Release of methane from a volcanic basin as a mechanism for initial Eocene global warming-Reference-Cited by-同舟云学术

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Release of methane from a volcanic basin as a mechanism for initial Eocene global warming

Published:2004-06 Issue:6991 Volume:429 Page:542-545
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Svensen Henrik,Planke Sverre,Malthe-Sørenssen Anders,Jamtveit Bjørn,Myklebust Reidun,Rasmussen Eidem Torfinn,Rey Sebastian S.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/nature02566.pdf

Reference31 articles.

1. Kennett, J. P. & Stott, L. D. Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene. Nature 353, 225–229 (1991)

2. Schmitz, B. & Pujalte, V. Sea-level, humidity, and land-erosion records across the initial Eocene thermal maximum from a continental-marine transect in northern Spain. Geology 31, 689–692 (2003)

3. 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)

4. Dickens, G. R., Castillo, M. M. & Walker, J. C. G. A blast from the latest Paleocene: simulating first-order effects of massive dissociation of oceanic methane hydrate. Geology 25, 259–262 (1997)

5. Skogseid, J., Pedersen, T., Eldholm, O. & Larsen, B. T. Tectonism and magmatism during NE Atlantic continental break-up: the Vøring Margin. Geol. Soc. Spec. Publ. 68, 305–320 (1992)

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