Most people would consider fire to be an entirely destructive process, however given the right circumstances organic materials can be exquisitely preserved by charcoalification. We no doubt all know charcoal from the BBQ, but how many of us stop to consider what it actually is?

Charcoal is formed when organic material is subjected to high temperatures in the absence of oxygen. In this situation oxidation (burning) is not possible, however water and volatiles are driven off leaving behind a carbon-rich residue. This thermochemical alteration not only increases the preservation potential of the material in the fossil record, but can also preserve details down to a cellular level as a 'carbon skeleton'.

In this episode we discuss the importance of this greatly overlooked source of palaeontological information with Professor Andrew C. Scott of the Department of Earth Sciences, Royal Holloway University of London.