对虾养殖围隔生态系颗粒悬浮物的研究

对５个对虾养殖围隔生态系颗粒悬浮物进行了研究．结果表明,颗粒悬浮物总量波动在２０．８３～１７２．５０ｍｇ·Ｌ－１之间,平均７２．２６±３９．８７ｍｇ·Ｌ－１,其中颗粒有机物占６２％,颗粒无机物占３８％．颗粒有机物中,颗粒腐质与细菌占９８％,浮游生物占２％（其中浮游植物为浮游动物生物量的４．５０倍）．颗粒悬浮物浓度（ＴＭ）与水体透明度（Ｓ）呈显著相关性     

盐碱池塘围隔生态系统的悬浮物结构及有机碳库储量

1 998年 4～ 7月对高青盐碱池塘单养鲢和罗非鱼围隔生态系统颗粒悬浮物构成和各有机碳库储量及动态进行了研究。结果表明 ,浮游生物的干重 (PZ)占总颗粒悬浮物干物质 (TS)的 4.2 6%～ 2 5 .97% ,平均 1 2 %。各围隔浮游植物干重(DWP)平均值变化范围为 0 .1 6～ 0 .70 mg/L,有鱼围隔均比无鱼围隔的大。浮游动物干重 (DWZ)平均值变化范围为0 .3 2～ 2 .81 mg/L,养鲢围隔中最小 ,小于无鱼对照围隔 ,养罗非鱼围隔明显高于养鲢围隔。颗粒悬浮物的灰分含量平均值为 42 .3 8%。溶解有机碳 (DOC)、颗粒有机碳 (POC)库储量平均值分别为 5 .40± 1 .61 mg C/L和 1 .96± 0 .96mg/L。各处理围隔间颗粒有机物的 C/N比的平均值比较接近 ,总平均值为 6.97± 0 .2 4。 TOC、DOC和 POC比例为 1∶ 0 .73∶0 .2 7。浮游生物碳和腐质颗粒碳占 POC的比例的平均值分别为 3 4.65 %和 65 .3 5 %。腐质颗粒碳、浮游动物碳与浮游植物碳的比例为 9.2 9∶ 3 .71∶ 1。浮游生物碳中浮游动物碳占 78.8% ,浮游植物碳占 2 1 .2 %。浮游动物碳比浮游植物碳高 ,这可能是内陆盐水的通性。盐碱池塘围隔生态系统颗粒有机碳 (POC,mg C/L)与浮游植物叶绿素 a(Chla,μg/L)和悬浮颗粒有机物 (SO,mg/L)之间存在显著的正相关关系 ,其回归方程分别为     

武汉东湖颗粒悬浮物的结构与元素组成

本研究于1989-1990对武汉东湖营养水平不同的二个湖区的颗粒悬浮物的干物质结构和元素组成进行了分析。综合平均值表明,浮游动物的现存量约为浮游植物的1/4,浮游动物群落以小型的原生动物和轮虫占优势。从年平均值来看,浮游生物的干重占颗粒悬浮物干物质的2.5-7.6%,浮游生物碳量占颗粒悬浮物碳量的4.0-9.8%;颗粒悬浮物的碳/氮比与一般浮游植物的比值相似,但明显大于多数浮游动物;颗粒悬浮物的碳与干物重之比约为一般浮游生物的3/4;颗粒悬浮物的灰分含量约为45%,显着高于除硅藻以外的其它浮游生物。从数量上来看,有机碎屑是东湖生态系统颗粒悬浮物最重要的组成部分,而活体浮游生物只占颗粒悬浮物很小的一部分(<10%);这意味着在东湖来自以浮游植物为核心的食物网的有机碎屑的形成速率显着大于有机碎屑的矿化速率。       

刺参养殖池塘颗粒悬浮物结构及其沉积作用

对不投饵刺参养殖池塘的颗粒悬浮物结构及其沉积量和沉积速度进行了研究.结果表明:(1)各池塘总颗粒悬浮物重量(TS)为(73.1±20.5)mg/L,变动于46.0～132.0mg/L之间;颗粒无机物(IS)含量为(50.6±12.6)mg/L,变动于28.5～76.5mg/L之间,占总颗粒悬浮物的69.13%;浮游生物干重(PZ)为(0.675±0.706)mg/L,变动于0.064～2.814mg/L之间,其中浮游植物干重(DWP)为(0.541±0.622)mg/L,变动于0.062～2.582mg/L之间,浮游动物干重(DWZ) 为(0.135±0.200)mg/L,变动于0.002～1.160mg/L之间;颗粒腐质为(21.91±19.59)mg/L,变动于4.18～83.86mg/L之间,占总颗粒悬浮物的比例为29.95%.(2)总颗粒物沉积量为(19.44±16.34)g·m-2·d-1,变动于6.33～91.98g·m-2·d-1之间,沉降速度为(0.30±0.30)m·d-1,变动于0.08～1.63m·d-1之间,新生态颗粒有机物沉积量为(5.09±7.30)g·m-2·d-1,变化于0.14～31.27g·m-2·d-1之间,总颗粒物沉积量和新生态颗粒物沉积量均是底层高于表层.     

轮虫培育池生态系统各有机碳库储量及其日变化

2001年5～6月对辽宁省盘锦光合水产有限公司的两种模式轮虫培育池有机碳库储量及动态进行了研究.结果表明,静水池溶解有机碳（DOC）和颗粒有机碳（POC）库储量平均值分别为5.69±2.90 mg·L^-1和24.56 ± 2.12 mg·L^-1;流水池DOC和POC分别为9.61±3.17 mg·L^-1和24.13 ±2.91 mg·L^-1.流水池和静水池TOC、DOC和POC的比例分别为 1∶0.75∶0.25和1∶0.82∶0.18.POC含量高的池塘DOC含量也较高.流水池的POC、DOC周日变动幅度大,静水池昼夜变动幅度小.流水池POC含量白天(5:00～17:00)升高,静水池降低,夜间(15:00～23:00)两池POC含量均降低.从23:00至次日5:00上升,两池分别在17:00和5:00达到高峰.白天(5:00～17:00) 流水池DOC/POC升高,静水池降低;夜间(17:00～23:00)两池均上升,23:00 至次日5:00则呈下降趋势.     

卤虫培育池浮游生物生态学

2002年在内蒙古桑根达莱淖尔进行了卤虫养殖实验,研究了3个卤虫培育池的浮游生物、初级生产力、水化学因子、限制性营养盐及卤虫的生长,并探讨了各种生态因子与浮游植物、卤虫生长的关系。结果表明:实验期间共发现浮游生物27种(或属),其中浮游植物17种(或属),浮游动物10种(或属)。1#、2#、3#池的浮游植物平均生物量分别为2.41mg/L、1.72mg/L、1.31mg/L,蓝藻门和绿藻门占优势,优势种为小席藻、线形粘杆藻、小颤藻、普通小球藻、椭圆小球藻;浮游动物的平均生物量分别为24.47mg/L、22.04mg/L、19.27mg/L,轮虫占优势,优势种为褶皱臂尾轮虫、变异臂尾轮虫。盐度、pH、Cl-、Na K 、HCO3-、CO32-、ALK、总氮、总磷呈上升趋势,特别是Cl-、Na K 实验前后相差3000mg/L以上;SO42-呈下降趋势;TH、Ca2 、Mg2 无明显变化规律,实验前后基本平衡。温度、pH、溶解氧(DO)的昼夜变化明显,其昼夜差分别在10℃、0.5、1mg/L左右。从限制性营养盐来看属于磷限制,初级生产力极低,P/R系数>1.5。     

“海蜇-缢蛏-牙鲆-对虾”混养池塘悬浮颗粒物结构及其有机碳库储量

为了阐明"海蜇-缢蛏-牙鲆-中国对虾"混养池塘生态系统的结构和功能特征,并为不同养殖模式的碳循环研究和发展低碳渔业提供参考,于2013年5—10月对辽宁丹东东港地区(N 39°51';E 124°09')两个该种混养池塘的悬浮颗粒物结构及其有机碳储量进行了研究。结果表明,两个实验池塘总悬浮颗粒物含量分别为(67.12±6.03)mg/L和(70.05±7.63)mg/L,其中无机悬浮颗粒物占总悬浮颗粒物的72.57%和75.49%;有机悬浮颗粒物占总悬浮颗粒物的27.43%和24.51%。有机悬浮颗粒物中,腐质及细菌占总悬浮颗粒物的27.15%和24.20%;浮游植物干重占0.15%和0.22%;浮游动物干重占0.13%和0.09%。两个实验池塘悬浮颗粒物中的总有机碳(TOC)含量分别为(7.31±1.51)mg/L和(6.42±1.31)mg/L;其中溶解有机碳(DOC)占总有机碳的76.33%和70.56%;颗粒有机碳(POC)占总有机碳的23.67%和29.44%;细菌碳占总有机碳的7.96%和7.18%;腐质碳占总有机碳的14.70%和20.90%;浮游植物碳占总有机碳的0.56%和0.95%;浮游动物碳占总有机碳的0.45%和0.41%。实验池塘中总悬浮颗粒物含量相对较高,其中无机悬浮颗粒物是主要的组成部分;细菌和腐质是有机悬浮颗粒物主要的组成部分,说明腐质链在该种养殖生态系统的物质循环和能量流动中起主要作用。     

虾池生态系各有机碳库的储量

1997年6～8月于山东省海阳市黄海集团公司养虾场,采用围隔实验生态学方法研究了虾池生态系各有机碳库的储量,结果表明:溶解有机碳(DOC)、颗粒有机碳(POC)库储量(mgC/l)平均分别为9.95±2.04及3.10±1.60,DOC/POC比值平均为3.21.POC库中,腐质颗粒碳为总浮游生物碳的2倍.浮游植物碳、浮游动物碳、浮游细菌碳平均分别占总浮游生物碳的53%、13%及34%.腐质碳、总浮游生物碳平均分别占总有机碳(TOC)的92%及8%,腐质碳为总浮游生物碳的11.08倍.     

密云水库的浮游生物群落

2002年4～10月对密云水库浮游生物群落的调查结果显示：浮游植物有6门,58属,122种,细胞密度为565．30～10^4cells／L,4月份硅藻(Bacillariophyta)占优势,6～10月蓝藻(Cyanophyta)占绝对优势．浮游植物优势种群有水华微囊藻(Microcystis flas-aquae)、颗粒直链藻(Melosira granulata)、梅尼小环藻(Cyclotella meneghiniana)、角甲藻(Ceratium hirundinella)等。浮游动物有36种,密度为4761ind/L;浮游动物具有原生动物在数量上占绝对优势．轮虫次之,枝角类与桡足类数量较少的特点。浮游动物的优势种群有弹跳虫(Halteria grandinella)、急游虫(Stromlridium uiHde)、针簇多肢轮虫(Polyarthra trigla)、螺形龟甲轮虫(Keratella cochlearis)、广布中剑水蚤(Mesocyclops leuckarti)、长额象鼻蚤(Bosmlna longirostris)等．与1980年监测结果相比,密云水库浮游生物总密度上升较快,群落结构和优势种群也发生了明显变化．浮游生物优势种群的指示作用显示,在植物生长季节,库区水体已进入富营养状态。     

惠州西湖底泥疏浚对后生浮游动物群落的影响

结合在一个热带浅水湖泊--惠州西湖的一个子湖--湖所实施的底泥疏浚工程,对比分析了底泥疏浚前后部分水质指标和后生浮游动物群落的种类组成、丰度、生物量和物种多样性的变化,研究了底泥疏浚对平湖后生浮游动物群落的影响.结果表明:疏浚后平湖的部分水质指标较疏浚前有所恶化;后生浮游动物的丰度由疏浚前的186.08 ind.·L-1增加到659.22 ind.·L-1,其中轮虫和桡足类的丰度显著增加,枝角类丰度降低;生物最由1.49 mg.·L-1增加到3.72 mg.·L-1,其中轮虫和枝角类的生物量均有所增加,但其在浮游动物总生物量中所占比例却有所下降,桡足类的生物量则由0.08 mg·L-1增加到0.80 mg·L-1,在总生物量所占比例明显上升;Shannon-Weaner指数由2.24下降到1.84.底泥疏浚造成水体营养盐的上升,促进了浮游植物的生长,从而为浮游动物的种群发展提供了充足的食物供给,加之由于干湖底泥疏浚所导致的鱼类捕食压力的减少,多种因素共同导致了疏浚后平湖后生浮游动物种群的生物量、丰度和个体火小的增加.结果看,惠州西湖的清淤不能有效改善水质,也不能恢复生态系统,湖泊恢复必须结合其他措施.     

Carbon flow in a small turbid man-made impoundment

A shallow turbid man-made impoundment was studied intensively for five years. The carbon (C) budget indicated a well balanced system, where phytoplankton productivity and respiratory losses accounted for the major inputs and outputs. The carbon content was dominated by dissolved organic carbon, followed by detritus > fish > phytoplankton > bacteria > zooplankton > zoobenthos.From an analysis of a matrix flow model, three dominant components of C-flow in the system were identified, i.e. dissolved inorganic carbon (DIC), particulate organic carbon (POC) and fish. Phytoplankton and detritus were the important components of POC. The largest flow of C was through the largest pool, dissolved inorganic carbon (DIC), whilst the second largest flow was through the fifth largest pool, the phytoplankton. Phytoplankton was very important in determining the structure of the system, and variations in phytoplankton primary productivity influenced the entire system. This also applied to the input of organic material from macrophytes, but not to variations in the inflow and outflow of water from the impoundment.The input of detrital material from a littoral macrophyte community also markedly influenced the system. DOC was identified as a carbon buffer in the system, and differential flow occurred through this component upon variations in phytoplankton productivity.     

优化滩涂养殖水体生态结构和调节水质的研究

采用在滩涂鱼塘和虾池中接种小球藻和有益微生物的方法,探讨了调控滩涂养殖水体生态结构的浮游生物种群、数量、生物量及化学环境的可行性。结果表明,虾池和鱼塘中接种小球藻后,小球藻数量均大幅度增加,变为优势种群,分别是其对照的16.92倍、4.76倍;浮游动物生物量为4.32mg·L^-1和2.84mg·L^-1,分别比对照增加19.3%、2.5%,同样,光合细菌、酵母菌及硝化细菌显著地改变了水体藻类和浮游动物种群的组成、数量、比例及生物量等,“酵母菌＋硝化细菌”的处理,使水体氨态氮浓度下降最明显,为对照的44％,虾池生化耗氧和化学耗氧,为对照的56.5%和38.4%,增加了水体溶解氧和初级生产力。     

The origin of particulate organic matter and the diet of tilapia from an estuarine ecosystem subjected to domestic wastewater discharge: fatty acid analysis approach

The fatty acid composition of suspended particulate organic matter (POM) and tilapia (Oreochromis mossambicus) and potential sources of organic material in the Manko Estuary, Okinawa Island, Japan, were investigated to elucidate the origin of organic matter in suspended particulate matter and the contribution of these inputs to the diet of tilapia. Fatty acid fingerprints of POM revealed that diatoms, bacteria, and possible material input originating from domestic waste discharges contributed a major proportion of the organic matter pool in the estuary. The diet of tilapia is likely influenced by domestic waste-derived organic matter through a POM link. Because of their highly plastic feeding habits, tilapia may develop a feeding strategy of utilizing the most favorable food resources in the ecosystem. Tilapia likely does not prefer mangrove detritus as a food source as indicated by the absence of even-number long-chain fatty acids (LCFAs) in their tissues. Instead of mangrove detritus, tilapia preferentially utilized more palatable organic food sources in the water column, such as phytoplankton and its detrital matter. In addition to phytoplankton and bacterioplankton, the other dietary sources that contributed a minor fraction were possible green macroalgal materials and zooplankton.     

Habitat structure determines resource use by zooplankton in temperate lakes

While the importance of terrestrial linkages to aquatic ecosystems is well appreciated, the degree of terrestrial support of aquatic consumers remains debated. Estimates of terrestrial contributions to lake zooplankton have omitted a key food source, phytoplankton produced below the mixed layer. We used carbon and nitrogen stable isotope data from 25 Pacific Northwest lakes to assess the relative importance of particulate organic matter (POM) from the mixed layer, below the mixed layer and terrestrial detritus to zooplankton. Zooplankton and deep POM were depleted in 13C relative to mixed layer POM in lakes that can support deep primary production. A Bayesian stable isotope mixing model estimated that terrestrial detritus contributed <5% to zooplankton production, and confirms the role of lake optical and thermal properties; deep POM accounted for up to 80% of zooplankton production in the clearest lakes. These results suggest terrestrial support of lake zooplankton production is trivial.     

Nutritional value of detritus and algae in blenny territories on the Great Barrier Reef

The salariin blenny, Salarias patzneri, primarily ingests detrital aggregates and inorganic sediment, with small quantities of filamentous algae. Samples of particulate matter <125 μm and filamentous algae were collected from the territories of S. patzneri and the nutritional value of these resources assessed using organic content and protein/energy ratios calculated from protein, carbohydrate and lipid content. Samples were collected throughout the day, during both summer and winter, to enable temporal comparisons of nutritional value. The particulates <125 μm, which were predominantly amorphic detritus, accounted for 41±2% and 44±3% of the organic matter in the epilithic algal matrix (EAM) during the summer and winter, respectively, whilst filamentous algae accounted for 37±3% and 41±3% of the organic matter in the summer and winter, respectively. Carbohydrate and lipid concentration in the algal samples was significantly greater than in particulate matter <125 μm, although no significant difference was detected in protein levels of algal samples and particulates <125 μm. Consequently, the protein/energy ratio of particulates <125 μm in the summer (11±1 mg kJ⁻¹) and winter (10±1 mg kJ⁻¹) was similar to that of filamentous algae in the summer (9±1 mg kJ⁻¹) and winter (8±1 mg kJ⁻¹). These results suggest detrital aggregates are at least comparable to filamentous algae as a nutritional resource. The large contribution of high quality detritus to organic matter in the epilithic algal matrix collected from S. patzneri territories throughout the day and between seasons provides strong evidence that detritus is a valuable component of small territorial fish diets and is an integral part of coral reef food webs.     

The role of plankton biomass in controlling fluctuations of suspended matter in Lake Constance

The concentrations of particulate matter, expressed as dry weight (DW), particulate organic (POM), and inorganic material were measured at regular intervals in Lake Constance between February 1980 and December 1982. Maximum particle concentrations were recorded for the euphotic zone in summer (7 mg l⁻¹), while minima occurred during the early summer and in winter. Annual mean concentrations of DW within the entire water column varied between 0.6 and 0.7 mg l⁻¹. In the euphotic zone nearly 70% of DW is organic material. The inorganic particles originate either from phytoplankton (diatomaceous silicon, biogenic decalcification) or from the tributaries. Although phytoplankton biomass only comprises a relatively small proportion (i.e. 30% at maximum) of organic matter, it is the primary source of POM. Therefore, seasonal variations in phytoplankton control epilimnetic concentrations of POM in Lake Constance. Inorganic material comprises smaller proportions of suspended matter. Seasonal variations are related predominantly to fluctuations in biomass and therefore particulate inorganic matter is suggested to originate mainly from autochthonous sources. At the sampling station concentrations of inorganic particles supported by the main tributary, the Alpenrhein, only occasionally vary concomitantly with runoff.     

Interactions of detrital particulates and plankton

Detrital particulates, i.e. inorganic and non-living organic material of colloidal size and larger, span ten orders of magnitude in size and are ubiquitous in inland waters. Interactions between plankton and detrital particulates are reciprocal. Release of dissolved organics by living organisms enter the particulate size fraction by flocculation on bubbles or adsorption to inorganic particles. Bacteria benefit from attachment to particles and are agents in the aggregation of particulates. Nutrients released by decaying plankton can support phytoplankton growth. Potentially toxic compounds adsorb to particulates and then can enter pelagic food webs or sediment. Material egested by zooplankton contributes to the detrital pool which in turn is a food source for zooplankton.     

Influence of gizzard shad on phytoplankton size and primary productivity in mesocosms and earthen ponds in the southeastern U.S.

Gizzard shad (Dorosoma cepedianum), a filter feeding omnivore, can consume phytoplankton, zooplankton and detritus and is a common prey fish in U.S. water bodies. Because of their feeding habits and abundance, shad have the potential to affect primary productivity (and hence water quality) directly through phytoplankton grazing and indirectly through zooplankton grazing and nutrient recycling. To test the ability of shad to influence primary productivity, we conducted a 16-day enclosure study (in 2.36-m³ mesocosms) and a 3-year whole-pond manipulation in 2–5 ha earthen ponds. In the mesocosm experiment, shad reduced zooplankton density and indirectly enhanced chlorophyll a concentration, primary productivity, and photosynthetic efficiency (assimilation number). While shad did not affect total phytoplankton density in the mesocosms, the density of large phytoplankton was directly reduced with shad. Results from the pond study were not consistent as predicted. There were few changes in the zooplankton and phytoplankton communities in ponds with versus ponds without gizzard shad. One apparent difference from systems in which previous work had been conducted was the presence of high densities of a potential competitor (i.e., larval bluegill) in our ponds. We suggest that the presence of these extremely high larval bluegill densities (20–350 larval bluegill m^–3; 3–700 times higher density than that of larval gizzard shad) led to the lack of differences between ponds with versus ponds without gizzard shad. That is, the influence of gizzard shad on zooplankton or phytoplankton was less than the influence of abundant bluegill larvae. Differences in systems across regions must be incorporated into our understanding of factors affecting trophic interactions in aquatic systems if we are to be able to manage these systems for both water quality and fisheries.