Fusain
Fusain is a fossilised carbon deposit which, after some controversy, has been identified as fossilised charcoal.
Charcoal forms "only" in reduced atmosphere, while at that time the atmosphere had 50% more oxygen as in the present. Fusain is then formed through another process.
It is fibrous, black and opaque, and often preserves details of cell wall architecture. Wood-derived fusain usually takes the form of cubic blocks, whereas fusain from other plant material may take the form of thin films which are only visible under a microscope where the surrounding rock is dissolved by acid maceration. The material is silky and crumbles on the touch.
The loss of volatile elements during combustion means that fusain fossils are usually smaller than the original organism, but this same factor makes them unlikely to be eaten by any animals, enhancing their preservation potential.
Fusain shows characteristics diagnostic of pyrolysis in modern material: the cell walls of xylem are homogenized, and subsequently crack along their middles.
