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• W2055942616 abstract "Polar ice-core records suggest that an arctic or boreal source was responsible for more than 30% of the large increase in global atmospheric methane (CH 4 ) concentration during deglacial climate warming; however, specific sources of that CH 4 are still debated. Here we present an estimate of past CH 4 flux during deglaciation from bubbling from thermokarst (thaw) lakes. Based on high rates of CH 4 bubbling from contemporary arctic thermokarst lakes, high CH 4 production potentials of organic matter from Pleistocene-aged frozen sediments, and estimates of the changing extent of these deposits as thermokarst lakes developed during deglaciation, we find that CH 4 bubbling from newly forming thermokarst lakes comprised 33 to 87% of the high-latitude increase in atmospheric methane concentration and, in turn, contributed to the climate warming at the Pleistocene-Holocene transition." @default.
• W2055942616 created "2016-06-24" @default.
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• W2055942616 date "2007-10-26" @default.
• W2055942616 modified "2023-10-01" @default.
• W2055942616 title "Thermokarst Lakes as a Source of Atmospheric CH ₄ During the Last Deglaciation" @default.
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• W2055942616 doi "https://doi.org/10.1126/science.1142924" @default.
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