Graham K. Westbrook
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, UK
Kate E. Thatcher
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, UK
Eelco J. Rohling
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Alexander M. Piotrowski
Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, Cambridge University, Cambridge, UK
Heiko Pälike
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Anne H. Osborne
Bristol Isotope Group, Department of Earth Sciences, University of Bristol, Bristol, UK
Euan G. Nisbet
Department of Earth Sciences, Royal Holloway University of London, Egham, UK
Tim A. Minshull
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Mathias Lanoisellé
Department of Earth Sciences, Royal Holloway University of London, Egham, UK
Rachael H. James
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Veit Hühnerbach
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Darryl Green
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Rebecca E. Fisher
Department of Earth Sciences, Royal Holloway University of London, Egham, UK
Anya J. Crocker
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Anne Chabert
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Clara Bolton
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Agnieszka Beszczynska-Möller
Climate Sciences, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
Christian Berndt
National Oceanography Centre Southampton, University of Southampton, Southampton, UK
Leibniz Institute of Marine Sciences at University of Kiel (IFM-GEOMAR), Kiel, Germany
Alfred Aquilina
Organic Geochemistry Unit, Bristol Biogeochemistry Research Centre, School of Chemistry, University of Bristol, Bristol, UK
Geophysical Research Letters
More than 250 plumes of gas bubbles have been discovered emanating from the seabed of the West Spitsbergen continental margin, in a depth range of 150–400 m, at and above the present upper limit of the gas hydrate stability zone (GHSZ). Some of the plumes extend upward to within 50 m of the sea surface. The gas is predominantly methane. Warming of the northward-flowing West Spitsbergen current by 1°C over the last thirty years is likely to have increased the release of methane from the seabed by reducing the extent of the GHSZ, causing the liberation of methane from decomposing hydrate. If this process becomes widespread along Arctic continental margins, tens of Teragrams of methane per year could be released into the ocean.
Received 20 May 2009; accepted 30 June 2009; published 6 August 2009.
Citation: Westbrook, G. K., et al. (2009), Escape of methane gas from the seabed along the West Spitsbergen continental margin, Geophys. Res. Lett., 36, L15608, doi:10.1029/2009GL039191.
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