280
Dittert et al.
Berger WH (1979) Preservation of foraminifera. In: Lipps
JH, Berger WH, Buzas MA, Douglas RG, Ross CA
(eds) Foraminiferal Ecology and Palecology. Society
of Economic Paleontologists and Mineralogists,
Houston, 6, pp 105-155
Berger WH (1982) Increase of carbon dioxide in the atmosphere during deglaciation: the coral reefhypothesis. Naturwissenschaften 69: 87-88
Berger WH (1991) ProduktiviUit des Ozeans aus
geologischer Sicht: Denkmodelle und Beispiele. Z
Dtsch Geol Ges 142: 149-178
Berger WH, Adelseck CG, Mayer LA (1976) Distribution
of carbonate in surface sediments of the Pacific
Ocean. J Geophys Res 81(C): 2617-2627
Berger WH, Bonneau M-C, Parker FL (1982) Foraminifera
on the deep-sea floor: lysocline and dissolution rate.
Oceanol Acta 5(2): 249-258
Berger WH, Fischer K, Lai C, Wu G (1987) Ocean productivity and organic carbon flux. Part 1. Overview
and maps of primary production and export production. Scripps Inst Oceanogr, Univ California,
pp 1-67
Berger WH, Keir RS (1984) G lacial-Holocene changes
in atmospheric CO, and the deep-sea record. In:
Hansen JE, Takahashi T (eds) Climate processes and
climate sensitivity. Geophys Monogr 29, Maurice
Ewing Series, Washington DC, 5, pp337-351
Berger WH, Smetacek VS, Wefer G (1989) Ocean productivity and paleoproductivity - An overview. In:
Berger WH, Smetacek VS, Wefer G (eds) Productivity of the Ocean: Present and Past. J Wiley & Sons,
NewYork,pp 1-34
Berner RA (1977) Sedimentation and dissolution of
pteropods in the ocean. In: Andersen NR, Malahoff
A (eds) The Fate of Fossil Fuel CO, in the Oceans.
Plenum Press, New York, pp 243-260
Bickert T, Wefer G (1996) Late Quaternary deep water
circulation in the South Atlantic: Reconstruction
from carbonate dissolution and benthic stable isotopes. In: WeferG, BergerWH, SiedlerG, Webb OJ
(eds) The South Atlantic: Present and Past Circulation. Springer, Berlin Heidelberg New York,
pp 599-620
Bickert T, Cordes R, Wefer G (1997) Late Pliocene to MidPleistocene (2.6-1.0 M.Y.) carbonate dissolution in
the western equatorial Atlantic: Results of Leg 154,
Ceara Rise. In: Shackleton NJ, Curry WB, Richter C,
BralowerTJ (eds)Proc ODP Sci ResuIts 154, College
Station, TX, pp 229-237
Biscaye PE, Kolla V, Turekian KK (\976) Distribution of
calcium carbonate in surface sediments of the
Atlantic Ocean. J Geophys Res 81(C5): 2595-2603
Boltovskoy E (1991) La destruction des tests de
foraminiferes (experiences de laboratoire). Revue de
Micropaleontologie 34(1): 19-25
Boltovskoy E, Totah VI (1992) Preservation index and
preservation potential of some foraminiferal species.
J Foram Res 22(3): 267-273
Boyle EA (1988) Vertical oceanic nutrient fractionation
and glacial/interglacial CO, cycles. Nature 331:
55-56
Bramlette MN (1961) Pelagic sediments. In: Sears M (ed)
Oceanography. AAAS Publication, New York, 67,
pp345-366
Broecker WS, Peng TH (1982) Tracers in the Sea. Eldigio
Press, New York, pp 1-689
Broecker WS, Takahashi T (1978) The relationship between lysocline depth and in situ carbonate ion concentration. Deep-Sea Res 25F( I): 65-95
Brown SJ, Elderfield H (1996) Variations in Mg/Ca and
Sr/Ca ratios of planktonic foraminifera caused
by postdepositional dissolution: Evidence of shallow Mg-dependent dissolution. Paleoceanography
11(5): 543-551
Chave KE, Suess E (I 970) Calcium carbonate saturation
in sea water: Effects of dissolved organic matter.
Limnol Oceanogr 15: 633-637
CLIMAP Project members (1976) The surface of the iceage earth. Science 191(4232): 1131-1137
CLIMAP Project members (1984) The last interglacial
ocean. Quat Res 21: 123-224
Connary SD, Ewing M (1972) The nepheloid layer and
bottom circulation in the Guinea and Angola Basins.
In: Gordon AL (ed) Studies in physical oceanography: a tribute to Georg Wust on his 80th birthday.
Gordon and Breach, New York, 2, pp 169-184
Corliss BH, Honjo S (1981) Dissolution of deep-sea
benthic foraminifera. Micropaleontology 27(4):
356-378
Culkin F (\965) The major ion components of seawater.
In: Riley JP, Skirrow G (eds) Chemical Oceanography. Academic Press, New York, 1, pp 121-162
Curry WB, Lohmann GP (1990) Reconstructing past
particle fluxes in the tropical Atlantic Ocean.
Paleoceanography 5: 487-506
De Vernal A, Bilodeaul G, Hillaire-Marcel C, Kassou N
(1992) Quantitative Assessment of Carbonate Dissolution in Marine Sediments from Foraminifer Linings vs. Shell Ratios: Davis Strait, Northwest North
Atlantic. Geology 20: 527-530
Diester-Haass L, Muller PJ (1979) Processes influencing sand fraction composition and organic matter
content in surface sediments offW Africa (l2-19°N).
"Meteor" Forsch Ergebn C 31: 21-47
Dittert et al.
Berger WH (1979) Preservation of foraminifera. In: Lipps
JH, Berger WH, Buzas MA, Douglas RG, Ross CA
(eds) Foraminiferal Ecology and Palecology. Society
of Economic Paleontologists and Mineralogists,
Houston, 6, pp 105-155
Berger WH (1982) Increase of carbon dioxide in the atmosphere during deglaciation: the coral reefhypothesis. Naturwissenschaften 69: 87-88
Berger WH (1991) ProduktiviUit des Ozeans aus
geologischer Sicht: Denkmodelle und Beispiele. Z
Dtsch Geol Ges 142: 149-178
Berger WH, Adelseck CG, Mayer LA (1976) Distribution
of carbonate in surface sediments of the Pacific
Ocean. J Geophys Res 81(C): 2617-2627
Berger WH, Bonneau M-C, Parker FL (1982) Foraminifera
on the deep-sea floor: lysocline and dissolution rate.
Oceanol Acta 5(2): 249-258
Berger WH, Fischer K, Lai C, Wu G (1987) Ocean productivity and organic carbon flux. Part 1. Overview
and maps of primary production and export production. Scripps Inst Oceanogr, Univ California,
pp 1-67
Berger WH, Keir RS (1984) G lacial-Holocene changes
in atmospheric CO, and the deep-sea record. In:
Hansen JE, Takahashi T (eds) Climate processes and
climate sensitivity. Geophys Monogr 29, Maurice
Ewing Series, Washington DC, 5, pp337-351
Berger WH, Smetacek VS, Wefer G (1989) Ocean productivity and paleoproductivity - An overview. In:
Berger WH, Smetacek VS, Wefer G (eds) Productivity of the Ocean: Present and Past. J Wiley & Sons,
NewYork,pp 1-34
Berner RA (1977) Sedimentation and dissolution of
pteropods in the ocean. In: Andersen NR, Malahoff
A (eds) The Fate of Fossil Fuel CO, in the Oceans.
Plenum Press, New York, pp 243-260
Bickert T, Wefer G (1996) Late Quaternary deep water
circulation in the South Atlantic: Reconstruction
from carbonate dissolution and benthic stable isotopes. In: WeferG, BergerWH, SiedlerG, Webb OJ
(eds) The South Atlantic: Present and Past Circulation. Springer, Berlin Heidelberg New York,
pp 599-620
Bickert T, Cordes R, Wefer G (1997) Late Pliocene to MidPleistocene (2.6-1.0 M.Y.) carbonate dissolution in
the western equatorial Atlantic: Results of Leg 154,
Ceara Rise. In: Shackleton NJ, Curry WB, Richter C,
BralowerTJ (eds)Proc ODP Sci ResuIts 154, College
Station, TX, pp 229-237
Biscaye PE, Kolla V, Turekian KK (\976) Distribution of
calcium carbonate in surface sediments of the
Atlantic Ocean. J Geophys Res 81(C5): 2595-2603
Boltovskoy E (1991) La destruction des tests de
foraminiferes (experiences de laboratoire). Revue de
Micropaleontologie 34(1): 19-25
Boltovskoy E, Totah VI (1992) Preservation index and
preservation potential of some foraminiferal species.
J Foram Res 22(3): 267-273
Boyle EA (1988) Vertical oceanic nutrient fractionation
and glacial/interglacial CO, cycles. Nature 331:
55-56
Bramlette MN (1961) Pelagic sediments. In: Sears M (ed)
Oceanography. AAAS Publication, New York, 67,
pp345-366
Broecker WS, Peng TH (1982) Tracers in the Sea. Eldigio
Press, New York, pp 1-689
Broecker WS, Takahashi T (1978) The relationship between lysocline depth and in situ carbonate ion concentration. Deep-Sea Res 25F( I): 65-95
Brown SJ, Elderfield H (1996) Variations in Mg/Ca and
Sr/Ca ratios of planktonic foraminifera caused
by postdepositional dissolution: Evidence of shallow Mg-dependent dissolution. Paleoceanography
11(5): 543-551
Chave KE, Suess E (I 970) Calcium carbonate saturation
in sea water: Effects of dissolved organic matter.
Limnol Oceanogr 15: 633-637
CLIMAP Project members (1976) The surface of the iceage earth. Science 191(4232): 1131-1137
CLIMAP Project members (1984) The last interglacial
ocean. Quat Res 21: 123-224
Connary SD, Ewing M (1972) The nepheloid layer and
bottom circulation in the Guinea and Angola Basins.
In: Gordon AL (ed) Studies in physical oceanography: a tribute to Georg Wust on his 80th birthday.
Gordon and Breach, New York, 2, pp 169-184
Corliss BH, Honjo S (1981) Dissolution of deep-sea
benthic foraminifera. Micropaleontology 27(4):
356-378
Culkin F (\965) The major ion components of seawater.
In: Riley JP, Skirrow G (eds) Chemical Oceanography. Academic Press, New York, 1, pp 121-162
Curry WB, Lohmann GP (1990) Reconstructing past
particle fluxes in the tropical Atlantic Ocean.
Paleoceanography 5: 487-506
De Vernal A, Bilodeaul G, Hillaire-Marcel C, Kassou N
(1992) Quantitative Assessment of Carbonate Dissolution in Marine Sediments from Foraminifer Linings vs. Shell Ratios: Davis Strait, Northwest North
Atlantic. Geology 20: 527-530
Diester-Haass L, Muller PJ (1979) Processes influencing sand fraction composition and organic matter
content in surface sediments offW Africa (l2-19°N).
"Meteor" Forsch Ergebn C 31: 21-47