Gas hydrate destabilization and methane release events in the Krishna-Godavari Basin, Bay of Bengal

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dc.contributor.author Joshi, R.K.
dc.contributor.author Mazumdar, A.
dc.contributor.author Peketi, A.
dc.contributor.author Ramamurty, P.B.
dc.contributor.author Naik, B.G.
dc.contributor.author Kocherla, M.
dc.contributor.author Carvalho, M.A.
dc.contributor.author Mahalakshmi, P.
dc.contributor.author Dewangan, P.
dc.contributor.author Ramana, M.V.
dc.date.accessioned 2015-01-08T08:50:25Z
dc.date.available 2015-01-08T08:50:25Z
dc.date.issued 2014
dc.identifier.citation Marine and Petroleum Geology, vol.58; 2014; 476-489
dc.identifier.uri http://drs.nio.org/drs/handle/2264/4673
dc.description.abstract Methane release events have been linked to global warming, alteration of the carbon cycle and influence on biota. However, unequivocal evidence of paleomethane release events are limited. We report several negative carbon stable isotope excursions in planktic and benthic foraminifera in a core (MD161-8) from the Krishna-Godavari (K-G) Basin, Bay of Bengal. The most negative 13C spikes are recorded during the marine isotope stages MIS-4 and at the transition of MIS-5 to 4. Occurrence of highly 13C depleted (average 13C = -48±2.4 ‰ VPDB) authigenic high magnesian calcite are also reported within this time window from the core MD161-8. In the present work an unequivocal explanation for the observed 13C depletion in the marine planktic and benthic foraminifera is difficult to achieve solely from the optical/ electron microscopy or C-O stable isotope ratio analyses due to possible influence of diagenetic alteration. We attribute the observed episodic methane expulsion events, as inferred from the negative 13C excursions and earlier reports on the occurrence chemosynthetic bivalves and Mo concentration anomaly to the destabilization of the base of gas hydrate stability zone (BGHSZ). Sea level drop and shale tectonics induced focused fluid flow are the two possible causes of hydrate destabilization discussed here. Shale tectonics were possibly responsible for creating fault systems which acted as the conduit for gas flow through the sediment column and subsequent seepage. Shale and salt tectonics in the passive continental margins being a globally observed phenomenon, its role as an important driving force for enhanced methane emission needs detailed investigation to understand the climatic perturbations through geologic time. Additional evidence of methane emission from site MD161-15 further supports the link between shale tectonics and methane emission.
dc.language.iso en
dc.publisher Elsevier
dc.rights An edited version of this paper was published by Elsevier. Copyright [2014] Elsevier
dc.subject gas hydrate
dc.subject global warming
dc.subject tectonic
dc.subject carbon isotope
dc.title Gas hydrate destabilization and methane release events in the Krishna-Godavari Basin, Bay of Bengal
dc.type Journal Article


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