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- W972707924 endingPage "359" @default.
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- W972707924 abstract "This chapter gives a description of the chemistry, occurrence and diagenesis of different types of organic substances present in recent sediments. The term diagenesis is defined here as a geotransformation of organic matter under low temperatures, generally less than 5VC, which is controlled by physical, chemical and biological processes. Most of the organic matter produced in the biosphere is formed by biosynthesis with the help of solar energy. Organic matter has high energy content and low thermodynamic stability. Organic matter in sediments represents a complex mixture of organic compounds of different types and molecular size, which are mostly derived from plant material. The organic compounds present are composed mainly of carbon and hydrogen atoms and are sometimes accompanied by other elements, such as oxygen, nitrogen and sulphur. Organic matter in the biosphere is normally assimilated by macrophages, fungi, and microorganisms. When specific conditions prevail in the geosphere and the organic matter can be preserved, cleavage reactions, aromatization and other transformations take place, which produce thermodynamically more stable products." @default.
- W972707924 created "2016-06-24" @default.
- W972707924 creator A5048361250 @default.
- W972707924 creator A5084652151 @default.
- W972707924 date "1994-01-01" @default.
- W972707924 modified "2023-09-25" @default.
- W972707924 title "Chapter 10 Diagenesis of Organic Matter" @default.
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