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- W2283886170 abstract "The dissolved organic matter (DOM) pool in seawater is one of the largest exchangeable reservoirs of reduced carbon on our planet (Carlson, 2002). Its magnitude (~685 Gt carbon) is roughly of the same order as that of the atmospheric carbon dioxide pool (Hansell and Carlson, 1998; Hedges and Keil, 1995; Fasham et al., 2001). However, DOM constitutes only a miniscule fraction of seawater, as it is contained within an electrolyte-laden solution in which the mass of inorganic salts outweigh organics by several thousand-fold (Ratanathanawongs and Keil, 1997). The dilute nature of DOM in seawater makes exploring its formation, dynamics and fate an immense challenge. An intriguing aspect of DOM is that a large fraction of this dissolved organic pool is not readily available for biological consumption (Koike et al., 1990; Wells and Goldberg, 1991; Pakulski and Benner, 1994; Benner, 1997). Radioisotope studies have shown that the average residence time of DOM in the deep ocean can be of the order of ~ 6000 years, a time period long enough for these compounds to be cycled several times in the oceans before being degraded (Williams and Druffel, 1987; Druffel et al, 1992). Because of these extremely slow turnover times, it is believed that the semi-refractory fraction of DOM could be playing an unexpectedly significant role in mitigating the build-up of carbon dioxide in the earth’s atmosphere and reducing global warming (Hedges, 1992; Benner, 1997). In view of the above, understanding the processes regulating the dynamics and distribution of DOM in seawater, assumes tremendous importance for global biogeochemistry and climate change studies." @default.
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- W2283886170 date "2004-01-01" @default.
- W2283886170 modified "2023-09-23" @default.
- W2283886170 title "Dynamics of Dissolved Organic Matter and Microbes in Seawater through Sub-Micron Particle Size Analyses" @default.
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