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Greenland melt drives continuous export of methane from the ice-sheet bed

Research output: Contribution to journalLetter

  • Guillaume Lamarche-Gagnon
  • Jemma Wadham
  • Barbara Sherwood Lollar
  • Sandra Arndt
  • Peer Fietzek
  • Alex Beaton
  • Andrew Tedstone
  • Jon Telling
  • Elizabeth Bagshaw
  • Jon Hawkings
  • Tyler Kohler
  • J. D. Žárský
  • MC Mowlem
  • Alexandre Anesio
  • Marek Stibal
Original languageEnglish
Pages (from-to)73-77
Number of pages17
Issue number7737
Early online date2 Jan 2019
DateAccepted/In press - 8 Nov 2018
DateE-pub ahead of print - 2 Jan 2019
DatePublished (current) - 3 Jan 2019


Ice sheets are currently ignored in global methane budgets 1,2 . Although ice sheets have been proposed to contain large reserves of methane that may contribute to a rise in atmospheric methane concentration if released during periods of rapid ice retreat 3,4 , no data exist on the current methane footprint of ice sheets. Here we find that subglacially produced methane is rapidly driven to the ice margin by the efficient drainage system of a subglacial catchment of the Greenland ice sheet. We report the continuous export of methane-supersaturated waters (CH 4(aq) ) from the ice-sheet bed during the melt season. Pulses of high CH 4(aq) concentration coincide with supraglacially forced subglacial flushing events, confirming a subglacial source and highlighting the influence of melt on methane export. Sustained methane fluxes over the melt season are indicative of subglacial methane reserves that exceed methane export, with an estimated 6.3 tonnes (discharge-weighted mean; range from 2.4 to 11 tonnes) of CH 4(aq) transported laterally from the ice-sheet bed. Stable-isotope analyses reveal a microbial origin for methane, probably from a mixture of inorganic and ancient organic carbon buried beneath the ice. We show that subglacial hydrology is crucial for controlling methane fluxes from the ice sheet, with efficient drainage limiting the extent of methane oxidation 5 to about 17 per cent of methane exported. Atmospheric evasion is the main methane sink once runoff reaches the ice margin, with estimated diffusive fluxes (4.4 to 28 millimoles of CH 4 per square metre per day) rivalling that of major world rivers 6 . Overall, our results indicate that ice sheets overlie extensive, biologically active methanogenic wetlands and that high rates of methane export to the atmosphere can occur via efficient subglacial drainage pathways. Our findings suggest that such environments have been previously underappreciated and should be considered in Earth’s methane budget.

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    Accepted author manuscript, 1.96 MB, PDF document


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