Nitrification in Marine Systems

By Bess Ward. 2008

210 citations recorded by the source corpus.

Subfields: Ecology, Molecular Biology, Pollution

View Paper: https://www.semanticscholar.org/paper/834c596080c986d1fd1f4612e10c1a23cf85f0ed

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. J. Damashek
2. S. Newell
3. C. A. Francis
4. Bess Ward
5. J. Michael Beman
6. B. Popp
7. S. Alford
8. Ø. Varpe

In Molecular Biology

1. S. Newell
2. Bess Ward
3. J. Damashek
4. J. Michael Beman
5. B. Popp
6. S. Alford
7. C. A. Francis
8. S. Falk‐Petersen

In Pollution

1. S. Newell
2. J. Damashek
3. Bess Ward
4. C. A. Francis
5. J. Michael Beman
6. B. Popp
7. S. Alford

Citations in the corpus

• The importance of tidewater glaciers for marine mammals and seabirds in Svalbard, Norway (2014, background): “In the ocean this process is usually most pronounced at the bottom of the euphotic zone due to inhibition of nitri fi cation by light and because phytoplankton outcompetes nitrifying bacteria for ammonium uptake in the euphotic zone (Ward, 2008).”
• Nitrification and ammonium dynamics in Taihu Lake, China: seasonal competition for ammonium between nitrifiers and cyanobacteria (2017, background): “The ammonia and NO−2 oxidation steps are often tightly coupled, where the product of the first step serves as a substrate for the second step (Ward, 2008).”
• Microbial Nitrogen Cycling in Estuaries: From Genes to Ecosystem Processes (2018, background): “1) and is the only known aerobic pathway for oxidizing ammonia in the environment (Ward 2008) and thus linking the reduced N produced by remineralization to the oxidized substrates (nitrite and nitrate) required for the N-loss processes.”
• Ammonia oxidation rates and nitrification in the Arabian Sea (2011, background): “However, oxidation of ammonia (which is regenerated from reduced organic matter) through nitrification also produces nitrate in the euphotic zone, supporting 12%–32% of marine primary production globally [Yool et al., 2007] as well as the reservoir of nitrate in the deep ocean [Ward, 2008].”
• Quantification of ammonia oxidation rates and ammonia‐oxidizing archaea and bacteria at high resolution in the Gulf of California and eastern tropical North Pacific Ocean (2012, methodology): “15NH z 4 oxidation rate measurements—Ammonia oxidation rates were measured by adding 99 atom percent (at%) 15NH z4 to a concentration of 42 nmol L 21 and measuring the accumulation of 15N label in the oxidized NO 2 + NO 3 pool after incubation for , 24 h (Ward 2008).”