Implications of a Carbonate Ion Effect on Shell Carbon and Oxygen Isotopes
521
References
Archer D, Maier-Reimer E(1994)Effectof deep-seasedimentary calcite preservation on atmospheric CO 2
concentration. Nature 367: 260-263
Archer D, Winguth A, Lea DW, Mahowald N What
caused the glacial/interglacial atmospheric PCO,
cycles? Reviews of Geophysics, in review
BarnolaJM, Raynaud D, Korotkevich YS, Lorius C (1987)
Vostok ice core provides 160,000-year record of
atmospheric CO 2 • Nature 329: 408-414
Berger WH (1982) Increase of carbon dioxide in the atmosphere during deglaciation: The coral reef hypothesis. Naturwissenschaften 69: 87-88
Berger WH, Killingley JS, Vincent E (1978) Stable isotopes in deep-sea carbonates: Box core ERDC-92,
west equatorial Pacific. Oceanol Acta I: 203-216
Bijma J, Spero HJ, Lea DW (1998) Oceanic carbonate
chemistry and foraminiferal isotopes: new laboratory results. 6th International Conference on
Paleoceanography, Program and Abstracts, 78
Boyle EA (1988) The role of vertical chemical
fractionation in controlling late Quaternary atmospheric carbon dioxide. J Geophys Res 93: 15,
701-15,715
Boyle EA (1992) Cadmium and OBC paleochemical ocean
distributions during the stage 2 glacial maximum.
Annu Rev Earth Planet Sci 20: 245-287
Boyle EA, Keigwin LD (1982) Deep circulation of the
North Atlantic over the last 200,000 years:
Geochemical evidence. Science 218: 784-787
Boyle EA, Keigwin LD (1985/1986) Comparison of
Atlantic and Pacific paleochemical records for the
last 215,000 years: changes in deep ocean circulation and chemical inventories. Earth Planet Sci
Lett76: 135-150
Broecker WS (1982a) Glacial to interglacial changes in
ocean chemistry. Progr Oceanogr 11: 151-197
Broecker WS (1982b) Ocean chemistry during glacial
time. Geochim Cosmochim Acta 46: 1689-1705
Broecker WS (1986) Oxygen isotope constraints on
surface ocean temperatures. Quat Res 26: 121-134
Broecker WS, Henderson GM (1998) The sequence of
events surrounding Termination II and their implications for the cause of glacial-interglacial CO,
changes. Paleoceanography 13: 352-364
Broecker WS, Peng T-H (1993) What caused the glacial
to interglacial CO 2 change? In: Heimann M (ed) The
Global Carbon Cycle. Springer, Berlin Heidelberg New
York,pp95-115
Charles CD, Fairbanks RG (1990) Glacial to interglacial
changes in the isotopic gradients of Southern Ocean
surface water. In: Bleil U, Thiede J (eds) Geological History of the Polar Oceans: Arctic versus
Antarctic. Kluwer, Dordrecht, pp 519-538
Charles CD, Wright ID, Fairbanks RG (1993) Thermodynamic influences on the marine carbon isotope
record. Paleoceanography 8: 691-697
Charles CD, Lynch-StieglitzJ, Ninnemann U, Fairbanks
R (1996) Climate connections between the hemisphere revealed by deep sea sediment core ice core
correlations. Earth Planet Sci Lett 142: 19-27
Crowley TJ (1995) Ice age terrestrial carbon changes
revisited. Global Biogeochem Cycles 9: 377-389
Curry WB, Crowley TJ (1987) The Ol3C of equatorial
Atlantic surface waters: implications for ice age pC0 2
levels. Paleoceanography 2: 489-517
Curry WB, Lohmann GP (1982) Carbon isotopic changes
in benthic foraminifera from the Western South
Atlantic: reconstruction of glacial Abyssal circulation patterns. Quat Res 18: 218-235
Curry WB, Duplessy J-C, Labeyrie LD, Shackleton NJ
(1988) Changes in the distribution of Ol3C of deep
water EC0 2 between the last glaciation and the
Holocene. Paleoceanography 3: 317-342
Duplessy J-C, Shackleton NJ, Fairbanks RG, Labeyrie
L, Oppo D, Kallel N (1988) Deepwater source
variations during the last climatic cycle and their
impact on the global deepwater circulation.
Paleoceanography 3: 343-360
Duplessy J-C, Labeyrie L, Juillet-Leclerc A, Maitre F,
DupratJ, Sarnthein M (1991) Surface salinity reconstruction of the North Atlantic Ocean during the last
glacial maximum. OceanolActa 14: 311-324
Fairbanks RG (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
Guilderson TP, Fairbanks RG, Rubenstone JL (1994)
Tropical temperature variations since 20,000 years
ago: Modulating interhemispheric climate changes.
Science 263: 663-665
Jouzel J, Barkov NI, Barnola JM, Bender M, Chappeilaz
J, Genthon C, Kotlyakov VM, Lipenkov V, Lorius C,
Petit JR, Raynaud D, Raisbeck G, Ritz C, Sowers T,
Stievenard M, Yiou F, Yiou P (1993) Extending the
Vostok ice-core record of palaeoclimate to the penultimate glacial period. Nature 364: 407-412
Labeyrie LD, Duplessy JC (1985) Changes in the oceanic l3CJI'C ratio during the last 140 000 years: high
latitude surface water records. Palaeogeogr
Palaeoclimatol Palaeoecol5 0: 217-240
521
References
Archer D, Maier-Reimer E(1994)Effectof deep-seasedimentary calcite preservation on atmospheric CO 2
concentration. Nature 367: 260-263
Archer D, Winguth A, Lea DW, Mahowald N What
caused the glacial/interglacial atmospheric PCO,
cycles? Reviews of Geophysics, in review
BarnolaJM, Raynaud D, Korotkevich YS, Lorius C (1987)
Vostok ice core provides 160,000-year record of
atmospheric CO 2 • Nature 329: 408-414
Berger WH (1982) Increase of carbon dioxide in the atmosphere during deglaciation: The coral reef hypothesis. Naturwissenschaften 69: 87-88
Berger WH, Killingley JS, Vincent E (1978) Stable isotopes in deep-sea carbonates: Box core ERDC-92,
west equatorial Pacific. Oceanol Acta I: 203-216
Bijma J, Spero HJ, Lea DW (1998) Oceanic carbonate
chemistry and foraminiferal isotopes: new laboratory results. 6th International Conference on
Paleoceanography, Program and Abstracts, 78
Boyle EA (1988) The role of vertical chemical
fractionation in controlling late Quaternary atmospheric carbon dioxide. J Geophys Res 93: 15,
701-15,715
Boyle EA (1992) Cadmium and OBC paleochemical ocean
distributions during the stage 2 glacial maximum.
Annu Rev Earth Planet Sci 20: 245-287
Boyle EA, Keigwin LD (1982) Deep circulation of the
North Atlantic over the last 200,000 years:
Geochemical evidence. Science 218: 784-787
Boyle EA, Keigwin LD (1985/1986) Comparison of
Atlantic and Pacific paleochemical records for the
last 215,000 years: changes in deep ocean circulation and chemical inventories. Earth Planet Sci
Lett76: 135-150
Broecker WS (1982a) Glacial to interglacial changes in
ocean chemistry. Progr Oceanogr 11: 151-197
Broecker WS (1982b) Ocean chemistry during glacial
time. Geochim Cosmochim Acta 46: 1689-1705
Broecker WS (1986) Oxygen isotope constraints on
surface ocean temperatures. Quat Res 26: 121-134
Broecker WS, Henderson GM (1998) The sequence of
events surrounding Termination II and their implications for the cause of glacial-interglacial CO,
changes. Paleoceanography 13: 352-364
Broecker WS, Peng T-H (1993) What caused the glacial
to interglacial CO 2 change? In: Heimann M (ed) The
Global Carbon Cycle. Springer, Berlin Heidelberg New
York,pp95-115
Charles CD, Fairbanks RG (1990) Glacial to interglacial
changes in the isotopic gradients of Southern Ocean
surface water. In: Bleil U, Thiede J (eds) Geological History of the Polar Oceans: Arctic versus
Antarctic. Kluwer, Dordrecht, pp 519-538
Charles CD, Wright ID, Fairbanks RG (1993) Thermodynamic influences on the marine carbon isotope
record. Paleoceanography 8: 691-697
Charles CD, Lynch-StieglitzJ, Ninnemann U, Fairbanks
R (1996) Climate connections between the hemisphere revealed by deep sea sediment core ice core
correlations. Earth Planet Sci Lett 142: 19-27
Crowley TJ (1995) Ice age terrestrial carbon changes
revisited. Global Biogeochem Cycles 9: 377-389
Curry WB, Crowley TJ (1987) The Ol3C of equatorial
Atlantic surface waters: implications for ice age pC0 2
levels. Paleoceanography 2: 489-517
Curry WB, Lohmann GP (1982) Carbon isotopic changes
in benthic foraminifera from the Western South
Atlantic: reconstruction of glacial Abyssal circulation patterns. Quat Res 18: 218-235
Curry WB, Duplessy J-C, Labeyrie LD, Shackleton NJ
(1988) Changes in the distribution of Ol3C of deep
water EC0 2 between the last glaciation and the
Holocene. Paleoceanography 3: 317-342
Duplessy J-C, Shackleton NJ, Fairbanks RG, Labeyrie
L, Oppo D, Kallel N (1988) Deepwater source
variations during the last climatic cycle and their
impact on the global deepwater circulation.
Paleoceanography 3: 343-360
Duplessy J-C, Labeyrie L, Juillet-Leclerc A, Maitre F,
DupratJ, Sarnthein M (1991) Surface salinity reconstruction of the North Atlantic Ocean during the last
glacial maximum. OceanolActa 14: 311-324
Fairbanks RG (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
Guilderson TP, Fairbanks RG, Rubenstone JL (1994)
Tropical temperature variations since 20,000 years
ago: Modulating interhemispheric climate changes.
Science 263: 663-665
Jouzel J, Barkov NI, Barnola JM, Bender M, Chappeilaz
J, Genthon C, Kotlyakov VM, Lipenkov V, Lorius C,
Petit JR, Raynaud D, Raisbeck G, Ritz C, Sowers T,
Stievenard M, Yiou F, Yiou P (1993) Extending the
Vostok ice-core record of palaeoclimate to the penultimate glacial period. Nature 364: 407-412
Labeyrie LD, Duplessy JC (1985) Changes in the oceanic l3CJI'C ratio during the last 140 000 years: high
latitude surface water records. Palaeogeogr
Palaeoclimatol Palaeoecol5 0: 217-240