Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event-Reference-Cited by-同舟云学术

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Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

Published:2000-07 Issue:6794 Volume:406 Page:392-395
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Hesselbo Stephen P.,Gröcke Darren R.,Jenkyns Hugh C.,Bjerrum Christian J.,Farrimond Paul,Morgans Bell Helen S.,Green Owen R.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/35019044.pdf

Reference30 articles.

1. Jenkyns, H. C. The early Toarcian (Jurassic) anoxic event: stratigraphic, sedimentary and geochemical evidence. Am. J. Sci. 288, 101 –151 (1988).

2. Jenkyns H. C. & Clayton, C. J. Lower Jurassic epicontinental carbonates and mudstones from England and Wales: chemostratigraphic signals and the early Toarcian anoxic event. Sedimentology 144, 687–706 (1997).

3. Vakhrameev, V. A. Jurassic and Cretaceous Floras and Climates of the Earth (Cambridge Univ. Press, Cambridge, 1991).

4. Harries, P. J. & Little, C. T. S. The early Toarcian (Early Jurassic) and the Cenomanian–Turonian (Late Cretaceous) mass extinctions: similarities and contrasts. Palaeogeogr. Palaeoclimatol. Palaeoecol. 154, 39–66 (1999).

5. Küspert, W. G. in Cyclic and Event Stratification (eds Einsele, G. & Seilacher, A.) 482–501 (Springer, Berlin, Germany, 1982).

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