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- W2174725238 endingPage "575" @default.
- W2174725238 startingPage "565" @default.
- W2174725238 abstract "As organic matter produced in the euphotic zone of the ocean sinks through the mesopelagic zone, its composition changes from one that is easily characterized by standard chromatographic techniques to one that is not. The material not identified at the molecular level is called uncharacterized. Several processes account for this transformation of organic matter: aggregation/disaggregation of particles resulting in incorporation of older and more degraded material; recombination of organic compounds into geomacromolecules; and selective preservation of specific biomacromolecules. Furthermore, microbial activities may introduce new cell wall or other biomass material that is not easily characterized, or they may produce such material as a metabolic product. In addition, black carbon produced by combustion processes may compose a fraction of the uncharacterized organic matter, as it is not analyzed in standard biochemical techniques. Despite these poorly-defined compositional changes that hinder chemical identification, the vast majority of organic matter in sinking particles remains accessible to and is ultimately remineralized by marine microbes." @default.
- W2174725238 created "2016-06-24" @default.
- W2174725238 creator A5005350844 @default.
- W2174725238 creator A5023066145 @default.
- W2174725238 creator A5035917383 @default.
- W2174725238 date "2004-12-01" @default.
- W2174725238 modified "2023-10-17" @default.
- W2174725238 title "Particulate Organic Matter in the Sea: The Composition Conundrum" @default.
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