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 (CH 4 ) and stable carbon isotope ratios (δ 13 CH 4 ) 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.
Stable isotopes provide revised global limits of aerobic methane emissions from plants
D. Ferretti,John B. Miller,J. White,K. Lassey,D. Lowe,D. Etheridge
Published 2006 in Atmospheric Chemistry and Physics
ABSTRACT
PUBLICATION RECORD
- Publication year
2006
- Venue
Atmospheric Chemistry and Physics
- Publication date
2006-07-07
- Fields of study
Chemistry, Environmental Science
- Identifiers
- External record
- Source metadata
Semantic Scholar
CITATION MAP
EXTRACTION MAP
CLAIMS
- No claims are published for this paper.
CONCEPTS
- No concepts are published for this paper.
REFERENCES
Showing 1-19 of 19 references · Page 1 of 1
CITED BY
Showing 1-75 of 75 citing papers · Page 1 of 1