Plankton community composition in relation to availability and uptake of oxidized and reduced nitrogen

By G. Berg, M. Balode, I. Puriņa, Santa Bekere, Christian Béchemin, S. Maestrini. 2003

151 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/ba41fa76c548a4b85ea1c69dbcf714fc562d42f9

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In Ecology

1. J. Burkholder
2. P. Glibert
3. T. Kana
4. C. Heil
5. N. Wasmund
6. J. Raven
7. Jean-Pascal Torréton
8. S. Jacquet

In Oceanography

1. P. Glibert
2. J. Burkholder
3. T. Kana
4. C. Heil
5. J. Raven
6. Hayley M. Skelton
7. J. Alexander
8. Richard C. Dugdale

Citations in the corpus

• Comparative effects of urea, ammonium, and nitrate on phytoplankton abundance, community composition, and toxicity in hypereutrophic freshwaters (2011, background): “…urea will favor non– N2-fixing cyanobacteria (Berman and Chava 1999; Finlay et al. 2010), whereas NO {3 should favor diatoms (Berman and Chava 1999; Berg et al. 2003) when other nutrients are sufficient (Tilman et al. 1986), and chlorophytes should be stimulated by all N species (Fernandez and…”
• DON as a source of bioavailable nitrogen for phytoplankton (2006, unknown): “Berg et al. (2003a) used linear regression analysis to link the abundance of diatoms in the Gulf of Riga (Baltic Sea) with NO−3 uptake during spring; a negative correlation with DFAA uptake during the summer suggests that diatoms are not among the phytoplankton that exploit DON sources in this…”
• Comparison of nitrogen fixation rates determined with different methods: a study in the Baltic Proper (2005, background): “Dissolved organic nitrogen (DON) was determined from the difference between dissolved nitrogen and dissolved inorganic nitrogen (DIN).”
• Evidence for dissolved organic nitrogen and phosphorus uptake during a cyanobacterial bloom in Florida Bay (2004, background): “Mar Biol 129:377–387 Berg GM, Glibert PM, Jorgensen NOG, Balode M, Purina I (2001) Variability in inorganic and organic nitrogen uptake associated with riverine nutrient input in the Gulf of Riga, Baltic Sea.”
• Pluses and minuses of ammonium and nitrate uptake and assimilation by phytoplankton and implications for productivity and community composition, with emphasis on nitrogen‐enriched conditions (2016, background): “…reduced N forms, NH14 and urea, and the resulting communities are often dominated by mixotrophic dinoflagellates or (pico)cyanobacteria as well as bacteria (Eppley and Peterson 1979; Legendre and Rassoulzadegan 1995; Berg et al. 1997, 2003; LaRoche et al. 1997; Glibert 1998; Glibert et al. 2001).”
• Mixotrophy, a major mode of nutrition for harmful algal species in eutrophic waters (2008, background): “, 2007), as well as abundant ‘‘particulate’’ bacterial, algal, and other prey whose growth is stimulated by the elevated nutrients (e.g., Stoecker et al., 1997; Lewitus et al., 1999a; Berg et al., 2003; Adolf et al., 2008).”
• Response of phytoplankton communities to increased anthropogenic influences (southwestern lagoon, New Caledonia) (2006, background): “Taxon-specific relationships with DIN The trends linking abundances of large phytoplankton groups with the DIN concentrations determined in this study are in agreement with the results of Berg et al. (2003), who determined taxon-specific nitrogen uptake rates in the Baltic Sea.”
• Role of urea in microbial metabolism in aquatic systems: a biochemical and molecular review (2010, background): “Phytoplankton rates of growth on urea as sole N source Some field observations have suggested that urea may promote the growth of particular phytoplankton over others (e.g. flagellate species over diatoms; Antia et al. 1991, Glibert & Terlizzi 1999, Berg et al. 2003).”