深海来源芳烃类降解菌筛选与盐单胞菌芘降解能力测定

海洋来源的菌株在高盐污水类修复处理中有重要的应用前景,而烃类物质是污水中的重要组成部分,其中含有多个苯环的芳香烃族化合物,对人类和环境具有较大的毒性,而目前关于多环芳烃(PAHs)厌氧代谢的相关报道相对较少。本研究以PAHs(萘、菲和芘等)为唯一碳源和能源,通过厌氧富集对太平洋深海沉积物中的PAHs降解菌展开研究。富集物细菌菌群分析结果表明,盐单胞菌属(Halomonas)、海旋菌属(Thalassospira)、海杆菌属(Marinobacter)、海洋杆菌属(Oceanobacter)和食烷菌属(Alcanivorax)等是主要的功能类群;其中盐单胞菌属是最主要的功能类群。通过筛选分离获得一高效烃降解盐单胞菌株,鉴定并命名为泰坦尼克盐单胞菌(Halomonas titanicae) PA16-9,该菌与模式菌株Halomonas titanicae BH1^T的16S rRNA相似性为99.52%。基于16S rRNA基因序列比对搜寻NCBI数据库,发现Halomonas titanicae广泛存在于废水、活性污泥、油田、湿地等有机质复杂区域,生态位分布极广,可利用丰富多样的底物。通过生长实验表明,菌株PA16-9能在厌氧条件下以硝酸盐为主要电子受体,利用芘、苯并芘和十六烷等烃类物质为唯一碳源进行生长,在培养45 d后芘的降解率达到61.9%,期间亚硝酸盐逐渐积累,浓度达到约0.24 mmol/L。盐单胞菌广泛存在于厌氧烃降解富集菌群中,暗示了盐单胞菌属在厌氧烃代谢中可能发挥了重要作用,在实际应用上具有很大潜力。     

温度及pH对杀鲑气单胞菌生长的影响研究

利用A值法与活菌平板计数法,测定了杀鲑气单胞菌在不同条件下的生长曲线,研究了不同温度及pH对杀鲑气单胞菌(Aeromonas salmonicha)生长的影响。结果表明,活菌计数法更能真实的反映细菌数量的动态变化。在28℃,15℃,10℃,5℃条件下,随着温度降低,杀鲑气单胞菌生长速率明显下降;在pH6.0~8.0时,酸性条件能明显抑制杀鲑气单胞菌的生长;在28℃、pH7.5条件下,杀鲑气单胞菌生长速率最快,达到稳定期时细菌数量也最多。在养殖生产过程中,为了抑制杀鲑气单胞菌的生长繁殖,建议在不影响鱼类正常生长的条件下,尽量降低养殖水体温度并合理控制水体pH,以降低养殖鱼类发病率。     

海洋微生物对多环芳烃的降解

从海域沉积物中富集分离出以芘作为唯一碳源和能源的海洋微生物，以ST4富集培养的混合微生物作为研究对象；该海洋混合菌株能利用菲（Phe）、芘（Pyr)、荧蒽（Fla)等多种多环芳烃；在不同浓度的芘的降解中，当芘的浓度为50mg/dm^3时，其生长水平和降解速率最高；当芘的浓度为200mg/dm^3时，其生长受到抑制，芘几乎不能被降解。外加营养盐酵母浸出液和葡萄糖促进降解微生物的生长，提高降解速率。研究表明了海洋微生物在多环芳烃污染环境的生物修复应用前景。     

罗氏沼虾(Macrobrachium rosenbergii)致病性豚鼠气单胞菌(Aeromonas caviae)的分离鉴定及其特性分析

近年来细菌性疾病因病原菌种类繁多、覆盖区域广而影响了其养殖业的健康发展,造成较大的经济损失。从体表具有黑斑、肢体残损症状的罗氏沼虾(Macrobrachium rosenbergii)肝胰腺组织中分离得到1株病原菌,通过形态学观察、生理生化特性鉴定、16S rRNA序列和特定毒力基因检测鉴定,以及人工回归感染试验和药敏试验分析其致病性和耐药性。结果表明,该菌为豚鼠气单胞菌(Aeromonas caviae),含有aer、lip、gcat、ser和OMPA I等毒力基因;药敏试验显示其对头孢曲松、氯霉素等7种抗生素高度敏感,对恩诺沙星、阿米卡星及复方新诺明3种抗生素中度敏感,对四环素、环丙沙星等10种抗生素具有耐药性;人工回归感染实验表明该菌具有较高的致病性,对罗氏沼虾的半致死浓度为6.54×10⁵ CFU/mL。豚鼠气单胞菌作为水产养殖中的条件性致病菌,研究结果揭示了该菌株的部分生物学特性,有利于丰富豚鼠气单胞菌属的基础数据,同时也为罗氏沼虾养殖过程中的病害防控提供了一定参考依据。     

菲降解菌的分离鉴定及其降解性研究

采用微生物富集培养分离法对南洋油田不同油样中的菲降解菌进行了分离鉴定。分离得到2株以菲作为唯一碳源和能源的细菌菌株S17和S28,经革兰氏染色及显微镜形态观察,发现两者都是具有极生单鞭毛的革兰氏阴性、无芽孢杆菌。根据生理生化特性分析,以及16S rDNA序列同源性分析,两者属于假单胞菌属的不同种。菌株S17与食树脂假单孢菌(Pseudomonas resinovorans)序列同源性为97%;菌株S28则为高温假单胞菌(Pseudomonas thermaerum),其序列同源性达到100%。在以菲为唯一底物的条件下,菌株S28的生长速度是S17的2倍多,第4天即达到最大生长量,但是对于菲的降解而言,两者都在第10天达到最大,降解率分别为88.86%和82.02%,但是二者在起始的两天内对菲的降解效率最高,分别达到70.21%和72.74%,因此可用于菲污染的快速治理领域。     

斑点叉尾鮰(Ictalunes punctatus)源中间气单胞菌(Aeromonas media)分离鉴定及药敏特性

从湖南常德某养殖场死亡的斑点叉尾（Ictalunes punctatus）肝脏、肾脏、腹水及血水中分离到一株致病性菌株zy02。对该菌进行了形态特征观察、理化特性测定及分子生物学方法鉴定,用PCR方法同时扩增其16S rDNA和gyrB基因,分析了16S rDNA和gyrB两种基因序列的同源性,并构建了系统发生树。经生理生化测定和16S rDNA与gyrB基因序列分析,zy02株为中间气单胞菌。人工感染该菌后发病鱼表现为与自然发病类似症状,且从组织中再分离的细菌特性与原感染菌相同。腹腔注射后该菌株对斑点叉尾的半致死浓度为3.89×10⁶CFU/mL。菌株zy02对多西环素、庆大霉素及左氧氟沙星等高度敏感;对红霉素中度敏感;对阿莫西林、磺胺异噁唑、克林霉素及利福平等5种药物耐药。本研究为斑点叉尾该病防控提供了理论依据。     

海洋石油烃降解细菌T1和T2的分子鉴定分类

从天津滨海潮间带被石油烃严重污染的沉积物（千样含油量0．2g／g）中，筛选分离出能够以柴油为唯一碳源生长的细菌，对其中生物量大、单株菌降解效率较高的两株细菌T1和T2进行16SrDNA克隆，通过测定和比较16SrDNA的部分序列对这两株细菌进行分子鉴定，以期用于石油污染的微生物修复中。结果表明，T1与深红红螺菌（Rhodospirillum rubrum）的同源性为89％，．r2与施氏甲单孢杆菌（Pseudomonas stutzeri）的同源性为99％。     

邻苯二甲酸二甲酯及其异构体的好氧微生物降解

3种苯二甲酸二甲酯异构体(邻、间和对苯二甲酸二甲酯)主要应用于化学工业,作为增塑剂和生产聚酯的原料。用邻苯二甲酸二丁酯为惟一碳源,从红树林底泥中驯化、富集、培养、分离得到的微生物对邻苯二甲酸二甲酯(Dimethylphthalate,DMP)及其异构体对苯二甲酸二甲酯(Terephthalate,DMT)和间苯二甲酸二甲酯(Isophthalate,DMI)具有较强的降解作用。此菌株16SrDNA分子生物学的鉴定为Rhodococcusruber1k。实验得出该菌能够在苯二甲酸二甲酯作为惟一碳源和能源的培养基中生长。浓度为50mg·L-1的DMP、DMI和DMT分别在6、10、11d内可以完全被降解;DMP能够在好氧条件下被该菌快速降解,生成邻苯二甲酸一甲酯(monomethylphthalate,MMP)和邻苯二甲酸(phthalicacid,PA)2种主要中间产物,最终可以完全矿化成CO2和H2O;该菌对DMI和DMT的降解速度则比DMP慢。两者的降解中间产物间苯二甲酸一甲酯(MMI)和对苯二甲酸一甲酯(MMT)却不能被Rhodococcusruber1k继续降解而在培养基中积累。结果表明苯二甲酸二甲基酯的3种异构体能够被红树林底泥中的土著微生物降解。降解速度及降解途径与底物的化学结构有密切关系。     

虾类消化道菌群研究进展

虾类消化道内生活着大量的细菌，它们成为虾体内不可或缺的重要组成部分，影响着机体的生长与健康。文章综述虾类消化道菌群的来源、组成以及作用。这些细菌主要来源于水体和食物中，常见的优势菌主要有发光杆菌属、弧菌属、气单胞菌属、假单胞菌属等。消化道菌群既可以为宿主提供营养、辅助消化，又能够拮抗病原、影响宿主的健康。它们的组成与变化既与虾类自身的种类、发育时期以及健康状况等因素有关，也受到包括水环境的盐度、温度、氧气浓度、饵料和药物等因素的影响。     

中国鱼类名录Ⅻ--鳚亚目、(鱼衔)亚目、喉盘鱼亚目、鰕虎鱼亚目、微体鱼亚目、刺尾鱼亚目、带鱼亚目、鲭亚目、鲳亚目、金枪鱼亚目、攀鲈亚目、刺鳅亚目

鳚亚目 4 科 33 属 95 种，鰕虎鱼亚目 5 科 98 属 259 种，刺尾鱼亚目 5 科 11 属 65 种，鲈形目 19亚目 104 科 535 属 1799 种。     

The distribution of Mn,Fe, Cu,Ni, Co,Ga, Cr,V, Ba,Sr, Sn,Zn, and Pb,in some soil-sized particulates from the lower troposphere over the world ocean

Soil-sized particulates have been collected on board ship by a mesh technique from the lower troposphere of the North, Equatorial and South Atlantic Ocean, northern and southern Indian Ocean, South and East China Sea and various coastal localities.Spectrographic analysis reveals that, on average, the particulates have concentrations of Mn, Ni, Co, Ga, Cr, V, Ba, and Sr which are of the same order of magnitude as those in average crustal material. In contrast, the average concentrations of Pb, Sn, and Zn are one order of magnitude higher than those in average crustal material.Within this “world-wide” average there are significant geographical variations in the distributions of Pb, Sn, and Zn which may be related to anthropogenic sources.On the basis of trace-element distributions lower tropospheric soil-sized marine particulates have been divided into four genetic components; local, zonal, inter-zonal, and global. The proportions of these components vary geographically, and each component may have both a natural and an anthropogenic fraction.     

Distribution, abundance, and growth of larval tautog, Tautoga onitis, in Buzzards Bay, Massachusetts, USA

Tautog, Tautoga onitis, is an abundant species of fish in estuaries of the northeastern United States. Planktonic tautog larvae are abundant in summer in these estuaries, but there is little information on rates of growth of tautog larvae feeding on natural assemblages of food in the plankton. We examined abundance and growth of larval tautog and environmental factors during weekly sampling at three sites along a nearshore‐to‐offshore transect in Buzzards Bay, Massachusetts, USA during summer 1994. This is the first study of a robust sample size (336 larvae) to estimate growth rates of field‐caught planktonic tautog larvae feeding on natural diets, using the otolith daily‐growth‐increment method. The study was over the entire summer period when tautog larvae were in the plankton. The sampling sites contrasted in several environmental variables including temperature, dissolved oxygen (DO), and chlorophyll a concentration. There was a temporal progression in the abundance of tautog larvae over the summer, in relation to location and temperature. Tautog larvae were first present nearshore, with a pronounced peak in abundance occurring at the nearshore sites during the last 2 weeks in June. Larvae were absent at this time further offshore. From late June through August, larval abundance progressively decreased nearshore, but increased offshore although never approaching the abundance levels observed at the nearshore sites. The distribution and abundance of tautog larvae appeared to be related to a nearshore‐to‐offshore seasonal warming trend and a nearshore decrease in DO. Otoliths from 336 larvae ranging from 2.3 to 7.7 mm standard length had otolith increment counts ranging from 0 to 19 increments. Growth of larval tautog was estimated at 0.23 mm·day^?1, and length of larvae prior to first increment formation was estimated at 2.8 mm indicating that first increment formation occurs 3–4 days after hatching at 2.2 mm. Despite spatial and temporal differences in environmental factors, there were no significant differences in growth rates at any of three given sites over time, or between sites. Because larval presence only occurred at a narrow range of temperature (17–23.5 °C) and DO (6.5–9.3 mg·l^?1), in situ differences in growth did not appear to be because of differences in larval distribution and abundance patterns relative to these parameters.     

Cadmium,cobalt, copper,iron, lead,nickel and zinc in Indian Ocean water

Results of trace-metal analyses of water samples obtained during a cruise with the Soviet R.V. “Akademik Kurchatov” in the Indian Ocean are presented. The determinations were performed on board with atomic absorption spectrophotometry after a two-stage dithiocarbamate—Freon extraction procedure. Trace-metal concentrations found are in the same range as those found recently for similar open-ocean areas by other workers. The values for lead and zinc are probably high due to contamination. Vertical profiles indicate biogenic processes as controlling factors for the increase of cadmium, copper and nickel concentrations with depth. Iron shows an irregular depth distribution as a result of large random variations in concentration.     

The behavior of Zn,Cd, Cu,Ni, Co,Fe, and Mn in anoxic baltic waters

In June 1981, dissolved Zn, Cd, Cu, Ni, Co, Fe, and Mn were determined from two detailed profiles in anoxic Baltic waters (with extra data for Fe and Mn from August 1979). Dramatic changes across the O₂H₂S interface occur in the abundances of Cu, Co, Fe, and Mn (by factors of ?100). The concentrations of Zn, Cd, and Ni at the redox front decrease by factors between 3 to 5.Equilibrium calculations are presented for varying concentrations of hydrogen sulfide and compared with the field data. The study strongly supports the assumption that the solubility of Zn, Cd, Cu, and Ni is greatly enhanced and controlled by the formation of bisulfide and(or) polysulfide complexes. Differences between predicted and measured concentrations of these elements are mainly evident at lower ΣH₂S concentrations.Cobalt proved to be very mobile in anoxic regions, and the results indicate that the concentrations are limited by CoS precipitation. The iron (Fe²⁺) and manganese (Mn²⁺) distribution in sulfide-containing waters is controlled by total flux from sediment-water interfaces rather than by equilibrium concentrations of their solid phases (FeS and MnCO₃). The concentrations of these metals are therefore expected to increase with prolonged stagnation periods in the basin.     

Arsenic,barium, germanium,tin, dimethylsulfide and nutrient biogeochemistry in Charlotte Harbor,Florida, a phosphorus-enriched estuary

Concentrations of dissolved nutrients (NO₃, PO₄, Si), germanium species, arsenic species, tin, barium, dimethylsulfide and related parameters were measured along the salinity gradient in Charlotte Harbor. Phosphate enrichment from the phosphate industry on the Peace River promotes a productive diatom bloom near the river mouth where NO₃ and Si are completely consumed. Inorganic germanium is completely depleted in this bloom by uptake into biogenic opal. The $\text{Ge}\text{Si}$ ratio taken up by diatoms is about 0·7 × 10^?6, the same as that provided by the river flux, confirming that siliceous organisms incorporate germanium as an accidental trace replacement for silica. Monomethylgermanium and dimethylgermanium concentrations are undetectable in the Peace River, and increase linearly with increasing salinity to the seawater end of the bay, suggesting that these organogermanium species behave conservatively in estuaries, and are neither produced nor consumed during estuarine biogenic opal formation or dissolution. Inorganic arsenic displays slight removal in the bloom. Monomethylarsenic is produced both in the bloom and in mid-estuary, while dimethylarsenic is conservative in the bloom but produced in mid-estuary. The total production of methylarsenicals within the bay approximately balances the removal of inorganic arsenic, suggesting that most biological arsenic uptake in the estuary is biomethylated and released to the water column. Dimethylsulfide increases with increasing salinity in the estuary and shows evidence of removal, probably both by degassing and by microbial consumption. An input of DMS is observed in the central estuary. The behavior of total dissolvable tin shows no biological activity in the bloom or in mid-estuary, but does display a low-salinity input signal that parallels dissolved organic material, perhaps suggesting an association between tin and DOM. Barium displays dramatic input behavior at mid-salinities, probably due to slow release from clays deposited in the harbor after catastrophic phosphate slime spills into the Peace River.