Clues to Ocean History: a BriefOverview of Proxies
41
Altabet MA, Francois R, Murray DW, Prell WL (1995)
Climate-related variations in denitrification in the
Arabian Sea from sediment 15NP 4 N ratios. Nature
373: 506-509
Altenbach A V, Sarnthein M (1989) Productivity record
of benthic foraminifera. In: Berger WH, Smetacek V,
Wefer G (eds) Productivity of the Ocean: Present and
Past. J Wiley & Sons, New York, pp 255-269
Anderson RF, Bacon MP, Brewer PG (1983) Removal of
Th-230 and Pa-231 at ocean margins. Earth Planet Sci
Lett 66: 73-90
Archer DE (1991) Equatorial pacific calcite preservation
cycles: production or dissolution. Paleoceanography6: 561-571
ArcherD, Maier-ReimerE(1994)Effectofdeep-sea sedimentary calcite preservation on atmospheric CO 2
concentration. Nature 367: 260-263
Archer D, Emerson S, Reimers C (1989) Dissolution of
calcite in deep-sea sediments: pH and 02 microelectrode results. Geochim Cosmochim Acta 53:
2831-2846
Arrhenius GOS (1952) Sediment cores from the east
pacific. Reports of the swedish deep-sea expedition
1947-19485: 1-228
Bacon MP, Anderson RF (1982) Distribution of thorium
isotopes between dissolved and particulate forms
in the deep sea. J Geophys Res 87: 2045-2056
Bard E, Hamelin B, Fairbanks RG (1990a) U-Th ages
obtained by mass spectrometry in corals from
barbados: sea level during the past 130,000 years.
Nature 346: 456-458
BardE, Hamelin B, Fairbanks RG, Zindler A (1990b) Calibration of the 14C time scale over the past 30,000 years
using mass spectrometric U-Th ages from Barbados
corals. Nature 345: 405-410
BardE, ArnoldM, Fairbanks RG, HamelinB (1993) 23"Th_
234U and I'C ages obtained by mass spectrometry on
corals. Radiocarbon 35: 191-199
Bamola 1M, Raynaud D, Korotkevich YS, Lorius C (1987)
Vostok ice core provides 160,000-year-record of atmospheric CO 2 • Nature 329: 408-414
Beck IW, Edwards RL, Ito E, Taylor FW, Recy J, Rougerie
F, JoanntP, Henin C (1992) Sea-surface temperatures
from coral skeletal strontium/calcium ratios. Science
257: 644-647
Bender M, Sowers T, Labeyrie L (1994) The Dole effect
and its variations during the last 130.000 years as
measured in the Vostok ice core. Global Biogeochem
Cycles 8: 363-376
Bentaleb I, Fontugne M, Descolas-Gros C, Girardin C,
Mariotti A, Pierre C, Poisson A (1996) Organic carbon isotope composition of phytoplankton and seasurface PC0 2 reconstruction in the Southern Indian
Ocean during the last 50,000 years. Org Geochem 24:
399-410
Berger A, Loutre MF (1991) Insolation values for the
climate of the last 10 million years. Quat Sci Rev 10:
297-317
Berger WH (1970) Planktonic foraminifera: Selective
solution and the lysocline. Mar Geol8: 111-138
Berger WH (1971) Sedimentation of planktonic
foraminifera. Mar Geol11 : 325-358
Berger WH (1976) Biogenous deep-sea sediments: production, preservation and interpretation. In: Riley JP,
Chester R (eds) Treatise on Chemical Oceanography,
Vol 5. Academic Press, London, pp 265-388
Berger WH (1981) Paleoceanography: the deep-sea
record. In: Emiliani C (ed) The Sea, Vol 7. WileyInterscience, N ew York, pp 1437-1519
Berger WH (1989) Global maps of ocean productivity.
In: Berger WH, Smetacek VS, Wefer G (eds) Productivity of the Ocean: Present and Past. Dahlem
Konferenzen, J Wiley & Sons, Chichester,
pp429-455
Berger WH (1996) An algorithm for reconstruction of
atmospheric CO 2 from deep sea sediments. Naturwissenschaften83: 519-522
Berger WH, Gardner JV (1975) On the determination of
Pleistocene temperatures from planktonic
foraminifera. JForamRes 5: 102-113
Berger WH, Herguera JC (1992) Reading the sedimentary record of the ocean's productivity. In: Falkowski
PG, Woodhead AD (eds) Primary Productivity and
Biogeochemical Cycles in the Sea. Plenum Press,
New York, pp 455-486
Berger WH, Keir RS (1984) Glacial-Holocene changes
in atmospheric CO 2 and the deep-sea record. In:
Hansen JE, Takahashi T (eds) Climate Processes and
Climate Sensitivity, Vol 29. Amer Geophys Union,
pp337-351
Berger WH, Lange CB (1998) Silica depletion in the
thermocline of the glacial North Pacific: corollaries
and implications. Deep-Sea Res II 45: 1885-1904
Berger WH, Vincent E (1986) Deep-sea carbonates: reading the carbon isotope signal. Geol Rundsch 75:
249-269
Berger WH, Wefer G (1990) Export production:
Seasonality and intermittency, and paleoceanographic implications. Palaeogeogr Palaeoclimatol
Palaeoecol89: 245-254
Berger WH, Diester-Haass L, Killingley JS (1978)
Upwelling off Northwest Africa: the Holocene decrease as seen in carbon isotopes and
sedimentological indicators. Oceano 1 Acta I: 3-7
41
Altabet MA, Francois R, Murray DW, Prell WL (1995)
Climate-related variations in denitrification in the
Arabian Sea from sediment 15NP 4 N ratios. Nature
373: 506-509
Altenbach A V, Sarnthein M (1989) Productivity record
of benthic foraminifera. In: Berger WH, Smetacek V,
Wefer G (eds) Productivity of the Ocean: Present and
Past. J Wiley & Sons, New York, pp 255-269
Anderson RF, Bacon MP, Brewer PG (1983) Removal of
Th-230 and Pa-231 at ocean margins. Earth Planet Sci
Lett 66: 73-90
Archer DE (1991) Equatorial pacific calcite preservation
cycles: production or dissolution. Paleoceanography6: 561-571
ArcherD, Maier-ReimerE(1994)Effectofdeep-sea sedimentary calcite preservation on atmospheric CO 2
concentration. Nature 367: 260-263
Archer D, Emerson S, Reimers C (1989) Dissolution of
calcite in deep-sea sediments: pH and 02 microelectrode results. Geochim Cosmochim Acta 53:
2831-2846
Arrhenius GOS (1952) Sediment cores from the east
pacific. Reports of the swedish deep-sea expedition
1947-19485: 1-228
Bacon MP, Anderson RF (1982) Distribution of thorium
isotopes between dissolved and particulate forms
in the deep sea. J Geophys Res 87: 2045-2056
Bard E, Hamelin B, Fairbanks RG (1990a) U-Th ages
obtained by mass spectrometry in corals from
barbados: sea level during the past 130,000 years.
Nature 346: 456-458
BardE, Hamelin B, Fairbanks RG, Zindler A (1990b) Calibration of the 14C time scale over the past 30,000 years
using mass spectrometric U-Th ages from Barbados
corals. Nature 345: 405-410
BardE, ArnoldM, Fairbanks RG, HamelinB (1993) 23"Th_
234U and I'C ages obtained by mass spectrometry on
corals. Radiocarbon 35: 191-199
Bamola 1M, Raynaud D, Korotkevich YS, Lorius C (1987)
Vostok ice core provides 160,000-year-record of atmospheric CO 2 • Nature 329: 408-414
Beck IW, Edwards RL, Ito E, Taylor FW, Recy J, Rougerie
F, JoanntP, Henin C (1992) Sea-surface temperatures
from coral skeletal strontium/calcium ratios. Science
257: 644-647
Bender M, Sowers T, Labeyrie L (1994) The Dole effect
and its variations during the last 130.000 years as
measured in the Vostok ice core. Global Biogeochem
Cycles 8: 363-376
Bentaleb I, Fontugne M, Descolas-Gros C, Girardin C,
Mariotti A, Pierre C, Poisson A (1996) Organic carbon isotope composition of phytoplankton and seasurface PC0 2 reconstruction in the Southern Indian
Ocean during the last 50,000 years. Org Geochem 24:
399-410
Berger A, Loutre MF (1991) Insolation values for the
climate of the last 10 million years. Quat Sci Rev 10:
297-317
Berger WH (1970) Planktonic foraminifera: Selective
solution and the lysocline. Mar Geol8: 111-138
Berger WH (1971) Sedimentation of planktonic
foraminifera. Mar Geol11 : 325-358
Berger WH (1976) Biogenous deep-sea sediments: production, preservation and interpretation. In: Riley JP,
Chester R (eds) Treatise on Chemical Oceanography,
Vol 5. Academic Press, London, pp 265-388
Berger WH (1981) Paleoceanography: the deep-sea
record. In: Emiliani C (ed) The Sea, Vol 7. WileyInterscience, N ew York, pp 1437-1519
Berger WH (1989) Global maps of ocean productivity.
In: Berger WH, Smetacek VS, Wefer G (eds) Productivity of the Ocean: Present and Past. Dahlem
Konferenzen, J Wiley & Sons, Chichester,
pp429-455
Berger WH (1996) An algorithm for reconstruction of
atmospheric CO 2 from deep sea sediments. Naturwissenschaften83: 519-522
Berger WH, Gardner JV (1975) On the determination of
Pleistocene temperatures from planktonic
foraminifera. JForamRes 5: 102-113
Berger WH, Herguera JC (1992) Reading the sedimentary record of the ocean's productivity. In: Falkowski
PG, Woodhead AD (eds) Primary Productivity and
Biogeochemical Cycles in the Sea. Plenum Press,
New York, pp 455-486
Berger WH, Keir RS (1984) Glacial-Holocene changes
in atmospheric CO 2 and the deep-sea record. In:
Hansen JE, Takahashi T (eds) Climate Processes and
Climate Sensitivity, Vol 29. Amer Geophys Union,
pp337-351
Berger WH, Lange CB (1998) Silica depletion in the
thermocline of the glacial North Pacific: corollaries
and implications. Deep-Sea Res II 45: 1885-1904
Berger WH, Vincent E (1986) Deep-sea carbonates: reading the carbon isotope signal. Geol Rundsch 75:
249-269
Berger WH, Wefer G (1990) Export production:
Seasonality and intermittency, and paleoceanographic implications. Palaeogeogr Palaeoclimatol
Palaeoecol89: 245-254
Berger WH, Diester-Haass L, Killingley JS (1978)
Upwelling off Northwest Africa: the Holocene decrease as seen in carbon isotopes and
sedimentological indicators. Oceano 1 Acta I: 3-7