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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 7, issue 1
Atmos. Chem. Phys., 7, 237–241, 2007
https://doi.org/10.5194/acp-7-237-2007
© Author(s) 2007. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Atmos. Chem. Phys., 7, 237–241, 2007
https://doi.org/10.5194/acp-7-237-2007
© Author(s) 2007. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  17 Jan 2007

17 Jan 2007

Stable isotopes provide revised global limits of aerobic methane emissions from plants

D. F. Ferretti1,2, J. B. Miller3, J. W. C. White1, K. R. Lassey2, D. C. Lowe2, and D. M. Etheridge4 D. F. Ferretti et al.
  • 1University of Colorado, Boulder, CO, USA
  • 2National Institute of Water and Atmospheric Research Ltd, Wellington, New Zealand
  • 3National Oceanographic and Atmospheric Administration, Boulder, CO, USA
  • 4Marine and Atmospheric Research, Commonwealth Scientific and Industrial Research Organisation, Aspendale, Victoria, Australia

Abstract. Recently Keppler et al. (2006) discovered a surprising new source of methane – terrestrial plants under aerobic conditions, with an estimated global production of 62–236 Tg yr−1 by an unknown mechanism. This is ~10–40% of the annual total of methane entering the modern atmosphere and ~30–100% of annual methane entering the pre-industrial (0 to 1700 AD) atmosphere. Here we test this reported global production of methane from plants against ice core records of atmospheric methane concentration (CH4) and stable carbon isotope ratios (δ13CH4) over the last 2000 years. Our top-down approach determines that global plant emissions must be much lower than proposed by Keppler et al. (2006) during the last 2000 years and are likely to lie in the range 0–46 Tg yr−1 and 0–176 Tg yr−1 during the pre-industrial and modern eras, respectively.

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