Skip to main content

Advertisement

Log in

Pliocene warmth and gradients

  • Correspondence
  • Published:

From Nature Geoscience

View current issue Submit your manuscript

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Figure 1: Reconstructed and simulated mid-Pliocene SST changes from pre-industrial conditions.

References

  1. Fedorov, A. V. et al. Nature 496, 43–49 (2013).

    Article  Google Scholar 

  2. O'Brien, C. L. et al. Nature Geosci. 7, 606–611 (2014).

    Article  Google Scholar 

  3. Wara, M. W., Ravelo, A. C. & Delaney, M. L. Science 309, 758–761 (2005).

    Article  Google Scholar 

  4. Dowsett, H. J., Robinson, M. M., Stoll, D. K. & Foley, K. M. Stratigraphy 7, 189–198 (2010).

    Google Scholar 

  5. Zhang, Y. G., Pagani, M. & Liu, Z. Science 344, 84–87 (2014).

    Article  Google Scholar 

  6. Dekens, P. S., Ravelo, A. C., McCarthy, M. D. & Edwards, C. A. Geochem. Geophys. Geosyst. 9, Q10001 (2008).

    Article  Google Scholar 

  7. Haywood, A. M. et al. Clim. Past 9, 191–209 (2013).

    Article  Google Scholar 

  8. Pagani, M., Liu, Z., LaRiviere, J. & Ravelo, A. C. Nature Geosci. 3, 27–30 (2009).

    Article  Google Scholar 

  9. Brierley, C. et al. Science 323, 1714–1718 (2009).

    Article  Google Scholar 

  10. Pagani, M. Nature Geosci. 7, 555–556 (2014).

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Chris Brierley.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Brierley, C., Burls, N., Ravelo, C. et al. Pliocene warmth and gradients. Nature Geosci 8, 419–420 (2015). https://doi.org/10.1038/ngeo2444

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/ngeo2444

  • Springer Nature Limited

This article is cited by

Navigation