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Influence of Geochemical Processes on Stable Isotope Distribution in Marine Sediments

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Marine Geochemistry

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References

  • Adkins, J.F., McIntyre, K., Schrag, D.P., 2002. The salinity, temperature, and δ18O of the glacial deep ocean. Science 298: 1769–1773.

    Google Scholar 

  • Altabet, M., 1988. Variations in nitrogen isotopic composition between sinking and suspended particles: implications for nitrogen cycling and particle transformation in the open ocean. Deep-Sea Research 35: 535–554.

    Google Scholar 

  • Altabet, M., Francois, R., 1994. Sedimentary nitrogen isotopic ratio as recorder for surface ocean nitrate utilization. Global Biogeochemical Cycles 8: 103–116.

    Google Scholar 

  • Altabet, M., McCarthy, J., 1985. Temporal and spatial variation in the natural abundance of 15N in PON from a warm-core ring. Deep-Sea Research 32: 755–722.

    Google Scholar 

  • Altabet, M., Curry, W.B., 1989. Testing models of past ocean chemistry using foraminifera 15N/14N. Global Biogeochemical Cycles 3: 107–119.

    Google Scholar 

  • Altabet, M., Deuser, W.G., Honjo, S., Stienen, C., 1991. Seasonal and depth-related changes in the source of sinking particles in the North Atlantic. Nature 354: 136–139.

    Google Scholar 

  • Altenbach, A.v., Sarnthein, M., 1989. Productivity record in benthic foraminifera. In: Berger, W.H., Smetacek, V.S., Wefer, G., (eds), Productivity of the ocean: Present and Past. Wiley & Sons, New York, pp 255–269.

    Google Scholar 

  • Andersen, N., Müller, P.J., Kirst, G., Schneider, R.R., 1999. Late Quaternary PCO2 variations in the Angola Current inferred from alkenone δ13C and carbon demand estimated by δ15N. In: Fischer, G., Wefer, G., (eds), Proxies in Paleoceanography: Examples from the South Atlantic. Springer, Berlin, pp 469–488.

    Google Scholar 

  • Arthur, M.A., Anderson, T.F., Kaplan, I.R., Veizer, J., Land, L.S., 1983. Stable isotopes in sedimentary geology. SEPM Short Course No. 10. SEPM, Tulsa, OK, 432 pp.

    Google Scholar 

  • Bemis, B.E., Spero, H.J., Bijma, J., Lea, D.W., 1998. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations. Paleoceanography 13: 150–160.

    Google Scholar 

  • Berger, W.H., Smetacek, V.S., Wefer, G., 1989. Productivity of the ocean: Present and Past. Wiley & Sons, New York, 471 pp.

    Google Scholar 

  • Berger, W.H., Vincent, E., 1986. Deep-sea carbonates: reading the carbon-isotope signal. Geol Rundsch 75: 249–269.

    Google Scholar 

  • Berner, R.A., Raiswell, R., 1983. Burial of organic carbon and pyrite sulfur in sediments over Phanerozoic time: a new theory. Geochimica et Cosmochimica Acta 47: 885–892.

    Google Scholar 

  • Bickert, T., Pätzold, J., Samtleben, C., Munnecke, A., 1997. Paleoenvironmental changes in the Silurian indicated by stable isotopes in brachiopod shells from Gotland, Sweden. Geochimica et Cosmochimica Acta 61: 2717–2739.

    Google Scholar 

  • Bickert, T., Mackensen, A., 2003. Last Glacial to Holocene changes in South Atlantic deep water circulation. In: Wefer, G., Mulitza, S., Rathmeyer, V., (eds), The South Atlantic during the Late Quaternary. Springer, Berlin, pp. 671–695.

    Google Scholar 

  • Bickert, T., Wefer, G., 1999. South Atlantic and benthic foraminifer δ13C-deviations: Implications for reconstructing the Late Quaternary deep-water circulation. Deep-Sea Research, 46: 437–452.

    Google Scholar 

  • Bidigare, R.R., Fluegge, A., Freeman, K.H., Hanson, K.L., Hayes, J.M., Hollander, D., Jasper, J., King, L.L., Laws, E.A., Milder, J., Millero, F.J., Pancost, R., Popp, B.N., Steinberg, P.A., Wakeham, S.G., 1997. Consistent fractionation of 13C in nature and in the laboratory: Growth rate effects in some haptophyte algae. Global Biogeochem Cycles 11: 279–292.

    Google Scholar 

  • Birchfield, G.E., 1987. Changes in deep-ocean water δ18O and temperature from last glacial maximum to the present. Paleoceanography 2: 431–442.

    Google Scholar 

  • Bolliger, C., Schroth, M.H., Bernasconi, S.M., Kleikemper, J., and Zeyer, J., 2001. Sulfur isotope fractionation during microbial sulfate reduction by toluene-degrading bacteria. Geochimica et Cosmochimica Acta 65: 3289–3298.

    Google Scholar 

  • Broecker, W.S., 1982. Ocean chemistry during glacial time. Geochimica et Cosmochimica Acta 46: 1689–1705.

    Google Scholar 

  • Broecker, W.S., Maier-Reimer, E., 1992. The influence of air and sea exchange on the carbon isotope distribution in the sea. Global Biogeochemical Cycles 6: 315–320.

    Google Scholar 

  • Burkhardt, S., Riebesell, U., Zondervan, I., 1999. Stable carbon isotope fractionation by marine phytoplankton in response to daylength, growth rate, and CO2 availability. Marine Ecology Progress Series 184: 31–41.

    Google Scholar 

  • Canfield, D.E., 2001. Biogeochemistry of sulfur isotopes. Reviews in Mineralogy and Geochemistry 43: 607–636.

    Google Scholar 

  • Carpenter, S.J., Lohmann, K.C., Holden, P., Walter, L.M., Huston, T.J., Halliday, A.N., 1991. δ18O values, 87Sr/86Sr and Sr/Mg ratios of Late Devonian abiotic marine calcite: Implications for the composition of ancient seawater. Geochimica et Cosmochimica Acta 55: 1991–2010.

    Google Scholar 

  • Charles, C.D., Fairbanks, R.G., 1990. Glacial to interglacial changes in the isotopic gradients of the Southern Ocean surface water. In: Bleil, U., Thiede, J., (eds), Geological history of the Polar Oceans: Artic versus Antarctic. Kluwer, Dordrecht, pp 519–538.

    Google Scholar 

  • Cifuentes, L.A., Sharp, J.H., Fogel, M.L., 1988. Stable carbon and nitrogen isotope biogeochemistry in the Delaware estuary. Limnology and Oceanography 33: 1102–1115.

    Google Scholar 

  • Claypool, G.E., Holser, W.T., Kaplan, I.R., Sakai, H., Zak, I., 1980. The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation. Chemical Geology 28: 190–260.

    Google Scholar 

  • Cline, J.D., Kaplan, I.R., 1975. Isotopic fractionation of dissolved nitrate during denitrification in the easter tropical North Pacific Ocean. Marine Chemistry 3: 271–299.

    Google Scholar 

  • Coplen, T.B., 1996. More uncertainty than necessary. Paleoceanography 11: 369–370.

    Google Scholar 

  • Craig, H., Gordon, L.I., 1965. Deuterium and oxygen-18 variations in the ocean and marine atmosphere. In: Tongiorgi, E., (eds), Stable isotopes in oceanic studies and paleotemperatures. Consiglio Nazionale Delle Ricerche, Laboratorio di Geologia Nucleare, Pisa, pp 9–130.

    Google Scholar 

  • Curry, W.B., Oppo, D.W., 2005. Glacial water mass geometry and the distribution of δ13C of ΣCO2 in the western Atlantic Ocean. Paleoceanography 20: PA1017.

    Google Scholar 

  • de Lange, G.J., van Os, B., Pruysers, P.A., Middelburg, J.J., Castradori, D., van Santvoort, P., Müller, P.J., Eggenkamp, H., Prahl, F.G., 1994. Possible early diagenetic alteration of palaeo proxies. In: Zahn, R., Pedersen, T.F., Kaminski, M.A., Labeyrie, L., (eds), Carbon cycling in the glacial ocean: Constraints on the ocean’s role in global climate. Springer, Berlin, pp 225–258.

    Google Scholar 

  • Degens, E.T., 1969. Biogeochemistry of stable carbon isotopes. In: Eglington, G., Murphy, M.T.J., (eds), Organic geochemistry. Methods and results. Springer, Berlin, pp 304–329.

    Google Scholar 

  • Degens, E.T., Guillard, R.R.L., Sackett, W.M., Hellebust, J.A., 1968. Metabolic fractionation of carbon isotopes in marine plankton. I. Temperature and respiration experiments. Deep Sea Research 15: 1–9.

    Google Scholar 

  • Deines, P., 1981. The isotopic composition of reduced organic carbon. In: Fritz, P., Fontes, J.C., (eds), Handbook of environmental geochemistry, vol. 1., Elsevier, New York, pp 239–406.

    Google Scholar 

  • Derry, L.A., France-Lanord, C., 1996. Neogene growth of the sedimentary organic carbon. Paleoceanography 11: 267–276.

    Google Scholar 

  • Emrich, K., Ehhalt, D.H., Vogel, J.C., 1970. Carbon isotope fractionation during the precipitation of calcium carbonate. Earth and Planetary Science Letters 8: 363–371.

    Google Scholar 

  • Epstein, S., Buchsbaum, R., Lowenstam, H.A., Urey, H.C., 1953. Revised carbonate-water isotopic temperature scale. Bull Geol Soc Am 64: 1315–1325.

    Google Scholar 

  • Erez, J., Luz, B., 1983. Experimental paleotemperature equation for planktonic foraminifera. Geochimica et Cosmochimica Acta 47: 1025–1031.

    Google Scholar 

  • Fairbanks, R.G., 1989. A 17,000-year glacio-eustatic sea level record: Influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature 342: 637–642.

    Google Scholar 

  • Fairbanks, R.G., Charles, C.D., Wright, J.D., 1992. Origin of global meltwater pulses. In: Taylor, R.E., (eds), Radiocarbon after four decades. Springer, New York, pp 473–500.

    Google Scholar 

  • Faure, G., Mensing, T.M., 2005. Isotopes: Principles and applications, 3rd edition. John Wiley & Sons, New York, 928 pp.

    Google Scholar 

  • Fontugne, M.R., Calvert, S.E., 1992. Late Pleistocene variability of the carbon isotopic composition of organic matter in the eastern Mediterranean: Monitor of changes in carbon sources and atmospheric CO2 concentrations. Paleoceanography 7: 1–20.

    Google Scholar 

  • Francois, R., Altabet, M.A., Burckle, L.H., 1992. Glacial to interglacial changes in surface nitrate utilization in the Indian sector of the Southern Ocean as recorded by sediment δ15N. Paleoceanography 7: 589–606.

    Google Scholar 

  • Freudenthal, T., Neuer, S., Meggers, H., Davenport, R., Wefer, G., 2001. Influence of lateral particle advection and organic matter degradation on sediment accumulation and stable nitrogen isotope ratios along a productivity gradient in the Canary Islands region. Marine Geology, 177: 93–109.

    Google Scholar 

  • Fry, B., Jannasch, H.W., Molyneaux, S.J., Wirsen, C.O., Muramato, Ja., King, S., 1991. Stable isotopes of the carbon, nitrogen and sulfur cycles in the Black Sea and the Cariaco Trench. Deep-Sea Research 38,Suppl. 2: S1003–S1019.

    Google Scholar 

  • Gruber, N., Sarmiento, J.L., 1997. Global patterns of marine nitrogen fixation and denitrification. Global Biogeochem Cycles 11: 235–266.

    Google Scholar 

  • Habicht, K.S., Canfield, D.E., 1997. Sulfur isotope fractionation during bacterial sulfate reduction in organic-rich sediments. Geochimica et Cosmochimica Acta 61: 5351–5361.

    Google Scholar 

  • Hartmann, M., Nielsen, H., 1969. 34S Werte in rezenten Meeressedimenten und ihre Deutung am Beispiel einiger Sedimentprofile aus der westlichen Ostsee. Geologische Rundschau 58: 621–655.

    Google Scholar 

  • Hayes, J.M., 1993. Factors controlling the 13C contents of sedimentary organic compounds: principals and evidence. Marine Geology 113: 111–125.

    Google Scholar 

  • Hayes, J.M., Freeman, K.H., Popp, B.N., Hoham, C.H., 1990. Compound-specific analyses, a novel tool for reconstruction of ancient biogeochemical processes. Organic Geochemistry 16: 1115–1128.

    Google Scholar 

  • Hemming, N.G., Hanson, G.N., 1992. Boron isotopic composition and concentration in modern marine carbonates. Geochimica et Cosmochimica Acta 56: 537–543.

    Google Scholar 

  • Hemming, N.G., Hanson, G.N. 1994. A procedure for the isotopic analysis of boron by negative thermal ionization mass spectrometry. Chemical Geology 114: 147–156.

    Google Scholar 

  • Hemming, N.G., Reeder, R.J., Hanson, G.N., 1995. Mineral-fluid partitioning and isotopic fractionation of boron in synthetic calcium carbonate, Geochimica et Cosmochimica Acta 59: 371–379.

    Google Scholar 

  • Hoefs, J., 2004. Stable isotope geochemistry. 5th ed. Springer, Berlin, 244 pp.

    Google Scholar 

  • Holland, H.D., 1978. The chemistry of the atmosphere and oceans. Wiley, New York, 351 pp

    Google Scholar 

  • Holmes, M.E., Müller, P.J., Schneider, R.R., Segl, M., Wefer, G., 1997. Reconstruction of past nutrient utilization in the eastern Angola Basin based on sedimentary 15N/14N ratios. Paleoceanography 12: 604–614.

    Google Scholar 

  • Holser, W.T., 1997. Geochemical events documented in inorganic carbon isotopes. Palaeogeography, Palaeoclimatology, Palaeoecology 132: 173–182.

    Google Scholar 

  • Hönisch, B., Bijma, J., Russell, A.D., Spero, H.J., Palmer, M.R., Zeebe, R.E., Eisenhauer, A., 2003. The influence of symbiont photosynthesis on the boron isotopic composition of foraminifera shells. Mar. Micropaleontol. 49: 87–96.

    Google Scholar 

  • Hönisch B, Hemming NG (2004) Ground-truthing the boron isotope paleo-pH proxy in planktonic foraminifera shells: Partial dissolution and shell size effects. Paleoceanography 19: PA4010.

    Google Scholar 

  • Hönisch, B., Hemming, N.G., Grottoli, A.G., Amat, A., Hanson, G.N., Bijma, J., 2004. Assessing scleractinian corals as recorders for paleo-pH: Empirical calibration and vital effects. Geochimica et Cosmochimica Acta 68: 3675–3685.

    Google Scholar 

  • Irwin, H., Curtis, C., Coleman, M., 1977. Isotopic evidence for source of diagenetic carbonates formed during burial of organic-rich sediments. Nature 269: 209–213.

    Google Scholar 

  • Jacobs, S.S., Fairbanks, R.G., Horibe, Y., 1985. Origin and evolution of water masses near the antarctic continental margin: Evidence from H218O/H216O ratios in seawater. Antarctic Research Series 43: 59–85.

    Google Scholar 

  • Jasper, J.P., Hayes, J.M., 1990. A carbon isotope record of CO2 levels during the late Quaternary. Nature 347: 462–464.

    Google Scholar 

  • Jasper, J.P., Hayes, J.M., 1994. Reconstruction of Paleoceanic PCO2 levels from carbon isotopic compositions of sedimentary biogenic components. In: Zahn, R., Pedersen, T.F., Kaminski, M.A., Labeyrie, L., (eds), Carbon cycling in the glacial ocean: Constraints on the ocean’s role in global climate. Springer, Berlin, pp 323–342.

    Google Scholar 

  • Jørgensen, B.B., 1979. A theoretical model of the stable sulfur isotope distribution in marine sediments. Geochimica et Cosmochimica Acta 43: 363–374.

    Google Scholar 

  • Jørgensen, B.B., 1990. A thiosulfate shunt in the sulfur cycle of marine sediments. Science 249: 152–154.

    Google Scholar 

  • Jørgensen, B.B., Erez, J., Revsbech, N.P., Cohen, Y., 1985. Symbiontic photosynthesis in a planktonic foraminifera, Globigerinoides sacculifer (Brady), studied with microelectrodes. Limnol Oceanogr 30: 1253–1267.

    Google Scholar 

  • Jørgensen, B.B., Böttcher, M.E., Lüschen, H., Neretin, L.N., Volkov, I.I., 2004. Anaerobic methane oxidation and a deep H2S sink generate isotopically heavy sulfides in Black Sea sediments. Geochimica et Cosmochimica Acta 68: 2095–2118.

    Google Scholar 

  • Kakihana, H., Kotaka, M., Satoh, S., Nomura, M., Okamoto, M., 1977. Fundamental studies on the ion-exchange of boron isotopes. Bull. Chem. Soc. Japan 50: 158–163.

    Google Scholar 

  • Kaplan, I.R., Rittenberg, S.C., 1964. Microbiological fractionation of sulfur isotopes. J Gen Microbiol 34: 195–212.

    Google Scholar 

  • King, A.L., Howard, W.R., 2004. Planktonic foraminiferal δ13C records from Southern Ocean sediment traps: New estimates of the oceanic Suess effect. Global Biogeochemical Cycles 18, GB2007.

    Google Scholar 

  • Kroopnick, P., 1985. The distribution of 13C of ΣCO2 in the world oceans. Deep-Sea Research 32: 57–84.

    Google Scholar 

  • Kuypers, M.M.M., Lavik, G., Woebken, D., Schmid, M., Fuchs, B.M., Amann, R., Jørgensen B.B., Jetten, M.S.M., 2005. Massive nitrogen loss from the Benguela upwelling system through anaerobic ammonium oxidation. Proceedings of the National Academy of Science 102: 6478–6483.

    Google Scholar 

  • Kuypers, M.M.M., Sliekers, A.O., Lavik, G., Schmid, M., Jørgensen, B.B. Kuenen, J.G., Sinninghe Damsté, J.S., Strous, M., Jetten, M.S.M, 2003. Anaerobic ammonium oxidation by anammox bacteria in the Black Sea. Nature 422: 608–611.

    Google Scholar 

  • Kyser, T.K., 1995. Micro-analytical techniques in stable isotope geochemistry. Can Mineral 33: 261–278.

    Google Scholar 

  • Lawrence, J.R., 1989. The stable isotope geochemistry of deep-sea pore water. In: Fritz, P., Fontes, J.C., (eds), Handbook of environmental isotope geochemistry, vol. 3. Elsevier, Amsterdam, pp 317–356.

    Google Scholar 

  • Laws, E.A., Popp, B.N., Bidigare, R.R., Kennicutt, M.C., Macko, S.A., 1995. Dependence of phytoplankton carbon isotopic composition on growth rate and (CO2)aq: Theoretical considerations and experimental results. Geochimica et Cosmochimica Acta 59: 1131–1138.

    Google Scholar 

  • Lecuyer, C., Grandjean, P., Reynard, B., Albarede, F., Telouk, P., 2002. 11B/10B analysis of geological materials by ICP-MS PLasma 54: application to boron fractionation between brachiopod calcite and seawater. Chem Geol 186: 45–55.

    Google Scholar 

  • Lemarchand, D., Gaillardet, J., Lewin, E., Allègre, C., 2000. The influence of rivers on marine boron isotopes and implications for reconstructing past ocean pH. Nature 408: 951–954.

    Google Scholar 

  • Liu, K.K., Kaplan, I.R., 1989. The eastern tropical Pacific as a source of 15N-enriched nitrate in seawater off southern California. Limnol Oceanography 34: 820–830.

    Google Scholar 

  • Longinelli, A., 1989. Oxygen-18 and sulphur-34 in dissolved oceanic sulphate and phosphate. In: Fritz, P., Fontes, J.C., (eds), Handbook of environmental isotope geochemistry, vol. 3. Elsevier, Amsterdam, pp 219–255.

    Google Scholar 

  • Lynch-Stieglitz. J., Stocker, T.F., Broecker, W.S., Fairbanks, R.G., 1995. The influence of air-sea exchange on the isotopic composition of oceanic carbon: observations and modeling. Global Biogeochemical Cycles 9: 653–665.

    Google Scholar 

  • Lyons, T.W., Berner, R.A., 1992. Carbon-sulfur-iron systematics of the uppermost deep-water sediments of the Black Sea. Chemical Geology 99: 1–27.

    Google Scholar 

  • Mackensen, A., 2001. Oxygen and carbon stable isotope tracers of Weddell Sea water masses: New data and some paleoceanographic implications. Deep-Sea Research 48: 1401–1422.

    Google Scholar 

  • Mackensen, A., Hubberten, H.W., Bickert, T., Fischer, G., Fütterer, D.K. 1993. δ13C in benthic foraminiferal tests of Fontbotia wuellerstorfi (SCHWAGER) relative to δ13C of dissolved inorganic carbon in Southern Ocean deep water: implications for glacial ocean circulation models. Paleoceanography 8: 587–610.

    Google Scholar 

  • Mackensen, A., Hubberten, H.W., Scheele, N., Schlitzer, R., 1996. Decoupling of δ13CΣCO2 and phosphate in recent Weddell Sea Deep and Bottom Water: Implications for glacial Southern Ocean paleoceanography. Paleoceanography 11: 203–215.

    Google Scholar 

  • Matsumoto, R., 1992. Causes of the oxygen isotopic depletion of interstitial waters from sites 798 and 799, Japan Sea, Leg 128. Proc ODP, Sci Res 127/128: 697–703.

    Google Scholar 

  • McConnaughey, T.A., Burdett, J., Whelan, J.F., Paull, C.K., 1997. Carbon isotopes in biological carbonates: Respiration and photosynthesis. Geochimica et Cosmochimica Acta 61: 611–622.

    Google Scholar 

  • McCorkle, D.C., Corliss, B.H., Farnham, C.A., 1997. Vertical distributions and stable isotopic compositions of live (stained) benthic foraminifera from the North Carolina and California continental margins. Deep-Sea Research 44: 983–1024.

    Google Scholar 

  • McCorkle, D.C., Emerson, S.R., 1988. The relationship between pore water carbon isotopic composition and bottom water oxygen concentration. Geochimica et Cosmochimica Acta 52: 1169–1178.

    Google Scholar 

  • McCorkle, D.C., Emerson, S.R., Quay, P.D., 1985. Stable carbon isotopes in marine porewaters. Earth and Planetary Science Letters 74: 13–26.

    Google Scholar 

  • McCorkle, D.C., Keigwin, L.D., Corliss, B.H., Emerson, S.R., 1990. The influence of microhabitats on the carbon isotopic composition of deep-sea benthic foraminifera. Paleoceanography 5: 161–185.

    Google Scholar 

  • McCorkle, D.C., Martin, P.A., Lea D.W., Klinkhammer, G.P., 1995. Evidence of a dissolution effect on benthic foraminiferal shell chemistry: δ13C, Cd/Ca, Ba/Ca, and Sr/Ca results from the Ontong Java Plateau. Paleoceanography 10: 699–714.

    Google Scholar 

  • Merrit, D.A., Hayes, J.M., 1994. Factors controlling precision and accuracy in isotope-ratio-monitoring mass spectrometry. Anal Chem 66: 2336–2347.

    Google Scholar 

  • Miyake, Y., Wada, E., 1971. The isotope effect on the nitrogen in biochemical oxidation-reduction reactions. Rec Oceanogr Works Japan 11: 1–6.

    Google Scholar 

  • Montoya, J.P., 1994. Nitrogen fractionation in the modern ocean: Implications for the sedimentary record. In: Zahn, R., Pedersen, T.F., Kaminski, M.A., Labeyrie, L., (eds), Carbon cycling in the glacial ocean: Constraints on the ocean’s role in global change. Springer, Berlin, pp 259–279.

    Google Scholar 

  • Mook, W.G., Bommerson, J.C., Staverman, W.H., 1974. Carbon isotope fractionation between dissolved bicarbonate and gaseous carbon dioxide. Earth and Planetary Science Letters 22: 169–176.

    Google Scholar 

  • Mulitza, S., Donner, B., Fischer, G., Paul, A., Pätzold, J., Rühlemann, C. Segl, M., 2003. The South Atlantic oxygen isotope record of planktic foraminifera. In: The South Atlantic in the Late Quaternary: Reconstruction of Material Budgets and Current Systems. Wefer, G., Mulitza, S., and Ratmeyer, V., editors. Springer, Berlin, pp. 121–142.

    Google Scholar 

  • Müller, P.J., Schneider, R., Ruhland, G., 1994. Late Quaternary pCO2 variations in the Angola Current: Evidence from organic carbon δ13C and alkenone temperatures. In: Zahn, R., Pedersen, T.F., Kaminski, M.A., Labeyrie, L., (eds), Carbon cycling in the glacial ocean: Constraints on the ocean’s role in global change. Springer, Berlin, pp 343–366.

    Google Scholar 

  • Newman, J.W., Parker, P.L., Behrens, E.W., 1973. Organic carbon ratios in Quaternary cores from the Gulf of Mexico. Geochimica et Cosmochimica Acta 37: 225–238.

    Google Scholar 

  • Nielsen, H., Ricke, W., 1964. Schwefel-Isotopen-Verhältnisse von Evaporiten aus Deutschland: ein Beitrag zur Kenntnis von 34S im Meerwasser-Sulfat. Geochimica et Cosmochimica Acta 28: 577–591.

    Google Scholar 

  • Nissenbaum, A., Presley, B.J., Kaplan, I.R., 1972. Early diagenesis in a reducing fjord, Saanich Inlet, British Columbia-I. Chemical and isotopic changes in major components of interstitial water. Geochimica et Cosmochimica Acta 36: 1007–1027.

    Google Scholar 

  • Ohmoto, H., Kaiser, C.J., Geer, K.A., 1990. Systematics of sulphur isotopes in recent marine sediments and ancient sediment-hosted basemetal deposits. Univ Western Australia Publ 23: 70–120.

    Google Scholar 

  • O’Leary, M.H., 1981. Carbon isotope fractionation in plants. Phytochemistry 20: 553–567.

    Google Scholar 

  • Palmer, M.R., Pearson, P.N., 2003. A 23,000-year record of surface water pH and PCO2 in the Western Equatorial Pacific Ocean. Science 300: 480–482.

    Google Scholar 

  • Park, R., Epstein, S., 1960. Carbon isotope fractionation during photosynthesis. Geochimica et Cosmochimica Acta 21: 110–126.

    Google Scholar 

  • Pearson, P.N., Palmer, M.R., 2000. Atmospheric carbon dioxide concentrations over the past 60 million years. Nature 406: 695–699.

    Google Scholar 

  • Pearson, P.N., Ditchfield, P.W., Singano, J., Harcourt-Brown, K.G., Nicholas, C.J., Olsson, R.K., Shackleton, N.J. and Hall, M.A., 2001. Warm tropical sea surface temperatures in the Late Cretaceous and Eocene epochs. Nature 413: 481–487.

    Google Scholar 

  • Popp, B.N., Anderson, T.F., Sandberg, P.A., 1986. Brachiopods as indicators of original isotopic compositions in some Paleozoic limestones. Geological Society America Bulletin 97: 1262–1269.

    Google Scholar 

  • Popp, B.N., Laws, E.A., Bidigare, R.R., Dore, J.E., Hanson, K.L., Wakeham, S.G., 1998. Effect of phytoplankton cell geometry on carbon isotopic fractionation. Geochimica et Cosmochimica Acta 62: 69–77.

    Google Scholar 

  • Popp, B.N., Parekh, P., Tilbrook, B., Bidigare, R.R., Laws, E.A., 1997. Organic carbon δ13C variations in sedimentary rocks as chemostratigraphic and paleoenvironmental tools. Palaeogeography, Palaeoclimatology, Palaeoecology 132: 119–132.

    Google Scholar 

  • Popp, B.N., Tagiku, R., Hayes, J.M., Louda, J.W., Baker, E.W., 1989. The post-paleozoic chronology and mechanism of δ13C depletion in primary marine organic matter. American Journal of Sciences 289: 436–454.

    Google Scholar 

  • Raab, M., Spiro, B., 1991. Sulfur isotopic variations during seawater evaporation with fractional crystallization. Chemical Geology 86: 323–333.

    Google Scholar 

  • Railsback, L.B., 1990. Influence of changing deep ocean circulation on the Phanerozoic oxygen isotopic record. Geochimica et Cosmochimica Acta 54: 1501–1509.

    Google Scholar 

  • Raiswell, R., 1997. A geochemical framework for the application of stable sulphur isotopes to fossil pyritization. Journal of the Geological Society, London 154: 343–356.

    Google Scholar 

  • Raiswell, R., Berner, R.A., 1985. Pyrite formation in euxinic and semi-euxinic sediments. American Journal of Sciences 285: 710–724.

    Google Scholar 

  • Raiswell, R., Berner, R.A., 1986. Pyrite and organic matter in Phanerozoic normal marine shales. Geochimica et Cosmochimica Acta 50: 1967–1976.

    Google Scholar 

  • Rau, G.H., Froehlich, P.N., Takahashi, T., Des Marais, D.J., 1991. Does sedimentary organic δ13C record variations in Quaternary ocean [CO2(aq)]? Paleoceanography 6: 335–347.

    Google Scholar 

  • Rau, G.H., Riebesell, U., Wolf-Gladrow, D., 1997. CO2aq-dependent photosynthetic 13C fractionation in the ocean: A model versus measurements. Global Biogeochemical Cycles 11: 267–278.

    Google Scholar 

  • Reynaud, S., Hemming, N.G., Juillet-Leclerc. A., Gattuso. J.P., 2004. Effect of pCO2 and temperature on the boron isotopic composition of a zooxanthellate coral: Acropora sp. Coral Reefs 23: 539–546.

    Google Scholar 

  • Rink, S., Kühl, M., Bijma, J., and Spero, H. J., 1998. Microsensor studies of photosynthesis and respiration in the symbiontic foraminifer O. universa.. Marine Biology, 131: 583–596.

    Google Scholar 

  • Rost, B., Zondervan, I., Riebesell, U., 2002. Lightdependent carbon isotope fractionation in the coccolithophorid Emiliania huxleyi. Limnol. Oceanogr. 47: 120–128.

    Google Scholar 

  • Rühlemann, C., Frank, M., Hale, W., Mangini, A., Mulitza, S., Müller, P.J., Wefer, G., 1996. Late Quaternary productivity changes in the western equatorial Atlantic: Evidence from 230Th-normalized carbonate and organic carbon accumulation rates. Marine Geology 135: 127–152.

    Google Scholar 

  • Sanyal, A., and Bijma, J., 1999. A comparative study of northwest Africa and eastern equatorial Pacific upwelling zones as sources of CO2 during glacial periods based on boron isotope paleo-pH estimation, Paleoceanography 14: 753–759.

    Google Scholar 

  • Sanyal, A., Hemming, N.G., Broecker, W.S., Lea, D.W., Spero, H.J., Hanson, G.N., 1996. Oceanic pH control on the boron isotopic composition of foraminifera: Evidence from culture experiments. Paleoceanography 11: 513–517.

    Google Scholar 

  • Sanyal, A., Nugent, M., Reeder, R.J., Bijma, J., 2000. Seawater pH control on the boron isotopic composition of calcite: Evidence from inorganic calcite precipitation experiments. Geochim. Cosmochim. Acta. 64: 1551–1555.

    Google Scholar 

  • Sanyal, A., Bijma, J., Spero, H.J., Lea, D.W., 2001. Empirical relationship between pH and the boron isotopic composition of G. sacculifer: Implications for the boron isotope paleo-pH proxy. Paleoceanography 16: 515–519.

    Google Scholar 

  • Sanyal, A., Hemming, N.G., Hanson, G.N., Broecker, W.S., 1995. Evidence for a higher pH in the glacial ocean from boron isotopes in foraminifera. Nature 373: 234–236.

    Google Scholar 

  • Sarnthein, M., Winn, K., Jung, S.J.A., Duplessy, J.C., Labeyrie, L., Erlenkeuser, H., Ganssen G., 1994. Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography 9: 209–268.

    Google Scholar 

  • Schmidt, G.A., Bigg, G.R., and Rohling, E.J., 1999. Global seawater oxygen-18 database. http://data.giss.nasa.gov/o18data/.

    Google Scholar 

  • Schneider, R., Dahmke, A., Kölling, A., Müller, P.J., Schulz, H.D., Wefer, G., 1992. Strong deglacial minimum in the δ13C 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.

    Google Scholar 

  • Schrag, D.P., and DePaolo, D.J., 1993. Determination of δ18O of seawater in the deep ocean during the last glacial maximum: Paleoceanography, 8: 1–6.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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 CO2(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.

    Google Scholar 

  • 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 CO2 in the oceans. Plenum, New York, pp 401–427.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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.

    Google Scholar 

  • Spero, H.J., 1992. Do planktonic foraminifera accurately record shifts in the carbon isotopic composition of δCO2? Marine Micropaleontology 19: 275–285.

    Google Scholar 

  • 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.

    Google Scholar 

  • Spero, H.J., Lea, D.W., 1993. Intraspecific stable isotope variability in the planktic foraminifera Globigerinoides sacculifer: Results from laboratory experiments. Marine Micropaleontology 22: 221–234.

    Google Scholar 

  • 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.

    Google Scholar 

  • Strauss, H., 1997. The isotopic composition of sedimentary sulfur through time. Palaeogeography, Palaeoclimatology, Palaeoecology 132: 97–118.

    Google Scholar 

  • Sweeney, R.E., Kaplan, I.R., 1980. Natural abundances of 15N as a source indicator for near-shore marine sedimentary and dissolved nitrogen. Marine Chemistry 9: 81–94.

    Google Scholar 

  • 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 9–26.

    Google Scholar 

  • 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.

    Google Scholar 

  • 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. 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater. Chemical Geology 161, 59–88. With data update 2004: http://www.science.uottawa.ca/geology/isotope_data/.

    Google Scholar 

  • 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: 159–172.

    Google Scholar 

  • Vinogradov, A.P., Grinenko, V.A., Ustinov, V.I., 1962. Isotopic composition of sulfur compounds in the Black Sea. Geokhimiya 10: 973–997.

    Google Scholar 

  • Voss, M., Altabet, M.A., von Bodungen, B., 1996. δ15N in sedimenting particles as indicator of euphoticzone processes. Deep-Sea Research 43: 33–47.

    Google Scholar 

  • Wada, E., Hattori, A., 1978. Nitrogen assimilation effects in the assimilation of inorganic nitrogenous compounds by marine diatoms. Geomicrobiol J 1: 85–101.

    Google Scholar 

  • 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.

    Google Scholar 

  • Waelbroeck, C., Mulitza, S., Spero, H., Dokken, T., Kiefer, T., Cortijo, E., 2004. A global compilation of Holocene planktonic foraminiferal δ18O: relationship between surface water temperature and δ18O, Quaternary Science Reviews 24: 853–868.

    Google Scholar 

  • Wallmann, K., 2001. The geological water cycle and the evolution of marine δ18O values. Geochimica et Cosmochimica Acta 65: 2469–2485.

    Google Scholar 

  • Wefer, G., Berger, W.H., 1991. Isotope paleontology: growth and composition of extant calcareous species. Marine Geology 100: 207–248.

    Google Scholar 

  • Wefer, G., Heinze, P.M., Berger, W.H., 1994. Clues to ancient methane release. Nature, 369: 282.

    Google Scholar 

  • Weiss, R.F., 1974. Carbon dioxide in water and seawater: The solubility of a non-ideal gas. Marine Chemistry 2: 203–215.

    Google Scholar 

  • Weiss, R.F., Östlund, H.G., Craig, H., 1979. Geochemical studies of the Weddell Sea. Deep-Sea Research 26: 1093–1120.

    Google Scholar 

  • Williams, L.B., Ferell, R.E., Hutcheon, I., Bakel, A.J., Walsh, M.M., Krouse, H.R., 1995. Nitrogen isotope geochemsitry of organic matter and minerals during diagenesis and hydrocarbon migration. Geochimica et Cosmochimica Acta 59: 765–779.

    Google Scholar 

  • Wu, G., Berger, W.H., 1989. Planktonic foraminifera: differential dissolution and the Quaternary stable isotope record in the west Equatorial Pacific. Paleoceanography 4: 181–198.

    Google Scholar 

  • Zahn, R., Keir, R., 1994. Tracer-nutrient correlations in the upper ocean: observational and box model constraints on the use of benthic foraminiferal δ13C and Cd/Ca as paleo-proxies for the intermediatedepth ocean. In: Zahn, R., Pedersen, T.F., Kaminski, M.A., Labeyrie, L., (eds), Carbon cycling in the glacial ocean: Constraints on the ocean’s role in global change. Springer, Berlin, pp 195–223.

    Google Scholar 

  • Zahn, R., Mix, A.C., 1991. Benthic foraminiferal δ18O in the ocean’s temperature-salinity-density field: Constraints on ice age thermohaline circulation. Paleoceanography 6: 1–20.

    Google Scholar 

  • Zeebe, R.E., Wolf-Gladrow, D.A., Bijma, J., Hšnisch, B., 2003. Vital effects in foraminifera do not compromise the use of d11B as a paleo-pH indicator: Evidence from modeling. Paleoceanography 18: PA 1043.

    Google Scholar 

  • Zeebe, R.E., and Sanyal, A., 2002. Comparison of two potential strategies of planktonic foraminifera for house building: Mg2+ or H+ removal? Geochim. Cosmochim. Acta, 66: 1159–1169.

    Google Scholar 

  • Zeebe, R.E., 1999. An explanation of the effect of seawater carbonate concentration on foraminiferal oxygen isotopes. Geochimica et Cosmochimica Acta 63: 2001–2007.

    Google Scholar 

  • Zeebe, R.E., 2001. Seawater pH and isotopic paleotemperatures of Cretaceous oceans. Palaeogeography, Palaeoclimatology, Palaeoecology, 170:49–57.

    Google Scholar 

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  1. Fachbereich Geowissenschaften, Universität Bremen, 28359, Bremen, Germany

    Torsten Bickert

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Bickert, T. (2006). Influence of Geochemical Processes on Stable Isotope Distribution in Marine Sediments. In: Schulz, H.D., Zabel, M. (eds) Marine Geochemistry. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-32144-6_10

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