Fayl:Oceanic Food Web.jpg
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Deutsch: Biogeochemische Kreisläufe im Ozean. Mikroorganismen dominieren die Kohlenstoffumwandlungen am Anfang der Nahrungskette, indem sie anorganischen Kohlenstoff verbrauchen und partikuläre sowie gelöste organische Substanz produzieren. Partikuläres Material kann oxidiert werden oder Aggregate bilden und in die Tiefsee oder sogar zum Meeresboden absinken. Gelöste organische Substanz verteilt sich innerhalb dieses Kreislaufs auf kurze (labile) oder lange (refraktäre) Zeitskalen in diskrete Pools.
English: Biogeochemical cycling in the ocean. Microorganisms dominate transformations of carbon at the base of the food web, consuming inorganic carbon and producing particulate and dissolved organic matter. Particulate material can be oxidized or form aggregates and sink to the deep ocean or even to the seafloor. Dissolved organic matter partitions into discrete pools of that cycle on short (labile) or long (refractory) time scales. |
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| Manba | Office of Biological and Environmental Research of the U.S. Department of Energy Office of Science |
| Muallif | Template:Joye et al 2022, https://doi.org/10.1007/978-3-030-90383-1 15 originally from Oak Ridge National Laboratory |
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This work is in the public domain in the United States because it is a work prepared by an officer or employee of the United States Federal Government as part of that person’s official duties under the terms of Title 17, Chapter 1, Section 105 of the US Code.
Note: This only applies to original works of the Federal Government and not to the work of any individual U.S. state, territory, commonwealth, county, municipality, or any other subdivision. This template also does not apply to postage stamp designs published by the United States Postal Service since 1978. (See § 313.6(C)(1) of Compendium of U.S. Copyright Office Practices). It also does not apply to certain US coins; see The US Mint Terms of Use.
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