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1.
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(Gene Bank: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Cu~(2+)浓度和培养基中Na Cl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℃、Cu~(2+)浓度6.93 mmol/L、Na Cl浓度37.03 g/L,培养基p H为6,接种量1%,培养时间36 h,半乳糖浓度0.3 g/L,硝酸铵浓度7 g/L,卡拉胶浓度0.5 g/L。优化后发酵上清液酶活力达到15.21 U/m L,与优化前相比提高了1.5倍。  相似文献   

2.
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   

3.
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   

4.
微藻培养过程中氮缺失有利于油脂和生物量的积累，然而不同氮源条件下微藻生长与生物量的研究有限，限制了生物油脂的相关研究。本文研究通过研究南极冰藻Chlamydomonas sp.ICE-L在不同氮源条件下的细胞生长与油脂积累，进一步探究其作为富集油脂微藻的潜力。研究发现：在含有NH4CL的培养基中，Chlamydomonas sp.ICE-L生长速率最大；在含有NH4NO3的条件下，获得了最大干重量0.28 g/L。最高油脂含量0.21 g/g是在缺氮条件下获得，同时得到干重0.24 g/L。在多不饱和脂肪酸的产出方面，NH4NO3和NH4Cl为氮源培养基时要好于缺氮和KNO3培养基，在NH4NO3和NH4Cl为氮源的培养条件下ICE-L胞内C18：3和C20：5的含量高。比较而言，缺氮和KNO3培养基时C16：0、C18：1和C18：2的含量要高。  相似文献   

5.
Vertical distributions of phytoplankton biomass, compositions and size structure were investigated during the spring-intermonsoon (April 22 to 30) of 2010 along transact 10°N of the Bay of Bengal, northern Indian Ocean. Surface phytoplankton biomass (Chl a) was (0.065§0.009) μg/L, being greater than 80% of which was contributed by pico-phytoplankton (<3 μm). The Chl a concen- tration vertically increased to the maximal values at deep chlorophyll maximum (DCM) layer that shoaled eastwards from 75 to 40 m. The Chl a biomass at DCM layer generally varied between 0.2 and 0.4 μg/L, reaching the maximum of 0.56 μg/L with micro-phytoplankton cells (>20 μm) accounting for 58% and nano- (3-20 μm) or pico-cells for 15% and 27%, respectively. In particular, the cells concentration coupling well with phosphate level was observed at middle layer (75-100 m) of 87° to 89°E, dominated by micro-cells diatoms (e.g., Chaetoceros atlanticus v. neapolitana, Chaetoceros femur and Pseudonitzschia sp.) and cyanobacteria (i.e., Trichodesmium hildebrandtii), with the cells concentration reached as high as 4.0×104 and 4.3×104 cells/L. At the rest of the trans- act however, dino°agellates (e.g., Amphisdinium carterae and Prorocentrum sp.) were the dominant species, with the cells concentration varying from 0.3×103 to 6.8×103 cells/L. Our results also in- dicate that the regulation of large cells (micro-, nano-) on phytoplankton biomass merely occurred at DCM layer of the Bay.  相似文献   

6.
采用响应面法对1株高产卡拉胶酶的印度尼西亚热泉菌Bacillus sp.Lc50-1的发酵条件进行优化。分别以培养温度、pH值、C源、N源、金属离子及接种量作为唯一变量进行单因素实验,筛选出对酶活有显著影响的单因素取值范围;参考单因素实验结果,再利用Box-Behnken设计及响应面分析法进行回归分析以确定最佳发酵条件。结果表明,培养温度、卡拉胶浓度(C源)、蛋白胨浓度(N源)、KCl浓度(金属离子)与酶活存在着显著的相关性,通过求解回归方程得到Bacillus sp.Lc50-1的最佳发酵条件为:培养温度47.5℃、蛋白胨0.25%、卡拉胶0.3%、KCl 21.55mmol·L-1,优化后发酵上清液的酶活达到8.9U·mL-1,比优化前提高了1.5倍。  相似文献   

7.
黄杆菌种类多、分布广,但从深海海山环境中发现黄杆菌新物种的报道还没有。2017年我们从西太平洋卡罗琳深海海山水域分离到一株细菌XN-5T,经16S rRNA基因序列测定表明,该菌与黄杆菌属(Flavobacterium)内系统发育关系最近模式菌株F.degerlachei LMG 21915T、F.frigoris LMG 21922T之间的相似性分别为97.5%和97.8%。本研究采用形态学观察、生理生化特征、遗传特征、脂肪酸和极性脂测定等方法,对该菌株进行了详细的多相分类鉴定。结果表明,XN-5T菌株在16S rRNA基因系统发育、生长温度、淀粉、酪蛋白水解、硝酸盐还原,产α-半乳糖苷酶、α-葡萄糖苷酶、β-葡萄糖苷酶,同化L-阿拉伯糖、D-甘露醇、N-乙酰-氨基葡萄糖、葡萄糖酸钾,发酵蔗糖、阿拉伯糖,以及脂肪酸、极性脂组成等方面,均与相近模式菌株有所差异。综合多相分类鉴定数据,我们判定XN-5T菌株为Flavobacterium属内的一个新种,命名为Flavobacterium pacifica sp. nov。  相似文献   

8.
研究拉恩氏菌(Rahnella sp. PJT09)胞外多糖的发酵条件,并进行多糖结构分析。通过单因素试验及正交试验确定拉恩氏菌Rahnella sp. PJT09发酵产糖的最适培养基组成为(g/L):蔗糖40,酵母膏3,NaCl 0.5,ZnCl20.3,K2HPO41;最佳发酵条件为每250 mL三角瓶装液量为100 mL,接种量为3%(体积分数),初始pH值为6.0,28℃,160 r/min培养54 h。在此条件下,Rahnella sp. PJT09多糖产量可达18.51 g/L。采用高效凝胶渗透色谱技术(HPGPC)测定了多糖的分子量,13C-NMR技术确定多糖的结构。研究表明,Rahnella sp. PJT09多糖为重均分子量320 kDa的-β2→6-D-果聚糖。  相似文献   

9.
双眉藻(Amphora sp.)是糙刺参(Stichopus horrens)喜食的优良饵料。本文采用光密度法分别测定了该藻在光照强度28～149 μmol/(m2·s)、温度20～35℃、盐度25~45 和氮质量浓度0～7 500 mg/L、磷质量浓度0～440 mg/L、硅质量浓度0～1 500 mg/L 以及氮磷硅多因子组合情况下的比生长速率, 探讨了光照、温度、盐度和不同质量浓度的氮、磷、硅单因子及多因子组合对该藻生长的影响, 以及该藻的最适生长条件。单因子试验结果表明, 该藻在光照范围为35～149 μmol/(m2·s)时都能良好生长, 最适光照为56～99 μmol/(m2·s), 低温时该藻生长缓慢, 最适生长温度为25～30℃。Amphora sp.为广盐性, 在盐度25～45 都能较好生长, 最适盐度为30～35。氮、磷、硅的最适质量浓度分别是750～7 500 mg/L、44 mg/L和150mg/L, 磷对该藻生长的影响比氮更显著。正交实验结果表明, 氮、磷、硅的最佳质量浓度分别为75 mg/L、44 mg/L 和150 mg/L, 最佳配比为2.4:1:3.4, 与其他底栖硅藻的相应指标存在一定的差异, 可能是物种和地域环境差异引起的, 反映出该藻适应高温、强光特殊栖息环境的特征。  相似文献   

10.
为对南极菌Psychrobacter sp.B-3产胞外糖的发酵条件进行优化,以温度、pH、不同碳源、不同氮源、不同金属离子及海水配比作为唯一变量进行单因素实验,筛选出对产糖有显著影响的单因素取值范围;在此基础上,利用Plackett-Burman实验设计筛选出影响产多糖的3个主要因素,即酵母粉、陈海水配比和装液量.然后通过Box-Behnken实验设计及响应面分析法进行回归分析,得出了南极菌Psychrobacter sp.B-3发酵条件系统优化的结果为:酵母粉1.1 g/L,陈海水与自来水的配比为2:1,装液量为50％,蛋白胨6.0 g/L,接种量1.5％,培养时间64 h,BaCl20.03 g/L,温度10℃,转速150 r/min,pH为7.0.优化后发酵液中的糖含量由优化前的444 μg/mL提高到624 μg/mL,相比初始糖产量提高了40％.结果表明,响应面法可显著优化南极菌Psychrobacter sp.B-3液体发酵产胞外糖的条件.  相似文献   

11.
Coastal inundation associated with extreme sea levels is the main factor which leads to the loss of life and property whenever a severe tropical cyclonic storm hits the Indian coasts. The Andhra and Orissa coasts are most vulnerable for coastal inundation due to extreme rise in sea levels associated with tropical cyclones. Loss of life may be minimized if extreme sea levels and associated coastal flooding is predicted well in advance. Keeping this in view, location specific coastal inundation models are developed and applied for the Andhra and Orissa coasts of India. Several numerical experiments are carried out using the data of past severe cyclones that struck these regions. The simulated inland inundation distances are found to be in general agreement with the reported flooding.  相似文献   

12.
Grain size and water content in box-core sediments from the Clarion-Clipperton fracture zone (C-C zone) in the northeast equatorial Pacific were analyzed in detail to understand the downcore variations across a hiatus between Quaternary and Tertiary layers. Grain-size distributions in the topmost core sediments show two modes: a coarse mode (peaked at 50 μm) and a fine mode (at 2-25 μm). The coarse mode disappears gradually with depth accompanied by the dissolution of siliceous fossil tests, whereas the fine mode coarsens due to the formation of authigenic minerals. Water content increases abruptly across a color boundary between an upper pale brown layer and a lower dark brown layer that is the hiatus between Quaternary and Tertiary layers. Abundant smectites and microvoid molds, which are created by the prolonged fossil dissolution in the underlying sediment, are attributed for the abrupt downcore variation of water content. Overall variations in grain size and water content in the topmost core sediments in the western C-C zone are possibly constrained by the dissolution of biogenic siliceous fossils. Variations in geotechnical properties related to these changes must be considered in the design of nodule collectors.  相似文献   

13.
This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake.  相似文献   

14.
This study tests the hypothesis that the in situ void ratio of surficial marine sediments may be predicted from shear wave velocity-depth data with a reliability equal to that of other methods currently available. Shear wave velocity is fundamentally controlled by the number of grain-to-grain contacts per unit volume of material and by the effective stress across those contacts. In this study, three previously established empirical formulae are used to predict void ratio from velocity-depth data. Field data were acquired along a transect off the northern Californian coast across which water depth increased from 35 to 70 m and seafloor sediment type varied from sand to silty-sand, respectively. A towed seafloor sled device was used to collect shear wave refraction data, and a marked, systematic decrease in velocity was observed along the line, ranging from 35-70 m/s for the coarse, near-shore material to 25-40 m/s for the finer, offshore deposits. Void ratios predicted from these velocities were compared with data measured directly from box-core samples. Of the formulae used for prediction, two agree remarkably well with the control data. Both predicted and control values increase from 0.6-0.8 for the sandy material to 1.1-1.5 for the silty-sand. Thus, this study does not disprove the hypothesis set and demonstrates the potential of field shear wave velocity-depth data as a means of delineating spatial variation in void ratio for surficial marine sediments in a remote, nondestructive manner.  相似文献   

15.
Particulate samples were collected from the Changjiang river system during a flood period, in May 1997, and POC, stable isotope and lipids associated with particles were examined. Results showed the decrease (0.84% ～ 1.88%) of organic carbon content from the upper reaches to the estuary.δ13C values of particulate organic carbon was in the range of -24.9×10-3 to -26.6×10-3, which were close to the isotopic signature of continental C3 vegetation. Total particulate n-alkanes concentrations varied from 1.4 to 10.1μg/dm3,or from 23.7 to 107μg/g of total suspended matter. Fatty acids were present in all the samples, from 1.4 to 5.4μg/dm3, with saturated and unsaturated straight-chain and branched compounds in the carbon number range from C12 to C30. Both δ13C and the ratio of carbon content to nitrogen content indicate the predominance of terrestrial inputs (soil organic matter) among the particles. The biomarker approach has been used to identify the relative portion of terrigenous and autochthonous fraction in the particulate samples. The distribution of fatty acids suggests a striking phytoplanktonic and microbial signal in most particle samples. The terrestrial alkanes are used to estimate the contribution of terrestrial inputs along the mainstream.  相似文献   

16.
Current trends of development of satellite derived bathymetry (SDB) models rely on applying calibration techniques including analytical approaches, neuro-fuzzy systems, regression optimization and others. In most of the cases, the SDB models are calibrated and verified for test sites, that provide favorable conditions for the remote derivation of bathymetry such as high water clarity, homogenous bottom type, low amount of sediment in the water and other factors. In this paper, a novel 3-dimensional geographical weighted regression (3GWR) SDB technique is presented, it binds together methods already presented in other studies, the geographically weighted local regression (GWR) model, with depth dependent inverse optimization. The proposed SDB model was calibrated and verified on a relatively difficult test site of the South Baltic near-shore areas with the use of multispectral observations acquired by a recently launched Sentinel-2 satellite observation system. By conducted experiments, it was shown that the proposed SDB model is capable of obtaining satisfactory results of RMSE ranging from 0.88 to 1.23[m] depending on the observation and can derive bathymetry for depths up to 12m. It was also shown, that the proposed approach may be used operationally, for instance, in the continuous assessment of temporal bathymetry changes, for areas important in the context of ensuring local maritime safety.  相似文献   

17.
As a part of the environmental impact assessment studies, geotechnical properties of sediments were determined in the Central Indian Basin. The undrained shear strength and index properties of the siliceous sediments were determined on 20 box cores of uniform dimension collected from various locations in five preselected sites. The maximum core length encountered was 41 cm and most of the sediments were siliceous oozes consisting of radiolarian or diatomaceous tests. The shear strength measurements revealed that surface sediments deposited in recent times (0-10 cm) have a shear strength of 0-1 kPa; this value increases with depth, reaching 10 kPa at 40 cm deep. Older sediments have greater strength because of compaction. Water content varies in the wide range of 312-577% and decreases with depth. The clay minerals such as smectite and illite are dominant and show some control over water content. Wet density, specific gravity, and porosity do not indicate any notable variation with depth, thereby indicating a uniform, slow rate of sedimentation. The average porosity of sediments is 90.2%, specific gravity 2.18, and wet bulk density 1.12 g/cm 3 . Sediments exhibit medium to high plasticity characteristics, with the average plasticity index varying between 105% and 136%. Preliminary studies on postdisturbance samples showed an increase in natural water content and a decrease in undrained shear strength of sediments in the top 10- to 15-cm layer.  相似文献   

18.
The rare earth element (REE) distribution in nine deep-sea ferromanganese nodules and their associated siliceous sediments from the Central Indian Ocean Basin (CIOB) have been studied to elucidate the REE relationship among them. Total REE concentration varies from 398-928 ppm in the nodules and 137-235 ppm in the associated sediments, suggesting two- to four-fold enrichment in the nodules compared to associated sediments. REE of nodules and their associated sediments show a positive correlation, suggesting REE are supplied from a common source such as seawater. The positive correlation between REE of nodules and sediments from the CIOB is contrary to the competitive scavenging of REE between nodules and sediment in the equatorial Pacific Ocean. REEs in the nodules are carried by Fe, P, and Ti, whereas in the sediment they are carried by P and Mn phases. A similar REE fractionation pattern with middle REE enrichment over heavy and light REE in both the nodules and their associated sediment suggest fractionation is independent of REE abundance and their carrier phases.  相似文献   

19.
Detailed acoustic surveys of benthic sediments were conducted in July 1995 and September 1998 in the vicinity of Humboldt Bay, California. During these surveys, a band of enhanced acoustic backscatter was observed offshore from the bay entrance, approximately parallel to the isobaths, in water depths ranging from 16-24 m. In order to assess the cause of the increase in backscatter levels, a more comprehensive study was conducted in August and September 1999 using 100 kHz side-scan sonar, bottom grab sampling and underwater video recording. New observations indicated that a dense population of sand dollars ( Dendraster excentricus ) coincided with the enhanced backscatter band. Compared to the two previous acoustic studies, the central section of the band expanded westward by 180 m and the southern section of the band shifted eastward by 160 m, possibly resulting from a change in the biological or physical factors which influence the location and breadth of sand dollars. The relationship between high sand dollar abundance and enhanced acoustic backscatter was further verified in the nearshore region off Samoa Beach California, where a dense, banded population of sand dollars was previously observed. Video footage confirmed the presence of a band of sand dollars, also nominally parallel to the isobaths, in water depths of 8-15 m. A band of enhanced backscatter coincided with the dense sand dollar population. The identification of dense aggregations of sand dollars through enhanced acoustic backscatter could lead to the use of acoustic techniques to study sand dollar distributions and abundance.  相似文献   

20.
Vast reserves of marine minerals are known to occur within the Mexican Exclusive Economic Zone. These reserves include: (1) heavy mineral placers rich in titanium and iron along the coast of San Antonio del Mar, Baja California and the southern States of Oaxaca and Guerrero; (2) phosphorites, which represent the only source for superphosphate fertilizers along the Pacific coast off the Baja California peninsula and the Gulf of Tehuantepec; and (3) manganese oxide deposits in nodule and crusts located adjacent to the Clarion-Clipperton Zone and containing high concentrations of Cu + Ni + Co (up to 1.9%), which are essential for the steel and super-alloy industries. Few but important efforts toward surveying these deposits have been carried out by Mexican and international researchers. Relevant data generated by these investigations are reviewed here and put together in a single document. Adequate knowledge of Mexican mineral resources is essential for the development of management strategies when offshore mining starts during this century. Thus, the review discusses the economics inherent to ocean mining in Mexico, setting baselines for future exploration and development activities in the Mexican Exclusive Economic Zone.  相似文献   

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