Methane hydrate dissociation across the Oligocene–Miocene boundary
Author:
Funder
Texas Sea Grant Grants-in-Aid of Graduate Research Program
Texas AM University Triads for Transformation Program
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://www.nature.com/articles/s41561-022-00895-5.pdf
Reference98 articles.
1. Ruppel, C. D. & Kessler, J. D. The interaction of climate change and methane hydrates. Rev. Geophys. 55, 126–168 (2017).
2. Hester, K. C. & Brewer, P. G. Clathrate hydrates in nature. Ann. Rev. Mar. Sci. 1, 303–327 (2009).
3. Jiang, G., Kennedy, M. J. & Christie-Blick, N. Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates. Nature 426, 822–826 (2003).
4. Berner, R. A. Examination of hypotheses for the Permo-Triassic boundary extinction by carbon cycle modeling. Proc. Natl Acad. Sci. USA 99, 4172–4177 (2002).
5. Dickens, G. R., O’Neil, J. R., Rea, D. K. & Owen, R. M. Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene. Paleoceanography 10, 965–971 (1995).
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