Skip to main content

Advertisement

Log in

Palaeoclimate

A balmy Arctic

  • News & Views
  • Published:

From Nature

View current issue Submit your manuscript

Analyses of sediments retrieved from a drifting ice island suggest that the Arctic Ocean may have been ice free and as warm as 15 °C about 70 million years ago. Therein is a challenge for climate models.

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: Average annual sea surface temperature for the Cretaceous predicted by an ocean–atmosphere climate model.

References

  1. Jenkyns, H. C., Forster, A., Schouten, S. & Sinninghe Damsté, J. S. Nature 432, 888–892 (2004).

    Article  ADS  CAS  Google Scholar 

  2. Schouten, S., Hopmans, E., Schefuß, E. & Sinninghe Damsté, J. S. Earth Planet. Sci. Lett. 204, 265–274 (2002).

    Article  ADS  CAS  Google Scholar 

  3. Schouten, S. et al. Geology 31, 1069–1072 (2003).

    Article  ADS  CAS  Google Scholar 

  4. Tarduno, J. et al. Science 282, 2241–2244 (1998).

    Article  ADS  CAS  Google Scholar 

  5. Morton, J. Fruits of Warm Climates (Creative Resources Systems, Miami, 1987).

    Google Scholar 

  6. Poulsen, C., Barron, E., Peterson, W. & Wilson, P. Paleoceanography 14, 679–697 (1999).

    Article  ADS  Google Scholar 

  7. Otto-Bliesner, B., Brady, E. & Shields, C. J. Geophys. Res. 107, 10.1029/2001JD000821 (2002).

  8. Barron, E. Earth Sci. Rev. 19, 305–338 (1983).

    Article  ADS  Google Scholar 

  9. Bice, K. & Norris, R. Paleoceanography 17, 10.1029/2002PA000778 (2002).

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Poulsen, C. A balmy Arctic. Nature 432, 814–815 (2004). https://doi.org/10.1038/432814a

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/432814a

  • Springer Nature Limited

This article is cited by

Navigation