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What Caused the Glacial to Interglacial CO2 Change?

  • Conference paper
The Global Carbon Cycle

Part of the book series: NATO ASI Series ((ASII,volume 15))

Abstract

Scenarios put forward to explain the 80 µatm glacial to interglacial change in atmospheric CO2 content are evaluated. The conclusion is that no single mechanism is adequate. Rather, contributions from temperature, sea ice, biologic pumping, nutrient deepening, and CаCOз cycling must be called upon. The observation that the 13C/12C ratio for Antarctic foraminifera was 0.9±0.1‰ lower during glacial than during interglacial time constitutes a huge fly in the ointment for all scenarios proposed to date.

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Author information

Authors and Affiliations

  1. Lamont-Doherty Geological Observatory of Columbia University, 10964, Palisades, NY, USA

    W. S. Broecker & T.-H. Peng

  2. Environmental Sciences Divison, Oak Ridge National Laboratory, 37830, Oak Ridge, TN, USA

    T.-H. Peng

Authors
  1. W. S. Broecker
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  2. T.-H. Peng
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Editor information

Editors and Affiliations

  1. Max-Planck Institut für Meteorologie, Bundesstrasse 55, D-20146, Hamburg, Germany

    Martin Heimann

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© 1993 Springer-Verlag Berlin Heidelberg

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Broecker, W.S., Peng, TH. (1993). What Caused the Glacial to Interglacial CO2 Change?. In: Heimann, M. (eds) The Global Carbon Cycle. NATO ASI Series, vol 15. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-84608-3_4

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  • DOI: https://doi.org/10.1007/978-3-642-84608-3_4

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-84610-6

  • Online ISBN: 978-3-642-84608-3

  • eBook Packages: Springer Book Archive

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