Biogeochemical Consequences of Nonvertical Methane Transport in Sediment Offshore Northwestern Svalbard

Author:

Treude T.12ORCID,Krause S.3ORCID,Steinle L.4ORCID,Burwicz E.3ORCID,Hamdan L. J.5,Niemann H.4678ORCID,Feseker T.9,Liebetrau V.3,Krastel S.10ORCID,Berndt C.3ORCID

Affiliation:

1. Department of Earth, Planetary and Space SciencesUniversity of California Los Angeles CA USA

2. Department of Atmospheric and Oceanic SciencesUniversity of California Los Angeles CA USA

3. GEOMAR Helmholtz Centre for Ocean Research Kiel Kiel Germany

4. Department of Environmental SciencesUniversity of Basel Basel Switzerland

5. School of Ocean Science and EngineeringUniversity of Southern Mississippi Ocean Springs MS USA

6. Department of Marine Microbiology and BiogeochemistryNIOZ Royal Netherlands Institute for Sea Research, and Utrecht University Utrecht The Netherlands

7. Department of Earth Sciences, Faculty of GeosciencesUtrecht University Utrecht The Netherlands

8. CAGE – Centre for Arctic Gas Hydrate, Environment and Climate, Department of GeosciencesUiT The Arctic University of Norway Tromsø Norway

9. MARUM Center for Marine Environmental Sciences and Department of GeosciencesUniversity of Bremen Bremen Germany

10. Institute of GeosciencesUniversity of Kiel Kiel Germany

Funder

Alexander von Humboldt-Stiftung

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

Reference109 articles.

1. Methane hydrate stability and anthropogenic climate change

2. Mantle‐Derived Helium and Multiple Methane Sources in Gas Bubbles of Cold Seeps Along the Cascadia Continental Margin

3. Temporal Constraints on Hydrate-Controlled Methane Seepage off Svalbard

4. BerndtC. Dumke I. Feseker T. Graves C. Franek P. Hissmann K. Hühnerbach V. Krastel S. Lieser K. Niemann H. Steinle L. &Treude T.(2014).Fluid dynamics and slope stability offshore W‐Spitsbergen: Effect of bottom water warming on gas hydrates and slope stability ‐ Cruise No. MSM21/4 ‐ August 12 ‐ September 11 2012 ‐ Reykjavik (Iceland) ‐ Emden (Germany) in MARIA S. MERIAN‐Berichte edited p. 96 DFG‐Senatskommission für Ozeanographie Bremen.https://doi.org/10.2312/cr_msm21_4

5. Rising Arctic Ocean temperatures cause gas hydrate destabilization and ocean acidification

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