New evidence suggests that seismic waves from the Chicxulub meteorite impact doubled the eruption rate of lavas on the opposite side of the planet — a combination that led to the mass extinction at the end of the Cretaceous period.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Notes
References
Renne, P. R. et al. Science 350, 76–78 (2015).
Courtillot, V. E. & Renne, P. R. C. R. Geosci. 335, 113–140 (2003).
Schulte, P. et al. Science 327, 1214–1218 (2010).
Renne, P. R. et al. Science 339, 684–687 (2013).
Richards, M. A. et al. Geol. Soc. Am. Bull. 127, 1507–1520 (2015).
Manga, M. & Brodsky, E. Annu. Rev. Earth Planet. Sci. 34, 263–291 (2006).
Chenet, A.-L. et al. J. Geophys. Res. 114, B06103 (2009).
Fram, M. S. & Lesher, C. E. Nature 363, 712–715 (1993).
Author information
Authors and Affiliations
Corresponding author
Related links
Rights and permissions
About this article
Cite this article
Duncan, R. Deadly combination. Nature 527, 172–173 (2015). https://doi.org/10.1038/527172a
Published:
Issue Date:
DOI: https://doi.org/10.1038/527172a