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. 2002 Mar 26;99(7):4172–4177. doi: 10.1073/pnas.032095199

Figure 3.

Figure 3

Plots of oceanic δ13C and atmospheric CO2 vs. time as a result of the input of methane hydrate-derived CH4 to the atmosphere or oceans. It is assumed that the methane is oxidized essentially instantaneously to CO2 in either case. (A) δ13C. (B) CO2.