10 Influence of Geochemical Processes on Stable Isotope Distribution in Marine Sediments
368
Schmidt, G.A., Bigg, G.R., and Rohling, E.J., 1999.
Global seawater oxygen-18 database. http://
data.giss.nasa.gov/o18data/.
Schneider, R., Dahmke, A., Kölling, A., Müller, P.J.,
Schulz, H.D., Wefer, G., 1992. Strong deglacial minimum in the δ
13 C record from planktonic foraminifera
in the Benguela Upwelling Region: paleoceanographic
signal or early diagenetic imprint. In: Summerhayes,
C.P., Prell, W.L., Emeis, K.C., (eds), Upwelling systems: Evolution since the early Miocene. Geological
Society Special Publication 63, pp 285-297.
Schrag, D.P., and DePaolo, D.J., 1993. Determination
of δ
18 O of seawater in the deep ocean during the last
glacial maximum: Paleoceanography, 8: 1-6.
Schrag, D.P., DePaolo, D.J., and Richter, F.M., 1995.
Reconstructing past sea surface temperatures correcting for diagenesis of bulk marine carbonate:
Geochimica et Cosmochimica Acta 59: 2265-2278.
Schulte, S., Benthien, A., Andersen, N., Müller, P.J.,
Rühlemann, C., Schneider, R.R., 2003. Stable carbon
isotopic composition of the C37:2 alkenone: A
proxy for CO 2(aq) concentration in oceanic surface
waters? In: The South Atlantic in the Late
Quaternary: Reconstruction of Material Budgets and
Current Systems. G. Wefer, S. Mulitza and V.
Ratmeyer, (eds), Springer, Berlin, pp. 195-211.
Shackleton, N.J., 1977. Tropical rainforest history and
the equatorial Pacific carbonate dissolution cycles.
In: Anderson, N.R., Malahoff, A., (eds), Fate in
fossil fuel CO 2 in the oceans. Plenum, New York, pp
401-427.
Shackleton, N.J., Opdyke, N.D., 1973. Oxygen isotope
and paleomagnetic stratigraphy of equatorial Pacific
core V 28-238: Oxygen isotope temperatures and ice
volumes on a 10^5 year scale. Quartenary Research
3: 39-55.
Sigman, D.M., Altabet, M., Francois, R., McCorkle,
D.C., Gaillard, J.F., 1999. The isotopic composition
of diatom - bound nitrogen in Southern Ocean
sediments. Paleoceanography, 14, 118 – 134.
Spero, H.J., 1992. Do planktonic foraminifera accurately record shifts in the carbon isotopic composition of ΣCO 2 ? Marine Micropaleontology 19:
275-285.
Spero, H.J., Bijma, J., Lea, D.W., Bemis, B.E., 1997.
Effect of seawater carbonate chemistry on planktonic foraminiferal carbon and oxygen isotope
values. Nature 390: 497-500.
Spero, H.J., Lea, D.W., 1993. Intraspecific stable isotope variability in the planktic foraminifera
Globigerinoides sacculifer: Results from laboratory
experiments. Marine Micropaleontology 22: 221234.
Spivack, A.J., Edmond, J.M., 1986. Determination of
boron isotope ratios by thermal ionization mass
spectrometry of the dicesium metaborate cation.
Anal Chem 58: 31-35.
Strauss, H., 1997. The isotopic composition of sedimentary sulfur through time. Palaeogeography,
Palaeoclimatology, Palaeoecology 132: 97-118.
Sweeney, R.E., Kaplan, I.R., 1980. Natural abundances
of
15 N as a source indicator for near-shore marine
sedimentary and dissolved nitrogen. Marine
Chemistry 9: 81-94.
Sweeney, R.E., Liu, K.K., Kaplan, I.R., 1978. Oceanic
nitrogen isotopes and their uses in determining the
source of sedimentary nitrogen. In: Robinson, B.W.,
(eds), Stable isotopes in earth sciences. Dept.
Scientific and Industrial Research, Wellington, pp 92 6 .
Valley, J.W., and Cole, D.R., (eds), 2001. Stable Isotope
Geochemistry. Reviews in Mineralogy and Geochemistry, The Mineralogical Society of America,
Blacksburg, vol. 43, pp. 662.
Veizer, J., Ala, D., Azmy, K., Bruckschen, P., Buhl, D.,
Bruhn, F., Carden, G.A.F., Diener, A., Ebneth, S.,
Godderis, Y., Jasper, T., Korte, C., Pawellek, F.,
Podlaha, O., Strauss, H., 1999.
87 Sr/
86 Sr, δ
13 C and δ
18 O
evolution of Phanerozoic seawater. Chemical Geology 161, 59-88. With data update 2004: http://
www.science.uottawa.ca/geology/isotope_data/.
Veizer, J., Bruckschen, P., Pawellek, F., Diener, A.,
Podlaha, O.G., Carden, G.A.F., Jasper, T., Korte, C.,
Strauss, H., Azmy, K., Ala, D., 1997. Oxygen isotope
evolution of Phanerozoic seawater. Palaeogeography, Palaeoclimatology, Palaeoecology 132: 159172.
Vinogradov, A.P., Grinenko, V.A., Ustinov, V.I., 1962.
Isotopic composition of sulfur compounds in the
Black Sea. Geokhimiya 10: 973-997.
Voss, M., Altabet, M.A., von Bodungen, B., 1996. δ
15 N
in sedimenting particles as indicator of euphoticzone processes. Deep-Sea Research 43: 33-47.
Wada, E., Hattori, A., 1978. Nitrogen assimilation
effects in the assimilation of inorganic nitrogenous
compounds by marine diatoms. Geomicrobiol J 1:
85-101.
Wada, E., Minagawa, M., Mizutani, H., Tsuji, T.,
Imaizumi, R., Karasawa, K., 1987. Biogeochemical
studies on the transport of organic matter along the
Otsuchi River watershed, Japan. Estuarine, Coastal
and Shelf Sciences 25: 321-336.
Waelbroeck, C., Mulitza, S., Spero, H., Dokken, T.,
Kiefer, T., Cortijo, E., 2004. A global compilation
of Holocene planktonic foraminiferal δ
18 O: relationship between surface water temperature and δ
18 O,
Quaternary Science Reviews 24: 853-868.
Wallmann, K., 2001. The geological water cycle and the
evolution of marine δ
18 O values. Geochimica et
Cosmochimica Acta 65: 2469-2485.
Wefer, G., Berger, W.H., 1991. Isotope paleontology:
growth and composition of extant calcareous
species. Marine Geology 100: 207-248.
Wefer, G., Heinze, P.M., Berger, W.H., 1994. Clues to
ancient methane release. Nature, 369: 282.
Weiss, R.F., 1974. Carbon dioxide in water and seawater:
The solubility of a non-ideal gas. Marine Chemistry
2: 203-215.
Weiss, R.F., Östlund, H.G., Craig, H., 1979. Geochemical
studies of the Weddell Sea. Deep-Sea Research 26:
1093-1120.
Williams, L.B., Ferell, R.E., Hutcheon, I., Bakel, A.J.,
Walsh, M.M., Krouse, H.R., 1995. Nitrogen isotope
368
Schmidt, G.A., Bigg, G.R., and Rohling, E.J., 1999.
Global seawater oxygen-18 database. http://
data.giss.nasa.gov/o18data/.
Schneider, R., Dahmke, A., Kölling, A., Müller, P.J.,
Schulz, H.D., Wefer, G., 1992. Strong deglacial minimum in the δ
13 C record from planktonic foraminifera
in the Benguela Upwelling Region: paleoceanographic
signal or early diagenetic imprint. In: Summerhayes,
C.P., Prell, W.L., Emeis, K.C., (eds), Upwelling systems: Evolution since the early Miocene. Geological
Society Special Publication 63, pp 285-297.
Schrag, D.P., and DePaolo, D.J., 1993. Determination
of δ
18 O of seawater in the deep ocean during the last
glacial maximum: Paleoceanography, 8: 1-6.
Schrag, D.P., DePaolo, D.J., and Richter, F.M., 1995.
Reconstructing past sea surface temperatures correcting for diagenesis of bulk marine carbonate:
Geochimica et Cosmochimica Acta 59: 2265-2278.
Schulte, S., Benthien, A., Andersen, N., Müller, P.J.,
Rühlemann, C., Schneider, R.R., 2003. Stable carbon
isotopic composition of the C37:2 alkenone: A
proxy for CO 2(aq) concentration in oceanic surface
waters? In: The South Atlantic in the Late
Quaternary: Reconstruction of Material Budgets and
Current Systems. G. Wefer, S. Mulitza and V.
Ratmeyer, (eds), Springer, Berlin, pp. 195-211.
Shackleton, N.J., 1977. Tropical rainforest history and
the equatorial Pacific carbonate dissolution cycles.
In: Anderson, N.R., Malahoff, A., (eds), Fate in
fossil fuel CO 2 in the oceans. Plenum, New York, pp
401-427.
Shackleton, N.J., Opdyke, N.D., 1973. Oxygen isotope
and paleomagnetic stratigraphy of equatorial Pacific
core V 28-238: Oxygen isotope temperatures and ice
volumes on a 10^5 year scale. Quartenary Research
3: 39-55.
Sigman, D.M., Altabet, M., Francois, R., McCorkle,
D.C., Gaillard, J.F., 1999. The isotopic composition
of diatom - bound nitrogen in Southern Ocean
sediments. Paleoceanography, 14, 118 – 134.
Spero, H.J., 1992. Do planktonic foraminifera accurately record shifts in the carbon isotopic composition of ΣCO 2 ? Marine Micropaleontology 19:
275-285.
Spero, H.J., Bijma, J., Lea, D.W., Bemis, B.E., 1997.
Effect of seawater carbonate chemistry on planktonic foraminiferal carbon and oxygen isotope
values. Nature 390: 497-500.
Spero, H.J., Lea, D.W., 1993. Intraspecific stable isotope variability in the planktic foraminifera
Globigerinoides sacculifer: Results from laboratory
experiments. Marine Micropaleontology 22: 221234.
Spivack, A.J., Edmond, J.M., 1986. Determination of
boron isotope ratios by thermal ionization mass
spectrometry of the dicesium metaborate cation.
Anal Chem 58: 31-35.
Strauss, H., 1997. The isotopic composition of sedimentary sulfur through time. Palaeogeography,
Palaeoclimatology, Palaeoecology 132: 97-118.
Sweeney, R.E., Kaplan, I.R., 1980. Natural abundances
of
15 N as a source indicator for near-shore marine
sedimentary and dissolved nitrogen. Marine
Chemistry 9: 81-94.
Sweeney, R.E., Liu, K.K., Kaplan, I.R., 1978. Oceanic
nitrogen isotopes and their uses in determining the
source of sedimentary nitrogen. In: Robinson, B.W.,
(eds), Stable isotopes in earth sciences. Dept.
Scientific and Industrial Research, Wellington, pp 92 6 .
Valley, J.W., and Cole, D.R., (eds), 2001. Stable Isotope
Geochemistry. Reviews in Mineralogy and Geochemistry, The Mineralogical Society of America,
Blacksburg, vol. 43, pp. 662.
Veizer, J., Ala, D., Azmy, K., Bruckschen, P., Buhl, D.,
Bruhn, F., Carden, G.A.F., Diener, A., Ebneth, S.,
Godderis, Y., Jasper, T., Korte, C., Pawellek, F.,
Podlaha, O., Strauss, H., 1999.
87 Sr/
86 Sr, δ
13 C and δ
18 O
evolution of Phanerozoic seawater. Chemical Geology 161, 59-88. With data update 2004: http://
www.science.uottawa.ca/geology/isotope_data/.
Veizer, J., Bruckschen, P., Pawellek, F., Diener, A.,
Podlaha, O.G., Carden, G.A.F., Jasper, T., Korte, C.,
Strauss, H., Azmy, K., Ala, D., 1997. Oxygen isotope
evolution of Phanerozoic seawater. Palaeogeography, Palaeoclimatology, Palaeoecology 132: 159172.
Vinogradov, A.P., Grinenko, V.A., Ustinov, V.I., 1962.
Isotopic composition of sulfur compounds in the
Black Sea. Geokhimiya 10: 973-997.
Voss, M., Altabet, M.A., von Bodungen, B., 1996. δ
15 N
in sedimenting particles as indicator of euphoticzone processes. Deep-Sea Research 43: 33-47.
Wada, E., Hattori, A., 1978. Nitrogen assimilation
effects in the assimilation of inorganic nitrogenous
compounds by marine diatoms. Geomicrobiol J 1:
85-101.
Wada, E., Minagawa, M., Mizutani, H., Tsuji, T.,
Imaizumi, R., Karasawa, K., 1987. Biogeochemical
studies on the transport of organic matter along the
Otsuchi River watershed, Japan. Estuarine, Coastal
and Shelf Sciences 25: 321-336.
Waelbroeck, C., Mulitza, S., Spero, H., Dokken, T.,
Kiefer, T., Cortijo, E., 2004. A global compilation
of Holocene planktonic foraminiferal δ
18 O: relationship between surface water temperature and δ
18 O,
Quaternary Science Reviews 24: 853-868.
Wallmann, K., 2001. The geological water cycle and the
evolution of marine δ
18 O values. Geochimica et
Cosmochimica Acta 65: 2469-2485.
Wefer, G., Berger, W.H., 1991. Isotope paleontology:
growth and composition of extant calcareous
species. Marine Geology 100: 207-248.
Wefer, G., Heinze, P.M., Berger, W.H., 1994. Clues to
ancient methane release. Nature, 369: 282.
Weiss, R.F., 1974. Carbon dioxide in water and seawater:
The solubility of a non-ideal gas. Marine Chemistry
2: 203-215.
Weiss, R.F., Östlund, H.G., Craig, H., 1979. Geochemical
studies of the Weddell Sea. Deep-Sea Research 26:
1093-1120.
Williams, L.B., Ferell, R.E., Hutcheon, I., Bakel, A.J.,
Walsh, M.M., Krouse, H.R., 1995. Nitrogen isotope