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- W1004029657 abstract "The carbon cycle in the oceans can be schematized by: (1) the fixation of carbon dioxide during primary production, (2) secondary production resulting from phytoplankton consumption, and (3) the destruction and mineralization of dead organisms restoring carbon dioxide and nutrients to the water. This cycle is not perfect and a fraction of the organic matter escapes as soluble or particulate matter. This matter, also called detritus, supplements the organics added from atmospheric dusts, river inputs and land weathering, and together form the non-living organic matter which participates in the oceanic geochemical cycles and the sedimentation phenomena. Most of the studies of particulate matter in the oceans concern themselves with suspensions recovered on filters and do not take into account the difference between detritus and living matter. Therefore, it is very difficult to estimate the respective impact of biological and chemical processes. Two different techniques may be utilized to recover particulate matter: filtration or centrifugation. Filtration is most widely employed, but the variety of filter types and porosities used makes any comparison between the results difficult." @default.
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- W1004029657 date "1981-01-01" @default.
- W1004029657 modified "2023-10-18" @default.
- W1004029657 title "Chapter 4 Non-Living Particulate Matter" @default.
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- W1004029657 doi "https://doi.org/10.1016/s0422-9894(08)70326-x" @default.
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