News & Views | Published:

Palaeoclimate

Carbon–ocean gateway links

Nature Geoscience volume 10, pages 164165 (2017) | Download Citation

A global cooling trend culminated in the glaciation of Antarctica during the Eocene–Oligocene transition. Simulations suggest that ocean circulation changes and enhanced drawdown of atmospheric carbon dioxide can explain this climate shift.

Access optionsAccess options

Rent or Buy article

Get time limited or full article access on ReadCube.

from$8.99

All prices are NET prices.

References

  1. 1.

    , , & Nat. Geosci. 10, 213–216 (2017).

  2. 2.

    , & Earth Planet. Sci. Lett. 242, 343–353 (2006).

  3. 3.

    et al. Nature 523, 580–584 (2015).

  4. 4.

    J. Geophys. Res. 82, 3843–3860 (1977).

  5. 5.

    , , & Earth Planet. Sci. Lett. 236, 459–470 (2005).

  6. 6.

    & Science 312, 428–430 (2006).

  7. 7.

    , & Paleoceanography 29, 308–327 (2014).

  8. 8.

    & Nature 421, 245–249 (2003).

  9. 9.

    , , , & Science 309, 600–603 (2005).

  10. 10.

    et al. Nature 455, 652–657 (2008).

  11. 11.

    , & Nature 461, 1110–1113 (2009).

  12. 12.

    & Earth Planet. Sci. Lett. 210, 151–165 (2003).

  13. 13.

    & Proc. Natl Acad. Sci. USA 105, 16065–16070 (2008).

  14. 14.

    et al. in Proceedings of the Integrated Ocean Drilling Program (eds Norris, R. D., Wilson, P. A., Blum, P. & Expedition 342 Scientists) Vol. 342 (Integrated Ocean Drilling Program, 2014).

Download references

Author information

Affiliations

  1. Howie Scher is at the School of the Earth, Ocean and Environment, University of South Carolina, 701 Sumter Street, Columbia, South Carolina 29208, USA

    • Howie Scher

Authors

  1. Search for Howie Scher in:

Corresponding author

Correspondence to Howie Scher.

About this article

Publication history

Published

DOI

https://doi.org/10.1038/ngeo2895

Newsletter Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing