Abstract
Precise and detailed measurements have been made of the 13C content of both planktonic and benthic foraminifera in core V 19-30. Using the approach developed by Broecker, a record of atmospheric CO2 concentration during the past 120,000 years has been derived which provides independent confirmation that the CO2 concentration in the glacial-age atmosphere was much lower than it is today.
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References
Kroopnick, P. M., Margolis, S. V. & Wong, C. S. in The Fate of Fossil Fuel CO2 in The Oceans (eds Anderson, R. L. N. & Malahoff, A.) 295–321 (Plenum, New York, 1977).
Broecker, W. S. Progr. Oceanogr. 11, 151–197 (1982).
Delmas, R. J., Ascensiom, J.-M. & Legrand, M. Nature 284, 155–157 (1980).
Neftel, A., Oeschger, H., Schwander, J., Stauffer, B. & Zumbrunn, R. Nature 295, 220–223 (1982).
Shackleton, N. J. in The Fate of Fossil Fuel CO2 in The Oceans (eds Anderson, N. R. & Malahoff, A.) 401–427 (Plenum, New York, 1977).
Ninkovich, D. & Shackleton, N. J. Earth planet. Sci. Lett. 27, 20–34 (1975).
Fairbanks, R. G., Sverdlove, M., Free, R., Wiebe, P. H. & Be, A. W. H. Nature 298, 841–844 (1982).
Berger, W. H., Killingley, J. S. & Vincent, E. Oceanol. Acta 1, 203–216 (1978).
Shackleton, N. J. & Opdyke, N. D. Quat. Res. 3, 39–55 (1973).
Shackleton, N. J. Proc. R. Soc. B280, 169–182 (1969).
Graham, D. W., Corliss, B. H., Bender, M. L. & Keigwin, L. D. Jr Mar. Micropalaeont. 6, 483–497 (1980).
Bloom, A. L., Broecker, W. S., Chappell, J. M. A., Matthews, R. K. & Mesolella, K. J. Quat. Res. 4, 185–205 (1974).
Shackleton, N. J., Hall, M. A. & Imbrie, J. Earth planet. Sci. Lett. (in the press).
Pedersen, T. F. Geology 11, 16–19 (1983).
Hays, J. D., Imbrie, J. & Shackleton, N. J. Science 194, 1121–1132 (1976).
Keir, R. S. & Berger, W. H. J. geophys. Res. 88, 6027–6038 (1983).
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Shackleton, N., Hall, M., Line, J. et al. Carbon isotope data in core V19-30 confirm reduced carbon dioxide concentration in the ice age atmosphere. Nature 306, 319–322 (1983). https://doi.org/10.1038/306319a0
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DOI: https://doi.org/10.1038/306319a0
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