The δ¹³C content of calcareous nannofossils as an indicator of Quaternary paleoproductivity in the Southwest Pacific region

References

• Anderson , T. F. and Steinmetz , J. C. 1981 . Isotopic and biostratigraphical records of calcareous nannofossils in a Pleistocene core . Nature , 294 : 741 – 744 .
   Google Scholar
• Anderson , T. F. and Steinmetz , J. C. 1983 . Stable isotopes in calcareous nannofossils: potential application to deep-sea paleo-environmental reconstructions during the Quaternary . Utrecht micropaleotological bulletin , 30 : 189 – 204 .
   Google Scholar
• Barton C. E. Bloemendal J. Paleomagnetism of sediments collected during Leg 90, southwest Pacific Initial reports of the Deep Sea Drilling Project Kennett J. P. et al. U.S. Government Printing Office Washington 1986 90 1273 1316 in
   Google Scholar
• Bouvier-Soumagnac , Y. 1985 . 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 , Jerusalem : Lodged in the Library, Hebrew University . Unpublished M. Sc. thesis
   Google Scholar
• Bradford , J. M. and Roberts , P. E. 1978 . Distribution of reactive phosphorus and plankton in relation to upwelling and surface circulation around New Zealand . New Zealand journal of marine and freshwater research , 12 : 1 – 15 .
   Web of Science ®Google Scholar
• Broecker , W. S. 1982 . “ Glacial and interglacial changes in ocean chemistry ” . In Climatic variability in the oceans. Progress in oceanography Edited by: Kraus , E. B. and Hanson , H. P. Vol. 11 , 151 – 197 . in
   Google Scholar
• CLIMAP Project Members . 1976 . The surface of the ice-age Earth . Science , 191 : 1131 – 1137 .
   PubMed Web of Science ®Google Scholar
• Craig , H. 1970 . Abyssal carbon-13 in the South Pacific . Journal of geophysical research , 75 : 691 – 695 .
   Google Scholar
• Dal Pont , G. and Newell , B. 1963 . Suspended organic matter in the Tasman Sea . Australian journal of marine and freshwater research , 14 : 155 – 165 .
   Google Scholar
• Dudley , W. C. , Blackwelder , P. L. , Brand , L. E. and Duplessy , J. C. 1986 . Stable isotopic composition of coccoliths . Marine micropaleontology , 10 : 1 – 8 .
   Google Scholar
• Duplessy , J. C. 1982 . Circulation des eaux profondes nord Atlantiques au cours du dernier cycle climatique . Bulletin Institute geologie bassin d'Aquitaine, Bordeaux , 31 : 379 – 391 .
   Google Scholar
• Duplessy , J. C. and Shackleton , N. J. 1985 . Response of global deep-water circulation to Earth's climate change 135 000–107 000 years ago . Nature , 316 : 500 – 507 .
   Web of Science ®Google Scholar
• Duplessy , J. C. , Blanc , P. L. and Bé , A. W. H. 1981 . Oxygen-18 enrichment of planktonic foraminifera due to gametogenic calcification below the euphotic zone . Science , 213 : 1247 – 1250 .
   PubMed Web of Science ®Google Scholar
• Duplessy , J. C. , Shackleton , N. J. , Matthews , R. K. , Prell , W. , Ruddiman , W. F. , Caralp , M. and Hendy , C. H. 1984 . 13C record of benthic foraminifera in the last interglacial ocean: implications for the carbon cycle and the global deep water circulation . Quaternary research , 21 : 225 – 243 .
   Google Scholar
• Jenkins , C. J. 1985 . “ Erosion and deposition at abyssal depths in the Tasman Sea: a seismic stratigraphic study of bottom-current patterns ” . In The University of Sydney Ocean Sciences Institute report Vol. 4 , 53 p
   Google Scholar
• Kahn , M. I. and Williams , D. F. 1981 . Oxygen and carbon isotopic composition of living planktonic foraminifera from the northeast Pacific Ocean . Palaeogeography, palaeoclimatology, palaeoecology , 33 : 47 – 69 .
   Web of Science ®Google Scholar
• Kroopnick , P. 1974 . The dissolved O2-CO2-13C system in the eastern equatorial Pacific . Deep-sea research , 27 : 211 – 227 .
   Google Scholar
• Kroopnick , P. 1985 . The distribution of C-13 of T CO2 in the world oceans . Deep-sea research , 32 : 57 – 84 .
   Google Scholar
• Labeyrie , L. D. and Duplessy , J. C. 1985 . Changes in the oceanic 13C/12C ratio during the last 140 000 years: high-latitude surface water records . Palaeogeography, palaeoclimatology, palaeo-ecology , 50 : 217 – 240 .
   Google Scholar
• Margolis , S. V. , Kroopnick , P. M. , Goodney , D. E. , Dudley , W. C. and Mahoney , M. 1975 . Oxygen and carbon isotopes from calcareous nannofossils as paleoclimatic indicators . Science , 189 : 555 – 557 .
   PubMed Web of Science ®Google Scholar
• Nelson C. S. Hendy C. H. Dudley W. C. Quaternary isotope stratigraphy of Hole 593, Challenger Plateau, south Tasman Sea: preliminary observations based on foraminifers and calcareous nannofossils Initial reports of the Deep Sea Drilling Project Kennett J. P. et al. U.S. Government Printing Office Washington 1986 90 1413 1424 in
   Google Scholar
• Okada , H. and Honjo , S. 1973 . The distribution of oceanic coccolithophorids in the Pacific . Deep-sea research , 20 : 355 – 374 .
   Google Scholar
• Schiffelbein , P. A. and Thierstein , H. R. 1981 . Late Pleistocene coccolith isotope stratigraphy: effects of floral change . EOS transactions of the American Geophysical Union , 62 : 938 – 938 .
   Google Scholar
• Shackleton , N. J. 1977 . “ Carbon 13 in Uvigerina: Tropical rainforest history and the equatorial Pacific carbonate dissolution cycles ” . In The fate of fossil fuel CO₂ in the oceans , Edited by: Anderson , R. L. N. and Malahoff , A. 401 – 427 . New York : Plenum . in
   Google Scholar
• Valencia , M. J. 1977 . Pacific Pleistocene paleoclimatic stratigraphies: a comparative analysis of results . Quaternary research , 8 : 339 – 354 .
   Google Scholar
• Volat , J-L. , Pastouret , L. and Vergnaud-Grassini , C. 1980 . Dissolution and carbonate fluctuations in Pleistocene deep-sea cores: a review . Marine geology , 34 : 1 – 28 .
   Google Scholar