The Journal of Geology has just published a new paper on Permian
extinctions. It is:

Retallack, G. J., and A. H. Jahren, 2008, Methane Release from 
Igneous Intrusion of Coal during Late Permian Extinction Events
Journal of Geology. vol. 116, no. 1, pp. 1-20.

http://www.journals.uchicago.edu/doi/abs/10.1086/524120

"Abstract

Unusually large and locally variable carbon isotope excursions 
coincident with mass extinctions at the end of the Permian 
Period (253 Ma) and Guadalupian Epoch (260 Ma) can be attributed 
to methane outbursts to the atmosphere. Methane has isotopic 
values (δ13C) low enough to reduce to feasible amounts the 
carbon required for isotopic mass balance. The duration of the 
carbon isotopic excursions and inferred methane releases are here 
constrained to <10,000 yr by counting annual varves in lake 
deposits and by estimating peat accumulation rates. On 
paleogeographic maps, the most marked carbon isotope excursions 
form linear arrays back to plausible methane sources: end-Permian 
Siberian Traps and Longwood-Bluff intrusions of New Zealand and 
end-Guadalupian Emeishan Traps of China. Intrusion of coal 
seams by feeder dikes to flood basalts could create successive 
thermogenic methane outbursts of the observed timing and 
magnitude, but these are unreasonably short times for 
replenishment of marine or permafrost sources of methane. 
Methane released by fracturing and heating of coal during 
intrusion of large igneous provinces may have been a planetary 
hazard comparable with bolide impact"

Yours,

Paul




      
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