44
Weferetal.
ocean. Quat Res 21: 123-224
Conley DJ (1998) An interlaboratory comparions for the
measurements of biogenic silica in sediments. Mar
Chern 63: 39-48
Corliss BH (1985) Microhabitats of benthic foraminifera
within deep - sea sediments. Nature 314: 435-438
Corliss BH, Chen C (1988) Morphotype patterns of
norwegian sea deep-sea benthic foraminifera and
ecological implications. Geology 4: 716-719
Craig H, Gordon LS (1965) Deuterium and oxygen 18
variations in the ocean and the marine atmosphere.
In: Tongiorgi E (ed) Stable isotopes in oceanographic studies and paleo-temperatures. Consiglio
nazionale delle ricerche, Laboratorio di Geologia
Nucleare, Pisa, pp 9-130
Curry WB, Duplessy J-C, Labeyrie LD, Shackleton NJ
(1988) Changes in the distribution of Ol3C of deep
water CO 2 between the glaciation and the Holocene.
Paleoceanography 3: 317-342
Curry WB, Ostermann DR, Guptha MV, Ittekkot V (1992)
Foraminiferal production and monsoonal forcing in
the Arabian Sea: evidence from sediment traps. In:
Summerhayes CP, Prell WL, Emeis K-C (eds)
Upwelling systems: Evolution since the Early
Miocene. Geol Soc Spec Pub164, pp 93-106
Dansgaard W, Tauber H (1969) Glacier oxygen-I 8 content and Pleistocene ocean temperatures. Science
166: 499-502
Darling KF, Wade CM, Kroon D, Brown AJL (1997)
Planktic foraminiferal molecular evolution and their
polyphyletic origins from benthic taxa. Mar
Micropaleontol30: 251-266
De Baar HJW, Saager PM, Nolting RF, van der Meer J
(1994) Cadmium versus phosphate in the world
ocean. Mar Chern 46: 261-281
De la Rocha CL, Brzezinski MA, DeNiro MJ (1997)
Fractionation of silicon isotopes by marine diatoms
during biogenic silica formation. Geochim
Cosmochim Acta 61 : 5051-5056
De la Rocha CL, Brzezinski MA, DeNiro MJ, Shemesh
A (1998) Silicon isotope composition of diatoms as
an indicator of past oceanic changes. Nature 395:
680-683
Degens ET, Epstein S (1962) Relation between 1'0/ 16 0
ratios in coexisting carbonate, cherts and diatomites.
Amer Assoc Petrol Geol Bull 46: 534-542
Dehairs F, Chesselet R, Jedwab J (1980) Discrete suspended particles of barite and the barium cycle in
the open ocean. Earth Planet Sci Lett 49: 528-550
Delaney ML, Filippelini GM (1994) An apparent contradiction in the role of phosphorus in Cenozoic chemical mass balances for the world ocean.
Paleoceanography 9: 513-527
Delaney ML, Be A WH, Boyle EA (1985) Li, Sr, Mg, and
Na in foraminiferal calcite shells from laboratory
culture, sediment traps, and sediment cores. Geochim
Cosmochim Acta49: 327-1341
De Leeuw JW, van der Meer FW, Rijpstra WIC, Schenk
PA (1980) On the occurrence and structural identification of long chain alkenones and hydrocarbons
in sediments. In: Douglas AG, Maxwell JR (eds) Advances in Organic Chemistry. Pergamon, New York,
pp211-221
De Leeuw JW, Frewin NL, Van Bergen PF, Sinninghe
Damste JS, Collinson ME (1995) Organic carbon as
a palaeoenvironemental indicator in the marine realm.
In: Bosence DWJ, Allison PA (eds) Marine
Palaeoenvironmental Analysis from Fossils. Geol
Soc Spec Pub183, pp 43-71
DeMaster DJ (1981) The supply and accumulation of
silica in the marine environment. Geochim
Cosmochim Acta45: 1715-1732
DeMenocal PB, Ruddirnan WF, Pokras EM (1993) Influences of high- and low-latitude processes on African terrestrial climate: Pleistocene eolian records
from equatorial Atlantic Ocean Drilling Program Site
663. Paleoceanography 8: 209-242
Diekmann B, Petschick R, Gingele FX, Fiitterer D,
Abelmann A, Brathauer U, Gersonde R, Mackensen
A (1996) Clay mineral fluctuations in late Quaternary
sediments of the Southeastern South Atlantic: Implications for past changes of deep water advection.
In: Wefer G, BergerWH, SiedlerG, Webb DJ (eds)
The South Atlantic: Present and Past Circulation.
Springer, Berlin Heidelberg New York, pp 621-644
Dittert N, Henrich R (subm) Carbonate dissolution in the
South Atlantic Ocean: Evidence by Globigerina
bulloides' ultrastructure breakdown. Deep-Sea Res
Dugdale RC, Goering JJ (1967) Uptake of new and regenerated forms of nitrogen in primary productivity. LinmolOceanogr 12: 196-206
Dugdale RC, Wilkerson FP (1998) Silicate regulation of
new production in the equatorial Pacific upwelling.
Nature 391: 270-273
Dugdale RC, Wilkerson FP, Minas HJ (1995) The role of
a silicate pump in driving new production. Deep-Sea
Res 42: 697-719
Dunbar R, Wefer G (1984) Stable isotopic fractionation
in benthic foraminifera from the Peruvian continental margin. Mar Geol 59: 215-225
Duplessy J-C, Shackleton NJ, Fairbanks RG, Labeyrie
LD, Oppo D, Kalle! N (1988) Deep water source variations during the last climatic cycle and their impact
on the global deep water circulation.
Weferetal.
ocean. Quat Res 21: 123-224
Conley DJ (1998) An interlaboratory comparions for the
measurements of biogenic silica in sediments. Mar
Chern 63: 39-48
Corliss BH (1985) Microhabitats of benthic foraminifera
within deep - sea sediments. Nature 314: 435-438
Corliss BH, Chen C (1988) Morphotype patterns of
norwegian sea deep-sea benthic foraminifera and
ecological implications. Geology 4: 716-719
Craig H, Gordon LS (1965) Deuterium and oxygen 18
variations in the ocean and the marine atmosphere.
In: Tongiorgi E (ed) Stable isotopes in oceanographic studies and paleo-temperatures. Consiglio
nazionale delle ricerche, Laboratorio di Geologia
Nucleare, Pisa, pp 9-130
Curry WB, Duplessy J-C, Labeyrie LD, Shackleton NJ
(1988) Changes in the distribution of Ol3C of deep
water CO 2 between the glaciation and the Holocene.
Paleoceanography 3: 317-342
Curry WB, Ostermann DR, Guptha MV, Ittekkot V (1992)
Foraminiferal production and monsoonal forcing in
the Arabian Sea: evidence from sediment traps. In:
Summerhayes CP, Prell WL, Emeis K-C (eds)
Upwelling systems: Evolution since the Early
Miocene. Geol Soc Spec Pub164, pp 93-106
Dansgaard W, Tauber H (1969) Glacier oxygen-I 8 content and Pleistocene ocean temperatures. Science
166: 499-502
Darling KF, Wade CM, Kroon D, Brown AJL (1997)
Planktic foraminiferal molecular evolution and their
polyphyletic origins from benthic taxa. Mar
Micropaleontol30: 251-266
De Baar HJW, Saager PM, Nolting RF, van der Meer J
(1994) Cadmium versus phosphate in the world
ocean. Mar Chern 46: 261-281
De la Rocha CL, Brzezinski MA, DeNiro MJ (1997)
Fractionation of silicon isotopes by marine diatoms
during biogenic silica formation. Geochim
Cosmochim Acta 61 : 5051-5056
De la Rocha CL, Brzezinski MA, DeNiro MJ, Shemesh
A (1998) Silicon isotope composition of diatoms as
an indicator of past oceanic changes. Nature 395:
680-683
Degens ET, Epstein S (1962) Relation between 1'0/ 16 0
ratios in coexisting carbonate, cherts and diatomites.
Amer Assoc Petrol Geol Bull 46: 534-542
Dehairs F, Chesselet R, Jedwab J (1980) Discrete suspended particles of barite and the barium cycle in
the open ocean. Earth Planet Sci Lett 49: 528-550
Delaney ML, Filippelini GM (1994) An apparent contradiction in the role of phosphorus in Cenozoic chemical mass balances for the world ocean.
Paleoceanography 9: 513-527
Delaney ML, Be A WH, Boyle EA (1985) Li, Sr, Mg, and
Na in foraminiferal calcite shells from laboratory
culture, sediment traps, and sediment cores. Geochim
Cosmochim Acta49: 327-1341
De Leeuw JW, van der Meer FW, Rijpstra WIC, Schenk
PA (1980) On the occurrence and structural identification of long chain alkenones and hydrocarbons
in sediments. In: Douglas AG, Maxwell JR (eds) Advances in Organic Chemistry. Pergamon, New York,
pp211-221
De Leeuw JW, Frewin NL, Van Bergen PF, Sinninghe
Damste JS, Collinson ME (1995) Organic carbon as
a palaeoenvironemental indicator in the marine realm.
In: Bosence DWJ, Allison PA (eds) Marine
Palaeoenvironmental Analysis from Fossils. Geol
Soc Spec Pub183, pp 43-71
DeMaster DJ (1981) The supply and accumulation of
silica in the marine environment. Geochim
Cosmochim Acta45: 1715-1732
DeMenocal PB, Ruddirnan WF, Pokras EM (1993) Influences of high- and low-latitude processes on African terrestrial climate: Pleistocene eolian records
from equatorial Atlantic Ocean Drilling Program Site
663. Paleoceanography 8: 209-242
Diekmann B, Petschick R, Gingele FX, Fiitterer D,
Abelmann A, Brathauer U, Gersonde R, Mackensen
A (1996) Clay mineral fluctuations in late Quaternary
sediments of the Southeastern South Atlantic: Implications for past changes of deep water advection.
In: Wefer G, BergerWH, SiedlerG, Webb DJ (eds)
The South Atlantic: Present and Past Circulation.
Springer, Berlin Heidelberg New York, pp 621-644
Dittert N, Henrich R (subm) Carbonate dissolution in the
South Atlantic Ocean: Evidence by Globigerina
bulloides' ultrastructure breakdown. Deep-Sea Res
Dugdale RC, Goering JJ (1967) Uptake of new and regenerated forms of nitrogen in primary productivity. LinmolOceanogr 12: 196-206
Dugdale RC, Wilkerson FP (1998) Silicate regulation of
new production in the equatorial Pacific upwelling.
Nature 391: 270-273
Dugdale RC, Wilkerson FP, Minas HJ (1995) The role of
a silicate pump in driving new production. Deep-Sea
Res 42: 697-719
Dunbar R, Wefer G (1984) Stable isotopic fractionation
in benthic foraminifera from the Peruvian continental margin. Mar Geol 59: 215-225
Duplessy J-C, Shackleton NJ, Fairbanks RG, Labeyrie
LD, Oppo D, Kalle! N (1988) Deep water source variations during the last climatic cycle and their impact
on the global deep water circulation.