鱼虾混养生态系中细菌动态变化的研究

中国对虾和黑鲷混养生态系中几种主要细菌的动态变化研究结果表明 ,养殖初期 ,鱼虾混养池水体中异养菌总量和硝酸盐还原菌数量较低 ,但高于对照的对虾单养池 .随着养殖时间的推移 ,对照池的两种菌的菌量急剧增加 ,8、9月份菌量仍维持在较高水平 ;而混养池的菌量在高温季节虽有增加 ,但仍保持在 10 4 cells·ml-1范围内 ,增长幅度远远低于对照池 ,且 9月底开始下降 .底泥中的细菌数量与水体中细菌有相似的变化规律 ,但一般高于同期水中菌量 1～ 2个数量级 .混养池中的弧菌数量一直低于同期对照池 .可见 ,鱼虾混养可通过对养殖生态系中细菌的激活和调节作用 ,调节生态系统的物质循环 ,使其保持高速、稳定运行 ,为对虾生长提供一个健康而稳定的环境 ,同时增加综合养殖效益     

食物浓度对角突臂尾轮虫种群增长、个体大小和卵大小的影响

以蛋白核小球藻为食物 ,应用群体累积培养法研究了食物浓度对角突臂尾轮虫种群增长、个体大小和卵大小等的影响 .结果表明 ,食物浓度对角突臂尾轮虫种群增长率、个体大小和卵大小均有极显著影响 .其中 ,轮虫种群增长率与食物浓度间呈曲线相关 ;当食物浓度为 8.2 4 5 3× 10 6cells·ml-1时 ,种群增长率达最大值 0 .6 0 85d-1;在所研究的食物浓度范围内 ,轮虫个体具有随食物浓度的增大而增大的趋势 ,轮虫卵体积在中等食物浓度范围 (6 .0× 10 6～ 9.0× 10 6cells·ml-1)时较大     

黄河上游玛曲段春季浮游生物群落结构特征

为了了解黄河上游玛曲段的水质状况,于2006年4—5月对黄河玛曲段干流浮游生物的群落组成进行了调查。结果表明：全段的浮游植物共有5门23种（属）,浮游植物密度为3.2×10⁴～54×10⁴ cells·L^-1,平均密度为19.7×10⁴ cells·L^-1,生物量为0.069～0.464 mg·L^-1,平均生物量为0.228 mg·L^-1,其中密度最高的为齐哈玛,生物量最高的为玛曲大桥;浮游动物共有2门10种（属）,密度为670～1273 cells·L^-1,平均为881.56 cells·L^-1,生物量为0.044～0.089 mg·L^-1,平均为0.064 mg·L^-1;该河段浮游生物组成多以冷水性为主;浮游植物多样性指数介于2～3,表明黄河上游玛曲段水质呈轻度污染;浮游生物丰富度与均匀度值均较低,群落结构组成不稳定,易受外界环境的干扰。     

盐度与体重对台湾罗非鱼耗氧率的影响

在盐度为淡水、7、14、2 1、2 8和 35的条件下 ,测定了 3个体重组 (1.5 7～ 4.87g ,7.0 7～ 18.2 3g和31.5 0～ 5 2 .41g)的台湾红罗非鱼的耗氧率 ,方差分析表明 ,盐度对台湾红罗非鱼的耗氧率有极显著的影响(P <0 .0 1) .体重范围为 1.5 7～ 18.2 4g时 ,盐度 7实验组的耗氧率最高 ,分别为 0 .41mgO2 ·g-1·h-1(1.5 7～ 4.78g)和 0 .34mgO2 ·g-1·h-1(7.0 7～ 18.2 3g) ,体重范围为 31.5 0～ 5 2 .41g时 ,耗氧率最高值出现在盐度 35组 ,为 0 .30mgO2 ·g-1·h-1.耗氧率最低值也因体重范围的不同而出现在不同的盐度 ,体重范围为1.5 7～ 4.78g时 ,盐度 14组的耗氧率最低 ,为 0 .2 8mgO2 ·g-1·h-1,体重范围在 7.0 7～ 5 2 .41g时 ,耗氧率的最低值均出现在盐度 2 1组 ,其中体重范围 7.0 7～ 18.2 3g的最低值为 0 .2 2mgO2 ·g-1·h ,而体重范围31 5 0～ 5 2 .41g的最低耗氧率为 0 .13mgO2 ·g-1·h-1.协方差分析表明 ,盐度和体重对台湾红罗非鱼的耗氧率存在极显著的交互作用 (P <0 .0 1) .     

两种有鳞类爬行动物消化道微生物的研究

从北草蜥的胃、小肠和大肠中分离出 7个属 8种细菌和 2个属的霉菌 ,从中国石龙子的胃、小肠和大肠中分离到 6个属 7种细菌和 3个属的霉菌 ,酵母菌和放线菌都未发现。北草蜥胃、小肠和大肠中的细菌数量分别为 2 2 7× 1 0 6,2 0 6× 1 0 6和 9 78× 1 0 8个 / g ;霉菌数量为 2 5× 1 0 4 ,2 1 5× 1 0 4 ,1 33× 1 0 4个 /g。细菌在中国石龙子胃、小肠和大肠中的数量分布依次为 3 51× 1 0 6,2 2 5× 1 0 6,1 4 2× 1 0 9个 /g;霉菌分布数量为 2 1 9× 1 0 4 ,1 67× 1 0 4 和 1 61× 1 0 4 个 / g     

鹤山退化生态系统恢复过程中土壤微生物的特性

对鹤山丘陵荒坡人工植被土壤生物特性进行了研究,结果表明鹤山人工植被中土壤微生物的数量以马占相思林较高,为6.164×106g-1drysoil,接近村边次生自然林(6.323×106g-1drysoil);其次是果园和红荷木林,分别为5.115×106和4.083×106g-1drysoil;松林中微生物数量最少,仅为1.424×106g-1drysoil。土壤微生物的组成以细菌为主,占微生物总数的71.4%-87.7%,其次是放线菌,为总数的9.2%-22.7%,真菌相对较少(1.1%-9.6%)。细菌的数量与微生物总数的变化趋势相一致。人工植被中土壤微生物生物量(mgCmic(100g)-1drysoil)是马占相思林(57.11)>果园(47.79)>红荷木林(42.55)>松林(29.68),与相应的土壤有机碳(gCorgkg-1drysoil)顺序相吻合[马占相思林(16.13)>果园(13.40)>红荷木林(12.59)>松林(11.89)],与土壤生物数量的变化趋势亦相似。与1988年用同一种方法的采样分析结果相比,人工植被中微生物的总数、细菌的数量及其占微生物总数的比率均有所提高,意味着在植被恢复过程中土壤质地得到了改善,其中以马占相思林的土壤恢复速率相对较快。     

Fast repair of purine deoxynucleotide radical cations by rutin and quercetin

Repair effects of rutin and quercetin on purine deoxynucleotide radical cations were studied using pulse radiolysis technique. On electron pulse irradiation of N2 saturated deoxynucleotide aqueous solution containing 20 mmol/L K2S2O8, 200 mmol/L f-BuOH and rutin or quercetin, the transient absorption spectra of the deoxynucleotide radical cations decayed quickly. At the same time, the spectra of flavonoid phenoxyl radicals formed within several dozen microseconds. The results indicated that deoxynucleotide radical cations can be repaired by flavonoids. The rate constants of the repair reactions were 3.8 × 108-4.4×108 mol-1 · L · s-1 and 1.3×108-1.8×108 mol-1 · L · s-1 for dAMP and dGMP radical cations, respectively.     

温度和食物浓度对三品系萼花臂尾轮虫实验种群动态的影响

应用个体培养方法,研究了温度(20、25和30℃)和藻类食物浓度(1．5×10^6、3．0×10^6、6．0×10^6和9．0×10^6cells·ml^-1)对青岛、芜湖、广州三品系萼花臂尾轮虫种群动态的影响．结果表明,温度仅对轮虫的世代时间和种群内禀增长率有显著影响,而品系对所有生命表参数均无显著影响．轮虫种群的内禀增长率随培养温度的升高而增大,世代时间则随培养温度的升高而缩短．食物浓度仅对轮虫的生命期望值和平均寿命有显著影响,品系对轮虫的净生殖率、世代时间、生命期望值和平均寿命也有显著影响．三品系间,以广州品系轮虫的净生殖率、世代时间、生命期望值和平均寿命最大,芜湖品系最短．当食物浓度为3．0×10^6cells·ml^-1时,轮虫的生命期望值和平均寿命最长,9．0×10^6cells·ml^-1时最短．各品系轮虫的净生殖率、世代时间、总生殖率、生命期望值和平均寿命均随培养温度的升高而减小,广州品系的净生殖率除外．轮虫种群的内禀增长率和广州品系轮虫的总生殖率则随培养温度的升高而增大．青岛和广州品系轮虫的各生命表参数,均与食物浓度呈曲线相关,但芜湖品系仅世代时间、平均寿命和生命期望值随食物浓度的增大而缩短．     

鼎湖山马尾松人工林土壤硝态氮和铵态氨动态研究

 本文用离子交换树脂袋法(lon exchange resin bag method),测定了鼎湖山马尾松人工林土壤硝态氮和铵态氮动态情况。结果表明,鼎湖山马尾松林土壤硝态氮和铵态氮均具有明显的季节性变化,以春季最高和夏季最低。硝态氮在0～10cm和10～20cm两土层的年平均值分别为1.722和1.429μg．d-1·g-1干树脂,铵态氮在0～10cm和10～20cm的年平均值则分别为19.137和14.696μg·d-1·g-1干树脂。硝态氮和铵态氮在试验的大部分季节表现出显著的直线相关关系(P<0.05),表明了铵态氮供应是调节硝化速率的一个重要因子。     

颗石藻与环境

全球海洋中颗石藻(coccolith)的年产量估计为536800×108～5368000×108t,为食植性动物提供食物531432×108～5314320×108t,产生碳酸盐约12.8×108t,固定碳2000×108t,从大气圈和水圈中吸收CO27333×108t(为世界CO2年排放量的32倍).光合作用放出氧6943×108t.在海洋生物中居重要地位,对维护地球表面生态平衡起重要作用.     

Sulfide fluxes in a microbial mat from the Ebro Delta, Spain

The sulfur cycle of Ebro Delta microbial mats was studied in order to determine sulfide production and sulfide consumption. Vertical distribution of two major functional groups involved in the sulfur cycle, anoxygenic phototrophic bacteria and dissimilatory sulfate-reducing bacteria (SRB), was also studied. The former reached up to 2.2×10⁸ cfu cm^–3 sediment in the purple layer, and the latter reached about 1.8×10⁵ SRB cm^–3 sediment in the black layer. From the changes in sulfide concentrations under light-dark cycles it can be inferred that the rate of H₂S production was 6.2 μmol H₂S cm^–3 day^–1 at 2.6 mm, and 7.6 μmol H₂S cm^–3 day^–1 at 6 mm. Furthermore, sulfide consumption was also assessed, determining rates of 0.04, 0.13 and 0.005 mmol l^–1 of sulfide oxidized at depths of 2.6, 3 and 6 mm, respectively. Electronic Publication     

Diversity and vertical distribution of magnetotactic bacteria along chemical gradients in freshwater microcosms

The vertical distribution of magnetotactic bacteria along various physico-chemical gradients in freshwater microcosms was analyzed by a combined approach of viable cell counts, 16S rRNA gene analysis, microsensor profiling and biogeochemical methods. The occurrence of magnetotactic bacteria was restricted to a narrow sediment layer overlapping or closely below the maximum oxygen and nitrate penetration depth. Different species showed different preferences within vertical gradients, but the largest proportion (63-98%) of magnetotactic bacteria was detected within the suboxic zone. In one microcosm the community of magnetotactic bacteria was dominated by one species of a coccoid "Alphaproteobacterium", as detected by denaturing gradient gel electrophoresis in sediment horizons from 1 to 10 mm depth. Maximum numbers of magnetotactic bacteria were up to 1.5 x 10(7) cells/cm3, which corresponded to 1% of the total cell number in the upper sediment layer. The occurrence of magnetotactic bacteria coincided with the availability of significant amounts (6-60 microM) of soluble Fe(II), and in one sample with hydrogen sulfide (up to 40 microM). Although various trends were clearly observed, a strict correlation between the distribution of magnetotactic bacteria and individual geochemical parameters was absent. This is discussed in terms of metabolic adaptation of various strains of magnetotactic bacteria to stratified sediments and diversity of the magnetotactic bacterial communities.     

Detection of ingested bacteria in benthic ciliates using fluorescence in situ hybridization

Fluorescence in situ hybridization (FISH) was applied to detect ingested natural bacteria within the food vacuoles of ciliates harvested from the natural sediment. In addition to this important qualitative aspect, FISH was also successfully used to measure the bacterivory of a culture of the ciliate Tetrahymena pyriformis on natural field sediment bacteria. In this feeding experiment, we compared the FISH technique with the only available alternative technique using fluorescently stained sediment (FS-sediment). The ingestion rate of unstained sediment bacteria determined by FISH was 4.6 bacteria per ciliate and hour. In contrast, Tetrahymena pyriformis cells that fed on bacteria from FS-sediment ingested 12.7 bacteria per ciliate and hour. Bacterial abundances in the sediment were equal in both sediment types (4 x 10(8) cells g sediment dry weight(-1)) when determined by DAPI counts. However, when analyzed using DTAF-counts, the number of bacteria in the FS-sediment increased to 9.7 x 10(8) cells g sediment dry weight(-1). From our findings we conclude that bacterivory by ciliates is overestimated when FS-sediment is used because DTAF stains bacteria as well as protein-containing detritus particles, which are also ingested by many ciliates. In contrast, FISH is a direct, a posteriori method that specifically stains phylogenetic lineages, e.g. eubacteria, after ingestion and thereby avoids a false determination of the number of ingested bacteria. Thus this method can also be used for the study of natural ciliate bacterivory in benthic systems.     

长江口低氧区异养细菌及氮磷细菌分布

2009年8月15-28日,对长江口低氧高发海域的异养细菌、无机磷细菌、有机磷细菌、反硝化细菌和氨化细菌的空间分布特征进行初步研究.结果表明:氨化细菌数量最高,表层水、底层水和表层沉积物的数量均值分别为307.52×104个·L-1、184.50×104个·L-1和199.97×102个·g-1;其次为异养细菌,数量均值分别为87.35×104 cfu·L-1、86.85×104cfu·L-1和64.26×102cfu·g-1;再次为有机磷细菌,数量均值分别为19.26×104 cfu·L-1、18.82×104cfu·L-1和19.56×102cfu·g-1;无机磷细菌只分布在长江口内和河口南槽至舟山海域,数量均值分别为18.50×104cfu·L-1、31.00×104cfu·L-1和7.17×102cfu·g-1;反硝化细菌分布广,但数量较低,均值分别为3.94×104个·L-1、23.08×104个·L-1和6.22×102个·g-1.相关性分析结果说明:盐度、硝酸盐、磷酸盐、硅酸盐和pH是影响水体和表层沉积物异养细菌、磷细菌和反硝化细菌分布的主要因子;底层水和表层沉积物异养细菌、磷细菌与水温呈显著正相关;底层水异养细菌和有机磷细菌与溶解氧(DO)呈显著正相关;表层沉积物无机磷细菌与DO呈显著正相关,氨化细菌与DO呈显著负相关.聚类分析结果说明:低氧对表层沉积物的细菌群落结构产生影响.     

Estimation of methanotroph abundance in a freshwater lake sediment

The numbers of methane-oxidizing bacteria (methanotrophs) in the sediments of Lake Washington were estimated using three culture-independent methods. Quantitative slot-blot hybridizations were performed with type I and type II methanotroph-specific probes. These data were compared to data from quantitative hybridizations using a pmoA-specific probe and a eubacterial probe. From the combined hybridization data, the methanotroph population in Lake Washington was estimated to be 3.6 x 10(8)-7.4 x 10(8) cells/g dry weight. Methanotroph community structure and number were also investigated using polar lipid fatty acid (PLFA) analysis. Analysis of biomarker PLFAs characteristic of both type I (16:1 omega 8) and type II (18:1 omega 8) methanotrophs was used to estimate the abundance of these bacteria in Lake Washington sediments. From the PLFA data, the methanotroph population in Lake Washington was estimated to be 7.1 x 10(8)-9.4 x 10(9) cells/g dry weight. As a third method of quantitation, we calculated the methanotroph population using the total methane oxidation rate for whole cells in Lake Washington sediment to be 1.3 x 10(8)-1.2 x 10(9) cells/g dry weight. The three independent estimates of the number of methanotrophs in Lake Washington sediment agree within a two- to fourfold range. These data suggest that the three techniques used in this study detect the functionally significant population of methanotrophs in Lake Washington. Furthermore, these techniques will be useful for obtaining estimates of methanotroph abundance in additional environments.     

我国东南沿海亚历山大藻休眠孢囊的分布和萌发研究

对4个海域的塔玛亚历山大藻(Alerandrium tamarense)和链状亚历山大藻(A．catenella)休眠孢囊的分布及萌发进行了研究．结果表明,厦门港仅在X1和X2站位有分布,且密度很小(0．4个·g-1);广西只在G2站位有发现,密度较少(2．5个·g-1泥样)．闽江口有3个站位有分布,M4站位的4～6cm层密度最大,达到6个·g-1泥样;长江口的孢囊分布广、密度大,DG-26站位的8～10cm层孢囊密度达到了23．2个·g-1泥样．孢囊的分布与沉积物底质类型、沉积速率、海流都有一定的关系．光照对孢囊萌发没有影响,温度升高导致萌发率和存活率均增大,而萌发时间缩短;在低氧条件下(0．01mgO2L-1),孢囊萌发率为0．亚历山大藻孢囊在合适的环境条件下终年都会萌发     

Application of antisera raised against sulfate-reducing bacteria for indirect immunofluorescent detection of immunoreactive bacteria in sediment from the German Baltic Sea.

Polyclonal rabbit antisera raised against sulfate-reducing bacteria (SRB) could detect several distinct populations of bacteria in sediment from the German Baltic Sea. The depth distribution of immunoreactive bacteria was determined by an indirect immunofluorescence filter method. Anti-Desulfovibrio desulfuricans DSM 1926 serum showed maximum bacterial numbers at a depth of 18 cm, with a concentration of 60 x 10(6) cells cm-3. With anti-Desulfovibrio baculatus DSM 2555 serum, counts were highest at the same depth, approaching 0.7 x 10(6) cells cm-3. Other significantly smaller populations were observed. Anti-SRBStrain 1 (lactate,vibrio) maxima were at 0 to 4 cm and at 17 to 18 cm. Anti-SRBStrain 2 (lactate,vibrio) serum showed several local maxima. Anti-SRBStrain 3 (lactate,oval) serum detected one single peak at a depth of 10 to 12 cm. Also determined were rates of sulfate reduction, total bacterial counts by acridine orange staining, and the viable counts by dilution series on anaerobic lactate medium. The total bacterial counts were highest (180 x 10(6) cells cm-3) at 3 to 4 cm and dropped to 24 x 10(6) cells cm-3 at 10 to 11 cm but showed additional local maxima reaching 140 x 10(6) cells cm-3 at a depth of 17 to 18 cm. Viable counts probable number) were above 10(5) CFU cm-3 at 0 to 3.6 cm but remained below 10(3) CFU at 7.2 to 18 cm. The sulfate reduction rate was maximal (107 nmol cm-3 day-1) at a depth of 1 to 2 cm, dropped to 10 nmol cm-3 day-1 at 12 to 13 cm, and reached 38 nmol cm-3 day-1 at 17 to 18 cm.     

泥螺养殖滩涂异养菌群和弧菌的检测

1　引　　言泥螺 (Ｂｕｌｌａｃｔａｅｘａｒａｔａ)隶属腹足纲软体动物 ,肉质鲜嫩、营养丰富 ,是浙江沿海重要的滩涂养殖品种 .至 2 0 0 0年浙江省养殖面积已达 1.13× 10 4ｈｍ2 ,由于实行生态养殖 ,本轻利厚 ,广受养农的青睐 .随着泥螺养殖生产的发展 ,养殖业的自身污染和陆源排污水的大量入海 ,养殖生态环境越趋恶化 ,使生物病原大量滋生 ,自 1995年以来常诱发养殖泥螺的暴发性死亡 .有关海洋滩涂环境细菌的研究至今未见报道 .为探明泥螺养殖周期内暴发性死亡与滩涂环境的关系 ,对养殖滩涂的细菌菌群组成及其生态特性进行了检测分析 .2…     

Large fraction of dead and inactive bacteria in coastal marine sediments: comparison of protocols for determination and ecological significance

It is now universally recognized that only a portion of aquatic bacteria is actively growing, but quantitative information on the fraction of living versus dormant or dead bacteria in marine sediments is completely lacking. We compared different protocols for the determination of the dead, dormant, and active bacterial fractions in two different marine sediments and at different depths into the sediment core. Bacterial counts ranged between (1.5 +/- 0.2) x 10(8) cells g(-1) and (53.1 +/- 16.0) x 10(8) cells g(-1) in sandy and muddy sediments, respectively. Bacteria displaying intact membrane (live bacterial cells) accounted for 26 to 30% of total bacterial counts, while dead cells represented the most abundant fraction (70 to 74%). Among living bacterial cells, nucleoid-containing cells represented only 4% of total bacterial counts, indicating that only a very limited fraction of bacterial assemblage was actively growing. Nucleoid-containing cells increased with increasing sediment organic content. The number of bacteria responsive to antibiotic treatment (direct viable count; range, 0.3 to 4.8% of the total bacterial number) was significantly lower than nucleoid-containing cell counts. An experiment of nutrient enrichment to stimulate a response of the dormant bacterial fraction determined a significant increase of nucleoid-containing cells. After nutrient enrichment, a large fraction of dormant bacteria (6 to 11% of the total bacterial number) was "reactivated." Bacterial turnover rates estimated ranged from 0.01 to 0.1 day(-1) but were 50 to 80 times higher when only the fraction of active bacteria was considered (on average 3.2 day(-1)). Our results suggest that the fraction of active bacteria in marine sediments is controlled by nutrient supply and availability and that their turnover rates are at least 1 order of magnitude higher than previously reported.     

Microbial production and consumption of dimethyl sulfide (DMS) in a sea grass (Zostera noltii)-dominated marine intertidal sediment ecosystem (Bassin d'Arcachon, France)

The relation between net dimethyl sulfide (DMS) production and changes in near surface (0-5 mm) oxygen concentrations in a sea grass (Zostera noltii Hornem)-covered intertidal sediment ecosystem was examined during a diel cycle. Sediment covered with Zostera was found to be more oxygenated than uncovered sediment during the period of photosynthesis. This phenomenon was probably caused by radial oxygen loss of the Zostera root-rhizome system. The population sizes of the three functional groups of microbes mainly responsible for the concentration of DMS, the dimethylsulfoniopropionate (DMSP)-demethylating, DMSP-cleaving and DMS-oxidizing bacteria, were quantified by most probable number (MPN) methodologies. Sediments with Zostera supported substantially higher populations of both aerobic (149x10(6) cm(-3) DMSP-utilizing and 0.4x10(6) cm(-3) DMS-oxidizing) and anaerobic (43x10(6) cm(-3) DMSP-utilizing and 0.4x10(6) cm(-3) DMS-oxidizing) microorganisms than sediments without Zostera (DMSP-utilizing aerobes and anaerobes both 2x10(6) cm(-3) and DMS-oxidizing aerobes and anaerobes both 0.2x10(6) cm(-3)). Experiments conducted with sediment cores and sediment slurries suggested that the net production of DMS in these sediments was significantly lower during oxic periods than during anoxic periods. Intact sediment cores with and without Zostera produced DMS when incubated under anoxic/dark conditions (97.0 and 53.6 nmol DMS m(-2) h(-1), respectively), while oxic/light-incubated cores did not produce detectable amounts of DMS. In addition, kinetic parameter values (V(max) and K(m)) for DMSP degradation in cell suspensions of isolated DMSP-demethylating and DMSP-cleaving bacteria were measured and compared to documented values for other strains. Both V(max) and K(m) values for DMSP-demethylating organisms were found to be relatively low (14.4-20.1 nmol DMSP mg protein(-1) min(-1) and 4.1-15.5 μM, respectively) while these parameter values varied widely in the group of the DMSP-cleaving organisms (6.7-1000 nmol DMSP mg protein(-1) min(-1) and 2-2000 μM, respectively). It was hypothesized that a diel rhythm in DMS emission occurred, with a relatively low net production during the day and a high net production during the night. Environmental changes which result in increased anoxic conditions in coastal sediments, such as an increase in eutrophication, may therefore result in increased atmospheric DMS emission rates.