Organic geochemistry is the study of the origins and fates of organic matter in the geosphere, and it encompasses studies of coals, oils, sediments and natural waters. It is a relatively new field of endeavor which traces its origins to the identification by Trieibs in 1934 of alkyl metalloporphyrins related to chlorophyll in crude oils. This landmark research provided the first convincing evidence for the biological origin of some of the constituents of petroleum. Since then the field has expanded greatly and has become considerably more interdisciplinary as it seeks answers to how organic matter is produced, transported, recycled, transformed and preserved in modern and ancient environments.
Much of organic geochemistry can be classified into general themes such as production and fate of organic matter in aquatic ecosystems; chemical composition of biologically produced organic matter; the effect of environmental conditions on the preservation and degradation of organic matter in...
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Cross-references
Biomarker: coals; Coal: organic petrography; Coal: origin and diagenesis; Coal: types and characteristics; Coal: vitrinite reflectance and maturity assessment; Geochemistry: low temperature; Hydrogen isotopes; Laboratory simulations of oil and natural gas formation; Occurrence of organic facies; Oil seeps and coastal bitumens; Oil shales; Oil–oil and oil–source rock correlation; Organic matter in fossils; Organic matter in meteorites; Organics: contemporary degradation and preservation; Organics: sources and depositional environments; Peat; Petroleum; Petroleum: hydrothermal; Petroleum: in-reservoir biodegradation; Petroleum: kinetic modeling; Petroleum: primary migration; Petroleum: surface geochemistry; Petroleum: types, occurrence and reserves; Porphyrins; Precambrian organic matter; Sulfate reduction; Sulfur isotopes
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Volkman, J.K. (1998). Organic geochemistry . In: Geochemistry. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4496-8_226
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DOI: https://doi.org/10.1007/1-4020-4496-8_226
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