湘江干流浮游生物群落结构及水质状况分析

为了解湘江干流水质与生物群落现状, 2010-2011年对湘江的水质和浮游生物的分布进行了采样分析, 利用香农-威纳多样性指数分析湘江干流浮游生物群落特征, 并结合水质理化指标评价其水体营养状态。结果表明, 共检出浮游植物8门99属164种, 丰度变化在(1.83-51.1)104cells/L, 生物量变化在0.03-0.60 mg/L; 浮游动物80种, 密度变化在2.16-76.34个/L, 生物量变化在0.01-1.95 mg/L。各采样点的浮游植物多样性指数变化在2.47-5.43, 浮游动物多样性指数变化在1.63-3.38, 浮游生物的多样性较好, 显示出湘江干流的浮游生物群落处于较稳定的状态。对湘江m-m指示种种类组成和群落结构分析, 结果显示湘江水体属于中污带水质; 综合营养状态指数(TIL)在38.27-51.97, 均值为43.73, 属于中营养水平; 综合水质生物学和化学评价结果可知湘江干流的水质较差, 但无明显向富营养化转化的趋势。       

三亚珊瑚礁分布海区浮游生物的群落结构

为了更好地了解珊瑚礁区生物群落应对环境变化的生态响应机制,以及浮游生物群落结构与珊瑚礁发展发育的关系,我们于2006年10月26日至11月10日对三亚珊瑚礁保护区9个有珊瑚礁分布的站点进行了浮游生物群落结构的调查.共鉴定出浮游植物种类61属130种(包括变种、变型),其中硅藻门48属101种,甲藻门10属25种,蓝藻门2属3种,金藻门1属1种.硅藻门的角毛藻属(Chaetoceros)种类最多,根管藻属(Rhizosolenia)的种类次之.调查海区浮游植物的细胞丰度范围为348-11,320个/L,平均为3,247个/L.在浮游植物群落中硅藻占绝对优势,平均丰度为3,230个/L,占总密度的99.5％.调查海区共鉴定出浮游动物76种,其中桡足类29种,水母类17种,浮游幼虫10种,毛颚类7种,被囊类6种,浮游腹足类4种,十足类、多毛类和介形类各1种.调查海区浮游动物的密度范围为43-190个/m3,平均为114个/m3.优势类群为桡足类、各类幼虫和毛颚类,平均分别占浮游动物总密度的28.5％,27.7％和13.6％.各站位浮游植物的多样性指数和均匀度平均分别为3.98和0.70,浮游动物的多样性指数和均匀度平均分别为4.37和0.87.鹿回头和大东海海域的浮游植物密度大,而生物多样性指数低.活的造礁石珊瑚种数和覆盖率高的站点的浮游生物多样性也较高.     

灞河城市段浮游生物群落结构时空变化及其与环境因子的关系

为了解灞河城市段浮游生物群落结构及其与环境因子之间的关系,于2016年9月至2017年7月每2个月进行一次采样分析。调查期间共鉴定出浮游植物7门63属,其中绿藻门种类数最多(34.9%),其次为硅藻门(30.2%);浮游动物4类45种,以轮虫(48.9%)和原生动物(24.4%)为主。浮游植物和浮游动物的丰度分别为0.73×104—98.5×104个/L和20—1084个/L,在时空分布上均呈现下游高于上游的趋势,峰值均出现在夏季。根据水体透明度、溶解氧、总磷、总氮、高锰酸盐指数和重金属等理化指标、浮游生物丰度、Shannon-Wiener多样性指数和Margalef丰富度指数对灞河城市段水质状况进行综合评价,结果显示,所研究流域总体为中污状态,上游景观河道内的水生植物对水体具有一定的修复能力。典范对应分析表明,水温、总氮、pH、溶解氧和汞是浮游植物群落分布的主要影响因子;影响浮游动物群落分布的主要因子为水温、总氮、总磷、叶绿素a和汞。     

灞河城市段浮游生物群落结构时空变化及其与环境因子的关系

为了解灞河城市段浮游生物群落结构及其与环境因子之间的关系,于2016年9月至2017年7月每2个月进行一次采样分析。调查期间共鉴定出浮游植物7门63属,其中绿藻门种类数最多(34.9%),其次为硅藻门(30.2%);浮游动物4类45种,以轮虫(48.9%)和原生动物(24.4%)为主。浮游植物和浮游动物的丰度分别为0.73×10~4—98.5×10~4个/L和20—1084个/L,在时空分布上均呈现下游高于上游的趋势,峰值均出现在夏季。根据水体透明度、溶解氧、总磷、总氮、高锰酸盐指数和重金属等理化指标、浮游生物丰度、Shannon-Wiener多样性指数和Margalef丰富度指数对灞河城市段水质状况进行综合评价,结果显示,所研究流域总体为中污状态,上游景观河道内的水生植物对水体具有一定的修复能力。典范对应分析表明,水温、总氮、pH、溶解氧和汞是浮游植物群落分布的主要影响因子;影响浮游动物群落分布的主要因子为水温、总氮、总磷、叶绿素a和汞。     

浙江水源地水库浮游动物丰度和生物量与水质参数的通径分析

为探明浙江水源地水库浮游动物群落特征及与环境因子的关系, 达到用浮游动物群落参数监测水源地水库水质的目的。于2014年1月至2016年10月, 对10个饮用水源地水库(K1—K10)展开了水质参数、浮游动物丰度和生物量的季节调查。采用多元逐步回归与通径分析的方法, 研究了浙江水源地水库环境因子与浮游动物群落之间的相互关系和作用过程。结果表明, 2014—2016年水库浮游动物平均密度97.5 ind./L, 主要由桡足类无节幼体(占36.3%)、轮虫(28.4%)和剑水蚤(20.0%)组成。平均生物量289.3 μg/L, 主要由枝角类(占39.3%)、剑水蚤(29.0%)和哲水蚤(14.5%)组成。Chl. a含量是春、夏季水库浮游动物丰度的决策因子, TP含量是秋、冬季群落丰度波动的限制因子, 春季TN通过N﹕P比率影响群落丰度。DO含量是冬季和夏季水库浮游动物生物量发展的决策因子, 冬季DO通过降低N﹕P比促进群落生物量发展。水库浮游动物现存量受到了TP含量消长、N﹕P比率变化, 以及最终反映的水体Chl.a含量共同影响。     

鄱阳湖不同水文期浮游生物群落结构特征和影响因素及水质评价

为阐明鄱阳湖不同水文期浮游生物群落结构特征及其影响因素, 研究于2017年8月(丰水期)和12月(枯水期)在鄱阳湖湖区典型水域设置5个采样点进行浮游生物采样调查。研究期间共鉴定浮游植物8门75属186种, 丰水期与枯水期均以硅藻门和绿藻门为主。共鉴定浮游动物4类76种, 丰水期与枯水期均以原生动物和轮虫为主。方差分析显示: 浮游植物密度与生物量在不同水文期之间的差异均为极显著(P<0.01), 浮游动物丰水期密度高于枯水期, 但无显著差异(P>0.05), 浮游动物生物量(P<0.05)在不同水文期差异显著。冗余分析(RDA)显示: 丰水期透明度和浮游生物呈显著负相关关系, 电导率和浮游生物呈显著正相关。透明度、电导率与营养盐是影响丰水期浮游生物群落结构的主要环境因素, 枯水期水温和溶解氧是驱动鄱阳湖浮游生物群落生态分布的主要环境因素。基于Shannon-Wiener(H′)、Margalef(d)和Pielou(J)等生物多样性指数的水质评价结果表明: 鄱阳湖研究区域水质状态处于寡污-中污之间。研究揭示了2个水文期对通江湖泊浮游生物的影响: 季节变化不改变湖泊浮游生物的物种组成及优势种, 但显著影响浮游生物的丰度及多样性。     

长江口及其邻近水域鱼类浮游生物群落的时空格局

根据2007年长江口及其邻近水域4个航次调查资料, 探讨了该水域的鱼类浮游生物群落物种组成和多样性的季节变化特征。结果表明, 2007年共捕获鱼类浮游生物6,463个, 隶属12目28科45种, 以鳀科丰度最高, 占总丰度的76.5%。长江口鱼类浮游生物包括4种生态类型: 淡水型(2种), 半咸水型(14种), 沿岸型(10种)和近海型(16种)。 其中, 近海型物种个体数量最多, 占2007年长江口鱼类浮游生物总丰度的74.55%。鳀(Engraulis japonicus)在4个季节均有出现, 对长江口鱼类浮游生物丰度贡献最大。鱼类浮游生物在物种组成上存在明显的季节变化: 白氏银汉鱼(Allanetta bleekeri)在春季占绝对优势, 鳀是夏季优势度最高的种类, 秋季除鳀外, 前颌间银鱼(Hemisalanx prognathus)成为优势种; 鱼类浮游生物丰度高度集中在优势种上, 各季节优势种对总丰度贡献超过89%。群落物种数量、丰度、丰富度指数、均匀度指数和多样性指数, 在夏季最高, 春季和秋季次之, 冬季最低。长江口鱼类浮游生物群落物种组成和多样性的季节变化特征体现了鱼类繁殖迁移策略和鱼类对环境变异的响应。     

雅鲁藏布江湘河流域浮游生物群落结构的探究与多样性分析

为了探究雅鲁藏布江湘河流域生物群落结构及物种多样性现状,为西藏地区湘河流域浮游生物资源的保护及开发利用提供科学依据。本研究于2017年3～4月对湘河流域浮游生物进行了生物采样与调查,共设置采样点8个。本次调查共检出浮游植物6门61种,其中硅藻门为优势种,共41种,占总种类数的67.21%;绿藻门、蓝藻门次之,分别占总种类数的11.48%;甲藻门、隐藻门与金藻门种类较少。浮游植物密度范围为0.43×10~5～7.2×10~5cells/L,生物量范围为0.036～2.03 mg/L。共检出浮游动物3门44种,其中原生动物门为优势种,共30种,占总种类数的68.18%;轮虫13种;枝角类1种。浮游动物密度范围为1.5×10~5～1.66×10~6cells/L,生物量范围为0.9×10~(-3)～5.7×10~(-2)mg/L。各调查点浮游植物/浮游动物Shannon-Wiener多样性指数(H)和均匀度指数(E)平均分别为4.38/3.13和0.93/0.93。多项指数综合评价表明,湘河流域水质处于轻度污染或清洁状态,浮游生物群落结构单一,密度及生物量较低,生态环境较脆弱。     

三门湾健跳港网箱养殖区浮游生物多样性的夏季调查

调查了三门湾健跳港海水养殖区夏季浮游生物的种类组成、密度和多样性指数,并将浮游生物群落指标与水质理化因子进行相关分析。共发现浮游生物29种,其中浮游植物14种,第一优势种为中勒骨条藻(Skeletonema costatum);浮游动物15种,第一优势种为太平洋纺锤水蚤(Acartia pacifica)。表层浮游植物的平均密度为43 328ind·L^-1,Shannon-Weiner多样性指数为0.826;浮游动物平均密度为389ind.m^-3,Shannon-Weiner多样性指数为2.964。相关分析结果表明:无机氮、无机磷促使了浮游植物大量繁殖,并使浮游动物多样性指数提高。网箱养鱼区水体富营养化指数与浮游植物多样性指数之间有一定的正相关关系,与浮游动物多样性指数之间呈显著的正相关关系。     

巴丹吉林沙漠盐湖微生物多样性

【目的】研究内蒙古巴丹吉林沙漠碱性盐湖中的原核生物多样性及其与环境因子之间的关系。【方法】利用分子生物学方法构建16S rRNA基因克隆文库,对盐湖中的嗜盐碱微生物进行系统发育分析;利用R语言绘图,对不同盐湖的微生物群落结构进行对比研究。【结果】该区域盐湖含盐量很高,矿化度达165g/L-397 g/L。同时,水体呈强碱性,p H均在10以上。三个湖的盐度和p H值等理化参数有梯度变化,因此微生物多样性和群落结构存在明显差异。整体而言,细菌的多样性大于古菌。样品中含有的主要的细菌门类为γ-变形菌亚门(Gammaproteobacteria)、拟杆菌门(Bacteroidetes)、α-变形菌亚门(Alphaproteobacteria)、厚壁菌门(Firmicutes)、疣微菌门(Verrucomicrobia),古菌则全部属于广古菌门(Euryarchaeota)中的盐杆菌科(Halobacteriaceae)。【结论】盐度是决定细菌群落结构的主要因素,古菌群落结构则由多种环境因素综合影响。一些已知的嗜盐碱菌,如Roseinatronobacter spp.、Halohasta spp.等,可以生活在比其盐度和碱度生长范围更高的极端盐碱环境中。此外,样品中还含有大量未培养的嗜盐碱细菌和古菌,对进一步开发极端盐碱环境中的微生物资源有重要意义。     

Observations on the incidence and seasonal fluctuations of certain crustacean larvae in the plankton of the South-West Coast of India

The seasonal fluctuations in the incidence of planktonic organisms and the larval forms of certain crustaceans such as crabs, barnacles and post larvae of prawns in the plankton of the south-west coast of India have been followed for a period of three years from 1963. South-west monsoon period is the least productive period for zooplankton in this area. Brachyuran zoeae, post larvae of prawns and barnacle nauplii occur in the plankton throughout the year with distinct peaks for different groups. The zoeae ofUca annulipes occur in the plankton from September to May with a peak during November–December. The zoeae ofPortunus pelagicus are present in the plankton from September to June and their abundance is in February–March. The post larvae ofMetapenaeus affinis are found in the inshore plankton from November to June with the peak in March. The nauplii ofBalanus amphitrite communis occur in the plankton in all the months of the year, the peak incidence has been during November January. The zoeae ofU. annulipes are found to tolerate better the medium saline conditions. Of the ecological factors, salinity of the ambient water and the availability of planktonic food for the larvae seem to influence the seasonal fluctuations of these crustacean larvae in this locality.     

Impact of salinity on the anaerobic metabolism of phosphate-accumulating organisms (PAO) and glycogen-accumulating organisms (GAO)

The use of saline water as secondary quality water in urban environments for sanitation is a promising alternative towards mitigating fresh water scarcity. However, this alternative will increase the salinity in the wastewater generated that may affect the biological wastewater treatment processes, such as biological phosphorus removal. In addition to the production of saline wastewater by the direct use of saline water in urban environments, saline wastewater is also generated by some industries. Intrusion of saline water into the sewers is another source of salinity entering the wastewater treatment plant. In this study, the short-term effects of salinity on the anaerobic metabolism of phosphate-accumulating organisms (PAO) and glycogen-accumulating organisms (GAO) were investigated to assess the impact of salinity on enhanced biological phosphorus removal. Hereto, PAO and GAO cultures enriched at a relatively low salinity level (0.02 % W/V) were exposed to salinity concentrations of up to 6 % (as NaCl) in anaerobic batch tests. It was demonstrated that both PAO and GAO are affected by higher salinity levels, with PAO being the more sensitive organisms to the increasing salinity. The maximum acetate uptake rate of PAO decreased by 71 % when the salinity increased from 0 to 1 %, while that of GAO decreased by 41 % for the same salinity increase. Regarding the stoichiometry of PAO, a decrease in the P-release/HAc uptake ratio accompanied with an increase in the glycogen consumption/HAc uptake ratio was observed for PAO when the salinity increased from 0 to 2 % salinity, indicating a metabolic shift from a poly-P-dependent to a glycogen-dependent metabolism. The anaerobic maintenance requirements of PAO and GAO increased as the salinity concentrations risen up to 4 % salinity.     

Occurrence of aquatic invertebrates of the wheatbelt region of Western Australia in relation to salinity

The wheatbelt region of Western Australia has been extensively cleared of indigenous vegetation for agriculture and is now severely affected by dryland salinity. Wetlands that were once freshwater are now saline and others are under threat, as are the animals and plants that inhabit them. Rising groundwater is also affecting the many naturally saline playas. To provide a framework for setting conservation priorities in this region a biological survey was undertaken, including sampling of aquatic invertebrates at 230 wetlands. In this paper, we have used data from the survey to summarise occurrence of species in relation to salinity. Total species richness at a wetland showed no response to salinity below 4.1 g l⁻¹ and then declined dramatically as salinity increased. When halophilic species were excluded from consideration, species richness was found to decline from 2.6 g l⁻¹. These patterns are compared to previous studies of richness-salinity relationships. There is some evidence that the freshwater invertebrate fauna of the wheatbelt may be comparatively salt tolerant, with 46% of freshwater species collected at salinities above 3 g l⁻¹ and 17% above 10 g l⁻¹, though these proportions differed between various invertebrate groups. While this tolerance will provide a buffer against the effects of mild salinisation, many species are at risk of regional extinction as salinisation becomes more widespread.     

盐度对滨海土壤细菌多样性和群落构建过程的影响

滨海盐土是重要的农业土地后备资源。微生物是土壤中物质循环的关键动力,然而盐度对土壤微生物群落特征影响的研究还很缺乏。本研究采集滨海地区的土壤样品,研究非盐、轻盐和高盐3组不同盐度对土壤细菌数量、多样性和群落构建的影响。结果表明: 与非盐和轻盐土壤相比,高盐土壤的脱氢酶活性和细菌数量显著降低,而细菌α多样性没有变化,细菌群落结构发生分异。利用零模型反演群落构建过程,发现盐度是细菌群落构建过程的主控因子,盐度主导的高确定性过程控制了滨海盐土细菌的群落结构。说明在现有的盐度范围内,高盐土壤中同样含有丰富的微生物种质资源,具有盐土改良的生物学基础,然而由于高确定性的群落构建机制,外源物种很难定殖于滨海盐土。因此,在利用微生物技术改良滨海盐土时,应尽可能筛选耐盐的土著菌种,提高定殖效率。     

Planktonuntersuchungen in einem holländischen Meeresarm vor und nach der Abdeichung

The Veersche Gat and the Zandkreek formed a sea-arm, which since its closure has been known as the Veerse Meer. Changes in the environment and plankton before and after the closure are reviewed. For the quantitative plankton investigations the method ofLohmann (1908) was applied. As parts of the Oosterschelde system the Veersche Gat and the Zandkreek were poly-euhaline biotopes. Partial isolation of the central stations of the Zandkreek was caused by the existence of a tidal divide at Wolfaartsdijk (Fig. 2). The effect of this divide was illustrated by aberrant chlorinity values and by different qualitative and quantitative composition of the plankton communities. The Zandkreek plankton appeared to be a neritic biocoenose, consisting of a phytoplankton community of mainly pelagic diatoms together with a zooplankton community with strongly littoral characteristics. The size of the standing crops generally increased towards the sea. Phytoplankton at the tidal divide sometimes showed an autochthonous development. Sometimes phytoplankton organisms occurring throughout the whole water body were seen to bloom notably within the area of the tidal divide. In summer a strong autochthonous development of littoral zooplankton made the standing crops within the Zandkreek larger than those of the Veersche Gat. In the second and third years after the formation of the Veerse Meer, a decline in salinity transferred this water body from a polyeuhaline into a meso-polyhaline environment. This decrease in salinity was coupled with a strong eutrophication, evidenced, for example, by high phosphorous contents of the water and caused by the discharge of water from the neighbouring polders and by pollution from sewage. The elimination of many polyhaline-marine species was associated with the gradual appearance of many brackish-water species with flagellates and dinoflagellates as the most important groups. At the same time the standing crops increased greatly. The severe winter at the beginning of 1963 resulted in a marked salinity stratification. In the course of the spring when the ice cover disappeared and the temperature of the upper layers rose, the halocline was combined with a thermocline, and this double stratification was observed until August, 1963, when the wind gradually succeeded in mixing all layers of the water.     

Production of the rotifer Brachionus plicatilis for aquaculture in Kuwait

Macrophytes, plankton samples, salinity and depth data were collected from wetlands in October 1981. Species diversity and distributions are recorded and relationships drawn between macrophytes and plankton occurrence. An examination of the data of Geddes et al. (1981) enables comparisons of species composition in a similar range of Western Australian lakes in 1978 at a different stage in the seasonal cycle. Comparison with the biota of salt lakes in Australia's eastern states and elsewhere lead to biogeographical speculations for the macrophytes and for some of the planktonic species.     

Variability in the inter-island environment of the Prince Edward Islands (Southern Ocean)

Variability in the oceanographic parameters and macrozooplankton and micronekton composition, densities and distributional patterns were investigated during a repeat survey conducted between the Prince Edward Islands in April 1998. Results of this study demonstrated the occurrence of pronounced water pulses along the inter-island trench. The location of the Subantarctic Front to the north of the island plateau, through its interactions with the island group, appeared to have a marked effect on the mesoscale dynamics of physical and biological parameters between and around the islands. Seawater temperature and salinity accounted for >40% of the variation in the zooplankton distribution during the trench studies. A total of 41 macroplankton and micronekton taxa, consisting of subantarctic, subtropical and Antarctic species, were identified. Numerical analyses revealed two major groupings of stations corresponding to an offshore and inshore region. Although there was no evidence for quantitative differences in macroplankton densities between the inshore surveys, offshore plankton biomass was at least three- to eightfold higher than during the trench surveys. The importance of water pulses in carrying stocks of large plankton between the islands appeared to be minimal, at least during the time when the investigation took place. Received: 1 November 1999 / Accepted: 12 February 2000     

The influence of local elevation on the effects of secondary salinity in remnant eucalypt woodlands: Changes in understorey communities

Increasing land salinization in Australia is predicted to lead to severe declines in species diversity in affected areas, and perhaps significant numbers of species extinctions. Much of the diversity that will be lost consists of understorey and mid-storey species, yet the overwhelming majority of research has focussed on salinity tolerance in tree species. We investigated how the presence of a shallow, saline water table affected the understorey species composition, species richness and species diversity in two remnant Eucalyptus wandoo Blakely woodlands in the Western Australian wheatbelt. Species richness and species diversity were significantly lower in areas with a shallow water table at elevations < 0.5 m above the lowest local elevation, compared with both higher elevations and with areas of low elevation without a shallow water table. Species composition (Bray-Curtis similarities) was also significantly different in low elevation, saline areas. At one site, saline areas were colonized by native and alien species that were not present in the surrounding vegetation, yet the community that has developed does not contain either the species or structural diversity of the surrounding system. At the other site, no colonisation of saline areas by new species occurred. Even though small differences in elevation (< 0.5 m) at our study sites were important in moderating the impacts of salinity in areas with a shallow water table, the loss of species diversity, species richness and structural complexity in low-lying elevations indicated that the ecological risk from secondary salinity to species associated only with drainage lines, seasonally wet flats and other low-lying areas is severe. The priority is to identify those vegetation communities that are restricted to only low relative elevations within the landscape and that only occur in remnants predicted to be at a high risk of developing a shallow and saline water table.     

Salinity as a determinant of the structure of biological communities in salt lakes

The paper considers the extent to which salinity determines the structure of biological communities (composition and species richness and diversity) in saline lakes, i.e. inland bodies of water with salinities in excess of 3 g l-1. It also considers the extent to which oxygen, ionic composition, pH, hydrological patterns (degree of permanence and impermanence of water), geographical position, palaeoclimatic events, chance, human intervention, and biological interactions especially predation determine biological communities in salt lakes. It suggests that salinity is less significant as a determinant of community structure in salt lakes than has been assumed. This revised version was published online in July 2006 with corrections to the Cover Date.     

The biology and evolution of Antarctic saline lakes in relation to salinity and trophy

. Five brackish to hypersaline lakes (Highway, Ace, Pendent, Williams and Rookery) in the Vestfold Hills, eastern Antarctica were investigated during the austral summer of 1999/2000. The aims were to characterise the functional dynamics of the plankton and gain an understanding of how the different environments in the lakes have led to the evolution of different communities. The plankton was dominated by microorganisms and differed across the salinity spectrum in relation to trophy, age and the presence of meromixis. However, some elements of the plankton were common to all of the lakes, e.g. the mixtrophic ciliate, Mesodinium rubrum, which reached abundances of 2.7᎒⁵ l^-1 and spanned a salinity gradient of 4-63‰. Marine dinoflagellate species also occurred in all of the lakes, often at high abundances in Highway Lake, Pendent Lake and Lake Williams. During December (mid-summer), primary production showed an increase along the salinity gradient from Highway Lake to Lake Williams; however, it was low in hyper-nutrified Rookery Lake because of the turbidity of the waters. Bacterial production followed the same trend and was extremely high in Rookery Lake (327 µg l^-1 h^-1 in January). The lakes possessed a marine microbial plankton that has become very simplified through time, and now contains a small number of highly successful species, which were pre-adapted to surviving in extreme Antarctic lakes.