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Isotopic composition of methane released from wetlands: Implications for the increase in atmospheric methane

Journal Article · · Global Biogeochemical Cycles; (USA)
Measurements of the delta-C{sup 13} of methane released from tropical, temperate, and arctic wetland sites are reported. The mean delta C{sup 13} values (relative to PDB carbonate standard) for peat bogs and Alaskan tundra are {minus}53 + or{minus}8, {minus}66 + or{minus}5 and {minus}64 + or{minus}5{per thousand}, respectively. These measurements combined with methane flux estimates yield a flux-weighted global average delta-C{sup 13} value of {minus}59 + or{minus}6{per thousand} for methane released from wetlands, a major natural methane source. The agreement between the measured delta-C{sup 13} for methane emitted from wetlands and the calculated steady state value of approximately {minus}6{per thousand} for the delta-C{sup 13} of preindustrial methane sources suggests that methane was predominantly produced biogenically in the preindustrial era. The industrial era time rate of change of the delta-C{sup 13} of the global methane flux is calculated from estimates of the growth rate of the major anthropogenically derived methane sources and the C{sup 13} composition of these sources, and compared to the measured change in the delta-C{sup 13} of methane during the last 300 years. Based on these results, it is estimated that 13 + or{minus}8% of the current global methane flux is derived abiogenically from natural gas and biomass burning, whereas the remainder is derived biogenically primarily from wetlands, rice paddies, and livestock. 40 refs., 5 figs., 2 tabs.
OSTI ID:
6943466
Journal Information:
Global Biogeochemical Cycles; (USA), Journal Name: Global Biogeochemical Cycles; (USA) Vol. 2:4; ISSN GBCYE; ISSN 0886-6236
Country of Publication:
United States
Language:
English