Organic geochemists also have an interest in studying the diagenesis of biogenic substances in petroleum and how they are transformed in sediment and fossils. While 90% of this organic material is insoluble in common organic solvents – called kerogen – 10% is in a form that is soluble and can be extracted, from where biogenic compounds can then be isolated. Saturated linear fatty acids and pigments have the most stable chemical structures and are therefore suited to withstanding degradation from the diagenesis process and being detected in their original forms. However, macromolecules have also been found in protected geological regions. Typical sedimentation conditions involve enzymatic, microbial and physicochemical processes as well as increased temperature and pressure, which lead to transformations of biogenic substances. For example, pigments that arise from dehydrogenation of chlorophyll or hemin can be found in many sediments as nickel or vanadyl complexes. A large proportion of the isoprenoids in sediments are also derived from chlorophyll. Similarly, linear saturated fatty acids discovered in the Messel oil shale of the Messel Pit in Germany arise from organic material of vascular plants.
Additionally, alkanes and isoprenoids are found in soluble extracts of Precambrian rock, indicating the probable existence of biological material more than three billion years ago. However, there is the potential that these organic compounds are abiogenic in nature, especially in Precambrian sediments. While Studier et al.’s (1968) simulations of the synthesis of isoprenoids in abiogenic conditions did not produce the long-chain isoprenoids used as biomarkers in fossils and sediments, traces of C-C isoprenoids were detected. It is also possible for polyisoprenoid chains to be stereoselectively synthesised using catalysts such as Al(CH) – VCl. However, the probability of these compounds being available in the natural environment is unlikely.