7
The Biogeochemistry of Iron
268
Mayer, L.M., Jorgensen, J., Schnitker, D., 1991.
Enhencement of diatom frustule dissolution by iron
oxides. Marine Geology, 99: 263-266.
McAllister, C.D., Parsons, T.R. and Strickland, J.D.H.,
1960. Primary productivity and fertility at station
“P” in the north-east Pacific Ocean. Journal du
Conseil, 25: 240-259.
McMurtry, G.M., Chung-Ho, W. and Hsueh-Wen, Y.,
1983. Chemical and isotopic investigation into the
origin of clay minerals from the Galapagos
hydrothermal mound field. Geochimica Cosmochimica Acta, 47: 291-300.
Mehra, O.P. and Jackson, M.L., 1960. Iron oxide
removal from soils and clays by a dithionite-citrate
system buffered with sodium carbonate. Proceedings
of the National Conference on Clays and Clay
Mineralogy, 7: 317-327.
Michalopoulos, P. and Aller, R.C., 1995. Rapid clay
mineral formation in Amazon delta sediments:
Reverse weathering and oceanic cycles. Science,
270: 614-617.
Millero, F.J., Sotolongo, S. and Izaguirre, M., 1987. The
oxidation kinetic of Fe(II) in seawater. Geochimica
Cosmochimica Acta, 51: 793-801.
Morris, R.V., Lauer, H.V. Jr., Lawson, C.A., Gibson, E.K.
Jr., Nace, G.A. and Stewart C., 1985. Spectral and
other physicochemical properties of submicron
powders of hematite (α-Fe 2 O 3 ), maghemite (γ-Fe 2 O 3 ),
magnetite (Fe 3 O 4 ), goethite (α-FeOOH), and
lepidocrocite (γ-FeOOH). Journal of Geophysical
Research, 90: 3126-3144.
Mortimer, R.J.G., Coleman, M.L., 1997. Microbial
influence on the oxygen isotopic composition of
diagenetic siderite. Geochimica Cosmochimica Acta,
61: 1705-1711.
Munch, J.C. and Ottow, J.C.G., 1980. Preferential
reduction of amorphous to crystalline iron oxides by
bacterial activity. Journal of Soil Science,129: 152 1 .
Munch, J.C. and Ottow, J.C.G., 1982. Einfluß von
Zellkontakt und Eisen(III)oxidform auf die bakterielle Eisenreduktion. Zeitschrift der Pflanzenernährung und Bodenkunde, 145: 66-77.
Murray, R.W. and Leinen, M., 1993, Chemical transport
to the seafloor of the equatorial Pacific across a
latitudinal transect at 135°W: Tracking sedimentary
major, minor, and rare earth element fluxes at the
equator and the inner tropical convergence zone.
Geochimica Cosmochimica Acta, 57: 4141-4163.
Myers, C.R. and Nealson, K.H., 1988a. Bacterial
manganese reduction and growth with manganese
oxide as the sole electron acceptor. Science, 240:
1319-1321.
Myers, C.R. and Nealson, K.H., 1988b. Micorbial
reduction of manganese oxides: Interactions with
iron and sulfur. Geochimica Cosmochimica Acta, 52:
2727-2732.
Nittrouer, C.A., DeMaster, D.J., McKee, B.A., Cutshall,
N.H., Larsen, I.L., 1983/1984. The effect of sediment mixing on Pb-210 accumulation rates for the
Washington continental shelf. Marine Geology, 54:
201-221.
Norrish, K., Taylor, R.M., 1961. The isomorphous
replacement of iron by aluminium in soil goethites.
Journal of Soil Sciences, 12: 294-306.
Ottley, C.J., Davison, W., Edmunds, W.M., 1997.
Chemical catalysis of nitrate reduction by iron(II).
Geochimica Cosmochimica Acta, 61: 1819-1828.
Ottow, J.C.G., 1969. Der Einfluss von Nitrat, Chlorat,
Sulfat, Eisenoxidform und Wachstumsbedingungen
auf das Ausmass der bakteriellen Eisenreduktion.
Zeitschrift der Pflanzenernährung und Bodenkunde,
124: 238-253.
Peiffer, S., Dos Santos Afonso, M., Wehrli, B. and
Gächter, R., 1992. Kinetics and mechanism of the
reaction of H 2 S with lepidocrocite. Environmental
Science and Technology, 26: 2408-2412.
Pena, F. and Torrent, J., 1984. Relationships between
phosphate sorption and iron oxides in alfisols from
a river terrace sequence of Mediterranean Spain.
Geoderma, 33: 283-296.
Postma, D., 1982, Pyrite and siderite formation in
brackish and freshwater swamp sediments. American
Journal of Science, 282: 1151-1183.
Postma, D., 1985. Concentration of Mn and separation
from Fe in sediments. Kinetics and stoichiometry of the
reaction between birnessite and dissolved Fe(II) at 10°C.
Geochimica Cosmochimica Acta, 49: 1023-1033.
Postma, D., Jakobsen, R., 1996, Redox zonation:
Equilibrium constraints on the Fe(II)/SO4-reduction
interface. Geochimica Cosmochimica Acta, 60:
3169-3175.
Poulton, S.W. and Raiswell, R., 2002, The lowtemperature geochemical cycle of iron: from continental fluxes to marine sediment deposition. American Journal of Science, 302: 774-805.
Poulton, S.W., Krom, M.D., and Raiswell, R., 2004. A
revised scheme for the reactivity of iron
(oxyhydr)oxide minerals towards dissolved sulfide.
Geochimica Cosmochimica Acta, 68: 3703-3715.
Prospero, J.M., 1981. Eolian transport to the world
ocean. In: Emiliani, C. (ed), The sea, 7, Wiley, New
York, pp. 801-874.
Prospero, J.M., Glaccum, R.A. and Nees, R.T., 1981.
Atmospheric transport of soil dust from Africa to
South America. Nature, 289: 570-572.
Pyzik, A.J. and Sommer, S.E., 1981, Sedimentary iron
monosulfides: kinetics and mechanisms of formation. Geochimica Cosmochimica Acta, 45: 687-698.
Raiswell, R., Buckley, F., Berner, R.A. and Anderson,
T.F., 1988. Degree of pyritisation as a paleoenvironmental indicator of bottom water oxygenation. Journal of Sedimentary Petrology, 58: 812819.
Raiswell, R., Canfield, D.E. and Berner, R.A., 1994. A
comparison of iron extraction methods for the
determination of degree of pyritisation and the
recognition of iron-limited pyrite formation. Chemical Geology, 111: 101-110.
Raiswell, R. and Canfield, D.E., 1996. Rates of reaction
between silicate iron and dissolved sulfide in Peru
Margin sediments. Geochimica Cosmochimica Acta,
60: 2777-2787.
The Biogeochemistry of Iron
268
Mayer, L.M., Jorgensen, J., Schnitker, D., 1991.
Enhencement of diatom frustule dissolution by iron
oxides. Marine Geology, 99: 263-266.
McAllister, C.D., Parsons, T.R. and Strickland, J.D.H.,
1960. Primary productivity and fertility at station
“P” in the north-east Pacific Ocean. Journal du
Conseil, 25: 240-259.
McMurtry, G.M., Chung-Ho, W. and Hsueh-Wen, Y.,
1983. Chemical and isotopic investigation into the
origin of clay minerals from the Galapagos
hydrothermal mound field. Geochimica Cosmochimica Acta, 47: 291-300.
Mehra, O.P. and Jackson, M.L., 1960. Iron oxide
removal from soils and clays by a dithionite-citrate
system buffered with sodium carbonate. Proceedings
of the National Conference on Clays and Clay
Mineralogy, 7: 317-327.
Michalopoulos, P. and Aller, R.C., 1995. Rapid clay
mineral formation in Amazon delta sediments:
Reverse weathering and oceanic cycles. Science,
270: 614-617.
Millero, F.J., Sotolongo, S. and Izaguirre, M., 1987. The
oxidation kinetic of Fe(II) in seawater. Geochimica
Cosmochimica Acta, 51: 793-801.
Morris, R.V., Lauer, H.V. Jr., Lawson, C.A., Gibson, E.K.
Jr., Nace, G.A. and Stewart C., 1985. Spectral and
other physicochemical properties of submicron
powders of hematite (α-Fe 2 O 3 ), maghemite (γ-Fe 2 O 3 ),
magnetite (Fe 3 O 4 ), goethite (α-FeOOH), and
lepidocrocite (γ-FeOOH). Journal of Geophysical
Research, 90: 3126-3144.
Mortimer, R.J.G., Coleman, M.L., 1997. Microbial
influence on the oxygen isotopic composition of
diagenetic siderite. Geochimica Cosmochimica Acta,
61: 1705-1711.
Munch, J.C. and Ottow, J.C.G., 1980. Preferential
reduction of amorphous to crystalline iron oxides by
bacterial activity. Journal of Soil Science,129: 152 1 .
Munch, J.C. and Ottow, J.C.G., 1982. Einfluß von
Zellkontakt und Eisen(III)oxidform auf die bakterielle Eisenreduktion. Zeitschrift der Pflanzenernährung und Bodenkunde, 145: 66-77.
Murray, R.W. and Leinen, M., 1993, Chemical transport
to the seafloor of the equatorial Pacific across a
latitudinal transect at 135°W: Tracking sedimentary
major, minor, and rare earth element fluxes at the
equator and the inner tropical convergence zone.
Geochimica Cosmochimica Acta, 57: 4141-4163.
Myers, C.R. and Nealson, K.H., 1988a. Bacterial
manganese reduction and growth with manganese
oxide as the sole electron acceptor. Science, 240:
1319-1321.
Myers, C.R. and Nealson, K.H., 1988b. Micorbial
reduction of manganese oxides: Interactions with
iron and sulfur. Geochimica Cosmochimica Acta, 52:
2727-2732.
Nittrouer, C.A., DeMaster, D.J., McKee, B.A., Cutshall,
N.H., Larsen, I.L., 1983/1984. The effect of sediment mixing on Pb-210 accumulation rates for the
Washington continental shelf. Marine Geology, 54:
201-221.
Norrish, K., Taylor, R.M., 1961. The isomorphous
replacement of iron by aluminium in soil goethites.
Journal of Soil Sciences, 12: 294-306.
Ottley, C.J., Davison, W., Edmunds, W.M., 1997.
Chemical catalysis of nitrate reduction by iron(II).
Geochimica Cosmochimica Acta, 61: 1819-1828.
Ottow, J.C.G., 1969. Der Einfluss von Nitrat, Chlorat,
Sulfat, Eisenoxidform und Wachstumsbedingungen
auf das Ausmass der bakteriellen Eisenreduktion.
Zeitschrift der Pflanzenernährung und Bodenkunde,
124: 238-253.
Peiffer, S., Dos Santos Afonso, M., Wehrli, B. and
Gächter, R., 1992. Kinetics and mechanism of the
reaction of H 2 S with lepidocrocite. Environmental
Science and Technology, 26: 2408-2412.
Pena, F. and Torrent, J., 1984. Relationships between
phosphate sorption and iron oxides in alfisols from
a river terrace sequence of Mediterranean Spain.
Geoderma, 33: 283-296.
Postma, D., 1982, Pyrite and siderite formation in
brackish and freshwater swamp sediments. American
Journal of Science, 282: 1151-1183.
Postma, D., 1985. Concentration of Mn and separation
from Fe in sediments. Kinetics and stoichiometry of the
reaction between birnessite and dissolved Fe(II) at 10°C.
Geochimica Cosmochimica Acta, 49: 1023-1033.
Postma, D., Jakobsen, R., 1996, Redox zonation:
Equilibrium constraints on the Fe(II)/SO4-reduction
interface. Geochimica Cosmochimica Acta, 60:
3169-3175.
Poulton, S.W. and Raiswell, R., 2002, The lowtemperature geochemical cycle of iron: from continental fluxes to marine sediment deposition. American Journal of Science, 302: 774-805.
Poulton, S.W., Krom, M.D., and Raiswell, R., 2004. A
revised scheme for the reactivity of iron
(oxyhydr)oxide minerals towards dissolved sulfide.
Geochimica Cosmochimica Acta, 68: 3703-3715.
Prospero, J.M., 1981. Eolian transport to the world
ocean. In: Emiliani, C. (ed), The sea, 7, Wiley, New
York, pp. 801-874.
Prospero, J.M., Glaccum, R.A. and Nees, R.T., 1981.
Atmospheric transport of soil dust from Africa to
South America. Nature, 289: 570-572.
Pyzik, A.J. and Sommer, S.E., 1981, Sedimentary iron
monosulfides: kinetics and mechanisms of formation. Geochimica Cosmochimica Acta, 45: 687-698.
Raiswell, R., Buckley, F., Berner, R.A. and Anderson,
T.F., 1988. Degree of pyritisation as a paleoenvironmental indicator of bottom water oxygenation. Journal of Sedimentary Petrology, 58: 812819.
Raiswell, R., Canfield, D.E. and Berner, R.A., 1994. A
comparison of iron extraction methods for the
determination of degree of pyritisation and the
recognition of iron-limited pyrite formation. Chemical Geology, 111: 101-110.
Raiswell, R. and Canfield, D.E., 1996. Rates of reaction
between silicate iron and dissolved sulfide in Peru
Margin sediments. Geochimica Cosmochimica Acta,
60: 2777-2787.