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1.
从胶州湾污染区域的沉积物样品中筛选获得1株对重金属元素反应敏感的菌株,经鉴定为灰黄青霉(Penicillium griseofulvum),对该菌株在重金属胁迫下的生物学特征及酶的活性变化进行了研究,结果表明,一定量的重金属铜、锌离子对菌株产生显著的影响,并通过形态与色素变化的方式表现出来。当培养基中 Cu2+浓度为125 mg/dm3,Zn2+浓度为800 mg/dm3时,孢子萌发会完全受到抑制,同时菌丝也发生严重变异。菌株色素随着 Cu2+浓度的增加呈现从灰绿色到浅黄色的颜色变化,随着Zn2+浓度的增加呈现从灰绿色到白色的颜色变化。在菌株生长的离子浓度范围内,一定量的 Cu2+浓度能提高 CAT,GOD 酶的活性作用,在Cu2+浓度为25 mg/dm3时活性作用最强;在25～75 mg/dm3时,随着 Cu2+浓度的增加,活性作用逐渐减弱,浓度增加至100 mg/dm3时菌丝不能生长。Cu2+对菌体金属硫蛋白的影响不规则。在 Zn2+浓度为100～400 mg/dm3的培养基中,CAT,GOD酶和金属硫蛋白的活性作用随着Zn2+浓度的增加逐渐增强,在Zn2+浓度为400 mg/dm3时酶和金属硫蛋白活性达到最强。Zn2+浓度增加至600 mg/dm3 时,菌株不能生长。 相似文献
2.
《海洋学报》2010,(5)
从胶州湾污染区域的沉积物样品中筛选获得1株对重金属元素反应敏感的菌株,经鉴定为灰黄青霉(Penicillium griseofulvum),对该菌株在重金属胁迫下的生物学特征及酶的活性变化进行了研究,结果表明,一定量的重金属铜、锌离子对菌株产生显著的影响,并通过形态与色素变化的方式表现出来。当培养基中Cu2+浓度为125 mg/dm3,Zn2+浓度为800 mg/dm3时,孢子萌发会完全受到抑制,同时菌丝也发生严重变异。菌株色素随着Cu2+浓度的增加呈现从灰绿色到浅黄色的颜色变化,随着Zn2+浓度的增加呈现从灰绿色到白色的颜色变化。在菌株生长的离子浓度范围内,一定量的Cu2+浓度能提高CAT,GOD酶的活性作用,在Cu2+浓度为25 mg/dm3时活性作用最强;在25～75 mg/dm3时,随着Cu2+浓度的增加,活性作用逐渐减弱,浓度增加至100 mg/dm3时菌丝不能生长。Cu2+对菌体金属硫蛋白的影响不规则。在Zn2+浓度为100～400 mg/dm3的培养基中,CAT,GOD酶和金属硫蛋白的活性作用随着Zn2+浓度的增加逐渐增强,在Zn2+浓度为400 mg/dm3时酶和金属硫蛋白活性达到最强。Zn2+浓度增加至600 mg/dm3时,菌株不能生长。 相似文献
3.
为研究Cu对云龙石斑鱼(Epinephelus moara♀×Epinephelus lanceolatus♂)幼鱼的生态毒性及生理生化指标的影响,作者分析了Cu2+对幼鱼的安全质量浓度(CS)、组织损伤、酶活力、金属硫蛋白-2(MT-2)基因表达的影响。实验设置对照组以及0.1、0.2、0.4、0.8、1.2、2 mg/L等6个Cu2+实验组进行为期5 d的毒理实验。结果显示:Cu2+对云龙石斑鱼幼鱼的CS为0.0162 mg/L;Cu暴露诱发实验鱼的肝脏组织血窦扩张;鳃组织出现动脉瘤以及顶部棒状等现象;与对照组相比,随Cu2+浓度升高,肝脏组织总超氧化物歧化酶(SOD)活力显著下降;谷草转氨酶(GOT)活力先上升后下降;随Cu处理浓度升高,肝脏、鳃组织MT-2基因表达水平均逐渐上升;而脑组织中MT-2表达水平先上升后下降,但低浓度组较对照组差异不显著。结果表明,高浓度的Cu会造成云龙石斑鱼幼鱼的组织损伤、免疫酶活力降低等一系列不利影响,结果为云龙石斑鱼养殖生产过程中利用铜制剂防控病害的适宜剂量选择提供依据。 相似文献
4.
通过室内半静态暴毒实验, 在铜、铅、镉三种重金属的单一胁迫与两两联合胁迫条件下, 研究了繁殖期泥蚶(Tegillarca granosa)对重金属的富集规律。结果表明: 泥蚶对单一Cu2+、Pb2+、Cd2+的生物富集系数(BCF)分别为210.16～1 178.66、128.15～603.84 和198.84～659.37; 联合重金属胁迫条件下, Cd2+对Cu2+的富集具有一定的拮抗作用; Cd2+和Cu2+在泥蚶体内以可溶形式存在, 而Pb2+以不溶形式存在;Cu2+和Cd2+对泥蚶富集Pb2+有一定的协同效应; 砂滤海水中的暂养的泥蚶, 其体内的重金属含量除Cu2+外都较为稳定。 相似文献
5.
本研究提出了一种用于检测海水中锌离子（Zn2+）含量的电化学检测方法。该方法首先应用水热法合成SiO2@PDA-Sb复合材料,然后将该复合材料修饰到玻碳电极上制备SiO2@PDA-Sb-Nafion/GCE,利用差分脉冲阳极溶出伏安法（DPASV）对珠江口海水水样中Zn2+进行测定。研究结果表明,Zn2+在SiO2@PDA-Sb-Nafion/GCE上具有较强的溶出峰。在最优条件下,SiO2@PDA-Sb-Nafion/GCE对Zn2+浓度在1~1 000 nmol/L范围内可实现灵敏、准确的检测,Zn2+的检测出限为0.71 nmol/L。加标回收率实验显示Zn2+加标回收率为93.19%~100.12%,表明该方法可应用于现场海水样品Zn2+测定。本方法具有电极制作简单、稳定性和抗干扰性良好,能够提高现有测定方法的检测限和精确度,在现场海水检测痕量Zn2+具有较好的应用前景。 相似文献
6.
对一株分泌热稳定κ-卡拉胶酶印尼热泉菌进行了种属鉴定, 并采用响应面法对该菌发酵产酶条件进行了优化。鉴定结果表明, 该菌株属于芽孢杆菌属(Bacillus), 命名为Bacillus sp. Car19(GeneBank: KT865196)。发酵条件优化结果显示, 9个环境因子影响Bacillus sp. Car19产酶量。其中影响Bacillus sp. Car19产酶量的三个主要因素分别为培养温度、培养基中Cu2+浓度和培养基中NaCl浓度。综合次要因素对Bacillus sp. Car19产酶影响, Bacillus sp. Car19最佳产酶发酵条件为: 培养温度52.31℃、Cu2+浓度6.93 mmol/L、NaCl浓度37.03 g/L, 培养基pH为6, 接种量1%, 培养时间36h, 半乳糖浓度0.3 g/L,硝酸铵浓度7g/L, 卡拉胶浓度0.5g/L。优化后发酵上清液酶活力达到15.21 U/mL, 与优化前相比提高了1.5 倍。 相似文献
7.
可口革囊星虫(Phascolosoma esculenta)重组铁蛋白富集Pb2+等重金属特性和功能研究 总被引：1，自引：1，他引：0
利用可口革囊星虫重组铁蛋白富集Pb2+、Fe3+、Cd2+、Cr3+、Cu2+、Mn2+、Sn2+和Zn2+等8 种重金属离子后, 通过透射显微镜和傅里叶红外光谱测定蛋白的超微结构变化和内部基团特性。以 天然的马脾铁蛋白为对照, 观察重组铁蛋白与天然铁蛋白的差别。结果显示, 重组铁蛋白富集Pb2+ 和其它7 种重金属离子后蛋白体积大小与重金属离子种类直接相关。重组铁蛋白相对天然铁蛋白来 说在富集不同种类重金属离子后, 除了非特异性酰胺特征峰和蛋白特征峰外, 还出现一些专门富集 某些重金属离子的特异基团, 如:-CH3、-CH2-、-CH-、-NH-、-SO3-、-COOH、-S=S-和-C-S-C 等。 通过细胞实验进一步验证了铁结合蛋白能够通过富集重金属离子Pb2+来保护小鼠成骨前体细胞 MRC3T3-E1, 使细胞的死亡率明显降低(P<0.05). 相似文献
8.
采用改良的微孔板法测定了12株弧菌的形成生物膜的效果,选择形成生物膜效果最好的副溶血弧菌ND-02,进一步研究了环境因子对其生物膜形成的影响。实验结果显示副溶血弧菌ND-02菌株在静置培养24~36 h后形成成熟的生物膜,在起始菌浓度为107~108CFU/mL形成生物膜的量最大;在30 ℃,NaCl浓度为3%~ 5%,pH偏弱碱性时的生物膜OD590值最大;Ca2+ 促进副溶血弧菌生物膜的形成,而Mg2+ 抑制生物膜的形成;副溶血弧菌在分别经大黄鱼表皮黏液、肠黏液和肝脏提取液包被的的基质上形成生物膜的作用明显,鳃黏液和脾脏提取液中次之,肌肉提取液包被后生物膜形成量最低。以上结果表明,副溶血弧菌ND-02菌株能形成稳定而明显的生物膜,而且生物膜的形成受温度、NaCl浓度、pH值等环境因子的影响。 相似文献
9.
微生物降解羽毛既可保护环境又能实现废物的资源化利用,具有显著的经济效益和社会效益。本研究从广西钦州港海鸭养殖淤泥筛选获得一株可高效降解羽毛的菌株Gxun-20,通过对该菌株形态特征、生理生化特性和16S rRNA基因序列进行分析,以确定菌株的分类,并对菌株产角蛋白酶的条件及酶学性质进行研究。结果表明：该菌为副短短芽孢杆菌(Brevibacillus parabrevis);菌株最适产酶条件为：温度34 ℃,初始pH 6.5,羽毛含量1.5%(质量分数),发酵48 h,角蛋白酶活性可达277.45 U/mL。菌株Gxun-20所分泌的角蛋白酶最适温度为50 ℃,且热稳定性较好,最适pH为7.5;金属离子Fe3+、Cu2+、Co2+、Fe2+和Mn2+对酶活性有显著抑制作用,而Ca2+、Na+对酶活性有明显促进作用;金属螯合剂乙二胺四乙酸(ethylene diamine tetraacetic acid, EDTA)可显著抑制酶的活性,蛋白酶抑制剂苯甲基磺酰氟(pheny methyl sulfonyl fluoride, PMSF)可完全抑制酶活性,表明该蛋白酶的活性中心含有金属离子和丝氨酸;异丙醇可使酶活性提高至129.34%,酶活性在十二烷基硫酸钠(sodium dodecyl sulfate, SDS)、吐温40溶液中保持稳定;酶的底物特异性结果表明,该酶对羽毛类β-角蛋白及酪蛋白降解能力较好,而对牛血清蛋白、I型胶原及人发类α 角蛋白降解能力较弱。海洋来源的副短短芽孢杆菌Gxun-20及其所产角蛋白酶在废弃羽毛降解方面具有良好的应用价值。 相似文献
10.
本研究利用三价钛还原法将标准样品、海水、湖水和雨水中硝酸根转化为N2O测试其氮氧同位素值,并优化实验条件（NO-3浓度、试剂量、反应时间和温度等）。结果表明：4 cm3硝酸根水样（浓度约为20 μmol/dm3）,加入100 mm3TiCl3溶液（浓度为150 g/dm3）,25 ℃反应24 h,NO-3还原为N2O的平均转化率为86.3%（n=5）。5种丰度硝酸根氮氧同位素标样校准曲线斜率分别为0.947和0.617,相关系数R2分别为0.999和0.994;方法检出限的NO-3浓度为2.5 μmol/dm3,其δ15N的标准偏差小于0.7‰(n=5),δ18OVSMOW值的标准偏差小于2.5‰(n=5);20 μmol/dm3硝酸根样品δ15N的标准偏差小于0.5‰（n=5),δ18OVSMOW值的标准偏差小于1.0‰（n=5）。该方法测定3种不同类型水样δ15N的标准偏差分别为0.3‰、0.6‰和0.5‰;δ18OVSMOW的标准偏差分别为2.1‰、2.0‰和1.6‰。三价钛还原法分析水体中硝酸根氮氧同位素操作步骤简单,测试效率高,但氧同位素结果需要系统校正。 相似文献
11.
Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths. 相似文献
12.
Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone. 相似文献
13.
The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics. 相似文献
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15.
《海洋学报(英文版)》2014,(9):F0003-F0003
<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology, 相似文献
16.
The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance. 相似文献
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The behaviour of an axially pre-loaded cylindrical member of an offshore structure, hit by a supply ship, has been investigated. The effects of axial pre-loading on the dynamic properties of members, the extent of damage and propagation of dynamic instability in the tubular members have also been investigated. Numerical models have been validated using available experimental data from the literature although these are mostly static with no pre-loading. Axial pre-loading was found to change the dynamic characteristics of some cylindrical members quite dramatically while it had no significant effect on others. The study examined whether there was any change in the behaviour between local and global modes when the loading was dynamic rather than static. The effect of damping on the dynamic instability of axially pre-loaded tubes under lateral dynamic loads was also studied. It was observed that for some geometries the quasi-static response can be used to define the boundary between bounded and unbounded dynamic responses. The main contribution of this study, compared with previous investigations reported in the literature, is that both pre-loading and dynamic effects have been included. 相似文献
19.
Rahul Sharma 《Marine Georesources & Geotechnology》2000,18(3):237-250
Observations on seafloor features from subbottom profiling and seabed photography data show that the undisturbed and natural conditions before the benthic disturbance undergo a substantial change after operation of the disturber. The effects can be seen in the form of deep trenches and grooves, formed by the action of the sleds and the pumping of the sediment along its path, as well as sediment piles on either side of the track. Biological traces such as fecal coils, casts, tubes, burrows, and trails get obliterated in the areas of disturbance and resedimentation. The smooth, uniform nature of the seafloor observed in predisturbance phase shows microtopographic changes in and around the disturbed area as a result of sediment excavation and resettlement. Vertical mixing as well as lateral transport of sediment alter the geological, biological, physical, and chemical conditions on the seafloor, which need to be monitored over time to assess the process and the time taken for restoration of environmental conditions. 相似文献
20.
Vance P. Vicente 《Marine Ecology》1989,10(2):179-191
Abstract. Long-term changes in the distributional patterns of commercial sponges ( Spongia spp. and Hippospongia spp.) within the West Indian Region indicates that: 1) commercial sponges had a widespread distribution throughout the whole West Indian Region and were ubiquitous in very shallow water until about the first half of the present century; 2) they were fished commercially not only in the traditional northern Caribbean sites (Florida, Gulf of Mexico, Bahamas) but also in the Greater ( e. g. , Hispaniola, Jamaica) and Lesser Antilles; and 3) they became extinct throughout most of the Lesser Antilles ( e. g. , Puerto Rico, Vieques, St. Thomas) sometime during the first half of this century. Mortalities of spongiids within the Antilles were found to differ from other marine mortalities in that: 1) species disappeared from a large region; 2) species vanished from different habitats and depths; and 3) natural populations never recovered. Species richness patterns suggest that commercial sponge genera ( Spongia and Hippospongia ) evolved under slightly cooler elimatic conditions than those found at present, and that these extinctions occurred as a direct or indirect effect of positive thermal anomalies in sea surface and atmospheric temperatures between 1900–1950. The concept that species diversity is stable on a regional scale is questioned. 相似文献