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Oxygen isotopes and sea level

Nature volume 324, pages 137–140 (1986)Cite this article

Abstract

From the time that detailed oxygen isotope records derived from foraminifera living in the constant-temperature environment of the abyssal ocean became available, there has been a discrepancy between the ice volume record that these records imply, and that derived from the altitude of dated coral terraces around the world. Here, we re-examine the data and conclude that the temperature of the abyssal ocean has been an actively varying component of the climate system.

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Authors and Affiliations

  1. Biogeography and Geomorphology, Research School of Pacific Studies, Australian National University, Canberra, Australia

    J. Chappell

  2. Godwin Laboratory for Quaternary Research, University of Cambridge, Free School Lane, Cambridge, CB2 3RS, UK

    N. J. Shackleton

Authors
  1. J. Chappell
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  2. N. J. Shackleton
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Chappell, J., Shackleton, N. Oxygen isotopes and sea level. Nature 324, 137–140 (1986). https://doi.org/10.1038/324137a0

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