Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Science 9 September 2005:
Vol. 309. no. 5741, pp. 1714 - 1717
DOI: 10.1126/science.1115193

Reports

Unexpected Changes to the Global Methane Budget over the Past 2000 Years

D. F. Ferretti,1,2* J. B. Miller,3 J. W. C. White,1 D. M. Etheridge,4 K. R. Lassey,2 D. C. Lowe,2 C. M. MacFarling Meure,4 M. F. Dreier,1 C. M. Trudinger,4 T. D. van Ommen,5 R. L. Langenfelds4

We report a 2000-year Antarctic ice-core record of stable carbon isotope measurements in atmospheric methane ({delta}13CH4). Large {delta}13CH4 variations indicate that the methane budget varied unexpectedly during the late preindustrial Holocene (circa 0 to 1700 A.D.). During the first thousand years (0 to 1000 A.D.), {delta}13CH4 was at least 2 per mil enriched compared to expected values, and during the following 700 years, an about 2 per mil depletion occurred. Our modeled methane source partitioning implies that biomass burning emissions were high from 0 to 1000 A.D. but reduced by almost ~40% over the next 700 years. We suggest that both human activities and natural climate change influenced preindustrial biomass burning emissions and that these emissions have been previously understated in late preindustrial Holocene methane budget research.

1 Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA.
2 National Institute of Water and Atmospheric Research Limited (NIWA), Post Office Box 14901, Wellington, New Zealand.
3 National Oceanic and Atmospheric Administration (NOAA), R/CMDL1, 325 Broadway, Boulder, CO 80305, USA.
4 Commonwealth Scientific and Industrial Research Organisation (CSIRO), Marine and Atmospheric Research, Private Bag 1, Aspendale, Victoria 3195, Australia.
5 Department of the Environment and Heritage, Australian Antarctic Division, and Antarctic Climate and Ecosystems CRC, Private Bag 80, Hobart, Tasmania 7001, Australia.

* To whom correspondence should be addressed. E-mail: d.ferretti{at}niwa.co.nz

Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Spatially explicit fire-climate history of the boreal forest-tundra (Eastern Canada) over the last 2000 years.
S. Payette, L. Filion, and A. Delwaide (2008)
Phil Trans R Soc B 363, 2299-2314
   Abstract »    Full Text »    PDF »
Critical issues in trace gas biogeochemistry and global change.
D. J Beerling, C Nicholas Hewitt, J. A Pyle, and J. A Raven (2007)
Phil Trans R Soc A 365, 1629-1642
   Abstract »    Full Text »    PDF »
Methane and nitrous oxide in the ice core record.
E. Wolff and R. Spahni (2007)
Phil Trans R Soc A 365, 1775-1792
   Abstract »    Full Text »    PDF »
Constraining past global tropospheric methane budgets with carbon and hydrogen isotope ratios in ice.
M. Whiticar and H. Schaefer (2007)
Phil Trans R Soc A 365, 1793-1828
   Abstract »    Full Text »    PDF »
Ice record of delta13C for atmospheric CH4 across the Younger Dryas-Preboreal transition..
H. Schaefer, M. J. Whiticar, E. J. Brook, V. V. Petrenko, D. F. Ferretti, and J. P. Severinghaus (2006)
Science 313, 1109-1112
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)