Impact of intensive cage fish farming on the phytoplankton and periphyton of a Scottish freshwater loch

Nutrients, phytoplankton and periphyton were monitored in a 71 ha shallow, unstratified lake used for intensive cage culture of rainbow trout. Inorganic nitrogen, ortho-phosphate and suspended solids were significantly higher near the cages and the bottom and, although declining during summer, nutrients did not reach levels which limit phytoplankton growth. Microcystis aeruginosa dominated the phytoplankton, with surface chlorophyll a reaching 189 µg l^–1 in August, but with no subsequent bloom collapse or deoxygenation. A sub-dominant community of vernal diatoms and Pediastrum spp. persisted. Periphyton was dominated by Melosira italica-subarctica. Algal species and water quality showed the lake to be highly eutrophic. Chlorophyll values predicted from a phosphorus-dependent eutrophication model agreed with observations but light limitation by self-shading and suspended farm wastes, aided by wind-induced turbulence, is believed to control algal growth rates and biomass. Implications for environmental management of intensive freshwater cage farms are discussed.     

Investigation of a toxic water-bloom of Microcystis aeruginosa (Cyanophyceae) in Lake Akersvatn,Norway

During the summer and fall of 1984 and 1985, the eutrophic Lake Akersvatn in south-eastern Norway, used as reserve drinking water reservoir, was found to produce heavy water-blooms of the colonial blue-green alga Microcystis aeruginosa. Samples of the water-bloom were found to be toxic using the mouse bioassay. No toxin was found free in the water as detected by HPLC and mouse bioassay. The toxic cells (minimum lethal dose 8–15 mg/kg body weight in mice) and purified toxin (minimum lethal dose 50 μg/kg body weight in mice) showed signs of poisoning in laboratory rats and mice identical to that of other hepatotoxin-producing M. aeruginosa blooms and strains reported from other parts of the world. The toxin has chemical properties similar to the cyclic heptapeptide reported for a South African M. aeruginosa toxin. The toxin from Lake Akersvatn bloom material has a molecular weight of 994. The toxic bloom of M. aeruginosa persisted from August to November in 1984 and reappeared in July of 1985. While water from Lake Akersvatn was not used for municipal water supply during this period, the presence of toxic blue-green algae in a drinking water reservoir indicates the need to develop monitoring and detection methods for toxic cells and toxin(s).     

Comparative studies on photosynthesis and phosphate metabolism of Cylindrospermopsis raciborskii with Microcystis aeruginosa and Aphanizomenon flos-aquae

The physiological differences for three bloom-forming cyanobacteria (Cylindrospermopsis raciborskii, Microcystis aeruginosa, and Aphanizomenon flos-aquae) were investigated. In comparison with M. aeruginosa and A. flos-aquae, C. raciborskii exhibited a significantly higher concentration of carotenoids, higher values in maximum photosynthesis rate (P_m), apparent photosynthetic efficieny (a), and maximum electron transport rate (ETR_max) during the growth period. In addition, higher extracellular alkaline phosphatase activities and lower light compensation point (I_c) were also detected in C. raciborskii (p < 0.05, ANOVA). Therefore, it is suggested that the higher photosynthetic activities, more effective uptake and utilization to phosphate, and low light requirements might play important roles in the occurrence and invasive behavior of C. raciborskii.     

The formation and degradation of cyanobacterium Aphanizomenon flos-aquae blooms: the importance of pH, water temperature, and day length

Investigation of annual changes in phytoplankton community structure in a small artificial eutrophic pond was carried out from May 2002 to April 2003. A heavy bloom of Aphanizomenon flos-aquae var. klebahnii Elenk. (Cyanobacteria) persisted in most of the water column from June to the end of October. In November, the A. flos-aquae bloom suddenly crashed and green algae were predominant until the end of spring. Weekly monitoring suggested strong involvement of the changes in abiotic factors in the cyanobacterial bloom degradation. To clarify the effects of pH, water temperature, and day length on the growth of A. flos-aquae, laboratory batch experiments were conducted. The results showed that A. flos-aquae could not grow below pH 7.1 and 11°C, and the growth tended to be suppressed under a 10L:14D photoperiod. pH, water temperature, and day length are vital factors in the growth of A. flos-aquae and, additionally, grazing by cyclopoid copepods also seemed important in bloom collapse.     

Notes on the growth and sporulation of a natural population of Aphanizomenon flos-aquae

Aphanizomenon flos-aquae contributed regularly to the summer phytoplankton in Kinnego Bay, a highly eutrophic part of Lough Neagh. Growth of the alga was variable in different years, and was apparently related to the duration of depletion of dissolved nitrate-nitrogen in the water. Although four growth pulses occurred during the study period, sporulation was only observed during one of these, when the population was very dense although evenly distributed down the water column. It seems that Aphanizomenon overwintered in Kinnego Bay as vegetative filaments and that production of akinetes was not necessary for perennation of the species. The observed sporulation in 1973 may have been induced by the high pH values caused by dense phytoplankton crops; no other measured environmental factors were particularly unfavourable to growth of Aphanizomenon at this time.     

Coupling of phytoplankton and detritus in a shallow,eutrophic lake (Lake Loosdrecht,The Netherlands)

An oscillating steady state is described of phytoplankton, dominated by Prochlorothrix hollandica and Oscillatoria limnetica, and sestonic detritus in shallow, eutrophic Lake Loosdrecht (The Netherlands). A steady-state model for the coupling of the phytoplankton and detritus is discussed in relation to field and experimental data on phytoplankton growth and decomposition. According to model predictions, the phytoplankton to detritus ratio decreases hyperbolically at increasing phytoplankton growth rate and is independent of a lake's trophic state. The seston in L. Loosdrecht contains more detritus than phytoplankton as will apply to many other lakes. The model provides a basis for estimating the loss rate of the detritus, including decomposition, sedimentation and hydraulic loss. In a shallow lake like L. Loosdrecht detritus will continue to influence the water quality for years.     

Dynamics of phytoplankton detritus in a shallow,eutrophic lake (Lake Loosdrecht,The Netherlands)

A study was made of the mortality and aerobic decomposition of light- and phosphorus-limited cultures of Oscillatoria limnetica, a dominant phytoplankton species in shallow, eutrophic Lake Loosdrecht (The Netherlands). When placed in the dark at 20 °C, most cells died and lysed within twelve days. The labile organic matter was completely decomposed within three weeks. Absorbance spectra indicated that blue green algae may contributed significantly to the refractory dissolved substances in the lake. Refractory particulate matter constituted from 7 to 24% of the biomass of O. limnetica, depending on the growth rate before incubation in the dark. The decomposition rate of this fraction was 0.005 d^–1. On a basis of a steady-state model of the dynamics of phytoplankton detritus, the areal organic dry weight concentration of the detritus in the lake is ca. 60 g m^–2. This means the quantities of detritus in the seston and epipelon are about equal.     

Dynamics of phytoplankton growth in the Waikato River,North Island,New Zealand

The Waikato River (latitude 38°S, longitude 176°E, North Island, New Zealand) is overwhelming y dominated by diatoms (mainly Melosira species) while blue-green and green algae are of minor importance. Both laboratory and in situ nutrient enrichment experiments showed enhanced growth of natural and index blue-green and green algae by addition of phosphate and nitrate. These algae were also shown to require higher temperature and light intensity than the diatoms. On the other hand, Waikato River with its higher silica content, moderate range of temperature and running water habitat was more favourable an environment for diatoms.     

The primary production of phytoplankton in Lake Vechten

The primary production of the phytoplankton of Lake Vechten (The Netherlands) (area, 4.7 ha; mean depth, 6 m), an unpolluted and stratified sandpit was investigated from 1969 to 1980 (except in 1971, 1975 and 1976) by the in situ ¹⁴C-technique. Other data collected include: solar radiation, transparency, oxygen and thermal structure. In winter and spring diatoms, Cryptophyceae and Chlorococcales were important algal groups, while in summer Dinophyceae and Chrysophyceae were important. The chlorophyll-a concentration was compared to the cellular biovolumes (= fresh weight) of the most abundant phytoplankton species. The primary production maxima occurred in winter, spring and during the summer stratification. The vertical profiles of photosynthesis exhibit light inhibition at surface to a maximum of 4 m. The maximum of zooplankton grazing in May–June caused a sharp decrease in the phytoplankton biomass and seston concentration accompanied by the highest transparency (clear water phase).The values for cellular C-fixation range from 10 to 1307 mg C · M^–2 · day^–1 (annual mean of 280 mg C · m^–2 · day^–1). High dark fixation (up to 100%) was encountered in the metalimnion and hypolimnion from July to October together with peaks of ¹⁴C-fixation due to a crowding of phytoplankton and phototrophic anoxic bacteria. Extracellular excretion by phytoplankton, investigated in 1977 to 1979, was 15% of the annual mean of the total C-fixation. The photosynthetic efficiency, turnover rates, and activity coefficients were low, particularly in the summer months when Ceratium hirundinella was predominant. The seasonal variations were controlled mainly by solar radiation and probably phosphate, the former being more important in the non-stratification period and the latter during the stratification period.     

查干湖湿地浮游植物与环境因子关系的多元分析

采用野外采样调查的方法,结合聚类(Cluster)、多维排序尺度(MDS)、冗余度分析(RDA)以及Shannon多样性指数、Pielou均匀度指数、Margalef丰度指数等手段,研究了查干湖湿地2012年平水期(5月)和丰水期(9月)浮游植物的种群结构特征、多样性及其与环境因子的相关性。调查期间共发现浮游植物127种,隶属于5门53属,其中硅藻门52种,占40.94%,绿藻门46种,占36.22%;蓝藻门25种,占19.69%。从浮游植物丰度看,平水期蓝藻最为丰富(占丰度的39.85%),其次为硅藻(占36.19%)和绿藻(占21.33%),而丰水期绿藻(占70.84%)占绝对优势。查干湖湿地研究区可划分为主湖区和新庙泡两个区域,浮游植物丰度时空差异显著:其平均值为平水期(658.0×104个/L)丰水期(459.3×104个/L),主湖区丰度是新庙泡的8—10倍。相关分析表明:平水期和丰水期浮游植物丰度均与盐度呈显著正相关;平水期浮游植物丰度与pH值、磷酸盐(PO3-4)显著负相关,说明平水期浮游植物丰度空间差异主要受盐度和营养盐的影响,主湖区盐度(52.0 mg/L)是新庙泡(16.0 mg/L)的3.3倍,同时主湖区的磷酸盐(PO3-4)(0.045 mg/L)是新庙泡(0.012 mg/L)的3.8倍;而丰水期由于营养盐没有显著差异,浮游植物丰度空间差异主要受盐度影响。除野外调查结果外,基于Bray-Curtis相似性计算的聚类和多维排序尺度分析也表明据研究区可划分为主湖区和新庙泡两个区域。RDA显示:影响查干湖湿地浮游植物分布的关键环境因子,平水期是pH值、TN和BOD5,丰水期是盐度、PO3-4和BOD5。平水期优势属喜低碱、低磷素、高氮素的生境,而丰水期优势属则喜欢微碱性、高盐度、高磷素、高BOD5的生境。调查期浮游植物优势种群为温带小型藻类,能迅速吸收营养盐并进行繁殖生长,在较高营养盐条件下可以形成较高的相对丰度。根据浮游植物生态指标对查干湖湿地水质污染程度进行现状评价表明查干湖湿地处于β-中度污染水平。     

亚热带水库浮游植物季节动态及其与环境因子的关系

以亚热带黄村水库流域为研究对象,探讨了浮游植物群落的季节变化及其与环境因子的关系。共鉴定出浮游植物51种,种类最多的是绿藻门（18种）（35.29%）,其次是硅藻门（15种）（29.41%）和蓝藻门（11种）（21.57%）。从浮游植物群落季节组成差异来看,春季（62.96%）和夏季（71.03%）蓝藻门丰度最高,秋季（56.11%）和冬季（80.74%）硅藻门丰度最高。黄村水库流域优势种尖尾蓝隐藻（Chroomonas acuta）和曲丝藻（Achnanthidium sp.）在春夏秋冬季节均存在。多样性指数表明该流域水体处于中营养状况。温度、电导率和营养盐是影响浮游植物群落组成最主要的环境因素。     

The effect of lake restoration measures on the physical,chemical and phytoplankton variables of Lake Bled

Monthly changes of physical, chemical and biological variables due a combination of artificial inflow of clean water, removal of hypolimnetic water, and diversion of sewage were studied in Lake Bled from December 1980 to December 1982.During the winter period 1981/82 the species composition of the phytoplankton changed. New species replaced those observed in previous years. We conclude that the combined effect of these three lake restoration measures was responsible for the sudden disappearance ofOscillatoria rubescens D.C. A marked decrease in some nutrients and an increase in temperature and oxygen concentration also occurred.     

Daily changes of uptake of inorganic carbon and nitrogen,and their relation to phytoplankton blooms in late spring-early summer in Lake Nakanuma,Japan

Daily changes of inorganic carbon and nitrogen uptake were measured in May in 1986 in Lake Nakanuma, Japan. Uptake of inorganic carbon and ammonium in the light-bottle experiments in the 1 m layers, showed daily changes similar to chlorophyll a changes, though the uptake activities peaked before chlorophyll a peaks (phytoplankton blooms) appeared. Potential growth rates of phytoplankton and observed growth rates were calculated from the uptake rates and chlorophyll a changes. The potential growth rates did not always correspond to the observed growth rates. The potential growth rates did not correlate with the loss rates. The correlation between the observed growth rates and the loss rates was better. These results suggest that though the increase of uptake activities may be necessary for occurrence of phytoplankton blooms, loss processes may affect the occurrence of blooms.     

Seasonal and long term changes of the phytoplankton in the lake Tortum in relation to environmental factors, Erzurum, Turkey

Seasonal changes in phytoplankton community structure of the lake Tortum were studied over one year period, from March 2002 to February 2003. The collected data were compared with the data collected 21 years ago. Chlamydomonas microsphaerella, Cyclotella krammeri, C. glomerata, and Ceratium hirundinella were identified to be dominant several times during the study period. Species diversity and biomass of the phytoplankton were very low in spite of sufficient and high levels of nutrient concentrations. Maximum phytoplankton density levels were observed during summer and late autumn. Phytoplankton density was positively correlated with nutrients, temperature and pH, and it was negatively correlated with Secchi depth and dissolved oxygen. Phytoplankton growths were negatively affected from water transparency and high levels of water mass transport (circulation) and velocity in the lake.     

巢湖铜绿微囊藻Chao 1910的基因组学和磷代谢通路分析

【背景】铜绿微囊藻(Microcystis aeruginosa)广泛分布于温带湖泊,因产生微囊藻毒素且易成为蓝藻水华优势藻株而备受关注。【目的】基于全基因组序列分析和基因转录水平验证,阐明从巢湖新分离的铜绿微囊藻Chao 1910的主要代谢通路和磷营养高效利用机制。【方法】通过第三代测序技术拼接获得Chao1910的全基因组序列,完成主要代谢通路的基因注释,并对与蓝藻水华优势藻株形成相关的磷代谢通路进行深入分析。【结果】比较基因组学表明,Chao1910藻株与日本铜绿微囊藻NIES-843的亲缘关系最近,其糖酵解、磷酸戊糖途径和核苷酸合成等代谢通路的基因组成非常保守,同时具有完整的磷转运、磷吸收、多聚磷酸盐合成/分解等磷营养高效利用的通路。不同于其他铜绿微囊藻,Chao 1910藻株不具有微囊藻毒素合成基因簇,推测其主要依靠对磷营养的高效利用获取生存竞争优势。【结论】Chao1910藻株是巢湖首株完成全基因组测序的铜绿微囊藻,这将有助于揭示其获得生存竞争优势的分子机制,为遏制巢湖蓝藻水华暴发提供依据。     

Spatial and temporal dynamics of the steady-state phytoplankton assemblages in a temperate shallow hypertrophic lake (Lake Manyas,Turkey)

Spatial and temporal dynamics of phytoplankton biomass and species composition in the shallow hypertrophic Lake Manyas, Turkey, were studied biweekly from January 2003 to December 2004 to determine steady-state phases in phytoplankton assemblages. Steady-state phases were defined when one, two or three coexisting species contributed to at least 80% of the standing biomass for at least 2 weeks and during that time the total biomass did not change significantly. Ten steady-state phases were identified throughout the study peiod. During those periods, Achnanthes microcephala (Kützing) Cleve twice dominated the phytoplankton biomass alone and contributed to more than 50% of the total biomass in seven phases. Microcystis aeruginosa (Kützing) Kützing, Anabaena spiroides Klebahn, Cyclotella stylorum Brightwell, Pediastrum boryanum (Turpin) Meneghini and Phacus pusillus Lemmermann were also represented once in steady-state phytoplankton assemblages. A. microcephala was dominant usually during cold periods of the year, while M. aeruginosa and A. spiroides were usually dominant in warm seasons. The total number of species showed a clear decrease during steady-state phases at all stations. All stations were significantly different in terms of the measured physical and chemical parameters (P < 0.05) and phytoplankton biomass (F = 117, P < 0.05).     

The phytoplankton of Lake Liddell,New South Wales: chlorophyll a concentrations,species seasonal succession,and covariation with nutrients

Samples of the phytoplankton in a freshwater lake, Lake Liddell, New South Wales (Lat: 32° 22 S, Long. 150° 1 E) were collected every 4 weeks between October 1987 and November 1988. Chlorophyll a concentrations ranged from 1.8 g 1^–1 to 9.1 g 1^–1 and were positively correlated with the following nutrient parameters: total and nett mass additions of nitrate/nitrite-N and total-N, total additions of Kjeldahl-N, and nett mass addition N-P ratios. There was no correlation between lake nutrient concentrations and chlorophyll a. Factors other than nutrient concentrations appeared to be effecting chlorophyll a concentrations as summer levels were low despite nutrient concentrations being at a maximum. In spring and summer the phytoplankton was dominated by chlorophytes, with dinoflagellates and diatoms most abundant in autumn. During winter cyanobacteria were the most abundant. The relative abundance of chlorophytes was positively correlated with in lake nitrate/nitrite-N concentrations whereas the relative abundance of cyanobacteria was negatively correlated with this parameter. Based on chlorophyll a concentrations and the phytoplankton flora Lake Liddell can be classified as mesotrophic.     

The effect of phytoplankton and suspended sediment on the growth of Corbicula fluminea (Bivalvia)

Juvenile Corbicula fluminea Müller (1774) were cultured at 15.3 °C in the laboratory on eight combinations of suspended sediment and phytoplankton. Sediment concentrations were 2.6, 25, 50, and 150 mg l^–1. Chlorophyll a levels were 15.6 and 62.5 µg l^–1. Clam tissue growth was found to be independent of silt concentration but increased at the higher chlorophyll level (p < 0.05). The growth experiment was repeated at 24 °C with chlorophyll a concentrations of 18.9 and 112.6 µg l^–1. Growth was again greater at the higher phytoplankton level (p < 0.05). These results demonstrate that Asiatic clam populations are food-limited most of the growing season in the Northern and Western portions of California's eutrophic Sacramento-San Joaquin Delta where chlorophyll a levels average less than the lower of these values. Comparisons of clam growth in the laboratory and estuary support the food limitation hypothesis as at the higher food concentration laboratory tissue growth was 2.3 and 3.8 times greater during the high and low temperature evaluations than in the estuary.     

基于CCA的典型调水水库浮游植物群落动态特征分析

调水水库是一类特殊的水体,其浮游植物群落的组成与动态的调节机制与其它水库存在较大的差别。为了解这类水库浮游植物群落的特征,于2005年1月-12月,对位于广东省珠海市的调水型供水水库--大镜山水库的浮游植物和相关的理化因子进行了2周1次的采样。全年共检测到浮游植物100种（属）;浮游植物丰度在0.86-106.27×106cells·L^-1之间,生物量在1.08-20.45mg·L^-1之间变化;全年以假鱼腥藻（Pseudanabaena sp.）为主要优势藻,肘状针杆藻（Synedra ulna.）在冬春为次优势藻,浮游植物群落相对比较稳定。运用典范对应分析（CCA）方法对浮游植物群落的组成及动态与环境因子之间的关系进行了分析和探讨。样品（cases）的CCA分析表明,全部的样品分布在主轴1和主轴2构成的4个象限内,与四季相对应,样品在4个象限的分布并不均匀,反映了热带水库所处的气候四季不分明的特点,冬春季很短,夏秋季较长,但夏秋与冬春有较为明显的分割;蓝藻门、裸藻门和硅藻门的藻类主要分布在夏、秋季所对应的象限内,而绿藻门的大部分,金藻门和隐藻门的藻类分布在冬、春季所对应的象限内。水温和降雨量是大镜山水库浮游植物群落结构动态的主要驱动因子,降雨量不仅影响水库水位,同时直接影响调水量和入库的营养盐负荷。     

Multivariate analysis of phytoplankton and related environmental factors,in a shallow hypertrophic lake

Data on some relevant environmental variables and phytoplankton species composition, collected from the hypertrophic shallow lake Albufera of Valencia (Spain) during 1980–88, were examined using Redundancy Analysis (RDA). The hydrological cycle of the lake is manipulated for rice cultivation in the area. Seasonality and the particular hydrological cycle of the lake were the principal factors influencing long-term phytoplankton dynamics. Annual or horizontal differences were less important than the seasonal factor. However, a trend of phosphate increase and underwater illumination decrease was observed between 1980 and 1988. These changes might be related to some species year-to-year variations, although in general interannual phytoplankton changes were scarce. Spatial phytoplankton differences were much smaller than physical and chemical differences, which were mainly related to loading and residence times at the different sampling zones. Shallowness, hypertrophy and the regular hydrological cycle of the Albufera for rice yield, seem to contribute to the maintenance of an almost stable and homogeneous algal community, mainly composed of filamentous cyanophytes. RDA analysis has proved to be an efficient method in yielding valuable information on phytoplankton-environment interactions and trends over a long series of data. It seems also a feasible technique to monitor the results of lake management and restoration in the future.