北冰洋微型浮游生物分布及其多样性

近年来随着全球气候变化对北冰洋生态环境的影响日益显现,北极微型浮游生物生态学研究得到了广泛的重视和实质性的进展。对北冰洋微型浮游生物的主要类群:异养细菌、古菌、光合异养原核生物和微型真核生物的分布及其多样性研究进展做了概述,并在此基础上展望了未来北冰洋微型浮游生物学研究。     

流式细胞仪在微型浮游植物生态学中的应用

微型浮游植物是水域生态系统中的初级生产者 ,是海洋生态系统存在的基础。习惯上浮游植物根据其粒径大小有分为小型浮游植物 (ｍｉｃｒｏ - ｐｈｙｔｏｐｌａｎｋｔｏｎ ,>2 0ｕｍ) ,微型浮游植物 (ｎａｎｏ - ｐｈｙｔｏｐｌａｎｋ ｔｏｎ ,<2 0ｕｍ ,>2ｕｍ )和超微型浮游植物( ｐｉｃｏ - ｐｈｙｔｏｐｌａｎｋｔｏｎ ,<2ｕｍ )三类[13 ] 。本文将后两类统称为微型浮游植物。在早期的多数研究中 ,检测技术和方法落后 :譬如测定水域中的生物量和叶绿素ａ含量常用的拖网方法 ,几乎丢失了所有的微型浮游植物 ;即使是实验室内常用 0 .45ｕｍ…     

微塑料污染对浮游生物影响研究进展

微塑料作为一种新型的环境污染物,大量存在于水环境中,给水生生物带来了极大的危害.浮游生物是水生食物链的基础,是水生生态系统物质循环和能量流动的重要环节;同时,浮游生物也是对各种环境污染物最敏感的类群.了解微塑料对浮游生物的影响是评价其生态风险的重要依据.本文介绍了环境中微塑料来源、特征及水生态系统微塑料污染现状,阐述了...     

大亚湾夏季和冬季超微型浮游生物的时空分布及环境调控

通过流式细胞法, 于2015 年夏季(7 月)和冬季(12 月)对大亚湾超微型浮游生物(聚球藻、超微型真核藻类和异养细菌)的时空变化及环境调控进行了比较研究。结果表明, 夏季聚球藻、超微型真核藻类和异养细菌的丰度分别为(44.56±46.26)×103 cells·mL^–1、(3.00±4.50)×103 cells·mL^–1 和(12.31±7.54)×105 cells·mL^–1, 冬季的丰度分别为(12.48±3.96)×103 cells·mL^–1、(0.78±0.71)×103 cells·mL^–1和(3.83±1.39)×105 cells·mL^–1。超微型浮游生物的丰度呈现为夏季高于冬季, 受到温度、溶解无机氮组成和透明度的影响。夏季表层丰度明显高于底层, 但冬季表底层无明显差异。在水平分布上, 夏季湾内高营养盐基本对应高丰度, 但石化区附近(S3 站)营养盐高丰度却较低, 范和港(S1 站)低营养盐丰度却较高; 湾口和湾外区主要受到外海水的影响, 超微型浮游生物的3 个类群丰度均较低。在沿岸流、海水垂直混合、外源营养盐输入等多个因素共同影响下, 冬季湾中部和大鹏澳附近的聚球藻丰度较高, 超微型真核藻类在湾口和范和港丰度较高, 异养细菌在湾内和湾西部丰度较高。两个季节超微型真核藻类和异养细菌呈显著正相关。     

香港水域夏季微型浮游动物摄食研究

20 0 0年 8月在香港牛尾海 ( A站 )和龙鼓水道 ( B站 )的 2个典型站位采样 ,用半现场的稀释法研究了夏季香港水域浮游植物的生长率和微型浮游动物对浮游植物的摄食压力等。结果表明 :A、B站浮游植物主要以硅藻为主 ,但 A站甲藻比重比 B站要高。A站 <5 μm的微型浮游植物比 B站要少 ,从细胞大小上 B站的浮游植物更易被微型浮游动物所摄食。A站微型浮游动物类群主要以异养鞭毛藻为主 ,而 B站为砂壳纤毛虫 ,其细胞丰度分别为 770和 62 0 ind./L。 A、B站浮游植物碳 /叶绿素 a浓度比率分别为 2 7.1 5和88.66。 A站浮游植物的内禀生长率相似于 B站 ,分别为 1 .0 4和 0 .98d- 1。浮游植物在 A站的净生长率是0 .33d- 1,而在 B站则出现了负增长 ,其净生长率是 - 0 .5 8d- 1。微型浮游动物在 A、B站的摄食率分别为0 .71和 1 .5 6d- 1,摄食压力分别占到了浮游植物现存量的 1 43.7%和 2 0 9.7% ,初级生产力的 78.6%和1 2 6.6% ,对浮游植物碳的摄食率分别达到 35 1和 5 5 2 μg C/( L·d)。A站的浮游植物生长要高于 B站 ,B站的微型浮游动物摄食压力要明显高于 A站。与其它海区比较香港水域微型浮游动物摄食压力处于中等水平。黑暗长时间培养实验的结果表明此水域微型浮游动物摄食率稀释法实验应在适量添加营养盐并在     

浮游植物和异养水生细菌的代谢偶联—了解湖沼物质循环的关键

本文的题目似乎是很专的,并且与我们内陆水域的湖沼学概论距离相当远。然而,湖沼的自养生产者,尤其是浮游植物,确与异养细菌的代谢密切地偶联着,异养细菌反而要利用初级生产产生的有机物质。合成和分解,这两个过程的规模是相等的,在初级生产时结     

罗非鱼对微型生态系统浮游生物群落和初级生产力的影响

本文报道罗非鱼不同放养密度对淡水微型生态系统结构与功能影响的部分研究结果。罗非鱼的捕食使微型生态系统中浮游动物密度下降,引起浮游植物密度、初级生产力和P/R系数的增长,同时使水柱透明度降低而pH值增高,以致于实验后期微型生态系统具有典型的富营养化水体的特征。就罗非鱼放养密度不同的微型生态系统而言,虽然其浮游生物密度和P/R系数存在显著的组(或部分组)间差异,但不同密度组的初级生产力水平和最终的理化状况相差不大,并且罗非鱼的收获量甚为接近。因此,实验条件下微型生态系统的群落结构和代谢的变化,按照营养级联假说不能很好地予以解释,表明微型生态系统是由捕食(下行影响)和理化因素(上行影响)共同调节或控制的。根据微型生态系统的实验结果推断,放养较大密度的罗非鱼,将会加速营养物负荷较高的天然水域富营养化的进程。     

微型生态系统中正磷酸直的周转时间的估算

在考查罗非鱼或鲢、鳙下行影响的微型生态系统实验后期,以水柱正磷酸盐（ＰＯ４－Ｐ）完全被浮游植物摄取所需要的时间为指标,估算了系统中ＰＯ４－Ｐ的周转时间,其中浮游折ＰＯ４－Ｐ摄取率是采用挂瓶法来测定和估算的。结果表明,两组实验中大多数有鱼系统的浮游植物ＰＯ４－Ｐ摄取率都显地比无鱼系统高,而ＰＯ４－Ｐ周转时间的估算值均显地小于无鱼系统,经相关分析测定,两组实验中浮游植物的ＰＯ４－Ｐ摄取率皆显地正     

北部湾北部海域夏季微型浮游动物对浮游植物的摄食压力

2011年8月份于北部湾北部海域5个观测站位获得的分层水样,分析了表层叶绿素a含量和表层微型浮游动物丰度以及类群组成;同时于现场采用稀释培养法研究了该海域浮游植物生长率(μ)和微型浮游动物的摄食率(g)。分析和测定结果表明:调查海区的微型浮游动物丰度400—1167个/L,类群组成以无壳纤毛虫为主;浮游植物的生长率为-1.50—1.13 d-1,微型浮游动物摄食率为0.33—1.08 d-1;推算微型浮游动物对浮游植物现存量以及初级生产力的摄食压力分别为28.1%—66.0%和-7.4%—438.4%。相对于中国其他海区,8月份北部湾北部海域微型浮游动物摄食速率处于中等水平。调查期间,广西沿海高生产力海区,浮游植物生长率大于微型浮游动物动物的摄食率,浮游植物生物量处于积累期;涠洲岛以南海域,浮游植物生产力较低,微型浮游动物摄食作用是控制浮游植物生长的重要因素。     

海水养虾池浮游运行对浮游植物牧食力的研究

利用常规显微镜直接计数法评估了海水养虾池浮游动物对浮游藻类的牧食力,测得虾池浮游运行对水柱浮游植物的总滤水率为８０．３８ｍｌ／（Ｌ·ｈ）,每个浮游动物的滤水率平均为１１．１３μｌ（ｉｎｄ·ｈ）,总牧食率为１０．５０μｇ／（Ｌ·ｈ）,即１．２５ｎｇ℃／（ｉｎｄ·ｈ）、浮游动物对水柱原位主要浮游藻类的选食,、以隐菏和舟形藻为最多,其次是扁藻和小环藻,６ｈ内对上述４种藻类的选食率为９２．６８％、７２．４     

Planktonic food web in marine mesocosms in the Eastern Mediterranean: bottom-up or top-down regulation?

A mesocosm experiment was conducted in order to studythe structure of the planktonic food web. The dynamicsof pico-, nano- and microplankton populations werefollowed during 40 days in four large (40 m³)enclosures. In three tanks a gradient of addednutrients (nitrogen and phosphorus) was applied, whilea fourth tank was used as a control. On day 14, thetop predator (sea bream Sparus aurata larvae)was introduced into the tanks and part of the watercolumn in each tank was isolated in a plastic bagwithout fish larvae, to act as a control forpredation. Physical parameters, chlorophyll aand nutrient concentrations, as well as planktonconcentrations were monitored. A diatom bloom wasobserved in all four tanks, in the first phase endingwith silicate depletion. Flagellate and dinoflagellateabundance subsequently increased, these organismsbeing limited by zooplankton grazing. The zooplanktonpopulations were controlled by both resources (mostlyflagellates) and predation (by fish larvae) asindicated by the results of the control experiments. This revised version was published online in July 2006 with corrections to the Cover Date.     

Impact of a Flood Event on the Planktonic Food Web of the Schelde Estuary (Belgium) in Spring 1998

To evaluate the effect of short-term changes in discharge on plankton dynamics, a station in the upper reaches of the Schelde estuary was monitored during 1 month in spring 1998 with a sampling frequency of 1–2 days. During this monitoring period, a flood event occurred during which discharge increased about 5-fold. This flood event had a strong effect on the composition of the planktonic community. Rotifers were strongly negatively affected by the flood event while densities of heterotrophic nanoflagellates and scuticociliates increased. Chlorophyll a concentration and abundance of bacteria, oligotrich ciliates and crustacean zooplankton did not respond clearly to the flood event. Although the flood event lasted only a few days it took more than 2 weeks for the planktonic community to return to its original composition.     

Structure of planktonic microbial food web in a brackish stratified Siberian lake

The distribution of primary components of the microbial community (autotrophic pico- and nanoplankton, phototrophic bacteria, heterotrophic bacteria, microscopic fungi, heterotrophic flagellates, ciliates and heliozoa) in the water column of Lake Shira, a steppe brackish-water, stratified lake in Khakasia, Siberia (Russia), were assessed in midsummer. Bacterioplankton was the main component of the planktonic microbial community, accounting for 65.3 to 75.7% of the total microbial biomass. The maximum concentration of heterotrophic bacteria were recorded in the monimolimnion of the lake. Autotrophic microorganisms contributed more significantly to the total microbial biomass in the pelagic zone (20.2–26.5%) than in the littoral zone of the lake (8.7–14.9%). First of all, it is caused by development of phototrophic sulphur bacteria at the oxic-anoxic boundary. The concentrations of most aerobic phototrophic and heterotrophic microorganisms were maximal in the upper mixolimnion. Heterotrophic flagellates dominated the protozoan populations. Ciliates were minor component of the planktonic microbial community of the lake. Heterotrophic flagellates were the most diverse group of planktonic eucaryotes in the lake, which represented by 36 species. Facultative and obligate anaerobic flagellates were revealed in the monimolimnion. There were four species of Heliozoa and only three of ciliates in the lake.     

Roles of food web and heterotrophic microbial processes in upper ocean biogeochemistry: Global patterns and processes

The growth and dynamics of plankton in the ocean vary with natural cycles, global climate change and the long-term evolution of ecosystems. The ocean is a large reservoir for CO₂ and the food webs in the upper ocean play critical roles in regulating the global carbon cycle, changes in atmospheric CO₂ and associated global warming. Microheterotrophs are a key component of the upper ocean food webs. Here, we report on the results of an analysis of the distribution of bacteria and related properties in the World Ocean. We found that, for the data set as a whole, there is a significant latitudinal gradient in all field-measured and computed bacterial properties, except growth rate. Gradients were, for the most part, driven by an equator-ward increase in the Southern Hemisphere. The biomass, rates of production and respiration and dissolved organic carbon concentrations were significantly higher in the Northern than the Southern hemispheres. In contrast, growth rates were the same in the two hemispheres. We conclude that the lower biomass and production in the Southern Hemisphere reflects greater top-down control by microbial grazers, which would be due to a lower abundance or activity of omnivorous zooplankton in the Southern than Northern Hemispheres. These large spatial differences in dynamics, structure and activity of the bacterial community and the microbial food web will be reflected in different patterns of carbon cycling, export and air–sea exchange of CO₂ and the potential ability of the ocean to sequester carbon.     

Relations among heterotrophic bacteria, chlorophyll-a, total phytoplankton, total zooplankton and physical and chemical features in the Paranoá reservoir, Brasília, Brazil

The plankton community, chlorophyll-a, heterotrophic bacteria and physical and chemical features of the Paranoá Reservoir were studied at monthly intervals at seven stations from March 1988 to March 1989. Thermal structure had a circulation period from May to July and stratification during the other months. The phytoplankton consisted of 76 taxa, was dominated by the cyanophyte Cylindrospermopsis raciborskii and attained concentrations ranging from 7,759,000 up to 98,160,000 org. l^–1. The zooplankton consisted of 36 taxa and was present in densities between 8 and 8,056 org. l^–1. In stations, or seasons with highly eutrophic conditions, there was a decrease in total phytoplankton and an increase in bacteria and total zooplankton. The results had spatial and temporal variations. Spatial variation demonstrated the existence of water quality deterioration at two or three sampling points. Temporal variation showed the influences of water column stability and the dry versus rainy seasons on nutrient concentrations and the planktonic community.     

Bacteria—A link among ecosystem constituents

Microbial ecology has undergone a revolution over the past two decades due to the numerous innovations in techniques, allowing bacteria to be detected more accurately by direct means. Thus, bacterial life can be distinguishedin situ by direct counting under epifluorescence microscopy; automatically counting and sizing by image analyzer equipped with epifluorescence microscopy or by use of flow cytometry; specific radioisotope techniques; and molecular techniques to detect specific taxa. All of these approaches do not require cultivation, which provides a biased view of bacterial communities in nature. Bacteria are abundant in aquatic environments and play important roles as links between dissolved nutrients and the grazers in the food web. The new techniques allow an evaluation of bacterial population dynamics and function in relation to other organisms of higher trophic levels. This mini review aims to show briefly the state-of-the-art in microbial ecology for ecologists concerned with organisms other than microbes, in order to develop further intensive study together with microbial ecologists.     

Responses to fish predation and nutrients by plankton at different levels of taxonomic resolution

1. To improve mechanistic understanding of plankton responses to eutrophication, a mesocosm experiment was performed in the shallow littoral zone of a south Swedish lake, in which nutrient and fish gradients were crossed in a fully factorial design. 2. Food chain theory accurately predicted total biomass development of both phyto‐ and zooplankton. However, separating zooplankton and algae into finer taxonomic groups revealed a variety of responses to both nutrient and fish gradients. 3. That both nutrients and fish are important for phytoplankton dynamics was seen more clearly when viewing each algal group separately, than drawing conclusions only from broad system variables such as chlorophyll a concentration or total phytoplankton biovolume. 4. In some taxa, physiological constraints (e.g. sensitivity to high pH and low concentrations of free CO₂) and differences in competitive ability may be more important for the biomass development than fish predation, grazing by herbivorous zooplankton, and nutrient availability. 5. We conclude that food chain theory accurately predicted responses in system variables, such as total zooplankton or algal biomass, which are shaped by the dynamics of certain strong interactors (‘keystone species’), such as large cladocerans, cyanobacteria and edible algae (<50 μm), whereas responses at finer taxonomic levels cannot be predicted from current theory.     

Dynamics and trophic roles of heterotrophic protists in the plankton of a freshwater tidal estuary

Freshwater tidal estuaries comprise the most upstream reaches of estuaries and are often characterised by the presence of dense bacterial and algal populations which provide a large food source for bacterivorous and algivorous protists. In 1996, the protistan community in the freshwater tidal reaches of the Schelde estuary was monitored to evaluate whether these high food levels are reflected in a similarly high heterotrophic protistan biomass. Protistan distribution patterns were compared to those of metazoan zooplankton to evaluate the possible role of top-down regulation of protists by metazoans. Apart from the algivorous sarcodine Asterocaelum, which reached high densities in summer, heterotrophic protistan biomass was dominated by ciliates and, second in importance, heterotrophic nanoflagellates (HNAN). HNAN abundance was low (annual average 2490 cells ml^–1) and did not display large seasonal variation. It is hypothesised that HNAN were top-down controlled by oligotrich ciliates throughout the year and by rotifers in summer. Ciliate abundance was generally relatively high (annual average 65 cells ml^–1) and peaked in winter (maximum 450 cells ml^–1). The decline of ciliate populations in summer was ascribed to grazing by rotifers, which developed dense populations in that season. In winter, ciliate populations were probably regulated `internally' by carnivorous ciliates (haptorids and Suctoria). Our observations suggest that, in this type of productive ecosystems, the microbial food web is mainly top-down controlled rather than regulated by food availability.     

Rotifers as predators on components of the microbial web (bacteria,heterotrophic flagellates,ciliates) — a review

Recent investigations have shown that processes within the planktonic microbial web are of great significance for the functioning of limnetic ecosystems. However, the general importance of protozoans and bacteria as food sources for rotifers, a major component of planktonic habitats, has seldom been evaluated. Results of feeding experiments and the analysis of the food size spectrum of rotifers suggest that larger bacteria, heterotrophic flagellates and small ciliates should be a common part of the food of most rotifer species. About 10–40 per cent of rotifers' food can consist of heterotrophic organisms of the microbial web. Field experiments have indicated that rotifer grazing should generally play a minor role in bacteria consumption compared to feeding by coexisting protozoans. However, according to recent experiments regarding food selection, rotifers should be efficient predators on protozoans. Laboratory experiments have revealed that even nanophagous rotifers can feed on ciliates. Preliminary microcosm and chemostat experiments have indicated that rotifers, due to their relatively low community grazing rates compared to the growth rates of bacteria and protozoans, should generally not be able (in contrast to some cladocerans) to suppress the microbial web via grazing, though they may structure it. Filter-feeding nanophagous rotifers (e.g. brachionids) seem to be significant feeders on the smaller organisms of the microbial web (bacteria, flagellates, small ciliates), whereas grasping species (e.g. synchaetids and asplanchnids) seem to be efficient predators on larger organisms (esp. ciliates). Another important role of rotifers is their feedback effect on the microbial web. Rotifers provide degraded algae, bacteria and protozoans to the microbial web and may promote microbial activity. Additional experimental work is necessary for a better understanding of the function of rotifers in aquatic ecosystems.