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On the nature of methane gas-hydrate dissociation during the Toarcian and Aptian oceanic anoxic events

Beerling, D.J.; Lomas, M.R.; Gröcke, D.R.

Authors

D.J. Beerling

M.R. Lomas



Abstract

The magnitude and timing of a major rapid negative carbon-isotope excursion recorded in marine and terrestrial matter through the Early Toarcian (Early Jurassic) and Early Aptian (Early Cretaceous) oceanic anoxic events (OAEs) have been proposed to be the result of large methane gas-hydrate dissociation events. Here, we develop and evaluate a global carbon-isotope mass-balance approach for determining the responses of each component of the exogenic carbon cycle (terrestrial biosphere, atmosphere and ocean). The approach includes a dynamic response of the terrestrial carbon cycle to methane-related CO2 increases and climatic warming. Our analyses support the idea that both the Early Toarcian and Early Aptian isotopic curves were indicative of large episodic methane releases (∼5000 and ∼3000 Gt respectively) promoting warm ‘greenhouse’ conditions in the Mesozoic. These events are calculated to have increased the atmospheric CO2 concentration by ∼900 and ∼600 ppmv respectively and land surface temperatures by 2.5° to 3.0°C. However, we show that much of the methane released from oceanic sediments is rapidly sequestered by terrestrial and marine components in the global carbon cycle, and this effect strongly attenuated the potential for ancient methane gas-hydrate dissociation events to act as major amplifiers in global warming. An increase in oceanic carbon sequestration is consistent with the deposition of globally distributed black shales during these OAEs. Our analyses point to the urgent need for high-resolution marine and terrestrial carbon-isotope records to better characterize the nature of the Toarcian and Aptian events and improve our interpretation of their consequences for the global carbon cycle.

Citation

Beerling, D., Lomas, M., & Gröcke, D. (2002). On the nature of methane gas-hydrate dissociation during the Toarcian and Aptian oceanic anoxic events. American journal of science (1880), 302(1), 28-49. https://doi.org/10.2475/ajs.302.1.28

Journal Article Type Article
Publication Date 2002-01
Deposit Date May 19, 2015
Journal American journal of science.
Print ISSN 0002-9599
Electronic ISSN 1945-452X
Publisher American Journal of Science
Peer Reviewed Peer Reviewed
Volume 302
Issue 1
Pages 28-49
DOI https://doi.org/10.2475/ajs.302.1.28
Public URL https://durham-repository.worktribe.com/output/1428384