Nitrogen in the Marine Environment 2008
DOI: 10.1016/b978-0-12-372522-6.00025-6
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Viruses, Bacteria, and the Microbial Loop

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Cited by 7 publications
(3 citation statements)
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“…However, because dissolved N is stable in a variety of chemical forms and oxidation states in aquatic environments, the N cycle is complex and involves feedbacks between various dissolved N pools and the microbes, including phytoplankton and bacteria, that mediate their production, consumption, and transformation. Phytoplankton and bacteria take up both organic N and inorganic N compounds, and the genetic capability for uptake and assimilation of this diverse N pool has recently been confirmed within individual microbes and microbial communities. , On the basis of recent genomic and physiological evidence, it has been hypothesized that cyanate (OCN – ), a reduced N compound, contributes to the N and C requirements of marine microbial communities. …”
mentioning
confidence: 99%
“…However, because dissolved N is stable in a variety of chemical forms and oxidation states in aquatic environments, the N cycle is complex and involves feedbacks between various dissolved N pools and the microbes, including phytoplankton and bacteria, that mediate their production, consumption, and transformation. Phytoplankton and bacteria take up both organic N and inorganic N compounds, and the genetic capability for uptake and assimilation of this diverse N pool has recently been confirmed within individual microbes and microbial communities. , On the basis of recent genomic and physiological evidence, it has been hypothesized that cyanate (OCN – ), a reduced N compound, contributes to the N and C requirements of marine microbial communities. …”
mentioning
confidence: 99%
“…Sediments are a key compartment for the functioning and quality of coastal lagoons by acting as a sink for organic matter ( Hewson and Fuhrman, 2008 ), potentially toxic elements (PTEs) (i.e., metals and metalloids), and inorganic nutrients such as N or P ( Jiménez-Cárceles et al, 2006 ; Sharifuzzaman et al, 2016 ). Conversely, sediments can transfer nutrients and PTEs into the water column by diffusion or when sediment particles are suspended by winds and currents.…”
Section: Introductionmentioning
confidence: 99%
“…Due to the presence of a high nutrient load in sediments, resident microbial communities are usually very dense, reaching up to 10 9 cells/g ( Luna et al, 2002 ; Petro et al, 2019 ), which is 3-4 orders of magnitude higher than microbial densities in the water column ( DeLong et al, 1999 ; Eilers et al, 2000 ). Furthermore, diffusion of O 2 through the sediment is limited ( Hewson and Fuhrman, 2008 ), which leads to redox zoning and changes in microbial metabolism. At the surface, organic matter is oxidized by aerobic microbes that deplete available O 2 ; in deeper layers, anaerobes use alternative electron acceptors such as NO 3 – , MnO 2 , amorphous FeOOH, and SO 4 2– ( Sørensen et al, 1979 ).…”
Section: Introductionmentioning
confidence: 99%