The global methane cycle: isotopes and mixing ratios, sources and sinks.
A review of the global cycle of methane is presented with emphasis on its isotopic composition. The history of methane mixing ratios, reconstructed from measurements of air trapped in ice-cores is described. The methane record now extends back to 420 kyr ago in the case of the Vostok ice cores from Antarctica. The trends in mixing ratios and in delta13C values are reported for the two Hemispheres. The increase of the atmospheric methane concentration over the past 200 years, and by 1% per year since 1978, reaching 1.7 ppmv in 1990 is underlined. The various methane sources are presented. Indeed the authors describe the methane emissions by bacterial activity under anaerobic conditions in wet environments (wetlands, bogs, tundra, rice paddies), in ruminant stomachs and termite guts, and that originating from fossil carbon sources, such as biomass burning, coal mining, industrial losses, automobile exhaust, sea floor vent, and volcanic emissions. Furthermore, the main sinks of methane in the troposphere, soils or waters via oxidation are also reported, and the corresponding kinetic isotope effects.
Bréas
O
O
European Commission Joint Research Centre, Institute for Reference Materials and Measurements, Isotope Measurements Unit, B-2440 Geel, Belgium olivier.breas@irmm.jrc.be
Guillou
C
C
Reniero
F
F
Wada
E
E
D000383:Agriculture; D000818:Animals; D001272:Atmosphere / Q000737:chemistry; D002247:Carbon Isotopes; D003903:Deuterium; D017753:Ecosystem; D004777:Environment; D005285:Fermentation; D005579:Fossil Fuels / Q000032:analysis; D019015:Geologic Sediments / Q000737:chemistry; D008697:Methane / Q000737:chemistry / Q000378:metabolism*; D012987:Soil / Q000032:analysis
D002247:Carbon Isotopes; D005579:Fossil Fuels; D012987:Soil; D003903:Deuterium; D008697:Methane