南亚热带磷限制水库中浮游植物群落对氮磷比变化的响应

为了解P限制水体中浮游植物群落对N、P营养盐的响应,通过添加N、P营养盐设置N/P梯度,对广东省流溪河水库中的浮游植物群落进行了研究。结果表明,添加N、P显著促进浮游植物的生长,浮游植物群落受P盐的影响比N盐显著;藻类的种属特异性导致浮游植物群落对氮磷营养盐的响应不一致,浮游植物总丰度与N/P比值不相关,其中隐球藻(Aphanocapsa sp.)、拟柱胞藻(Cylindrospermopsis raciborskii)和假鱼腥藻(Pseudanabaena sp.)等蓝藻适合在高N高P条件下生长,双对栅藻(Scenedesmus bijuga)等绿藻优势种偏好中N高P环境,而曲壳藻(Achnanthes sp.)、小环藻(Cyclotella sp.)等硅藻在低N低P的环境下占据优势;P浓度为0.8～2.0μmol/L时存在诱导浮游植物碱性磷酸酶活性的阈值,当P浓度大于2.0μmol/L时则抑制酶活性; P浓度为2.0μmol/L可能是浮游植物维持生长的最适浓度,浮游植物N/P维持动态平衡;藻细胞N/P、C/P与水体P浓度、N/P呈显著正相关,而藻细胞C/N受N影响更明显(P0.05)。这为热带亚热带水库的水质管理提供了理论参考。     

陶粒浮床对草鱼养殖池塘水质和浮游植物的影响

为了探讨陶粒浮床对草鱼养殖池塘浮游植物群落结构的影响, 将6个池塘随机分为两组, 分别为浮床组和对照组, 2013年510月对养殖池塘的藻类群落结构和水质因子进行定期采样分析。结果表明: 浮床组池塘水体透明度显著高于对照组(P0.05), 养殖后期, 浮床组主要营养盐指标显著低于对照组(P0.05), 微生物总数显著高于对照组(P0.05)。水质理化指标波动范围小, 系统稳定性较强。试验期间共检出浮游藻类8门111属179种, 其中绿藻93种, 蓝藻25种, 硅藻23种, 裸藻17种, 黄藻6种, 甲藻5种, 金藻5种, 隐藻5种。在养殖中后期, 陶粒浮床对藻类的种类组成有显著影响, 藻类种数明显高于对照组, 浮床组和对照组浮游植物数量范围分别为101. 95106614.95 106 ind./L和151.43106612.60 106 ind./L, 生物量范围分别为90.79402.85 mg/L和116.33831.55 mg/L, 到养殖中后期(8月份以后), 对照组浮游植物的生物量显著高于浮床组(P0.05)。绿藻门和蓝藻门的贡献率一直占总密度的90%以上。浮游植物群落呈明显的季节变化, 绿藻门呈先降低后升高的趋势, 蓝藻门相反。试验初期浮游植物的优势种为栅藻; 在试验开始30d后, 浮床组栅藻继续保持优势藻的地位, 对照组的优势种则变为平裂藻和微囊藻; 78月份, 浮床组和对照组的优势种均为蓝藻门的平裂藻, 9月份后优势藻逐渐由栅藻和绿球藻取代。浮床组和对照组藻类多样性指数无显著差异, 物种丰富度均呈逐渐下降的趋势, 范围为3.165.59, Shannon指数和Simpson指数均呈先降低后升高的趋势, 范围分别为1.502.46和0.540.87。陶粒浮床对改善池塘水质、丰富藻类种类组成、降低过高生物量和微囊藻爆发的风险有一定作用。       

浮游动物调控对浮游藻类的影响

浮游动物可以通过牧食作用来抑制浮游藻类的增长, 同时浮游动物排泄的营养盐又可以促进浮游藻类的增长,二者的强弱是浮游动物控制浮游藻类的关键。通过人为去除处理组水体中的浮游动物, 研究浮游动物生物量和群落结构的不同对富营养水体中浮游藻类的影响。研究结果显示处理组浮游动物总生物量低于空白组, 且缺乏大型枝角类溞属(Daphnia sp.); 去除浮游动物显著降低了水体中的总氮和总磷浓度以及浮游藻类生物量(叶绿素a), 同时增加了附着藻的生物量; 并且影响了浮游藻类群落结构: 对照组是空星藻(Coelastrum sp.)为优势种而处理组则为湖丝藻(Limnothrix sp.)和四集藻(Palmella sp.)。结果表明浮游动物排泄营养盐产生的上行效应大于牧食作用产生的下行效应。     

博斯腾湖浮游植物群落结构特征及其影响因子分析

2011年对博斯腾湖大湖区17个采样站位的浮游植物及水体主要理化因子进行了4次系统调查。结果表明, 在17个站位共鉴定出浮游植物127种（属）, 其中优势种（属）9种。浮游植物群落全年均以硅藻为主导, 冬、春季节, 浮游植物组成呈硅藻-甲藻型, 优势类群主要为贫-中营养型浮游藻类, 到夏、秋季节逐渐形成硅藻-绿藻型, 以富营养型的浮游藻类为优势类群。浮游植物总平均生物量为（2.512.95） mg/L, 生物量季节变动显著, 峰值出现在夏季, 冬季最低。基于Canoco的多变量分析表明: 环境变量共解释了浮游植物群落总变异的54.5%, 水温是影响浮游植物分布最重要的环境因子, 其次为枝角类丰度。水中氮含量是影响浮游植物丰度的主要因子, 同时浮游植物对水体有机物含量也有较大的影响。       

生物过滤和蔬菜浮床组合系统对温室甲鱼废水的处理效果

高浓度温室甲鱼养殖业废水的无序排放已严重危害了我国长三角地区农村生态环境.生物过滤和蔬菜浮床组合系统是温室甲鱼养殖废水生态化处理的潜在方式.为了探索生物过滤和蔬菜浮床组合系统处理温室甲鱼养殖废水的可行性,以及植物直接吸收同化作用对组合系统N、P去除的贡献率,本文选择空心菜、生菜和芹菜等3种蔬菜植物,开展了生物过滤和蔬菜浮床组合系统对温室甲鱼养殖废水的处理试验.结果表明:生物过滤与蔬菜浮床组合系统对废水化学需氧量(COD)、铵氮(NH4+-N)、总氮(TN)和总磷(TP)的去除率分别可达93.2%~95.6%、97.2%~99.6%、73.9%~93.1%和74.9%~90.0%.组合系统均表现出良好的碳氮磷同步脱除性能,空心菜系统对废水N、P的去除效能明显优于生菜和芹菜系统.蔬菜直接吸收作用并不是组合系统N、P去除的最主要途径,其贡献率仅为9.1%~25.0%,推测N、P主要依靠微生物作用去除.相对而言,空心菜对废水N、P的直接吸收贡献率最高,而蔬菜对N、P的直接吸收与植物生物量密切相关.研究结果显示,生物过滤和蔬菜浮床组合系统可以作为温室甲鱼养殖废水生态化处理的有效方式.     

巢湖双桥河底泥疏浚过程中浮游植物功能群分类研究

浮游植物功能群分类分析可以精确地反映水体环境变化对水生生物群落的影响。为探究巢湖双桥河底泥疏浚工程对浮游植物群落及水生生态系统的影响,对2017年6月—2018年3月双桥河底泥疏浚期间的水体理化因子、浮游植物群落结构和功能群划分开展了研究。研究发现,底泥疏浚工程能够大量削减双桥河水体中的氮、磷营养盐,但疏浚后的双桥河仍处于中-富营养状态;双桥河浮游植物群落依据其生态功能可划分为M、H1、H2、MP、S1、L_O、X2、X1、J、F、N、G、X3、C、D、Y、W1、L_M、E、T、S_N、K、P等23个功能群,绝对优势功能群为以微囊藻为主的M功能群和以硅藻为主的MP、P功能群。底泥疏浚工程对双桥河浮游植物种类的影响不大,但藻类密度和生物量在疏浚后有显著地下降,浮游植物多样性指数也有提升。将浮游植物功能群生物量与环境因子进行冗余分析(RDA)和Pearson分析发现,水环境因子变化对双桥河浮游植物功能群产生了较大影响,双桥河浮游藻类优势功能群由底泥疏浚前的M、MP、P、W1、Y类转变为底泥疏浚后的C、F、J、M、MP、P、Y类。其中,底泥疏浚工程造成的氮营养盐削减可以对双桥河浮游植物功能群产生较大影响。研究认为双桥河底泥疏浚工程在改善河流浮游植物生态功能,减轻水体污染程度上有积极的作用。     

潜水式生态介质箱对黑臭水体的修复效果

生态浮床作为一种常规治理技术得到了广泛使用,但其只能修复表层富氧水体,对下层缺氧水体的修复能力有限.本研究针对实际黑臭水体的修复需要,设计了潜水式生态介质箱(潜水组),并以传统的生态浮床(浮床组)为对照进行对比试验,研究修复前后黑臭水体的水质变化,考察了水生植物的生长状况及N、P积累能力.结果表明:随着修复时间的延长,两组处理对各污染物的去除率均逐渐升高,其中潜水组去除全氮(TN)、铵氮(NH4^+-N)、全磷(TP)的能力优于浮床组,但其去除化学需氧量(CODMn)的能力稍逊;潜水组植物(苦草)的生长状况优于浮床组植物(菖蒲),且苦草对水体中TN、TP的吸收积累能力和去除贡献率均优于菖蒲;此外,苦草的质膜透性、丙二醛和叶绿素含量均低于菖蒲,说明苦草更适于在黑臭水体中生长,该潜水式生态介质箱是新型的一体化原位修复装置,更适用于黑臭水体的修复实践.     

长期砷胁迫下大屯海浮游植物群落的季节性特征及其驱动因子

重金属是影响湖泊水质和生态健康的重要胁迫因子,系统识别生物对长期污染胁迫的响应模式是开展污染湖泊生态修复的重要基础。本研究以经历持续砷污染的大屯海为研究对象,于2017年6月—2018年3月对水体浮游植物和环境因子开展季节性调查。结果显示: 大屯海的浮游植物群落主要由蓝藻门组成,与已有研究反映的长期砷胁迫下浮游植物组成以蓝藻门等耐受属种为主的特征一致。相似性和方差分析结果表明,浮游植物群落结构和生物量存在显著的时间差异而空间差异不显著。Pearson相关分析表明,浮游植物总生物量与溶解性正磷酸盐和砷呈显著正相关,与砷对藻类生长产生的低促高抑效应一致,同时磷酸盐的增加可能降低了砷对藻类的毒性效应。冗余分析显示,溶解性营养盐和砷是影响浮游植物群落变化的显著因子。方差分解结果表明,营养盐和水温分别单独解释了群落结构变化的17.6%和3.8%,且与砷产生了较强的相互作用(15.1%);而砷对浮游植物的群落构建无显著的独立作用,反映了现有优势藻类具有对砷较强的耐受性从而对砷浓度的变化不敏感。因此,大屯海的优势浮游植物以耐砷藻类为主,砷对藻类产生的低促效应是污染湖泊修复中需要重点关注的生态效应之一。     

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。     

放养鲢鱼(Hypophthalmichys molitrix C et V)对水库围隔浮游生物群落的影响

本文研究在水库围隔实验生态系统中鲢鱼对浮游生物群落的影响。结果表明,放养鲢鱼后,浮游动物生物量、浮游植物生物量、叶绿素a和浮游植物毛产量分别下降了58.7％、63.6％、52.5％和65.0％;透明度、浮游植物群落多样性指数分别提高了18.2％、32.5％;铜绿微囊藻数量减少了90.6％“水华”得到明显抑制。但小型绿藻(<20μm)数量未出现显著变化,因而其在藻类生物量中所占比例反而提高了82.3％。围隔内可被鲢鱼滤食的大型藻类(硅藻、甲藻、隐藻和绿藻(>20μm))占藻类生物量的85.8％,因此鲢鱼的存在能明显限制浮游植物的生物量。此外,放养鲢鱼还显著降低了水体中的COD,TP,DO和pH值,这表明鲢鱼对水质有净化作用。     

分区集群式清洁养殖池塘浮游生物群落结构及水环境特征

以传统模式养殖池作对照,研究了分区集群式清洁养殖模式池塘浮游生物群落结构及其水环境特征。结果表明,集群模式池塘网箱内外TN(总氮)分别为1.22 mg/L和1.31 mg/L,TP(总磷)分别为0.169 mg/L和0.170 mg/L,传统模式TN、TP分别为1.76 mg/L和0.689 mg/L。共检出浮游植物6门169种,绿藻门占优。密集养殖区(网箱内)浮游植物生物量为24.54 mg/L,多样性指数2.52,清洁区(网箱外)生物量23.51 mg/L,多样性指数2.47;共检出浮游动物183种,轮虫类占优。密集养殖区浮游动物生物量3.53 mg/L,多样性指数1.82,清洁区生物量2.95 mg/L,多样性指数1.86,传统模式浮游植物、浮游动物生物量分别为49.12、0.53 mg/L,多样性指数分别为2.06、1.79。与传统模式相对比,集群模式池塘TN、TP降低,蓝藻比例下降,浮游植物生物量减少,浮游动物生物量增大,生物多样性指数提高,水环境有一定改善。     

基于氮磷比解析太湖苕溪水体营养现状及应对策略

生态化学计量学是评价水体营养状态的重要手段,利用其氮磷比指标探讨了我国太湖主要入湖河流苕溪的营养状态。野外监测结果显示,苕溪水体氮素超标严重,磷素污染轻度,硝酸盐、颗粒态磷为氮磷的主要赋存形态,且氮磷浓度呈现相似的季节变化规律,表明苕溪主要受农业面源污染影响。氮磷比分析表明,苕溪水体春、秋季处于磷素限制状态,夏季适合藻类生长,冬季低温条件下不利于藻类的大量繁殖;苕溪生物量增长受磷素限制,线性拟合亦显示其氮磷比主要受磷素波动的调控;苕溪干流大面积暴发蓝藻水华的风险较部分支流及死水区低,苕溪水入湖后,特别是夏季其暴发风险将显著提高。针对苕溪水体的富营养化现状,提出若干条水质改善应对策略。     

九龙江西溪漳州段浮游植物组成与环境因子的关系

分别在2010年的丰、平、枯3个时期,从浮游植物种类组成、生物量(叶绿素a含量)及其粒级结构等指标对九龙江漳州段浮游植物组成进行了调查,同时分析了其与环境因子间的关系,评估了该河段的水质质量。结果表明:研究区域微微型浮游植物占总生物量比例与温度存在显著的正相关性(P<0.05),小型浮游植物占总生物量比例与总氮成显著的负相关(P<0.05)。共鉴定出浮游植物7门59种,且在各时期均有差异;丰水期与枯水期相比,蓝藻比例上升(P<0.05),甲藻比例下降(P<0.05);研究水域Shannon-Wiener指数在1.0～3.0,为中度污染。典型对应分析表明,温度和营养盐是影响九龙江西溪漳州段浮游植物群落变化的主要环境因子。     

Long-term nutrient trends and harmful cyanobacterial bloom potential in hypertrophic Lake Taihu,China

Rapid economic development in China’s Lake Taihu basin during the past four decades has accelerated nitrogen (N) and phosphorus (P) loadings to the lake. This has caused a shift from mesotrophic to hypertrophic conditions, symptomized by harmful cyanobacterial blooms (CyanoHABs). The relationships between phytoplankton biomass as chlorophyll a (Chla) and nutrients as total nitrogen (TN) and total phosphorus (TP) were analyzed using historical data from 1992 to 2012 to link the response of CyanoHAB potential to long-term nutrient changes. Over the twenty year study period, annual mean Chla showed significantly positive correlations with both annual mean TN and TP (P < 0.001), reflecting a strong phytoplankton biomass response to changes in nutrient inputs to the lake. However, phytoplankton biomass responded slowly to annual changes in TN after 2002. There was not a well-defined or significant relationship between spring TN and summertime Chla. The loss of a significant fraction of spring N loading due to denitrification likely weakened this relationship. Bioavailability of both N and P during the summer plays a key role in sustaining cyanobacterial blooms. The frequency of occurrence of bloom level Chla (>20 μg L^?1) was compared to TN and TP to determine nutrient-bloom thresholds. A decline in bloom risk is expected if TN remains below 1.0 mg L^?1 and TP below 0.08 mg L^?1.     

Trophic structure, species richness and biodiversity in Danish lakes: changes along a phosphorus gradient

1. Using data from 71, mainly shallow (an average mean depth of 3 m), Danish lakes with contrasting total phosphorus concentrations (summer mean 0.02–1.0 mg P L?l), we describe how species richness, biodiversity and trophic structure change along a total phosphorus (TP) gradient divided into five TP classes (class 1–5: <0.05, 0.05–0.1, 0.1–0.2, 0.2–0.4,> 0.4 mg P L?1).
2. With increasing TP, a significant decline was observed in the species richness of zooplankton and submerged macrophytes, while for fish, phytoplankton and floating‐leaved macrophytes, species richness was unimodally related to TP, all peaking at 0.1–0.4 mg P L?1. The Shannon–Wiener and the Hurlbert probability of inter‐specific encounter (PIE) diversity indices showed significant unimodal relationships to TP for zooplankton, phytoplankton and fish. Mean depth also contributed positively to the relationship for rotifers, phytoplankton and fish.
3. At low nutrient concentrations, piscivorous fish (particularly perch, Perca fluviatilis) were abundant and the biomass ratio of piscivores to plankti‐benthivorous cyprinids was high and the density of cyprinids low. Concurrently, the zooplankton was dominated by large‐bodied forms and the biomass ratio of zooplankton to phytoplankton and the calculated grazing pressure on phytoplankton were high. Phytoplankton biomass was low and submerged macrophyte abundance high.
4. With increasing TP, a major shift occurred in trophic structure. Catches of cyprinids in multiple mesh size gill nets increased 10‐fold from class 1 to class 5 and the weight ratio of piscivores to planktivores decreased from 0.6 in class 1 to 0.10–0.15 in classes 3–5. In addition, the mean body weight of dominant cyprinids (roach, Rutilus rutilus, and bream, Abramis brama) decreased two–threefold. Simultaneously, small cladocerans gradually became more important, and among copepods, a shift occurred from calanoid to cyclopoids. Mean body weight of cladocerans decreased from 5.1 μg in class 1 to 1.5 μg in class 5, and the biomass ratio of zooplankton to phytoplankton from 0.46 in class 1 to 0.08–0.15 in classes 3–5. Conversely, phytoplankton biomass and chlorophyll a increased 15‐fold from class 1 to 5 and submerged macrophytes disappeared from most lakes.
5. The suggestion that fish have a significant structuring role in eutrophic lakes is supported by data from three lakes in which major changes in the abundance of planktivorous fish occurred following fish kill or fish manipulation. In these lakes, studied for 8 years, a reduction in planktivores resulted in a major increase in cladoceran mean size and in the biomass ratio of zooplankton to phytoplankton, while chlorophyll a declined substantially. In comparison, no significant changes were observed in 33 ‘control’ lakes studied during the same period.     

Determination of tipping points for aquatic plants and water quality parameters in fish pond systems: A multi-year approach

High levels of nutrients in fish ponds by fish farming may cause significant eutrophication leading to a loss in species richness and a decrease of cover of aquatic plants to phytoplankton dominance. This shift can be represented by a tipping point where a significant change in the state of the ecosystem is observed such as a change from high to low aquatic plants species richness and cover. A total of 100 fish ponds were studied during five years in the Dombes region, France, to determine tipping points in aquatic plant richness and cover using chlorophyll α (CHL), water transparency, Total N (TN) and Total P (TP) gradients with two statistical methods. The relationships between tipping points, nutrient loads and yearly variations in weather conditions were also evaluated. Looking at the five years data, tipping points were observed in aquatic plant richness at 6 and 60 μg/L for CHL, and at 3.90 mg/L for TN concentration; as well as at 70 cm for water transparency, but no tipping point was found with TP. For aquatic plant cover, tipping points were observed at 11 μg/L for CHL, 2.42 mg/L for TN, 0.05 mg/L for TP, and at 62 cm for water transparency. These tipping points showed a significant decrease of aquatic plant species richness and cover, linked to the nutrient concentrations which drive the competition between the primary producers phytoplankton and aquatic plants. However, tipping points could vary significantly between years. The inter-annual variability may be due to an early occurrence of phytoplankton blooms in some ponds in a year preventing the establishment of aquatic plants, and thus influencing the value of tipping points. Weather conditions influence the competition between primary producers by impacting chlorophyll α and nutrients concentrations. When weather conditions supported increased nutrient concentrations, the development of phytoplankton and aquatic plants was facilitated and tipping points in aquatic plant richness and cover occurred with relatively high values. Thus, a significant decrease of plant cover and richness occurred at higher level of nutrients compared to the other years. In these cases, aquatic plants dominated over phytoplankton for the spring period, and also often during summer. In conclusion, tipping points observed are mainly linked to the competition between aquatic plants and phytoplankton. In shallow and eutrophic systems like fish ponds where nutrients are not a limiting resource, weather conditions act temporarily during spring as the main regulator of this competition.     

Phytoplankton–zooplankton dynamics in periodic environments taking into account eutrophication

In this paper, we derive and analyze a mathematical model for the interactions between phytoplankton and zooplankton in a periodic environment, in which the growth rate and the intrinsic carrying-capacity of phytoplankton are changing with respect to time and nutrient concentration. A threshold value: “Predator’s average growth rate” is introduced and it is proved that the phytoplankton–zooplankton ecosystem is permanent (both populations survive cronically) and possesses a periodic solution if and only if the value is positive. We use TP (Total Phosphorus) concentration to mark the degree of eutrophication. Based on experimental data, we fit the growth rate function and the environmental carrying capacity function with temperature and nutrient concentration as independent variables. Using measured data of temperature on water bodies we fit a periodic temperature function of time, and this leads the growth rate and intrinsic carrying-capacity of phytoplankton to be periodic functions of time. Thus we establish a periodic system with TP concentration as parameter. The simulation results reveal a high diversity of population levels of the ecosystem that are mainly sensitive to TP concentration and the death-rate of zooplankton. It illustrates that the eruption of algal bloom is mainly resulted from the increasing of nutrient concentration while zooplankton only plays a role to alleviate the scale of algal bloom, which might be used to explain the mechanism of algal bloom occurrence in many natural waters. What is more, our results provide a better understanding of the traditional manipulation method.     

珠江口及毗邻海域营养盐对浮游植物生长的影响

基于2006年7月(夏季),10月(秋季)和2007年3月(春季)的现场调查数据,对珠江口及毗邻海域中的营养盐和叶绿素a等环境生态因子的时空分布特性进行了对比分析,研究了氮磷比与叶绿素a含量和种群多样性之间的联系,探讨了该海域营养盐对于浮游植物生长的影响。结果表明:(1)研究海域营养盐表现出较强的季节和空间差异性,总氮(TN)和总磷(TP)浓度均值春季(1.545 mg/L、0.056 mg/L)和夏季(1.570 mg/L、0.058 mg/L)均大于秋季(1.442 mg/L、0.034 mg/L),且春夏季浓度空间差异更明显。(2)调查期间海域营养盐含量超标现象突出,夏季尤为明显。无机氮(DIN)总体均值0.99 mg/L,超四类海水标准限值1倍,活性磷酸盐(PO4-P)总体均值0.021 mg/L,DIN∶PO4-P平均值为130;叶绿素a浓度与营养盐、p H、温度有较显著的相关性。(3)叶绿素a浓度较高的站位,具有较高的DIN∶PO4-P值,但浮游植物多样性指数偏低,优势种明显,主要为中肋骨条藻。氮磷比的改变会影响不同生长特性的浮游植物间的竞争和种群结构的改变;今后海洋污染治理中,在控制氮、磷污染时要注意氮磷比的改变可能造成的浮游生态影响。     

保安湖菹草种群的时空分布特征及环境效应分析

为了解近20年来保安湖菹草(Potamogeton crispus L.)种群的变化特征及其对水环境的影响, 研究以保安湖最大的湖区, 即主体湖为研究对象, 分季节对其沉水植物种类组成、生物量及水深(Z_M)、透明度(Z_SD)、水中总氮(TN)、总磷(TP)和浮游藻类叶绿素a(Chl. a)等环境指标进行了监测, 并分析了菹草在不同生活史阶段对环境影响的差异。结果表明: (1)2002年春季菹草生物量(B_P.c)均值为356 g/m2, 2012年上升至974 g/m2, 2019年为1901 g/m2, 菹草种群分布范围由中部扩展至整个湖区; (2)在春季菹草快速生长时, B_P.c与Z_M(Z_M≤3 m)呈显著正相关(r= 0.52, P<0.01), 与Chl. a呈显著负相关(r= –0.42, P<0.01), 与Z_SD、Z_SD/Z_M、TN、TP无相关关系; 有草区的Z_M(中位数为2.1 m)、Z_SD(中位数为0.93 m)和Z_SD/Z_M(中位数为0.48)显著高于无草区(1.8 m、0.45 m和0.28; P<0.05), 有草区的Chl. a(中位数为8.13 μg/L)显著低于无草区(14.10 μg/L; P<0.05); 有草区的Chl. a和TP的关系不明显, 无草区的Chl. a的含量随TP上升而增加, 且在相同TP条件下, 无草区Chl. a多数高于有草区; (3)在夏季菹草衰亡后, 夏季Z_SD/Z_M与B_P.c呈显著负相关(r= –0.47, P<0.01), Z_SD、TN、TP、Chl. a与B_P.c无相关关系; 无草区TN(中位数为1.30 mg/L)显著高于有草区(0.72 mg/L; P<0.05); 有草区和无草区的Chl. a均随TP的上升而增加, 在相同TP条件下, 无草区Chl. a和有草区差异不显著。以上结果表明近20年来保安湖菹草种群生物量呈上升趋势, 分布范围也在不断增加。在快速生长期(春季), 大量菹草的存在有利于水质的改善。在菹草衰亡(春末夏初)后, 其对水质产生的不利效应未持续整个夏季。     

Production of lower-trophic organisms during incubation of unaltered deep-sea water

Incubation of unaltered deep-sea water and grazing experiment of nano- and micro- protozooplankton during incubation of deep-sea water were carried out to quantitatively characterize the planktonic structures of lower-trophic organisms and clarify the trophic pathways and controlling mechanisms involved. Phytoplankton biomass increased to 637 mg as carbon weight in a 500-l tank on Day 7 and was dominant in the planktonic structure of lower-trophic organisms. Nitrates in the incubation water was depleted after Day 7 and phytoplankton biomass decreased rapidly. On the other hand, bacteria, heterotrophic nano-flagellates and ciliates increased toward the end of incubation and were dominant in the later days of incubation. In grazing experiments on microbial organisms, bacterivory is more important for the carbon pathway in microbial food webs than herbivory when phytoplankton biomass is less than that of bacteria (low P/B conditions), while herbivory is more important than bacterivory when phytoplankton biomass is more than that of bacteria (high P/B conditions). Deep-sea water exhibited high phytoplankton productivity due to inherent high nutrients values. After depletion of nutrients, phytoplankton decreased (due also to enhanced nano- and micro-zooplankton grazing) and microbial organisms dominated. Thus, nutrients in the incubation water control the planktonic structure of lower-trophic organisms.