Temporal Constraints on Hydrate-Controlled Methane Seepage off Svalbard

Author:

Berndt C.1,Feseker T.2,Treude T.1,Krastel S.1,Liebetrau V.1,Niemann H.3,Bertics V. J.1,Dumke I.1,Dünnbier K.1,Ferré B.4,Graves C.5,Gross F.1,Hissmann K.1,Hühnerbach V.5,Krause S.1,Lieser K.1,Schauer J.1,Steinle L.3

Affiliation:

1. GEOMAR Helmholtz Centre for Ocean Research Kiel, 24148 Kiel, Germany.

2. MARUM Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, 28359 Bremen, Germany.

3. Department of Environmental Sciences, University of Basel, 4056 Basel, Switzerland.

4. CAGE (Centre for Arctic Gas Hydrate, Environment, and Climate), Department of Geology, University of Tromsø, 9037 Tromsø, Norway.

5. National Oceanography Centre, Southampton SO14 3ZH, UK.

Abstract

What Does It All Mean? Strong emissions of methane have recently been observed from shallow sediments in Arctic seas. Berndt et al. (p. 284 , published online 2 January) present a record of methane seepage from marine sediments off the coast of Svalbard showing that such emissions have been present for at least 3000 years, the result of normal seasonal fluctuations of bottom waters. Thus, contemporary observations of strong methane venting do not necessarily mean that the clathrates that are the source of the methane are decomposing at a faster rate than in the past.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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