Display options
Share it on

Proc Natl Acad Sci U S A. 2009 Feb 24;106(8):2519-24. doi: 10.1073/pnas.0808212106. Epub 2009 Feb 03.

Wildfire responses to abrupt climate change in North America.

Proceedings of the National Academy of Sciences of the United States of America

J R Marlon, P J Bartlein, M K Walsh, S P Harrison, K J Brown, M E Edwards, P E Higuera, M J Power, R S Anderson, C Briles, A Brunelle, C Carcaillet, M Daniels, F S Hu, M Lavoie, C Long, T Minckley, P J H Richard, A C Scott, D S Shafer, W Tinner, C E Umbanhowar, C Whitlock

Affiliations

  1. Department of Geography, University of Oregon, Eugene, OR 97403, USA. [email protected]

PMID: 19190185 PMCID: PMC2650296 DOI: 10.1073/pnas.0808212106

Abstract

It is widely accepted, based on data from the last few decades and on model simulations, that anthropogenic climate change will cause increased fire activity. However, less attention has been paid to the relationship between abrupt climate changes and heightened fire activity in the paleorecord. We use 35 charcoal and pollen records to assess how fire regimes in North America changed during the last glacial-interglacial transition (15 to 10 ka), a time of large and rapid climate changes. We also test the hypothesis that a comet impact initiated continental-scale wildfires at 12.9 ka; the data do not support this idea, nor are continent-wide fires indicated at any time during deglaciation. There are, however, clear links between large climate changes and fire activity. Biomass burning gradually increased from the glacial period to the beginning of the Younger Dryas. Although there are changes in biomass burning during the Younger Dryas, there is no systematic trend. There is a further increase in biomass burning after the Younger Dryas. Intervals of rapid climate change at 13.9, 13.2, and 11.7 ka are marked by large increases in fire activity. The timing of changes in fire is not coincident with changes in human population density or the timing of the extinction of the megafauna. Although these factors could have contributed to fire-regime changes at individual sites or at specific times, the charcoal data indicate an important role for climate, and particularly rapid climate change, in determining broad-scale levels of fire activity.

References

  1. PLoS One. 2008 Mar 05;3(3):e0001744 - PubMed
  2. Science. 1999 Jan 8;283(5399):205-8 - PubMed
  3. Science. 2006 Aug 18;313(5789):940-3 - PubMed
  4. Chemosphere. 2002 Dec;49(8):845-63 - PubMed
  5. Ecology. 2006 Jul;87(7):1722-32 - PubMed
  6. Proc Natl Acad Sci U S A. 2007 Apr 17;104(16):6556-61 - PubMed
  7. Proc Natl Acad Sci U S A. 2007 Oct 9;104(41):16016-21 - PubMed
  8. Science. 2001 Jan 5;291(5501):112-4 - PubMed
  9. Science. 1993 Jul 9;261(5118):195-7 - PubMed
  10. Science. 1993 Nov 5;262(5135):885-9 - PubMed
  11. Ecol Appl. 2008 Mar;18(2):391-406 - PubMed
  12. Proc Natl Acad Sci U S A. 2007 Apr 3;104(14):5738-42 - PubMed
  13. Sci Total Environ. 2000 Nov 15;262(3):221-9 - PubMed
  14. Science. 2008 Aug 1;321(5889):680-4 - PubMed
  15. Ecology. 2008 Mar;89(3):729-43 - PubMed
  16. Proc Natl Acad Sci U S A. 2008 Aug 19;105(33):11651-4 - PubMed

Publication Types