长诏水库浮游植物群落结构及水质评价

于2010年5月、8月和11月对新昌长诏水库浮游植物群落进行了调查,运用Shannon多样性指数(H)、Simpson多样性指数(D)、Margalef丰富度指数(M)及Pielou均匀度指数(J)分析了浮游植物种群的多样性,并结合水质理化指标对长诏水库的富营养化程度及水质状况进行了综合评价.结果显示:长诏水库浮游植物有6门26属(种),其中,绿藻门10属(种),硅藻门9属(种),蓝藻门4属(种),隐藻门1属,甲藻门1属,黄藻门1属.浮游植物的丰度为5.73×105～7.73×105ind·L-1,平均为(6.71±0.81)×105 ind·L-1;生物量为0.73～1.03 mg·L-1,平均为(0.83±0.12) mg·L-1.在水平分布上,蓝藻门、硅藻门和绿藻门的丰度在各采样点中均较高;在季节分布上,硅藻门、绿藻门、蓝藻门分别在春季、夏季、秋季占绝对优势.总体上,浮游植物丰度和生物量在水库入水口较高,出水口较低.水库浮游植物的多样性较差,水质受到较重污染,且主要为氮、磷污染;富营养化程度为中-富营养化水平.     

一座南亚热带小型贫营养水库浮游植物群落结构及季节变化

库容大小是影响水体水动力学过程的一个重要变量,它能在很大程度决定生态系统的结构,特别是浮游植物的群落结构.为了解小型贫营养水库浮游植物的群落特点,于2006年4、8、12月对位珠海市的贫营养小型水库-吉大水库的浮游植物群落结构进行采样和计数分析.3次采样共检出浮游植物32种,浮游植物细胞丰度的变化范围在69～342 cells·mL^-1,生物量的变化范围在1.34～3.69 mg·L^-1,夏季浮游植物的丰度和生物量明显高于冬季.甲藻是最主要的优势种类,且相对优势度较为稳定.夏季,隐藻门的隐藻(Cryptomonas sp.)和绿藻门的鼓藻(Cosmarium spp.)大量出现,甲藻的相对优势度有所降低.冬季,隐藻数量急剧下降,但硅藻门的颗粒直链藻(Aulacoseira granulata)大量出现,与甲藻共同成为水体中的优势种.由降雨引起的营养盐浓度增加是浮游植物变化的主要影响因子,而透明度全年维持较高的水平为浮游植物的生长形成了有利条件,此外,较为稳定的水体和甲藻利用营养盐的能力使得甲藻成为浮游植物中的最主要的优势种.     

稻鱼共作生态系统浮游植物群落结构和生物多样性

稻鱼共作技术是中国传统农业的精华,通过对稻鱼共作系统水体浮游植物的种类组成、密度、生物量及多样性进行分析,明确该系统中浮游植物数量变化特性,为进一步开发利用这一经典农艺提供理论基础和实践依据。结果表明,稻田生态系统中浮游植物群落包含蓝藻门、甲藻门、隐藻门、裸藻门、绿藻门和硅藻门等6门,共38属93种。稻鱼共作显著增加稻田水体浮游植物的密度和生物量,降低硅藻和蓝藻的优势度,增加绿藻和裸藻的优势度,提高了稻田水体浮游植物多样性指数。     

太湖蠡湖冬季浮游植物群落结构特征与氮、磷浓度关系

根据2010年1月蠡湖的浮游植物与营养盐的同步监测资料,利用GIS技术,对蠡湖冬季浮游植物的种类组成、优势种、丰度及其空间分布和多样性等进行了分析。结果表明:浮游植物有7门27属,绿藻门种类最多共12种,占总种数的44.44%,其次是硅藻门和隐藻门,分别为7种和3种,占总种数的25.93%和11.11%;主要优势种为啮蚀隐藻(Cryptomonas erosa)、卵形隐藻(C.ovata)、尖尾蓝隐藻(Chroomonas acuta)和微囊藻(Microcystis aeruginisa);浮游植物平均丰度为1099.6×104ind·L-1,隐藻丰度分布趋势决定了浮游植物丰度的分布趋势;宝界桥至西堤湖区(B区)是浮游植物较为密集区,西堤以北湖区(A区)为浮游植物稀疏区;浮游植物群落Shannon物种多样性指数平均值为1.1,Pielou均匀度指数平均值为0.31。与2007年相比,2010年冬季浮游植物数量大幅增加,且主要优势种群也发生了较大的变化,由以绿藻为主向以隐藻为主演替。分析表明,磷是蠡湖冬季浮游植物生长的限制性因素,氮磷比的变化是导致冬季浮游植物数量增加的主要原因。     

浙南大罗山天河水库浮游植物群落结构的季节变化及对水质的指示作用

为了探究浙南地区山区水库浮游植物群落结构的季节变化及水质状况,于2019年2月—2020年1月对位于温州大罗山天河水库的浮游植物群落结构和水体理化因子进行了调查分析。结果表明: 天河水库浮游植物隶属于7门60属89种,全年浮游植物平均丰度为2.02×10⁵ cells·L^-1,年均生物量为0.26 mg·L^-1。硅藻门在全年均占优势,绿藻门在春、秋季占优势,而蓝藻门仅在夏季占优势,裸藻门和甲藻门在全年均有出现,隐藻门在秋、冬季均有出现,但不占优势。全年主要优势种有颗粒直链藻、尖针杆藻、隐头舟形藻、美丽星杆藻、假鱼腥藻、小新月藻、二角盘星藻、二角多甲藻、圆筒锥囊藻、卵形隐藻。冗余分析(RDA)显示,水库的水温、总氮、化学需氧量(COD_Mn)和 pH值是浮游植物群落结构的主要影响因子。分别运用Shannon指数、Pielou均匀度指数和Margalef丰富度指数,并结合浮游植物的丰度、优势种及综合营养状态指数分析了水体污染情况和富营养程度, 结果显示,天河水库水体介于寡污染到清洁水体带之间,为贫-中营养型水体。     

安徽沱湖夏季浮游植物群落结构特征与环境因子关系

为了揭示沱湖浮游植物群落结构特征及其与水环境因子的关系,于2016年7月(夏季),对沱湖流域上游至下游11个采样点浮游植物种类组成、细胞丰度、生物量等进行调查研究。结果显示,沱湖共有浮游植物96种(含变种),隶属8门48属,其中绿藻门(Chlorophyta)和硅藻门(Bacillariophyta)种类最多,绿藻门有23属39种,占总种数的40.63%,硅藻门有7属20种,占总种数的20.83%;其次为裸藻门(Euglenophyta),有5属17种,占总种数的17.71%,蓝藻门(Cyanophyta) 8属14种,占14.58%;甲藻门(Pyrrophyta) 2属2种,隐藻门(Cryptophyta) 1属2种,各占总种数的2.08%,黄藻门(Xanthophyta)与金藻门(Chrysophyta)均有1属1种,均占总种数的1.04%。绿藻和硅藻类物种在沱湖浮游植物群落结构中处于优势地位,沱湖夏季浮游植物种类组成表现为绿藻-硅藻型。沱湖夏季浮游植物细胞丰度与生物量从上游到下游呈逐渐增加趋势,细胞丰度与生物量平均值分别为4.022×106cells/L与3.046 mg/L,蓝藻门和绿藻门类群为沱湖浮游植物细胞丰度主体,硅藻门和裸藻门类群为沱湖浮游植物生物量的主体;上游浮游植物多样性指数与均匀度指数均略高于下游采样点,沱湖水质呈β中污型-无污染型,上游水质优于下游水质。浮游植物群落结构与水环境因子的典型对应分析(CCA)结果表明,电导率、透明度、水深及pH值等环境因子与沱湖夏季浮游植物群落结构有较强的相关性。     

水丰水库浮游植物群落特征及水质评价

于2015年6月-2019年10月对水丰水库浮游植物群落结构和水质状况进行了19次调查.结果表明:水丰水库共发现浮游植物7门43属76种(以丰度＞1000 cells ? L-1计),其中硅藻门33种,绿藻门27种,蓝藻门6种,裸藻门5种,隐藻门和甲藻门各2种,金藻门1 种;浮游植物丰度为1.20×104～6.03×1...     

海南西部近岸浮游植物的周年变化及主要关联因素

报道了2008—2009年4季度海南西部近岸浮游植物群落的周年动态并探讨其主要关联因素。165份样品经鉴定共有浮游植物4门74属155种(含5变型和2变种),周年平均丰度为(6.36±4.75)×103cells/L。硅藻在物种组成和丰度上均占绝对优势,其次为甲藻,蓝藻(束毛藻)在7月增殖。主要优势种为菱形海线藻(Thalassionema nitzschioides)、奇异棍形藻(Bacillaria paradoxa)、具槽帕拉藻(Paralia sulcata)、旋链角毛藻(Chaetoceros curvisetus)、笔尖根管藻(Rhizosolenia styliformis)、束毛藻(Trichodesmium spp.)、海洋原甲藻(Prorocentrum micans)等。物种组成的季节差异较大,10月浮游植物种类贫乏,1月次之,4月、7月最丰富。丰度10月最高,季节差异并不明显。束毛藻在4月、7月呈斑块状群聚分布。浮游植物周年平均丰度并不高(<1.0×104cells/L)。不同季节优势种有明显的交错和变化,菱形海线藻、奇异棍形藻、具槽帕拉藻为全年优势种。浮游植物物种多样性指数和均匀度都表现出较高的值,均匀度与多样性指数的季节变化特点基本一致,群落多样性高的季节物种均匀度也好。物种多样性指数指示调查区水体遭受污染程度低,水质状况优。调查区各季节的浮游植物丰度与温度之间无显著的相关关系,1月丰度与盐度则呈密切负相关关系。10月浮游植物丰度与无机氮(DIN)呈密切的正相关关系。7月浮游植物丰度与活性磷酸盐(PO4-P)呈密切的负相关关系。浮游动物对浮游植物的摄食压力直接影响到后者的丰度变动,并伴随着海区生态系统的相关复杂现象及生物学过程的作用。     

鄱阳湖-珠湖浮游植物群落结构时空变化特征与环境因子的关系

珠湖是鄱阳湖唯一具有重要饮用水水源供水功能的大型子湖和国家水质良好湖泊, 但长期以来对其浮游植物群落结构及其时空变化情况缺乏了解。为研究浮游植物在珠湖的空间分布特征及其与环境因子的关系, 2018年1月、7月、12月在珠湖设置13个采样点开展浮游植物调查。三期调查共鉴定浮游植物79种, 隶属于7门58属, 绿藻门和蓝藻门种类最丰富, 浮游植物平均生物量为4.80 mg·L-1, 平均细胞丰度为2.56×106 个·L-1。珠湖藻类在空间上分布存在差异, 在7月、1月内珠湖团林—四十里街湖区蓝藻较其他湖区优势明显, 在12月团林—四十里街湖区隐藻的优势度明显高于其他湖区, 双港湖区及县水源地湖区的硅藻较其他湖区优势明显。珠湖水质生物学评价结果表明, 珠湖目前处于中污型向重型过渡的状态。RDA分析显示, TDN、TN、CODMn、TP、WT等环境因子解释了物种与环境之间关系的93.96%, TDN是影响藻类生物量的主要环境因子。     

乌梁素海浮游细菌群落结构及其对富营养化因子的响应

【目的】揭示乌梁素海浮游细菌的群落结构及其对富营养化环境因子的响应,认识乌梁素海浮游细菌多样性,以丰富微生物与富营养化关系的理论。【方法】提取水体浮游细菌总DNA,利用细菌通用引物对63F/1387R进行PCR扩增,构建小口、沙尖北和红圪卜3个湖区16S rRNA基因克隆文库;以典型对应分析(CCA)方法解析浮游细菌群落结构对环境因子的响应。【结果】各湖区中富营养化程度最重的红圪卜位点细菌多样性、丰富度及均匀度最高,而富营养化程度最轻的小口位点细菌多样性、丰富度及均匀度最低。Proteobacteria、Bacteroidetes和Actinobacteria为水体中优势类群。α-、γ-、δ-Proteobacteria,Actinobacteria及Bacteroidetes等菌群丰度随着水体的富营养化程度改变而有显著的变化。各湖区皆存在许多可能具有污染物降解及驱动生源要素循环能力的细菌类群。CCA分析表明TN、NH4+、NO3-和COD等水体指标对浮游细菌群落结构组成的影响较大。此外,乌梁素海水体内未知细菌类群很多;且不同于一般淡水生态系统,乌梁素海中存在9.6%的轻度嗜盐碱性细菌。【结论】乌梁素海水体中浮游细菌多样性较高,细菌群落结构复杂、其类群组成与富营养化因子紧密相关。     

仙女湖及入湖河流浮游植物功能类群与环境因子的相互关系

文章分析了仙女湖及入湖河流浮游植物群落结构和功能类群的时空分布特征, 探讨了影响其时空分布规律的关键环境因子。调查期间共鉴定表层水体中浮游植物82种(属), 包括蓝藻15种(属), 绿藻33种(属), 硅藻23种(属), 甲藻3种(属), 裸藻5种(属), 隐藻2种(属), 金藻1种(属)。各季节平均密度和生物量分别在7.95×106—2.19×109 cells/L和10.52—792.91 mg/L变化。群落功能类群的结果表明, 冬、春河流生境中具硅质结构的无鞭毛个体浮游植物(硅藻门)占据主导地位(Ⅵ功能群), 而湖区生境中具鞭毛、中等到大型的单细胞或群体浮游植物(如隐藻和甲藻)具有明显优势(Ⅴ功能群); 而夏秋季节不同生境中虽然Ⅵ型浮游植物数量仍然相对较高, 但是具伪空胞的、较大表面积/体积比的丝状个体浮游植物(Ⅲ型)以及具胶质鞘、小的表面积/体积比的群体类的浮游植物(如蓝藻, Ⅶ功能群)在某些河流和湖泊生境中的比重有显著增长。功能类群与环境因子的相关分析表明: 冬、春季Ⅴ与Ⅵ功能群浮游植物生物量主要受到总氮和总磷水平影响; 而夏、秋季节Ⅲ与Ⅶ功能群浮游植物受到水温、浊度、总氮和总磷水平的多重影响。     

A five-year study of autotrophic winter picoplankton in Lake Balaton,Hungary

Picoeukaryotes dominate the phytoplankton of Lake Balaton—the largest shallow lake in Central Europe—in the winter period. We examined the annual dynamics of picoplankton abundance and composition in the lake in order to establish if the picoeukaryotes merely survive the harsher winter conditions or they are able to grow in the ice-covered lake when the entire phytoplankton is limited by low light and temperature. Lake Balaton has an annual temperature range of 1–29°C, and it is usually frozen between December and February for 30–60 days. In the spring-autumn period phycocyanin and phycoerythrin rich Cyanobacteria are the dominant picoplankters, and picoeukaryotes are negligible. Our five-year study shows the presence of three types of picophytoplankton assemblages in Lake Balaton: (1) Phycoerythrin-rich Cyanobacteria—the dominant summer picoplankters in the mesotrophic lake area; (2) Phycocyanin-rich Cyanobacteria—the most abundant summer picoplankters in the eutrophic lake area and; (3) Picoeukaryotes—the dominant winter picoplankters in the whole lake. The observed winter abundance of picoeukaryotes was high (up to 3 × 10⁵ cells ml⁻¹), their highest biomass (520 μg l⁻¹) exceeded the maximum summer biomass of picocyanobacteria (500 μg l⁻¹). Our results indicate that the winter predominance of picoeukaryotes is a regular phenomenon in Lake Balaton, irrespective of the absence or presence of the ice cover. Picoeukaryotes are able to grow at as low as 1–2°C water temperature, while the total phytoplankton biomass show the lowest annual values in the winter period. In agreement with earlier findings, the contribution of picocyanobacteria to the total phytoplankton biomass in Lake Balaton is inversely related to the total phytoplankton biomass, whereas no such relationship was observable in the case of picoeukaryotes.     

Cyanobacteria and cyanotoxins in the source water from Lake Chivero,Harare, Zimbabwe,and the presence of cyanotoxins in drinking water

The phytoplankton community and cyanotoxins in Lake Chivero (formerly Lake McIlwaine) and the presence of cyanotoxins in treated drinking water were investigated between 2003 and 2004. A typical seasonal succession of Cyanobacteria species occurred from January to April, Bacillariophyta from May to July, and Cryptophyta and Chlorophyta from August to December. Microcystis aeruginosa and M. wesenbergii, known producers of the toxin microcystin, and the non-toxic cyanobacterium M. novacekii dominated during summer. The highest concentrations of microcystins and lipopolysaccharide endotoxins occurred when cyanobacterial biomass was highest. Lipopolysaccharide endotoxin concentrations in the lake ranged between 8 and 3 200 Endotoxin Units (EU) ml^?1. Microcystin concentrations in treated water were below the recommended safe limit for drinking water. Lipopolysaccharide endotoxin concentrations in treated water ranged from 0.15 to 11 EU ml^?1. The phytoplankton community comprised non-microcystin-producing species for the greater part of the study period.     

惠州西湖游浮植物群落对生态系统修复的响应

2004年对广东惠州西湖实施了生态系统修复示范工程,示范区目前沉水植物丰富,水体常年清澈见底。通过2008年6月至2009年5月对示范区和未进行生态修复的平湖逐月进行浮游植物调查,研究了浮游植物群落对湖泊生态系统修复的响应。结果表明,与未修复的平湖相比,示范区浮游植物数量及群落结构均发生了很大变化。示范区全年浮游植物平均生物量和细胞丰度分别为0.31 mg/L和2.75×106cells/L,均远低于未修复的平湖的3.27 mg/L和197.46×106cells/L;平湖中蓝藻在全年大部分时间占有绝对优势,一些热带富营养化水体中的代表种类（假鱼腥藻）成为优势种类;而示范区蓝藻不占优势,取而代之的是一些隐藻、硅藻和甲藻门的种类。另外,示范区浮游植物丰富度增加,年平均Margalef物种丰富度指数为3.70,显著高于平湖的2.68。因此,重建以沉水生植物为优势的生态系统是抑制浮游植物发展和改善湖泊水环境的有效途径。     

Ecological impacts of water transfers on Lake Taihu from the Yangtze River,China

As an ecosystem responds to external environmental changes slowly due to its reorganization compared with the water quality and it has great influence on lake ecosystems, it is indispensable to evaluate ecological impacts from water transfers for the security of the water source in Lake Taihu. Evaluations were conducted by comparing the indicators exergy (Ex), structural exergy (Ex_st) and phytoplankton buffer capacity (β_((TP)/(Phy))) changes after water transfers from 2002 to 2007 with those reference statuses where the water transfers were not implemented from 1998 to 2001. Besides those three ecological indicators, affiliated indicators such as ratio of zooplankton biomass to phytoplankton biomass, diversity index and trophic state index were also involved in the evaluation. The results showed the water transfers altered the ecosystem status and had positive effects on Lake Taihu and most of its sub-zones, such as Gonghu Bay, Northwest Zone, Southwest Zone and Centre Zone in the post-transfer period. The seasonable trends indicated that the ecosystem health with environmental influences excluded in November and February was better than that in May and August during the water transfers from 2002 to 2007 and there were significant differences in the ecosystem health of the first and second stages during water transfers. The ecosystem health in May and August was better than in November and February during the first stage of the water transfers (from 2002 to 2004), while the opposite obtained during the second stage from 2005 to 2007 in Dongtaihu Bay and East Epigeal Zone. On the whole, water transfers serve to deter algal congregation in Lake Taihu.     

Sedimentation in Arctic Canada: Species composition and biomass of phytoplankton contributed to the marine sediments in Frobisher Bay

Summary Sedimentation of phytoplankton provides food and energy for zoobenthic communities. In this study the rates, species composition and biomass of phytoplankton input to Frobisher Bay sediments were examined during ice (late November to July) and open water (late July to October) periods from 1982 to 1985. The rates were higher on the sea bed than at 20 m. The minimum rate (3x10⁵ cells·m^-2·day^-1) of sedimentation occurred during the early part of the ice period. It increased as the ice thickened and reached a maximum of 2.8x10⁸ cells·m^-2·day^-1 after the phytoplankton bloom at the beginning of the open water period in the first two weeks of August. The sedimented phytoplankton was dominated by diatoms, with a great majority of pennate species during the spring (April to June) and centric forms during the summer (July to August). Green flagellates, dinoflagellates and chrysophytes occurred as a low percentage of the total population in all seasons. Other indicators (chlorophyll a and phaeopigments) showed highest biomass levels in the deepest traps. They were consistently low during the winter (December to March) and reached their maxima during the open-water period of summer. Their abundance was correlated with the seasonal cycle of the phytoplankton in the water column.     

Bottom-up effects of bream (Abramis brama L.) in Lake Balaton

Enclosures (17 m³) were used in the mesotrophic area of Lake Balaton to determine the impact of benthivorous bream (Abramis brama L.) on the lower trophic levels during summers of 1984–86. In enclosures with a fish biomass similar to the biomass in the eutrophic area of the lake, the number of phytoplankton species was highest. In enclosures with a low fish biomass the phytoplankton was dominated by the greens. A high biomass of bream in the mesotrophic basin caused bacterial production corresponding to that of the eutrophic part of the lake. Crustaceans were dominated by copepods and were unable to control phytoplankton peaks. Bottom-up effects of bream were more obvious than top-down effects and seem to be more important in the possible control of water quality.     

Shifts in water quality in a drinking water reservoir during and after the removal of cyprinids

Lake ülemiste, the drinking water reservoir of Estonia’s capital city Tallinn, was biomanipulated by manual removal of cyprinids in 2004–2006 and its impact on water quality in the vegetation period was studied. A total biomass of 156 tonnes corresponding to 160 kg ha⁻¹ of fish, predominantly cyprinids, were removed. A decline in the unit catches of fishing was observed. The removed fish biomass versus phosphorus concentration of the lake was considered sufficient to reduce the impact of cyprinids on water quality. The phosphorus removed within fish biomass corresponded to 38 μg l⁻¹ and 21% of the external phosphorus load of the fishing period. The mean total phosphorus concentration dropped from >50 to ≤36 μg l⁻¹. However, the densities of planktivorous young-of-the-year percids remained high and the role of zooplankton grazing in improving water quality was found non-significant or transient. The cladocerans biomass decreased and the small-sized Daphnia cucullata remained almost the only daphnid in Lake ülemiste during and after the manipulation. Predomination of filamentous cyanobacteria was replaced by a more diverse phytoplankton composition and co-domination of micro- and pico-sized colonial cyanobacteria during summer. Mean phytoplankton biomass decreased from 15 to 6 mg l⁻¹ primarily as a result of decreased in-lake TP availability. The Secchi disc transparency increased only in May 2005–2007. The effects of coincidental events, a decline of external loading of phosphorus and a simultaneous flushing induced by heavy rainfall, on lake water quality are discussed with some implications to the future management of the reservoir.     

Spatial and temporal photosynthetic compartments during summer in Antarctic Lake Kitiesh

Summary Four autotrophic compartments were recognised in Lake Kitiesh, King George Island (Southern Shetland) at the beginning of the summer in 1987: snow microalgae, ice bubble communities, phytoplankton in the water column and benthic communities of moss with epiphytes. Chlorophyll a concentration and pigment absorption spectra were obtained in these four compartments before and/or after the thawing of the ice cover. During the ice free period, carbon fixation and biomass was measured in the phytoplankton and in the benthic moss Campyliadelphus polygamus. From these measurements we conclude that the benthic moss is the most significant autotrophic component in this lake in terms of biomass, chlorophyll a content and primary productivity. The integral assimilation number (The ratio of carbon fixation per unit area to biomass per unit area) values were similar for both phytoplankton and the moss, ranging from 3.6 to 5.4 mg C (mg Chl a)^–1h^–1in phytoplankton and from 4.0 to 6.4 mgC (mg Chl a)^–1h^–1 in the benthic moss. This approach allows comparisons of carbon fixation efficiency of the chlorophyll a under a unit area between compartments in their different light environments.