In the field of paleochemotaxonomy the presence of biogenic substances in geological sediments is useful for comparing old and modern biological samples and species. These biological markers can be used to verify the biological origin of fossils and serve as paleo-ecological markers. For example, the presence of pristane indicates that the petroleum or sediment is of marine origin, while biogenic material of non-marine origin tends to be in the form of polycyclic compounds or phytane. The biological markers also provide valuable information about the degradation reactions of biological material in geological environments. Comparing the organic material between geologically old and recent rocks shows the conservation of different biochemical processes.