Titlebook: Geochemistry of Organic Matter in the Ocean; Evgenii A. Romankevich Book 1984 Springer-Verlag Berlin Heidelberg 1984 Matter.Ocean.chemistr

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Chemical Transformations of Lipids During Sedimentogenesis, lipids is the presence of higher alkyl radicals in the molecules. The sources of lipids in the seas and oceans are the auto- and heterotrophic organisms inhabiting the marine environment. The community of living organisms produces annually in the world oceans 7 × 10. tons of fatty substances (Bogor

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Duncan Waite,Lejf Moos,Chulsub Lewe to put to rational use its nutritive, mineral and power resources. The avalanche-like growth of information about various processes in the ocean was the result of new opportunities for its study, using up-to-date research ships, earth satellites and submersible vessels, and of the progress achieve

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https://doi.org/10.1007/978-1-349-24069-2ve analysis, OM is classified at present in the majority of works only as dissolved and particulate (suspended). Definition of the term “dissolved organic matter” (DOM) means distinguishing between these two arbitrarily identified forms of organic compounds in natural waters. No uniform opinion prev

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https://doi.org/10.1007/978-3-030-82315-3ended matter that sinks to the bottom, which in terms of C. approximates (1.2 – 3.7) × 10. tons yearly. The decomposition of the aquatic organic precipitation is practically the sole energy source of biogeochemical processes of authigenous mineral formation, that results in element dissemination and