Biogenic substance

A biogenic substance is a product made by or of life forms. While the term originally was specific to metabolite compounds that had toxic effects on other organisms, it has developed to encompass any constituents, secretions, and metabolites of plants or animals. In context of molecular biology, biogenic substances are referred to as biomolecules. They are generally isolated and measured through the use of chromatography and mass spectrometry techniques. Additionally, the transformation and exchange of biogenic substances can by modelled in the environment, particularly their transport in waterways.

The observation and measurement of biogenic substances is notably important in the fields of geology and biochemistry. A large proportion of isoprenoids and fatty acids in geological sediments are derived from plants and chlorophyll, and can be found in samples extending back to the Precambrian. These biogenic substances are capable of withstanding the diagenesis process in sediment, but may also be transformed into other materials. This makes them useful as biomarkers for geologists to verify the age, origin and degradation processes of different rocks.

Biogenic substances have been studied as part of marine biochemistry since the 1960s, which has involved investigating their production, transport, and transformation in the water, and how they may be used in industrial applications. A large fraction of biogenic compounds in the marine environment are produced by micro and macro algae, including cyanobacteria. Due to their antimicrobial properties they are currently the subject of research in both industrial projects, such as for anti-fouling paints, or in medicine.

During a meeting of the New York Academy of Sciences' Section of Geology and Mineralogy in 1903, geologist Amadeus William Grabau proposed a new rock classification system in his paper 'Discussion of and Suggestions Regarding a New Classification of Rocks'. Within the primary subdivision of "Endogenetic rocks" – rocks formed through chemical processes – was a category termed "Biogenic rocks", which was used synonymously with "Organic rocks". Other secondary categories were "Igneous" and "Hydrogenic" rocks.

In the 1930s German chemist Alfred E. Treibs first detected biogenic substances in petroleum as part of his studies of porphyrins. Based on this research, there was a later increase in the 1970s in the investigation of biogenic substances in sedimentary rocks as part of the study of geology. This was facilitated by the development of more advanced analytical methods, and led to greater collaboration between geologists and organic chemists in order to research the biogenic compounds in sediments.

Researchers additionally began to investigate the production of compounds by microorganisms in the marine environment during the early 1960s. By 1975, different research areas had developed in the study of marine biochemistry. These were "marine toxins, marine bioproducts and marine chemical ecology". Following this in 1994, Teuscher and Lindequist defined biogenic substances as "chemical compounds which are synthesised by living organisms and which, if they exceed certain concentrations, cause temporary or permanent damage or even death of other organisms by chemical or physicochemical effects" in their book, Biogene Gifte. This emphasis in research and classification on the toxicity of biogenic substances was partly due to the cytotoxicity-directed screening assays that were used to detect the biologically active compounds. The diversity of biogenic products has since been expanded from cytotoxic substances through the use of alternative pharmaceutical and industrial assays.

Through studying the transport of biogenic substances in the Tatar Strait in the Sea of Japan, a Russian team noted that biogenic substances can enter the marine environment due to input from either external sources, transport inside the water masses, or development by metabolic processes within the water. They can likewise be expended due to biotransformation processes, or biomass formation by microorganisms. In this study the biogenic substance concentrations, transformation frequency, and turnover were all highest in the upper layer of the water. Additionally, in different regions of the strait the biogenic substances with the highest annual transfer were constant. These were O₂, DOC, and DISi, which are normally found in large concentrations in natural water. The biogenic substances that tend to have lower input through the external boundaries of the strait and therefore least transfer were mineral and detrital components of N and P. These same substances take active part in biotransformation processes in the marine environment and have lower annual output as well.

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.