Reconstruction of Surface Ocean Nitrate Utilization
467
Pedersen TF (eds) Carbon Cycling in the Glacial
Ocean: Constraints on the Ocean's Role in Global
Change. Springer, Berlin Heidelberg New York,
pp259-279
Montoya JP, McCarthy JJ (1995) Isotopic fractionation
during nitrate uptake by phytoplankton grown in
continuous cultures. J Plankton Res 17: 436-464
Montoya JP, Wiebe PH, McCarthy JJ (1992) Natural
abundance of 15N in particulate nitrogen and
zooplankton in the Gulf Stream region and WannCore Ring 86A. Deep-Sea Res 39: 363-392
Moroshkin KV, Bubnov VA, Bulatov RP (1970) Water
circulation in the eastern South Atlantic. OceanologyIO:27-34
MUller PJ, Schneider R, Ruhland G (1994) Late Quaternary pCO z variations in the Angola Current: Evidence
from organic carbon /inc and alkenone temperatures.
In: Zahn R, Kaminski MA, Labeyrie L, Pedersen TF
(eds) Carbon Cycling in the Glacial Ocean: Constraints on the Ocean's Role in Global Change.
NATO ASI Series, Vol 17, Springer, Berlin Heidelberg
New York, pp 343-366
Nakatsuka T, HaradaN, MatsumotoE, HandaN, Oba T,
Ikehara M, Matsuoka H, Kimoto K (1995a) Glacialinterglacial migration of an upwelling field in the western equatorial Pacific recorded by sediment ISNf1 4 N.
Geophys Res Lett 22: 2525-2528
Nakatsuka T, Watanabe K, Handa N, Matsumoto E,
Wada E (1995b) Glacial to interglacial surface nutrient variations of Bering deep basins recorded by
/i 13 C and /ilsN of sedimentary organic matter.
Paleoceanography 10: 1047-1061
Nakatsuka T, Handa N, Harada N, Sugimoto T, Imaizumi
S (1997) Origin and decomposition of sinking
particulate organic matter in the deep water column
inferred from the vertical distributions of its /ilsN,
/inC and /i 14 C. Deep-Sea Res I 44: 1957-1979
Ostrom NE, Macko SA, DeibeID, Thompson RJ (1997)
Seasonal variation in the stable carbon and nitrogen
isotope biogeochemistry of a coastal cold ocean
environment. Geochim Cosmochim Acta 61:
2929-2942
Owens NJP (1985) Variations in the natural abundance
of I'N in estuarine suspended particulate matter: a
specific indicator of biological processing. Est Coast
Shelf Sci 20: 505-510
Packard IT, Garfield PC, Codispoti LA (1983) Oxygen
consumption and denitrification below the Peruvian
upwelling. In: Thiede J, Suess E (eds) Coastal
Upwelling, Its Sediment Record, Part A, Responses
of the Sedimentary Regime to Present Coastal
Upwelling. Plenum, pp 365-398
Pokras EM (1987) Diatom record oflate Quaternary climatic change in the eastern equatorial Atlantic and
tropical Africa. Paleoceanography 2: 273-286
Saino T, Hattori A (1980) ISN natural abundance in oceanic suspended particulate matter. Nature 283:
752-754
Schell DM, Barnett BA, Vinette KA (1998) Carbon and
nitrogen isotope ratios in zooplankton of the Bering,
Chukchi and Beaufort Seas. Mar Ecol Prog Ser
162: 11-23
Schneider RR (1991) Splitquartlire Produktivitlitslinderungen im ostlichen Angola-Becken: Reaktion
aufVariationen 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, MUller PJ, Ruhland G (1995) Late Quaternary surface circulation in the east equatorial South
Atlantic: Evidence from alkenone sea surface temperatures. Paleoceanography 10: 197-219
Schneider RR, Price B, MUller PJ, Kroon D, Alexander I
(1997) Monsoon related Zaire (Congo) sediment load
and influence of fluvial silicate supply on marine
productivity in the east equatorial Atlantic during
the last 200,000 years. Paleoceanography 12(3):
463-481
Schulz M, Stategger K (1997) Spectral analysis of unevenly spaced paleoclimatic time series. Computers
and Geosciences 23(9): 929-945
Servain J, Picaut J, Merle J (1982) Evidence of remote
forcing in the equatorial Atlantic Ocean. J Phys
Oceanogr 12: 457-463
Servain J, Picaut J, Busalacchi AJ (I 985) Interannual and
seasonal variability of the tropical Atlantic ocean
depicted by sixteen years of sea-surface temperature
and wind stress. In: Nihoul JCJ (ed) Coupled OceanAtmosphere Models. Elsevier, pp 211-237
Shannon LV, Agenbag JJ, Buys MEL (I 987) Large- and
mesoscale features ofthe Angola-Benguela front. S
Afr JMar Sci 5: 11-34
Skerman VBD, MacRae JC (1957) The influence of oxygen availability on the degree of nitrate reduction
by Pseudomonas denitr!ficans. Can J Microbiol 3:
505-526
SNEC II (1986) Datos Basicos de la campana
oceanografica SNEC II en las costas de Namibia,
Datos Inf, vol. 18, Gutierrez E, Marrase C, Rubies P
(eds) Telecopia, Barcelona, pp 1-63
467
Pedersen TF (eds) Carbon Cycling in the Glacial
Ocean: Constraints on the Ocean's Role in Global
Change. Springer, Berlin Heidelberg New York,
pp259-279
Montoya JP, McCarthy JJ (1995) Isotopic fractionation
during nitrate uptake by phytoplankton grown in
continuous cultures. J Plankton Res 17: 436-464
Montoya JP, Wiebe PH, McCarthy JJ (1992) Natural
abundance of 15N in particulate nitrogen and
zooplankton in the Gulf Stream region and WannCore Ring 86A. Deep-Sea Res 39: 363-392
Moroshkin KV, Bubnov VA, Bulatov RP (1970) Water
circulation in the eastern South Atlantic. OceanologyIO:27-34
MUller PJ, Schneider R, Ruhland G (1994) Late Quaternary pCO z variations in the Angola Current: Evidence
from organic carbon /inc and alkenone temperatures.
In: Zahn R, Kaminski MA, Labeyrie L, Pedersen TF
(eds) Carbon Cycling in the Glacial Ocean: Constraints on the Ocean's Role in Global Change.
NATO ASI Series, Vol 17, Springer, Berlin Heidelberg
New York, pp 343-366
Nakatsuka T, HaradaN, MatsumotoE, HandaN, Oba T,
Ikehara M, Matsuoka H, Kimoto K (1995a) Glacialinterglacial migration of an upwelling field in the western equatorial Pacific recorded by sediment ISNf1 4 N.
Geophys Res Lett 22: 2525-2528
Nakatsuka T, Watanabe K, Handa N, Matsumoto E,
Wada E (1995b) Glacial to interglacial surface nutrient variations of Bering deep basins recorded by
/i 13 C and /ilsN of sedimentary organic matter.
Paleoceanography 10: 1047-1061
Nakatsuka T, Handa N, Harada N, Sugimoto T, Imaizumi
S (1997) Origin and decomposition of sinking
particulate organic matter in the deep water column
inferred from the vertical distributions of its /ilsN,
/inC and /i 14 C. Deep-Sea Res I 44: 1957-1979
Ostrom NE, Macko SA, DeibeID, Thompson RJ (1997)
Seasonal variation in the stable carbon and nitrogen
isotope biogeochemistry of a coastal cold ocean
environment. Geochim Cosmochim Acta 61:
2929-2942
Owens NJP (1985) Variations in the natural abundance
of I'N in estuarine suspended particulate matter: a
specific indicator of biological processing. Est Coast
Shelf Sci 20: 505-510
Packard IT, Garfield PC, Codispoti LA (1983) Oxygen
consumption and denitrification below the Peruvian
upwelling. In: Thiede J, Suess E (eds) Coastal
Upwelling, Its Sediment Record, Part A, Responses
of the Sedimentary Regime to Present Coastal
Upwelling. Plenum, pp 365-398
Pokras EM (1987) Diatom record oflate Quaternary climatic change in the eastern equatorial Atlantic and
tropical Africa. Paleoceanography 2: 273-286
Saino T, Hattori A (1980) ISN natural abundance in oceanic suspended particulate matter. Nature 283:
752-754
Schell DM, Barnett BA, Vinette KA (1998) Carbon and
nitrogen isotope ratios in zooplankton of the Bering,
Chukchi and Beaufort Seas. Mar Ecol Prog Ser
162: 11-23
Schneider RR (1991) Splitquartlire Produktivitlitslinderungen im ostlichen Angola-Becken: Reaktion
aufVariationen 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, MUller PJ, Ruhland G (1995) Late Quaternary surface circulation in the east equatorial South
Atlantic: Evidence from alkenone sea surface temperatures. Paleoceanography 10: 197-219
Schneider RR, Price B, MUller PJ, Kroon D, Alexander I
(1997) Monsoon related Zaire (Congo) sediment load
and influence of fluvial silicate supply on marine
productivity in the east equatorial Atlantic during
the last 200,000 years. Paleoceanography 12(3):
463-481
Schulz M, Stategger K (1997) Spectral analysis of unevenly spaced paleoclimatic time series. Computers
and Geosciences 23(9): 929-945
Servain J, Picaut J, Merle J (1982) Evidence of remote
forcing in the equatorial Atlantic Ocean. J Phys
Oceanogr 12: 457-463
Servain J, Picaut J, Busalacchi AJ (I 985) Interannual and
seasonal variability of the tropical Atlantic ocean
depicted by sixteen years of sea-surface temperature
and wind stress. In: Nihoul JCJ (ed) Coupled OceanAtmosphere Models. Elsevier, pp 211-237
Shannon LV, Agenbag JJ, Buys MEL (I 987) Large- and
mesoscale features ofthe Angola-Benguela front. S
Afr JMar Sci 5: 11-34
Skerman VBD, MacRae JC (1957) The influence of oxygen availability on the degree of nitrate reduction
by Pseudomonas denitr!ficans. Can J Microbiol 3:
505-526
SNEC II (1986) Datos Basicos de la campana
oceanografica SNEC II en las costas de Namibia,
Datos Inf, vol. 18, Gutierrez E, Marrase C, Rubies P
(eds) Telecopia, Barcelona, pp 1-63