Clues to Ocean History: a Brief Overview of Proxies
45
Paleoceanography 3: 343-360
Duplessy J-C, Labeyrie LD, Juillet-Leclerc A, Maitre F,
Duprat J, Samthein M (1991) Surface salinity reconstruction of the North Altantic Ocean during the last
glaciaimaximum.OceanolActa 14: 311-324
Duplessy J-C, Bard E, Labeyrie L, Duprat J, Moyes J
(1993) Oxygen isotope records and salinity changes
in the northeastern Atlantic Ocean during the last
18,000 years. Paleoceanography 8: 341-350
Duplessy J-C, Labeyrie LD, Paterne M, Hovine S,
Fichefet T, Duprat J, Labracherie M (1996) High latitude deep water sources during the Last Glacial
Maximum and the inensify of the global oceanic circulation.In: Wefer G, Berger WH, Siedler G, Webb
DJ (eds) The South Atlantic: Present and Past Circulation. Springer, Berlin Heidelberg, pp 445-460
Dupont LM (1993) Vegetation zones in NW Africa during the Brunhes Chron reconstructed from marine
palynological data. Quat Sci Rev 12: 189-202
Dwyer GS, Cronin TM, Baker PA, Raymo ME, Buzas JS,
Correge T (1995) North Atlantic deep-water temperature change during late Pliocene and late Quaternary
climatic cycles. Science 270: 1347-13 51
Dymond J, Suess E, Lyle M (1992) Barium in deep-sea
sediment: a geochemical proxy for paleoproductivity. Paleoceanography 7: 163-182
Dymond J, Collier R, McManaus J, Honjo S, Manganini
S (1997) Can the aluminum and titanium contents of
ocean sediments be used to determine the
paleoproductivity of the oceans. Paleoceanography
12:586-593
Emerson S (1985) Organic carbon preservation in marine sediments. In: Sundquist ET, Broecker WS (eds)
The Carbon Cycle and Atmospheric CO 2 : Natural
Variations Archean to Present. Geophys Monogr 32,
Amer Geophys Union, Washington DC, pp 78-87
Emiliani C (1955) Pleistocene temperatures. J Geo163:
538-578
Eppley RW, Peterson BJ (1979) Particulate matter flux and
planktonic new production. Nature 282: 677-680
Epstein S, Buchsbaum R, Lowenstam HA, Urey HC
(1953) Revised carbonate-water isotopic temperature
scale. Bull Geol Soc Amer 64: 1315-1325
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
Fairbanks RG, Charles CD, Wright JD (1992) Origin of
global meltwater pulses. In: Taylor RE (ed) Radiocarbon after four decades. Springer, Berlin
Heidelberg New York, pp 473-500
Farley KA (1995) Cenozoic variations in the flux of
interplanetray dust recorded by 3He in a deep-sea
sediment. Nature 376: 153-156
Farley KA, Patterson DB (1995) A 100 kyr periodicity in
the flux of extraterrestrial 3 He to the seafloor. Nature
378: 600-603
FarquharGD, O'Leary MR, Berry JH (1982) On therelationship between carbon isotope discrimination and
the intercellular carbon dioxide concentration in
leaves. AustJ Plan Physio 9: 121-13 7
Farrell JW, Pedersen TF, Calvert SE, Nielsen B (1995)
Glacial-interglacial changes in nutrient utilization in
the equatorial Pacific Ocean. Nature 377: 514-517
Farrimond P, Eglington G, Brassel SC (1987) Alkenones
in Cretaceous black shales, Blake-Bahama basin,
western North Atlantic. Org Geochem 10: 897-903
Filippelini GM, Delaney ML (1994) The oceanic phosphorus cycle and continental weathering during the
Neogene. Paleoceanography 9: 643-652
Fischer G, Wefer G (1995) Downward particulate matter
fluxes in the eastern and western Equatorial Atlantic: a comparison. In: Tsunogai S, Iseki K, Koike I,
Oba T (eds) Global Fluxes of Carbon and ist related
Substances in the Coastal Sea - Open Ocean - Atmosphere System. Proceedings of the 1994-IGBP
symposium, Sapporo (Japan), pp 317-331
Fischer G, Schneider R, MUller PJ, Wefer G (1997) Anthropogenic CO 2 in Southern Ocean surface waters:
evidence from stable organic carbon isotopes. Terra
Nova9: 153-157
Fischer G, MUller PJ, Wefer G (1998) Latitudinal oI3C o ,.
variations in sinking matter and sediments from the
South Atlantic: effects of anthropogenic CO 2 and
implications for paleo-PC0 2 -reconstructions. J Mar
Syst 17:471-495
Fontugne MR, Duplessy J-C (1986) Variations of the
monsoon regime during the Upper Quaternary: Evidence from the carbon isotopic record of organic
matter in North Indian Ocean sediment cores.
Palaeogeogr Palaeoclimatol Palaeoecol56: 69-88
Francois R, AltabetMA, Burkle LH (1992) Glacial to interglacial changes in surface nitrate utilisation in the
Indian sector of the Southern Ocean as recorded by
sediment ol'N. Paleoceanography 7: 589-606
Francois R, Honjo S, Manganini S, Ravizza GE (1995)
Biogenic barium fluxes to the deep sea: Implications
for paleoproductivity reconstruction. Global
Biogeochem Cycles 9: 289-303
FrancoisR,AltabetMA, YuE-F, SigrnanDM, BaconMP,
Frank M, Bohrmann G, Bareille G, Labeyrie L (1997)
Contribution of Southern Ocean surface-water stratification to low atmospheric CO 2 concentrations during the last glacial period. Nature 389: 929-935
45
Paleoceanography 3: 343-360
Duplessy J-C, Labeyrie LD, Juillet-Leclerc A, Maitre F,
Duprat J, Samthein M (1991) Surface salinity reconstruction of the North Altantic Ocean during the last
glaciaimaximum.OceanolActa 14: 311-324
Duplessy J-C, Bard E, Labeyrie L, Duprat J, Moyes J
(1993) Oxygen isotope records and salinity changes
in the northeastern Atlantic Ocean during the last
18,000 years. Paleoceanography 8: 341-350
Duplessy J-C, Labeyrie LD, Paterne M, Hovine S,
Fichefet T, Duprat J, Labracherie M (1996) High latitude deep water sources during the Last Glacial
Maximum and the inensify of the global oceanic circulation.In: Wefer G, Berger WH, Siedler G, Webb
DJ (eds) The South Atlantic: Present and Past Circulation. Springer, Berlin Heidelberg, pp 445-460
Dupont LM (1993) Vegetation zones in NW Africa during the Brunhes Chron reconstructed from marine
palynological data. Quat Sci Rev 12: 189-202
Dwyer GS, Cronin TM, Baker PA, Raymo ME, Buzas JS,
Correge T (1995) North Atlantic deep-water temperature change during late Pliocene and late Quaternary
climatic cycles. Science 270: 1347-13 51
Dymond J, Suess E, Lyle M (1992) Barium in deep-sea
sediment: a geochemical proxy for paleoproductivity. Paleoceanography 7: 163-182
Dymond J, Collier R, McManaus J, Honjo S, Manganini
S (1997) Can the aluminum and titanium contents of
ocean sediments be used to determine the
paleoproductivity of the oceans. Paleoceanography
12:586-593
Emerson S (1985) Organic carbon preservation in marine sediments. In: Sundquist ET, Broecker WS (eds)
The Carbon Cycle and Atmospheric CO 2 : Natural
Variations Archean to Present. Geophys Monogr 32,
Amer Geophys Union, Washington DC, pp 78-87
Emiliani C (1955) Pleistocene temperatures. J Geo163:
538-578
Eppley RW, Peterson BJ (1979) Particulate matter flux and
planktonic new production. Nature 282: 677-680
Epstein S, Buchsbaum R, Lowenstam HA, Urey HC
(1953) Revised carbonate-water isotopic temperature
scale. Bull Geol Soc Amer 64: 1315-1325
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
Fairbanks RG, Charles CD, Wright JD (1992) Origin of
global meltwater pulses. In: Taylor RE (ed) Radiocarbon after four decades. Springer, Berlin
Heidelberg New York, pp 473-500
Farley KA (1995) Cenozoic variations in the flux of
interplanetray dust recorded by 3He in a deep-sea
sediment. Nature 376: 153-156
Farley KA, Patterson DB (1995) A 100 kyr periodicity in
the flux of extraterrestrial 3 He to the seafloor. Nature
378: 600-603
FarquharGD, O'Leary MR, Berry JH (1982) On therelationship between carbon isotope discrimination and
the intercellular carbon dioxide concentration in
leaves. AustJ Plan Physio 9: 121-13 7
Farrell JW, Pedersen TF, Calvert SE, Nielsen B (1995)
Glacial-interglacial changes in nutrient utilization in
the equatorial Pacific Ocean. Nature 377: 514-517
Farrimond P, Eglington G, Brassel SC (1987) Alkenones
in Cretaceous black shales, Blake-Bahama basin,
western North Atlantic. Org Geochem 10: 897-903
Filippelini GM, Delaney ML (1994) The oceanic phosphorus cycle and continental weathering during the
Neogene. Paleoceanography 9: 643-652
Fischer G, Wefer G (1995) Downward particulate matter
fluxes in the eastern and western Equatorial Atlantic: a comparison. In: Tsunogai S, Iseki K, Koike I,
Oba T (eds) Global Fluxes of Carbon and ist related
Substances in the Coastal Sea - Open Ocean - Atmosphere System. Proceedings of the 1994-IGBP
symposium, Sapporo (Japan), pp 317-331
Fischer G, Schneider R, MUller PJ, Wefer G (1997) Anthropogenic CO 2 in Southern Ocean surface waters:
evidence from stable organic carbon isotopes. Terra
Nova9: 153-157
Fischer G, MUller PJ, Wefer G (1998) Latitudinal oI3C o ,.
variations in sinking matter and sediments from the
South Atlantic: effects of anthropogenic CO 2 and
implications for paleo-PC0 2 -reconstructions. J Mar
Syst 17:471-495
Fontugne MR, Duplessy J-C (1986) Variations of the
monsoon regime during the Upper Quaternary: Evidence from the carbon isotopic record of organic
matter in North Indian Ocean sediment cores.
Palaeogeogr Palaeoclimatol Palaeoecol56: 69-88
Francois R, AltabetMA, Burkle LH (1992) Glacial to interglacial changes in surface nitrate utilisation in the
Indian sector of the Southern Ocean as recorded by
sediment ol'N. Paleoceanography 7: 589-606
Francois R, Honjo S, Manganini S, Ravizza GE (1995)
Biogenic barium fluxes to the deep sea: Implications
for paleoproductivity reconstruction. Global
Biogeochem Cycles 9: 289-303
FrancoisR,AltabetMA, YuE-F, SigrnanDM, BaconMP,
Frank M, Bohrmann G, Bareille G, Labeyrie L (1997)
Contribution of Southern Ocean surface-water stratification to low atmospheric CO 2 concentrations during the last glacial period. Nature 389: 929-935