Chemical Hydrography of the South Atlantic During the Last Glacial Maximum: Cd vs. δ13C

[1]  E. Yu,et al.  Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data , 1996, Nature.

[2]  E. Boyle,et al.  CALCITIC FORAMINIFERAL DATA CONFIRMED BY CADMIUM IN ARAGONITIC HOEGLUNDINA: APPLICATION TO THE LAST GLACIAL MAXIMUM IN THE NORTHERN INDIAN OCEAN , 1995 .

[3]  E. Boyle,et al.  Glacial enrichments of authigenic Cd And U in subantarctic sediments: A climatic control on the elements' oceanic budget? , 1995 .

[4]  E. Boyle,et al.  Authigenic cadmium enrichments in suboxic sediments: Precipitation and postdepositional mobility , 1995 .

[5]  Y. Rosenthal,et al.  Cd/Ca changes in a Deep Cape Basin Core over the past 730,000 years: Response of circumpolar deepwater variability to northern hemisphere ice sheet melting? , 1994 .

[6]  R. Jahnke,et al.  Evidence for enhanced phosphorus regeneration from marine sediments overlain by oxygen depleted waters , 1994 .

[7]  L. Keigwin,et al.  Depth profiles of δ13C in bottom water and core top C. wuellerstorfi on the Ontong Java Plateau and Emperor Seamounts , 1994 .

[8]  R. Fairbanks,et al.  Thermodynamic influences on the marine carbon isotope record , 1993 .

[9]  A. Mackensen,et al.  The δ13C in benthic foraminiferal tests of Fontbotia wuellerstorfi (Schwager) Relative to the δ13C of dissolved inorganic carbon in Southern Ocean Deep Water: Implications for glacial ocean circulation models , 1993 .

[10]  W. Broecker.  An Oceanographic Explanation for the Apparent Carbon Isotope‐Cadmium Discordancy in the Glacial Antarctic? , 1993 .

[11]  W. Broecker,et al.  The influence of air and sea exchange on the carbon isotope distribution in the sea , 1992 .

[12]  E. Jansen,et al.  Evidence for a bathyal front at 2000‐M depth in the glacial Pacific, based on a depth transect on Ontong Java Plateau , 1992 .

[13]  Richard G. Fairbanks,et al.  Evidence from Southern Ocean sediments for the effect of North Atlantic deep-water flux on climate , 1992, Nature.

[14]  R. Keir.  The effect of vertical nutrient redistribution on surface ocean δ13C , 1991 .

[15]  W. Berger,et al.  Paleoproductivity from benthic foraminifera abundance: Glacial to postglacial change in the west-equatorial Pacific , 1991 .

[16]  E. Boyle,et al.  Deglacial meltwater discharge, North Atlantic Deep Circulation, and abrupt climate change , 1991 .

[17]  A. Mix,et al.  Carbon 13 in Pacific deep and intermediate waters, 0-370 ka : implications for ocean circulation and Pleistocene CO2 , 1991 .

[18]  A. Gordon,et al.  Late Pleistocene Southern Ocean δ13C variability , 1990 .

[19]  Peter N. Schweitzer,et al.  Globorotalia truncatulinoides' Growth and chemistry as probes of the past thermocline: 1. Shell size , 1990 .

[20]  Laurent Labeyrie,et al.  The Last Deglaciation in the Southern Ocean , 1989 .

[21]  E. Boyle.  Cadmium: Chemical tracer of deepwater paleoceanography , 1988 .

[22]  J. Duplessy,et al.  Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the Holocene , 1988 .

[23]  Michael Sarnthein,et al.  Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years , 1988 .

[24]  M. Sarnthein,et al.  Benthic Isotope Evidence for Changes of the Mediterranean Outflow During the Late Quaternary , 1987 .

[25]  U. Förstner,et al.  Effect of sample pretreatment on the reliability of solid speciation data of heavy metals — implications sesfor the study of early diagenetic processes☆ , 1987 .

[26]  Edward A. Boyle,et al.  Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years : changes in deep ocean circulation and chemical inventories , 1985 .

[27]  J. Duplessy,et al.  13C Record of Benthic Foraminifera in the Last Interglacial Ocean: Implications for the Carbon Cycle and the Global Deep Water Circulation , 1984, Quaternary Research.

[28]  J. Reid,et al.  Abyssal characteristics of the World Ocean waters , 1983 .

[29]  M. Stuiver,et al.  Abyssal Water Carbon-14 Distribution and the Age of the World Oceans , 1983, Science.

[30]  E. Boyle,et al.  Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence , 1982, Science.

[31]  M. Bender,et al.  Carbon and oxygen isotopic disequilibria of recent deep-sea benthic foraminifera☆ , 1981 .

[32]  E. Boyle,et al.  On the Distribution of Copper, Nickel, and Cadmium in the Surface Waters of the North Atlantic , 1981 .

[33]  Edward A. Boyle,et al.  Cadmium, zinc, copper, and barium in foraminifera tests , 1981 .

[34]  W. Berger,et al.  Stable isotope composition of benthic foraminifera from the equatorial Pacific , 1981, Nature.

[35]  DOUGLAS F. Williams,et al.  The Early Nonstructural Chemical Diagenesis of Foraminiferal Calcite , 1977 .

[36]  E. Boyle.  LIMITS ON BENTHIC FORAMINIFERAL CHEMICAL ANALYSES AS PRECISE MEASURES OF ENVIRONMENTAL PROPERTIES , 1995 .

[37]  J. Erez,et al.  URANIUM IN FORAMINIFERAL CALCITE AS A RECORDER OF SEAWATER URANIUM CONCENTRATIONS , 1994 .

[38]  Y. Rosenthal.  Late quaternary paleochemistry of the Southern Ocean : evidence from cadmium variablity in sediments and foraminifera , 1994 .

[39]  E. Boyle.  Isotopic and elemental tracers in calcium carbonate fossils , 1994 .

[40]  E. Boyle.  A Comparison of Carbon Isotopes and Cadmium in the Modern and Glacial Maximum Ocean: Can We Account for the Discrepancies? , 1994 .

[41]  E. Boyle,et al.  Factors controlling the fluoride content of planktonic foraminifera: An evaluation of its paleoceanographic applicability , 1993 .

[42]  E. Boyle.  Cadmium and delta13C Paleochemical Ocean Distributions During the Stage 2 Glacial Maximum , 1992 .

[43]  P. Kroopnick.  The distribution of 13C of ΣCO2 in the world oceans , 1985 .

[44]  T. Pedersen.  Increased productivity in the eastern equatorial Pacific during the last glacial maximum (19,000 to 14,000 yr B.P) , 1983 .