Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming

Wallmann, Klaus, Riedel, Michael, Hong, W. L., Patton, H., Hubbard, A., Pape, T., Hsu, C. W., Schmidt, Christopher, Johnson, J. E., Torres, M. E., Andreassen, K., Berndt, Christian and Bohrmann, Gerhard (2018) Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming Nature Communication, 9 (Article number: 83 ). DOI 10.1038/s41467-017-02550-9.

s41467-017-02550-9.pdf - Published Version
Available under License ["licenses_description_cc_by_4.0" not defined].

Download (3324Kb) | Preview
41467_2017_2550_MOESM1_ESM.pdf - Supplemental Material
Available under License ["licenses_description_cc_by_4.0" not defined].

Download (1121Kb) | Preview

Supplementary data:


Methane seepage from the upper continental slopes of Western Svalbard has previously
been attributed to gas hydrate dissociation induced by anthropogenic warming of ambient
bottom waters. Here we show that sediment cores drilled off Prins Karls Foreland contain
freshwater from dissociating hydrates. However, our modeling indicates that the observed
pore water freshening began around 8 ka BP when the rate of isostatic uplift outpaced
eustatic sea-level rise. The resultant local shallowing and lowering of hydrostatic pressure
forced gas hydrate dissociation and dissolved chloride depletions consistent with our geochemical
analysis. Hence, we propose that hydrate dissociation was triggered by postglacial
isostatic rebound rather than anthropogenic warming. Furthermore, we show that methane
fluxes from dissociating hydrates were considerably smaller than present methane seepage
rates implying that gas hydrates were not a major source of methane to the oceans, but
rather acted as a dynamic seal, regulating methane release from deep geological reservoirs.

Document Type: Article
Keywords: Gas hydrate dissociation, Svalbard, isostatic rebound
Research affiliation: MARUM
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
OceanRep > The Future Ocean - Cluster of Excellence
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Refereed: Yes
DOI etc.: 10.1038/s41467-017-02550-9
ISSN: 2041-1723
Projects: MIGRATE, COST, SUGAR, Future Ocean, Ocean in the Earth System, NORCRUST
Date Deposited: 09 Jan 2018 10:29
Last Modified: 16 Jan 2018 10:32

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...