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Reconstruction of atmospheric CO2 from ice-core data and the deep-sea record of ontong Java plateau: the Milankovitch chron

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Abstract

We provide a reconstruction of atmospheric CO2 from deep-sea sediments, for the past 625000 years (Milankovitch chron). Our database consists of a Milankovitch template of sea-level variation in combination with a unique data set for the deep-sea record for Ontong Java plateau in the western equatorial Pacific. We redate the Vostok ice-core data of Barnola et al. (1987). To make the reconstructions we employ multiple regression between deep-sea data, on one hand, and ice-core CO2 data in Antarctica, on the other. The patterns of correlation suggest that the main factors controlling atmospheric CO2 can be described as a combination of sea-level state and sea-level change. For best results squared values of state and change are used. The square-of-sea-level rule agrees with the concept that shelf processes are important modulators of atmospheric CO2 (e.g., budgets of shelf organic carbon and shelf carbonate, nitrate reduction). The square-of-change rule implies that, on short timescales, any major disturbance of the system results in a temporary rise in atmospheric CO2.

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Authors and Affiliations

  1. Scripps Institution of Oceanography, University of California, 92093-0215, San Diego, California, USA

    Wolfgang H. Berger & Memorie K. Yasuda

  2. Geowissenschaften, Universität Bremen, D-28334, Bremen, Germany

    Torsten Bickert & Gerold Wefer

Authors
  1. Wolfgang H. Berger
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  2. Memorie K. Yasuda
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  3. Torsten Bickert
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  4. Gerold Wefer
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Berger, W.H., Yasuda, M.K., Bickert, T. et al. Reconstruction of atmospheric CO2 from ice-core data and the deep-sea record of ontong Java plateau: the Milankovitch chron. Geol Rundsch 85, 466–495 (1996). https://doi.org/10.1007/BF02369003

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  • DOI: https://doi.org/10.1007/BF02369003

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