488
Andersen et al.
Samthein M, Winn K, Duplessy J-C, Fontugne M (1988)
Global variations of surface ocean productivity in
low and mid latitudes: influence on CO 2 reservoirs
of the deep ocean and atmosphere during the last
21,000 years. Paleoceanography 3: 361-399
Schneider R (1991) Spiitquartiire Produktivitiitsanderungen im iistlichen Angola-Becken: Reaktion
auf Variationen im Passat-Monsun-Windsystem
und in der Advektion des Benguela-Kustenstroms.
Ber Fachber Geowiss Univ Bremen 21, pp 1-198
Schneider RR, Muller PJ, Wefer G (1994) Late Quaternary paleoproductivity changes off the Congo deduced from stable carbon isotopes of planktonic
foraminifera. Palaeogeogr Palaeoclimatol Palaeoecol
110: 255-274
Schneider RR, Millier PJ, Ruhland G (1995) Late Quaternary surface circulation in the east equatorial south
Atlantic: evidence from alkenone sea surface temperatures. Paleoceanography 10: 197-219
Siegenthaler U, Sarmiento JL (1993) Atmospheric carbon dioxide and the ocean. Nature 365: 119-125
Skirrow G (1975) The dissolved gases - carbon dioxide.
In: Riley JP, Skirrow G (eds) Chemical Oceanogr, Vol
2, 2nd edition, Academic Press, New York, pp 1-192
Takahashi K, WadaE, Sakamoto M (1991) Relationship
between carbon isotope discrimination and the specific growth rate of green algae Chlamydomonas
reinhardtii. JpnJLimnol52: 105-112.
Takahashi T, Tans PP, Fung I (1992) Balancing the
budget - Carbon dioxide sources and sinks, and the
effects ofindustry. Oceanus 35: 18-28
Takahashi T, Olafsson J, Goddard JG, Chipman DW,
Sutherland SC (1993) Seasonal variations of CO 2 and
nutrients in the high-latitude surface oceans: a comparative study. Global Biogeochem Cycles 7: 843-878
Taylor AH, Watson AJ, Ainsworth M, Robertson JE,
Turner DR (1991) A modelling investigation of the
role of phytoplankton in the balance of carbon at the
surface of the North Atlantic. Global Biogeochem
Cycles 5: 151-171
Thompson PA, Calvert SE (1994) Carbon isotope
fractionation by a marine diatom: the influence of
irradiance, daylength, pH, and nitrogen source.
LimnolOceanogr 39: 1835-1844
Thompson PA, Calvert SE (1995) Carbon isotope
fractionation by Emiliania huxleyi Limnol Oceanogr
40(4): 673-679
Thunell RC, Qingmin M, Calvert SE, Pedersen TF (1992)
Glacial-holocene biogenic sedimentation patterns in
the South China Sea: productivity variations and
surface water pC0 2 • Paleoceanography 7: 143-162
Volkman JK, Comer EDS, Eglinton G (1980) Transfonnations ofbiolipids in the marine food web and in underlying bottom sediments. Collog.Int. du CNRS 293,
Biogeochimie de la Matiere Organique a l'Interface
Eau-Sediment Marin, pp 185-197
Watson AJ, Robinson C, Robertson JE, Williams PJ Ie
B, Fasham MJR (1991) Spatial variability in the
sink for atmospheric carbon dioxide in the North
Atlantic. Nature 350: 50-53
Wefer G, cruise participants (1988) Bericht uber die
METEOR-FahrtM 6-6, Libreville -Las Palmas, 18.2.23.3.1988. Ber Fachber Geowiss Univ Bremen 3,
pp 1-97
Weiss RF (1974) Carbon dioxide in water and seawater:
The solubility of an non-ideal gas. Mar Chern 2:
203-215
WeissRF, Van WoyFA, SaiamehPK(1992)Surfacewater and atmospheric carbon dioxide and nitrous observations by shipboard automated gas chromatography: Results from expeditions between 1977 and
1990. Scripps Institution of Oceanography Reference, 92-11. ORNLlCDIAC-59, NDP-044. Carbon
Dioxide Information Analysis Center, Oak Ridge
National Laboratory, Oak Ridge, Tennessee,
pp 1-144
Westerhausen L, Samthein M, Struck U, Erlenkeuser H,
Poynter J (1994) PC0 2 variations of Equatorial surface waters over the last 330,000 years: the CS 13 C
record of organic carbon. In: Zalm R et al. (eds) Carbon Cycling in the Glacial Ocean: Constraints on the
Ocean's Role in Global Change, NATO ASI Series I
17, Springer, Berlin Heidelberg New York,
pp367-382
Wong WW, Sackett WM (1978) Fractionation of stable
carbon isotopes by marine phytoplankton. Geochim
CosmochimActa2: 243-254
Andersen et al.
Samthein M, Winn K, Duplessy J-C, Fontugne M (1988)
Global variations of surface ocean productivity in
low and mid latitudes: influence on CO 2 reservoirs
of the deep ocean and atmosphere during the last
21,000 years. Paleoceanography 3: 361-399
Schneider R (1991) Spiitquartiire Produktivitiitsanderungen im iistlichen Angola-Becken: Reaktion
auf Variationen im Passat-Monsun-Windsystem
und in der Advektion des Benguela-Kustenstroms.
Ber Fachber Geowiss Univ Bremen 21, pp 1-198
Schneider RR, Muller PJ, Wefer G (1994) Late Quaternary paleoproductivity changes off the Congo deduced from stable carbon isotopes of planktonic
foraminifera. Palaeogeogr Palaeoclimatol Palaeoecol
110: 255-274
Schneider RR, Millier PJ, Ruhland G (1995) Late Quaternary surface circulation in the east equatorial south
Atlantic: evidence from alkenone sea surface temperatures. Paleoceanography 10: 197-219
Siegenthaler U, Sarmiento JL (1993) Atmospheric carbon dioxide and the ocean. Nature 365: 119-125
Skirrow G (1975) The dissolved gases - carbon dioxide.
In: Riley JP, Skirrow G (eds) Chemical Oceanogr, Vol
2, 2nd edition, Academic Press, New York, pp 1-192
Takahashi K, WadaE, Sakamoto M (1991) Relationship
between carbon isotope discrimination and the specific growth rate of green algae Chlamydomonas
reinhardtii. JpnJLimnol52: 105-112.
Takahashi T, Tans PP, Fung I (1992) Balancing the
budget - Carbon dioxide sources and sinks, and the
effects ofindustry. Oceanus 35: 18-28
Takahashi T, Olafsson J, Goddard JG, Chipman DW,
Sutherland SC (1993) Seasonal variations of CO 2 and
nutrients in the high-latitude surface oceans: a comparative study. Global Biogeochem Cycles 7: 843-878
Taylor AH, Watson AJ, Ainsworth M, Robertson JE,
Turner DR (1991) A modelling investigation of the
role of phytoplankton in the balance of carbon at the
surface of the North Atlantic. Global Biogeochem
Cycles 5: 151-171
Thompson PA, Calvert SE (1994) Carbon isotope
fractionation by a marine diatom: the influence of
irradiance, daylength, pH, and nitrogen source.
LimnolOceanogr 39: 1835-1844
Thompson PA, Calvert SE (1995) Carbon isotope
fractionation by Emiliania huxleyi Limnol Oceanogr
40(4): 673-679
Thunell RC, Qingmin M, Calvert SE, Pedersen TF (1992)
Glacial-holocene biogenic sedimentation patterns in
the South China Sea: productivity variations and
surface water pC0 2 • Paleoceanography 7: 143-162
Volkman JK, Comer EDS, Eglinton G (1980) Transfonnations ofbiolipids in the marine food web and in underlying bottom sediments. Collog.Int. du CNRS 293,
Biogeochimie de la Matiere Organique a l'Interface
Eau-Sediment Marin, pp 185-197
Watson AJ, Robinson C, Robertson JE, Williams PJ Ie
B, Fasham MJR (1991) Spatial variability in the
sink for atmospheric carbon dioxide in the North
Atlantic. Nature 350: 50-53
Wefer G, cruise participants (1988) Bericht uber die
METEOR-FahrtM 6-6, Libreville -Las Palmas, 18.2.23.3.1988. Ber Fachber Geowiss Univ Bremen 3,
pp 1-97
Weiss RF (1974) Carbon dioxide in water and seawater:
The solubility of an non-ideal gas. Mar Chern 2:
203-215
WeissRF, Van WoyFA, SaiamehPK(1992)Surfacewater and atmospheric carbon dioxide and nitrous observations by shipboard automated gas chromatography: Results from expeditions between 1977 and
1990. Scripps Institution of Oceanography Reference, 92-11. ORNLlCDIAC-59, NDP-044. Carbon
Dioxide Information Analysis Center, Oak Ridge
National Laboratory, Oak Ridge, Tennessee,
pp 1-144
Westerhausen L, Samthein M, Struck U, Erlenkeuser H,
Poynter J (1994) PC0 2 variations of Equatorial surface waters over the last 330,000 years: the CS 13 C
record of organic carbon. In: Zalm R et al. (eds) Carbon Cycling in the Glacial Ocean: Constraints on the
Ocean's Role in Global Change, NATO ASI Series I
17, Springer, Berlin Heidelberg New York,
pp367-382
Wong WW, Sackett WM (1978) Fractionation of stable
carbon isotopes by marine phytoplankton. Geochim
CosmochimActa2: 243-254