一株抗硅藻附着的海绵附生菌的鉴定及发酵条件优化

为了从海绵共附生微生物中寻找天然高效抗污损活性物质,本文针对前期研究获取的4株具有显著抗硅藻附着的活性菌株进行活性验证和比较,选出其中最优菌株进行菌种鉴定及发酵条件优化.比较了活性菌株对小新月菱形藻(Nitzschia closterium)、咖啡双眉藻(Amphora coffeaeformis)、碎片菱形藻(Nitzschia frustulum)附着的抑制活性,确定菌株UST050418-715为最优菌株;通过16S r DNA的测序分析,结合平板的菌落形态和扫描电镜下菌体特征,鉴定活性菌株UST050418-715为短小芽孢杆菌(Bacillus pumilus).为优化该菌株的培养条件,选择了酵母粉、蛋白胨、Na Cl、p H值进行四因素三水平的正交实验,对菌株培养条件进行优化.发现选择的4个因素对应的菌株发酵产物对硅藻附着的抑制活性大小不同,影响显著性顺序是酵母粉蛋白胨Na Clp H值,综合菌株发酵产物活性、粗提物产量和菌株生长情况进行分析,确定菌株UST050418-715基于海洋2216E培养基的最佳发酵条件为:蛋白胨含量7.5 g/dm3,酵母粉含量3 g/dm3,Na Cl含量10.45 g/dm3,p H值9.5.     

热稳定κ-卡拉胶酶产生菌Bacillus sp. Car19的发酵条件优化

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。     

一株海绵附生菌Bacillus firmus的培养条件优化及α-GI活性成分初步分析

为寻找新型α-葡萄糖苷酶抑制(α-glucosidase inhibition,α-GI)活性化合物来源,针对前期研究发现的具有α-GI活性的海绵附生微生物坚强芽孢杆菌(Bacillus firmus),对其发酵培养条件进行优化,并对其活性组分中主要成分进行初步分析.以α-GI活性为主要检测对象,选出蛋白胨、酵母膏、Na Cl和p H值共4个因素进行正交优化试验.结合菌株生长情况和代谢产物产量指标,发现在MB培养基的基础上,蛋白胨质量浓度3 g/dm3、酵母膏质量浓度3 g/dm3、Na Cl质量浓度19.5 g/dm3、p H值为7.5的组合为最优培养条件.在优化后的培养条件下,规模化发酵该菌株,提取其代谢产物粗提物,经活性追踪下的二次色谱柱分离,获得一个高抑制活性组分,抑制率达82.4%.该组分经GC-MS分析后发现,活性组分中主要成分为环二肽类及哌啶酮类物质.本研究结果为寻找新型α-GI活性化合物提供了一个新的、可扩大生产的来源.     

海绵共附生微生物中具有α-葡萄糖苷酶抑制活性菌株的筛选与初步鉴定

通过建立α-葡萄糖苷酶抑制剂筛选模型,对美国圣璜岛海域海绵共附生微生物发酵产物进行活性筛选.其中,α-葡萄糖苷酶活性测试反应体系是在96孔酶标板中进行,在α-葡萄糖苷酶浓度为0.008 U/cm3,pH值为6.8,反应温度为37℃及测定生成物波长为405 nm的基础上,优化筛选模型.结果表明,模型的最佳筛选条件:底物PNPG的浓度为10 mmol/dm3、活性测试反应时间为25min,样品溶剂DMSO含量为2%(V/V).以α-葡萄糖苷酶抑制剂阿卡波糖作为阳性对照样品,根据优化后的抑制活性筛选模型对212株海绵共附生微生物的粗提物样品进行筛选.结果表明:19株微生物的粗提物抑制率大于50%;其中,抑制活性最高的5株菌株的粗提物,在浓度为0.4、0.6、0.8 mg/cm3时,其抑制活性均在70%以上,远远高于阿卡波糖的最高抑制率58%(1.6 mg/cm3).其中菌株HY936粗提物浓度在0.4 mg/cm3时,仍具有很高的α-葡萄糖苷酶抑制率79.3%.通过16SrDNA序列测定与分析,鉴定该菌株为坚强芽孢杆菌(Bacillus firmus).坚强芽孢杆菌代谢产物能显著抑制α-葡萄糖苷酶活性,这为研制新型α-葡萄糖苷酶抑制剂提供了有力的线索,对坚强芽孢杆菌有待作进一步的研究.     

热稳定k-卡拉胶酶产生菌Bacillus sp.Car19的发酵条件优化

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。     

壳聚糖酶高产菌株的筛选和发酵条件的研究

从采集的土样中分离到1株产壳聚糖酶能力较强的菌株OU01,并对OU01进行了16S rDNA序列、形态及生理生化鉴定分析。16S rDNA序列分析表明该菌属于微杆菌属;该菌的形态特征与生理生化鉴定结果表明该菌与Microbacteriumsp.的相似性最高;因此将其初步鉴定为微杆菌属(Microbacterium)。同时对该菌的发酵条件进行了初步研究:该菌的最适培养基组成为(g/L):chitosan 10,(NH4)2SO420,MgSO4.7H2O 1.3,K2HPO4.3H2O 1.4,Glucose 1,Yeast extract 3,NaCl 5,起始pH=6.30。最适发酵温度为30℃,最佳发酵时间为96 h,在上述最优条件下,该菌株产酶达到118 U/mL。Microbacteri-umsp.OU01菌株为壳聚糖酶的研究和应用提供了新的来源。     

海洋真菌Neosartorya fischeri 1008F1的次级代谢产物抑菌及抗肿瘤活性的研究

通过抑菌及抗肿瘤活性实验,明确海洋真菌Neosartorya fischeri 1008F1次级代谢产物中的活性有效组分。应用对峙培养法和生长速率法,对菌株的抑菌活性进行测定。应用MTT法,对菌株的抗肿瘤活性进行测定。应用凝胶(Sephadex LH-20)柱层析的方法,对菌株发酵产物的提取物进行分离。结果发现,海洋真菌Neosartorya fischeri 1008F1的水溶性提取物对番茄早疫菌(Alternaria solani)具有一定的抑制活性。菌株的粗提物浸膏经Sephadex LH-20柱梯度洗脱后,得到的组分B、C、D、E和F。在0.5 g/L的供试浓度下,组分B、C和D对胃癌细胞SGC-7901的抑制率均高于80%,而组分B、C、D、E和F对肝癌细胞BEL-7404的抑制率均高于70%。     

一株海洋解淀粉芽孢杆菌(Bacillus amyloliquefaciens)生产Macrolactin B的发酵条件优化

从浙江台州近海上层海水中分离到一株可产Macrolactin类大环内酯抗生素的海洋细菌,经形态特征分析及16S rRNA测序比对,鉴定并将其命名为解淀粉芽孢杆菌(Bacillus amyloliquefaciens)ESB-2。运用Minitab软件,通过Plackett-Burman和Box-Behnken实验及响应面分析对该菌生产Macrolactin B的发酵条件进行优化,得到该菌生产Macrolactin B的最佳发酵条件为：葡萄糖17.0mg/L,蛋白胨5mg/L,酵母粉1mg/L,FePO4 0.01mg/L,初始pH 6.0,培养温度27.2℃,接种量5%,装液量57.6%,培养时间4d,在优化发酵条件下,Macrolactin B的最高产量达到13.6μg/ ml,比优化前提高了8倍,为该活性物质药源问题的解决打下了良好基础。     

硝酸钠浓度对2株三角褐指藻生长及脂肪酸组成的影响

在温度为 (2 2± 1 )℃ ,盐度为 2 8的条件下 ,用含不同浓度硝酸钠 (75 ,3 75 ,75 0 ,11 2 5 ,1 5 0 0 ,1 875 mg/L)的培养基对青岛海洋大学微藻种质库保存的 2株三角褐指藻(Phaeodactylum tricornutum MACC/B1 1 8,MACC/B2 2 1 )进行培养。在指数生长期末期进行收获。测定了 2株硅藻的生长及脂肪酸组成。单因子方差分析结果表明 :硝酸钠浓度对 2株三角褐指藻相对生长率和影响差异不显著 ;对脂肪酸组成的影响因种而异 ,2株硅藻的主要脂肪酸为 1 4∶ 0 ,1 6∶ 0 ,1 6∶ 1 n- 7和 2 0∶ 5 n- 3 (EPA)     

Pseudomonas sp.在杀菌剂耐受条件下对X70管线钢的腐蚀行为研究

本研究选用一株野生型Pseudomonas sp.为试验菌株，选用X70管线钢作为代表性金属材料，通过细菌生长曲线测定、腐蚀失重测量、扫描电镜（SEM）观察等方法，初步研究在杀菌剂四羟甲基硫酸磷（THPS）耐受条件下Pseudomonas sp.对X70管线钢腐蚀行为的影响。结果表明，75 μL/L的THPS浓度在Pseudomonas sp.的耐受范围内，而且能够轻微促进X70试片表面的腐蚀；不添加THPS的含菌体系中Pseudomonas sp.能抑制X70试片表面的腐蚀；而在添加了75 μL/L THPS的含菌体系中，Pseudomonas sp.显著促进X70试片的腐蚀，并且试片表面附着的细菌数量相比于无杀菌剂的对照体系有所增加。因此，该研究表明在特定浓度范围内，与没有添加杀菌剂的含菌体系相比，杀菌剂THPS使Pseudomonas sp.从抑制腐蚀改变为促进腐蚀。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

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.     

A Review of Some Environmental Issues Affecting Marine Mining

This article reviews information recently available from existing marine and coastal mining for responses to environmental issues affecting marine mining at different depths. It is particularly but not exclusively concerned with those issues affecting seabed biodiversity impact and recovery. Much information has been gathered in the past 10 years from shallow mining operations for construction aggregate, diamonds, and gold, from coastal mines discharging tailings to shallow and deep water, and from experimental deep mining tests. The responses to issues identified are summarized in a series of eight tables intended to facilitate site-specific consideration. Since impacts can spread widely in the surface mixing layer SML, and can affect the biologically productive euphotic zone, the main issues considered arise from the depth of mining relative to the SML of the sea. Where mining is below the SML, the issue is whether it is environmentally better to bring the extraction products to the surface vessel for processing (and waste discharge), or to process the extraction products as much as possible on the seabed. Responses to the issues need to be sitespecific, and dependent on adequate preoperational environmental impact and recovery prediction. For deep tailings disposal from a surface vessel, there are four important environmental unknowns: (1) the possible growth of "marine snow" (bacterial flocs) utilizing the enormous quantities of fine tailings particles (hundreds or thousands of metric tons per day) as nuclei for growth, (2) the possibility that local keystone plankton and nekton species may migrate diurnally down to and beyond the depth of deep discharge and hence be subjected to tailings impact at depth, (3) the burrow-up capability of deep benthos and their ability to survive high rates of tailings deposition, and (4) the pattern and rate of dispersion of a tailings density current through the deep water column from discharge point to seabed. Actions to obtain relevant information in general and site-specifically are suggested.     

Increased Particle Fluxes at the INDEX Site Attributable to Simulated Benthic Disturbance

Particle fluxes were measured 7 m above the sea bottom during the predisturbance, disturbance, and postdisturbance periods by using time series sediment traps attached to seven deep-sea moorings deployed in the INDEX experiment site in the Central Indian Basin. The predisturbance particle fluxes varied between 22.3 to 55.1 mg m -2 day -1 . Increased and variable particle fluxes were recorded by the sediment traps during the disturbance period. The increase observed was 0.5 to 4 times more than the background predisturbance fluxes. The increases in particle fluxes (~4 times) recorded by the sediment trap located in the southwestern direction (DMS-1) were the greatest, which could be the result of preferential movement of resuspended particles generated during the deep-sea benthic disturbance along the general current direction prevailing in this area during the experimental period. Also, the traps located closer to the disturbance area recorded greater fluxes than did the traps far away, across the Deep Sea Sediment Resuspension System path. This variability in recorded particle fluxes by the traps around the disturbance area clearly indicates that physical characteristics such as grain size and density of the resuspended particles produced during the disturbance had an important effect on particle movement. The postdisturbance measurements during ~5 days showed a reduction in particle fluxes of ~50%, indicating rapid particle settlement.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.     

Determination of In Situ Sediment Shear Strength from Advanced Piston Corer Pullout Forces

The advanced piston corer (APC) has been used by the Ocean Drilling Program since 1985 for recovering soft sediments from the ocean floor. The pullout force measured on extracting the core barrel from the sediment is shown to correlate with the average shear strength of the sediment core measured in the ship's laboratory. A simple rule of thumb is derived relating the shear strength of the sediment to the pullout force. Multiple APC holes at individual sites allow the consistency of the pullout measurements to be assessed. The effects of different operational procedures during APC coring are also explored. Although generally applicable, the correlation between pullout force and laboratory measurements of shear strength breaks down for some APC holes, possibly because of the disturbance of some sediment types during the APC coring process. A better understanding of the physical process of APC coring, and its effect on the properties of the sediment both inside and immediately outside the core barrel, would indicate what confidence can be put on the measurement of pullout force as a way of evaluating the in situ shear strength of deep sea sediments.     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

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.     

《Acta Oceanologica Sinica》Vol. 33(2014) contents

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