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Palaeoclimate

Hidden glacial carbon

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Atmospheric CO2 levels were much lower during the last glacial maximum than in the pre-industrial period. Ice-core data and biogeochemical modelling suggest that difference is partly due to the greater mass of inert carbon in glacial terrestrial biomes.

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Figure 1: Carbon partitioned.

References

  1. Ciais, P. et al. Nature Geosci. 5, 74–79 (2012).

    Article  Google Scholar 

  2. Prentice, I. C. et al. J. Biogeogr. 27, 507–519 (2000).

    Article  Google Scholar 

  3. Tarasov, P. et al. J. Biogeogr. 27, 609–620 (2000).

    Article  Google Scholar 

  4. Elenga, H. et al. J. Biogeogr. 27, 621–634 (2000).

    Article  Google Scholar 

  5. Marchant, R. et al. Clim. Past 5, 725–767 (2009).

    Article  Google Scholar 

  6. Welp, L. R. et al. Nature 477, 579–582 (2011).

    Article  Google Scholar 

  7. Beer, J. et al. Science 329, 834–838 (2010).

    Article  Google Scholar 

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Correspondence to Martin Claussen.

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Claussen, M. Hidden glacial carbon. Nature Geosci 5, 6–7 (2012). https://doi.org/10.1038/ngeo1351

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