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Glacial cycles

Atmosphere and ocean chemistry

Nature Geoscience volume 3, pages 386387 (2010) | Download Citation

Low atmospheric carbon dioxide concentrations during glacial periods must have been accompanied by changes in surface-ocean carbonate chemistry. But it is unclear whether concurrent changes in the deep sea contributed to the glacial carbon dioxide decline.

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Author information

Affiliations

  1. Richard E. Zeebe is in the School of Ocean and Earth Science and Technology, Department of Oceanography, University of Hawaii at Manoa, 1000 Pope Road, MSB 504, Honolulu, Hawaii 96822, USA  zeebe@soest.hawaii.edu

    • Richard E. Zeebe
  2. Thomas M. Marchitto, Jr is in the Department of Geological Sciences and INSTAAR, University of Colorado, Boulder, INSTAAR, Campus Box 450, Boulder, Colorado 80309-0450, USA.  tom.marchitto@colorado.edu

    • Thomas M. Marchitto Jr

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DOI

https://doi.org/10.1038/ngeo882

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