The effect of upwelling on the distribution and stable isotope composition of Globigerina bulloides and Globigerinoides ruber (planktic foraminifera) in modern surface waters of the NW Arabian Sea

[1]  S. Noriki,et al.  Isotopic composition and morphology of living Globorotalia scitula: a new proxy of sub-intermediate ocean carbonate chemistry? , 2001 .

[2]  J. Jouzel,et al.  Oxygen isotope/salinity relationship in the northern Indian Ocean , 2001 .

[3]  J. Caulet,et al.  Paleoproductivity changes in the upwelling system of Socotra (Somali Basin, NW Indian Ocean) during the last 72,000years: evidence from biological signatures , 2000 .

[4]  D. Lea,et al.  Temperature influence on the carbon isotopic composition of Globigerina bulloides and Orbulina universa (planktonic foraminifera) , 2000 .

[5]  H. Spero,et al.  Field examination of the oceanic carbonate ion effect on stable isotopes in planktonic foraminifera , 2000 .

[6]  H. Niebler,et al.  The South Atlantic Carbon Isotope Record of Planktic Foraminifera , 1999 .

[7]  R. Zeebe An explanation of the effect of seawater carbonate concentration on foraminiferal oxygen isotopes , 1999 .

[8]  Jelle Bijma,et al.  Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations , 1998 .

[9]  Jelle Bijma,et al.  Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes , 1997, Nature.

[10]  Sang-Tae Kim,et al.  Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates , 1997 .

[11]  J. Duinker,et al.  Strong CO2 emissions from the Arabian Sea during south‐west monsoon , 1997 .

[12]  K. Kohfeld,et al.  Neogloboquadrina pachyderma (sinistral coiling) as paleoceanographic tracers in polar oceans: Evidence from northeast water polynya plankton tows, sediment traps, and surface sediments , 1996 .

[13]  D. Lea,et al.  Experimental determination of stable isotope variability in Globigerina bulloides: implications for paleoceanographic reconstructions , 1996 .

[14]  B. Malmgren,et al.  A High‐resolution record of Late Quaternary upwelling along the Oman Margin, Arabian Sea based on planktonic foraminifera , 1996 .

[15]  F. Millero Thermodynamics of the carbon dioxide system in the oceans , 1995 .

[16]  B. Malmgren,et al.  Monsoon upwelling effects on test size of some planktonic foraminiferal species from the Oman Margin, Arabian Sea , 1995 .

[17]  C. Hemleben,et al.  Population dynamics of the planktic foraminifer Globigerinoides sacculifer (Brady) from the central Red Sea , 1994 .

[18]  F. Millero,et al.  The dissociation constants of carbonic acid in seawater at salinities 5 to 45 and temperatures 0 to 45°C , 1993 .

[19]  D. Anderson,et al.  A 300 KYR Record of Upwelling Off Oman during the Late Quaternary: Evidence of the Asian Southwest Monsoon , 1993 .

[20]  J. Brock,et al.  Southwest Monsoon Circulation and Environments of Recent Planktonic Foraminifera in the Northwestern Arabian Sea , 1992 .

[21]  H. Spero Do planktic foraminifera accurately record shifts in the carbon isotopic composition of seawater ΣCO2 , 1992 .

[22]  A. Dickson Thermodynamics of the dissociation of boric acid in synthetic seawater from 273.15 to 318.15 K , 1990 .

[23]  D. Kroon,et al.  Northern Indian Ocean upwelling cells and the stable isotope composition of living planktonic foraminifers , 1989 .

[24]  R. Fairbanks,et al.  Carbon isotope composition of tropical surface water during the past 22,000 years , 1989 .

[25]  Christoph Hemleben,et al.  Modern Planktonic Foraminifera , 1988, Springer New York.

[26]  DOUGLAS F. Williams,et al.  Extracting environmental information from planktonic foraminiferal δ13C data , 1988, Nature.

[27]  J. Duplessy,et al.  Carbon and oxygen isotopic composition of planktonic foraminifera from laboratory culture, plankton tows and Recent sediment; implications for the reconstruction of paleoclimatic conditions and of the global carbon cycle , 1985 .

[28]  M. Bender,et al.  Tracers in the Sea , 1984 .

[29]  R. Gonfiantini Stable Isotope Reference Samples for Geochemical and Hydrological Investigations , 1984 .

[30]  J. Erez,et al.  Experimental paleotemperature equation for planktonic foraminifera , 1983 .

[31]  C. Kendall,et al.  Comparison of stable isotope reference samples , 1983, Nature.

[32]  R. Fairbanks,et al.  Seasonal stable isotopic variations in living planktonic foraminifera from bermuda plankton tows , 1981 .

[33]  DOUGLAS F. Williams,et al.  Oxygen and carbon isotopic composition of living planktonic foraminifera from the northeast Pacific Ocean , 1981 .

[34]  C. Hemleben,et al.  Seasonal changes in species composition, numbers, mass, size, and isotopic composition of planktonic foraminifera settling into the deep sargasso sea☆ , 1981 .

[35]  J. Erez,et al.  Comparison of isotopic composition of planktonic foraminifera in plankton tows, sediment traps and sediments , 1981 .

[36]  J. Duplessy,et al.  Oxygen and carbon isotopic composition and biogeographic distribution of planktonic foraminifera in the Indian Ocean , 1981 .

[37]  P. Wiebe,et al.  Foraminifera and Chlorophyll Maximum: Vertical Distribution, Seasonal Succession, and Paleoceanographic Significance , 1980, Science.

[38]  Frank J. Millero,et al.  The Thermodynamics of the Carbonate System in Seawater , 1979 .

[39]  N. Shackleton,et al.  Oxygen and carbon isotope studies in recent foraminifera from the southwest Indian ocean , 1978 .

[40]  DOUGLAS F. Williams,et al.  Carbon isotopic compositions of Recent planktonic foraminifera of the Indian Ocean , 1977 .

[41]  R. Weiss Carbon dioxide in water and seawater: the solubility of a non-ideal gas , 1974 .

[42]  Samuel Epstein,et al.  REVISED CARBONATE-WATER ISOTOPIC TEMPERATURE SCALE , 1953 .

[43]  F. Peeters,et al.  The seasonal and vertical distribution of living planktic foraminifera in the NW Arabian Sea , 2002, Geological Society, London, Special Publications.

[44]  Jonathan Craig,et al.  The tectonic and climatic evolution of the Arabian Sea Region. , 2002 .

[45]  G. Brummer,et al.  Fluxes of planktic foraminifera in response to monsoonal upwelling on the Somalia Basin margin. , 2000 .

[46]  C. Moos Reconstruction of upwelling intensity and paleo-nutrient gradients in the northwest Arabian Sea derived from stable carbon and oxygen isotopes of planktic foraminifera. , 2000 .

[47]  D. Lea,et al.  Reassessing foraminiferal stable isotope geochemistry: Impact of the oceanic carbonate system (experimental results) , 1999 .

[48]  R. Healy,et al.  Spatial variation of total CO2 and total alkalinity in the northern Indian Ocean : A novel approach for the quantification of anthropogenic CO2 in seawater , 1999 .

[49]  Gerold Wefer,et al.  Use of proxies in paleoceanography : examples from the South Atlantic , 1999 .

[50]  H. Niebler,et al.  Oxygen Isotope Values of Planktic Foraminifera: A Tool for the Reconstruction of Surface Water Stratification , 1999 .

[51]  B. Malmgren,et al.  Relationship between late Quaternary upwelling history and coiling properties of Neogloboquadrina pachyderma and Globigerina bulloides in the Arabian Sea , 1996 .

[52]  Kevin E. Kohler,et al.  A four-component ecosystem model of biological activity in the Arabian Sea , 1996 .

[53]  R. Mohan,et al.  Seasonal variability of the vertical fluxes of Globigerina bulloides (D'Orbigny) in the northern Indian Ocean , 1996 .

[54]  D. Kroon,et al.  Size and upwelling control of the stable isotope composition of Neogloboquadrina dutertrei (d'Orbigny), Globigerinoides ruber (d'Orbigny) and Globigerina bulloides d'Orbigny; examples from the Panama Basin and Arabian Sea , 1995 .

[55]  C. Hemleben,et al.  Foraminiferal Population Dynamics And Stable Carbon Isotopes , 1994 .

[56]  V. Ittekkot,et al.  Foraminiferal production and monsoonal upwelling in the Arabian Sea: evidence from sediment traps , 1992, Geological Society, London, Special Publications.

[57]  D. Kroon,et al.  Oxygen and carbon isotopes in planktonic foraminifera as indicators of upwelling intensity and upwelling-induced high productivity in sediments from the northwestern Arabian Sea , 1992, Geological Society, London, Special Publications.

[58]  R. Thunell,et al.  Planktonic foraminiferal faunal and stable isotopic indices of upwelling: a sediment trap study in the San Pedro Basin, Southern California Bight , 1992, Geological Society, London, Special Publications.

[59]  M. J. Deniro,et al.  The influence of symbiont photosynthesis on the δ18O and δ13C values of planktonic foraminiferal shell calcite , 1987 .

[60]  Wl Prell,et al.  Faunal and isotopic indices of monsoonal upwelling - western arabian sea , 1981 .

[61]  Michael I. Kahn Non-equilibrium oxygen and carbon isotopic fractionation in tests of living planktonic-foraminifera , 1979 .

[62]  E. Vincent,et al.  Sable isotopes in deep-sea carbonates - box core erdc-92, west equatorial pacific , 1978 .

[63]  N. Shackleton Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus Uvigerina: isotopic changes in the ocean during the last glacial , 1974 .

[64]  K. Wyrtki,et al.  Oceanographic atlas of the International Indian Ocean Expedition , 1971 .

[65]  H. Craig,et al.  Deuterium and oxygen 18 variations in the ocean and marine atmosphere , 1965 .