Resource ratios and phytoplankton species composition in a strongly stratified lake

被引:13
作者
Koiv, T [1 ]
Kangro, K [1 ]
机构
[1] Estonian Agr Univ, Inst Zool & Bot, Vortsjarv Limnol Stn, EE-61101 Rannu, Tartu, Estonia
关键词
resource ratios; phytoplankton; stratification; seasonal dynamics;
D O I
10.1007/s10750-005-4154-x
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
The epilimnetic phytoplankton and its relations to nutrient content in Lake Verevi through the whole vegetation period in 2000 were studied. Lake Verevi (surface 12.6 ha, mean depth 3.6 m, maximum depth I I in) is a hypertrophic hard-water lake, where the so-called spring meromixis occurs due to an extremely warm spring. Most dissolved nutrients in the epilimnion were low already in spring, and their concentrations were quite stable during the study period. The concentration of total silicon was very low in spring but increased rapidly in summer. Total phosphorus followed the pattern for stratified eutrophic lakes, and total nitrogen was quite high. The stoichiometric N:P ratio fluctuated between 25 and 81. The dynamics of phytoplankton biomass with a spring peak from April to May and a late summer peak from July to August is typical of Estonian eutrophic lakes. Green algae and chrysophytes occurred in the phytoplankton throughout the vegetation period. The spring peak was dominated by diatoms (Synedra ulna and Synedra acus var. angustissima) and the summer peak was caused by Aphanizomenon klebahnii and Ceratium hirundinella. The study showed that in physically stratified systems, the total concentration of limiting resources and plain physical factors (light and temperature) may be more important in the determination of phytoplankton dominants than different resource ratios. A combination of light and temperature optimum, along with nutrient utilization and transport capacity, effectively segregates phytoplankton species and can be used for the explanation of seasonal succession pattern.
引用
收藏
页码:123 / 135
页数:13
相关论文
共 34 条
[1]  
[Anonymous], METHODS SEAWATER ANA
[2]  
ARVOLA L, 1984, Aqua Fennica, V14, P129
[3]  
Bulgakov NG, 1999, ARCH HYDROBIOL, V146, P3
[4]  
Hansen H.P., 1999, METHODS SEAWATER ANA, DOI [10.1002/9783527613984.ch10, DOI 10.1002/9783527613984.CH10]
[5]   Long-term changes and seasonal development of phytoplankton in a strongly stratified, hypertrophic lake [J].
Kangro, K ;
Laugaste, R ;
Noges, P ;
Ott, I .
HYDROBIOLOGIA, 2005, 547 (1) :91-103
[7]  
LINDHOLM T, 1990, VERH INT VEREIN LIMN, V24, P657
[8]   Primary production of phytoplankton in a strongly stratified temperate lake [J].
Noges, T ;
Kangro, K .
HYDROBIOLOGIA, 2005, 547 (1) :105-122
[9]   The formation and dynamics of deep bacteriochlorophyll maximum in the temperate and partly meromictic Lake Verevi [J].
Noges, T ;
Solovjova, I .
HYDROBIOLOGIA, 2005, 547 (1) :73-81
[10]  
OLIVER GG, 2000, ECOLOGY CYANOBACTERI, P149