Variability in inorganic and organic nitrogen uptake associated with riverine nutrient input in the Gulf of Riga, Baltic Sea

被引:47
作者
Berg, GM
Glibert, PM
Jorgensen, NOG
Balode, M
Purina, I
机构
[1] Univ Maryland, Horn Point Environm Lab, Ctr Environm Sci, Cambridge, MD 21613 USA
[2] Royal Vet & Agr Univ, Dept Ecol, DK-1871 Frederiksberg C, Denmark
[3] Univ Latvia, Inst Aquat Ecol, LV-2169 Salaspils, Latvia
来源
ESTUARIES | 2001年 / 24卷 / 02期
关键词
D O I
10.2307/1352945
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 mug-at N 1(-1) in the northern region (mouth) and 41 +/- 5 mug-at N I-1 in the southern region (head) of the Gulf. Rates of nitrogen uptake, determined with N-15-labeled substrates, reflected differences in TDN concentration between the regions. In May, uptake of DIN+DON measured 0.17 and 0.43 mug-at N I-1 h(-1) in the northern and southern parts of the Gulf, respectively. In July, DIN+DON uptake measured 0.38 and 0.68 mug-at N I-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 <mu>m, while up to 67% of the community in the northern part was composed of cells > 5 mum. Our results indicate that DON was a major source of nitrogen to phytoplankton, particularly in the southern part of the Gulf.
引用
收藏
页码:204 / 214
页数:11
相关论文
共 85 条
[1]   A major biopolymeric component to dissolved organic carbon in surface sea water [J].
Aluwihare, LI ;
Repeta, DJ ;
Chen, RF .
NATURE, 1997, 387 (6629) :166-169
[2]   Bacterial utilization of different size classes of dissolved organic matter [J].
Amon, RMW ;
Benner, R .
LIMNOLOGY AND OCEANOGRAPHY, 1996, 41 (01) :41-51
[3]   RAPID-CYCLING OF HIGH-MOLECULAR-WEIGHT DISSOLVED ORGANIC-MATTER IN THE OCEAN [J].
AMON, RMW ;
BENNER, R .
NATURE, 1994, 369 (6481) :549-552
[4]  
ANDRUSHAITIS A, 1995, RIVER LOAD EUTROPHYI, P32
[5]  
ANDRUSHAITIS G, 1992, P 17 C BALT OC NORK
[6]   PROPOSAL FOR AN ABRIDGED NITROGEN TURNOVER CYCLE IN CERTAIN MARINE PLANKTONIC SYSTEMS INVOLVING HYPOXANTHINE-GUANINE EXCRETION BY CILIATES AND THEIR REUTILIZATION BY PHYTOPLANKTON [J].
ANTIA, NJ ;
BERLAND, BR ;
BONIN, DJ .
MARINE ECOLOGY PROGRESS SERIES, 1980, 2 (02) :97-103
[7]   THE ROLE OF DISSOLVED ORGANIC NITROGEN IN PHYTOPLANKTON NUTRITION, CELL BIOLOGY AND ECOLOGY [J].
ANTIA, NJ ;
HARRISON, PJ ;
OLIVEIRA, L .
PHYCOLOGIA, 1991, 30 (01) :1-89
[8]   Effects of nutrient enrichment on the growth rates and community structure of summer phytoplankton from the Gulf of Riga, Baltic Sea [J].
Balode, M ;
Purina, I ;
Béchemin, C ;
Maestrini, SY .
JOURNAL OF PLANKTON RESEARCH, 1998, 20 (12) :2251-2272
[9]  
Balode M., 1996, HARMFUL TOXIC ALGAL, P69
[10]   Organic nitrogen uptake and growth by the chrysophyte Aureococcus anophagefferens during a brown tide event [J].
Berg, GM ;
Glibert, PM ;
Lomas, MW ;
Burford, MA .
MARINE BIOLOGY, 1997, 129 (02) :377-387