It is a type of fossil found in any rock when organic material is compressed, leaving only a carbon residue or film.
When an organism is buried under many layers of sediment, pressure and heat increase during diagenesis and if the organism lacks a hard skeleton, it will only leave this thin film of carbon residue on rock surfaces.
As sediment piles up, the organism's remains are subjected to pressure and heat.
[1] Plant fossils often occur as a residue or film of carbon.
[2] The delicate fossils of the Burgess Shale include carbon film forms.