochimica Cosmochimica Acta,
47: 467-473.
Hüttel, M., Ziebis, W., Forster, S. and Luther, G.W. III,
1998. Advective transport affecting metal and
nutrient distributions and interfacial fluxes in
permeable sediments. Geochimica Cosmochimica
Acta, 62: 613-631.
Hyacinthe, C., and Van Cappellen, P., 2004. An
authigenic iron phosphate phase in estuarine
sediments: composition, formation and chemical
reactivity. Marine Chemistry, 91: 227-251.
Jensen, H.S., Mortensen, B.P., Andersen, F.Ø.,
Rasmussen, E. and Jensen, A., 1995. Phosphorus
cycling in a coastal marine sediment, Aarhus Bay,
Denmark. Limnology and Oceanography, 40: 908917.
Johnson, K.S., Coale, K.H., Elrod, V.A. and Tindale,
N.W., 1994. Iron photochemistry in seawater from
the equatorial Pacific. Marine Chemistry, 46: 319334.
Johnson, K.S., Gordon, R.M. and Coale, K.H., 1997.
What controls dissolved iron concentrations in the
world ocean? Marine Chemistry, 57: 137-161.
Johnson, C.M., Beard, B.L., Roden, E.E., Newman,
D.K., and Nealson, K.H., 2004. Isotopic constraints
on biogeochemical cycling of Fe. In: Geochemistry
of non-traditional stable isotopes, Eds: Johnson,
C.M., Beard, B.L., and Albarède, F., Reviews in
Mineralogy & Geochemistry, 55: 359-408.
Jørgensen, B.B., 1977. Bacterial sulfate reduction within
reduced microniches of oxidized marine sediments.
Marine Biology, 41: 7-17.
Kester, D.R. and Pytkowicz, R.M., 1967. Determination
of apparent dissociation constants of phosphoric
acid in sea water. Limnology and Oceanography, 12:
243-252.
Kostka, J.E. and Luther, G.W. III, 1994. Partitioning
and speciation of solid phase iron in saltmarsh
sediments. Geochimica Cosmochimica Acta, 58:
1701-1710.
Kostka, J.E. and Nealson, K.H., 1995. Dissolution and
reduction of magnetite by bacteria. Environmental
Science and Technology, 29: 2535-2540.
Kostka, J.E., Stucki, J.W., Nealson, K.H. and Wu, J.,
1996. Reduction of structural Fe(III) in smectite by
a pure culture of Shewanella putrefaciens Strain MR1. Clays and Clay Minerals, 44: 522-529.
König, I., Drodt, M., Suess, E., Trautwein, A.X., 1997.
Iron reduction through the tan-green color
transition in deep-sea sediments. Geochimica
Cosmochimica Acta, 61: 1679-1683
Krauskopf, K.B., 1956. Factors controlling the
concentration of thirteen trace metals in seawater.
Geochimica Cosmochimica Acta, 12: 331-334.
Krom, M.D., Berner, R.A., 1980. Adsorption of
phosphate in anoxic marine sediments. Limnology
and Oceanography, 25: 797-806.
Kuma, K., Nishioka, J., Matsunaga, K., 1994. Controls
of iron(III) hydroxide solubility in seawater: The
influence of pH and natural organic chelators.
Limnology and Oceanography, 41: 396-407.
Lear, P.R. and Stucki, J.W., 1989. Effects of iron
oxidation state on the specific surface area of
nontronite. Clays and Clay Minerals, 37: 547-552.
Leventhal, J. and Taylor, C., 1990. Comparison of
methods to determine the degree of pyritisation.
Geochimica Cosmochimica Acta, 54: 2621-2625.
Lord, C.J. III., 1980. The chemistry and cycling of iron,
manganese, and sulfur in salt marsh sediments. Ph.D.
thesis, University Delaware, 177 pp.
Lovley, D.R., 1987. Organic matter mineralization with
the
reduction
of
ferric
iron:
A
review.
Geomicrobiology Journal, 5: 375-399.
Lovley, D.R. and Phillips, E.J.P., 1988. Novel mode of
microbial energy metabolism: Organic carbon
oxidition coupled to dissimilatory reduction of iron
and manganese. Applied and Environmental
Microbiology, 54: 1472-1480
Lovley, D.R., 1991. Dissimilatory Fe(III) and Mn(IV)
reduction. Microbiological Reviews 55: 259-287.
Lovley, D.R., 1997. Microbial Fe(III) reduction in
subsurface environments. FEMS Microbiological
Reviews, 20: 305-313.
Lovley, D.R., Coates, J.D., Saffarini, D. and Lonergan,
D.J., 1997. Diversity of dissimilatory Fe(III)reducing bacteria. In: Winkelman, G. and Carrano,
C.J. (eds) Iron and Related Transition Metals in
Microbial
Metabolism,
Harwood
Academic
Publishers, Switzerland, pp. 187-215.
Lyle, M., 1983, The brown-green color transition in
marine sediments: A marker of the Fe(III)-Fe(II)
redox boundary. Limnology and Oceanography, 28:
1026-1033.
Mackenzie, F.T. and Garrels, R.M., 1966, Chemical mass
balance between rivers and oceans. American Journal
of Science, 264: 507-525.
Martin, J.H., Gordon, R.M., Fitzwater, S.E., Broenkow,
W.W., 1989. VERTEX: phytoplankton/iron studies
in the Gulf of Alaska. Deep-Sea Research, 36: 649680.
Martin, J.H., 1990. Glacial-interglacial CO 2 change: The
iron hypothesis. Paleoceanography, 5: 1-13.
Martin, J.H., Gordon, R.M. and Fitzwater, S.E.,
1991. The case for iron. In: Chisholm, S.W. and
Morel, F.M.M. (eds). What controls phytoplankton production in nutrient-rich areas of the
open sea?, ASLO Symposium, Lake San Marcos,
California, Feb. 22-24, 1991, Allen Press, Lawr e n c e .
Martin, J.H., Coale, K.H., Johnson, K.S. and Fitzwater,
S.E., 1994. Testing the iron hypothesis in
ecosystems of the equatorial Pacific Ocean. Nature,
371: 123-129.