Microbes, mud and methane: cause and consequence of recurrent Early Jurassic anoxia following the end-Triassic mass extinction-Reference-Cited by-同舟云学术

Microbes, mud and methane: cause and consequence of recurrent Early Jurassic anoxia following the end-Triassic mass extinction

Published:2013-03-19 Issue:4 Volume:56 Page:685-709
ISSN:0031-0239
Container-title:Palaeontology
language:en
Short-container-title:Palaeontology

Author:

van de Schootbrugge Bas¹,Bachan Aviv²,Suan Guillaume³,Richoz Sylvain⁴,Payne Jonathan L.²

Affiliation:

1. Palaeo-environmental Dynamics Group; Institute of Geosciences; Goethe University Frankfurt; Altenhöfer Allee 1 60438 Frankfurt am Main Germany

2. Geological and Environmental Sciences; Stanford University; 450 Serra Mall Stanford CA 94305 USA

3. UMR; CNRS 5276; LGLTPE; Université Lyon 1 F-69622 Villeurbanne France

4. Academy of Sciences; University of Graz; Heinrichstraße 26 8020 Graz Austria

Publisher

Wiley

Subject

Paleontology,Ecology, Evolution, Behavior and Systematics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/pala.12034/fullpdf

Reference188 articles.

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3. First record of the Early Toarcian Oceanic Anoxic Event from the Southern Hemisphere, Neuquen Basin, Argentina;Al-Suwaidi;Journal of the Geological Society of London,2010

4. Transgressive-regressive cycles and Jurassic palaeogeography of northeast Iberia;Aurell;Sedimentary Geology,2003

5. The Triassic-Jurassic boundary carbon isotope excursions expressed in taxonomically identified leaf cuticles;Bacon;Palaios,2011

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