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by apw 4476 days ago
The dead forests you mentioned may have became massive coal beds via the "charcoal route"; i.e. a global firestorm may have incinerated essentially the entire biosphere.

    The global debris layer created by the end-Cretaceous 
    impact at Chicxulub contained enough soot to indicate
    that the entire terrestrial biosphere had burned.
Source:

K-Pg extinction: Reevaluation of the heat-fire hypothesis; Robertson, Lewis, Sheehan & Toon, 2013; Journal of Geophysical Research: Biogeosciences

http://onlinelibrary.wiley.com/doi/10.1002/jgrg.20018/abstra...

1 comments

No, the coal beds are far older and far thicker than the bit of end-cretaceaous soot that paper is talking about. The K-Pg boundary sediments are thin: http://en.wikipedia.org/wiki/File:Cretaceous_Paleogene_clay_...

Your typical coal bed is quite a bit thicker: http://en.wikipedia.org/wiki/File:Coal_mine_Wyoming.jpg