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Variability in Inorganic and Organic Nitrogen Uptake Associated with Riverine Nutrient Input in the Gulf of Riga, Baltic Sea

Concentrations and rates of uptake of dissolved organic nitrogen (DON, free amino acids, and urea) and inorganic nitrogen (DIN, nitrate, and ammonium) were measured along two transects in the Gulf of Riga, a sub-basin of the Baltic Sea, during May and July 1996. Concentrations of total dissolved nit...

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Bibliographic Details
Published in:Estuaries 2001-04, Vol.24 (2), p.204-214
Main Authors: Berg, Gry Mine, Glibert, Patricia M., Niels O. G. Jørgensen, Balode, Maija, Purina, Ingrida
Format: Article
Language:English
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Summary:Concentrations and rates of uptake of dissolved organic nitrogen (DON, free amino acids, and urea) and inorganic nitrogen (DIN, nitrate, and ammonium) were measured along two transects in the Gulf of Riga, a sub-basin of the Baltic Sea, during May and July 1996. Concentrations of total dissolved nitrogen (TDN) were 23± 3 μ g-at N l-1 in the northern region (mouth) and 41± 5 μ g-at N l-1 in the southern region (head) of the Gulf. Rates of nitrogen uptake, determined with 15 N-labeled substrates, reflected differences in TDN concentration between the regions. In May, uptake of DIN+DON measured 0.17 and 0.43 μ g-at N l-1 h-1 in the northern and southern parts of the Gulf, respectively. In July, DIN+DON uptake measured 0.38 and 0.68 μ g-at N l-1 h-1 in the north and south, respectively. Most of the variability in total nitrogen flux between the northern and southern regions was due to heterogeneity of DON utilization. Uptake of urea and dissolved free amino acid were up to 6 and 3 times greater in the south compared to the north. As evidenced by size-fractionation, plankton size structure appeared to play a role in the uptake of DON. The community in the southern part was largely composed of cells < 5 μm, while up to 67% of the community in the northern part was composed of cells > 5 μm. Our results indicate that DON was a major source of nitrogen to phytoplankton, particularly in the southern part of the Gulf.
ISSN:0160-8347
1559-2723
1559-2758
1559-2731
DOI:10.2307/1352945