共查询到20条相似文献，搜索用时 281 毫秒
1.
鱿鱼皮明胶水解物降血压活性研究 总被引：4，自引：0，他引：4
探讨了秘鲁鱿鱼(Dosidicus eschrichitii Steenstrup)皮明胶水解物对血管紧张素转化酶(ACE)的抑制活性以及其降血压作用。采用超滤法对明胶水解液进行初步分离;采用比色法检测不同分子量范围鱿鱼皮明胶水解物组分的ACE抑制活性;采用两肾一夹型建立肾血管性高血压大鼠(RHR)模型,经口服预防给药30 d后,测定大鼠血压和血液中血管紧张素Ⅱ(AngⅡ)含量。试验结果表明鱿鱼皮明胶水解物体外均能明显抑制ACE的活性,其中UC-2和UF-2的半抑制浓度(IC50)分别为0.71和0.79 mg/mL。UF-2组分经口服预防给药可显著降低肾血管性高血压大鼠的动脉血压和大鼠血浆中的AngⅡ水平,具有较好的降血压效果。 相似文献
2.
采用DEAE-Toyopearl阴离子交换树脂、Bio-Gel P-100分子筛层析、Lactosyl-Sepharose4B亲和层析和Sephadex 75分子筛层析技术从日本海的海洋无脊椎动物磷沙蚕(Chaetopterus variopedatus)中分离出2种凝集素,通过体外细胞活性和酶活性实验观察它们的生物活性。结果表明,从海洋无脊椎动物磷沙蚕中分离出一种β-半乳糖特异性凝集素(CVL)和一种具有血凝活性,但不被经测试的单糖和糖蛋白所抑制的相对分子质量为30 000的蛋白质(CVL-1)。β-半乳糖特异性凝集素(CVL)具有体外抑制NB4白血病细胞株的活性和抑制小鼠脾细胞的活性,IC50分别为7.87 mg/L和22 mg/L。同时,另一种蛋白质(CVL-1)具有β-葡萄糖苷酶活性。 相似文献
3.
六种大型藻浸提液对中肋骨条藻的抑制及活性成分分离 总被引：1，自引：0，他引：1
为比较大型藻抑制赤潮藻的能力,研究了孔石莼、羊栖菜、长浒苔、马尾藻、蜈蚣藻和裙带菜的干粉末海水浸提液对中肋骨条藻的化感抑制作用并从长浒苔中分离出具有强抑制作用的组分.分析6种大型藻浸提液对中肋骨条藻的生长抑制率(Inhibitory rate,IR％)和120 h的半效应浓度(Effect concentration,EC50,120h)发现,孔石莼、羊柄菜、长浒苔、马尾藻和蜈蚣藻的浸提液在浓度达到2.4 g/L时可在实验周期内使中肋骨条藻全部致死,抑制率达到100％,全部致死所需时间分别为96、120、96、144和144 h,当浓度达到4.8 g/L时,6种大型藻均可全部杀死中肋骨条藻,6种大型藻对中肋骨条藻的EC50、120h分别为1.0、1.0、1.1、1.4、1.5和4.7 g/L.从长浒苔浸提液中分离的乙酸乙酯萃取组分具有强抑藻效果,受试条件下,其EC50值为0.08 mg/L.乙酸乙酯相气相色谱-质谱分析表明,组分至少包含14种物质,其中9-十八炔和邻苯二甲酸二异丁酯是含量最大的2种物质,各物质的抑藻活性尚需进一步研究.长浒苔具有很强的抑藻效果,具有应用于赤潮藻控制的潜力,研究结果为分离鉴定抑制中肋骨条藻的化感物质奠定了基础. 相似文献
4.
岩藻聚糖硫酸酯低聚糖的制备及其抗氧化活性研究 总被引：7，自引：0，他引：7
探讨H2O2降解岩藻聚糖硫酸酯的条件及其产物的抗氧化活性。采用Cu2 -H2O2体系降解原料Fucoidan,结果发现反应时间越长得到的高分子量的组分越少,而低分子量的低聚糖产量增加;H2O2浓度增高,水解所得主要组分的分子量明显减小;温度升高,水解速度明显加快;产物的硫酸根含量随反应温度和H2O2浓度的降低而增加。用Pyrogallol—Luminol系统对水解产物的抗氧化活性进行了研究,发现硫酸根含量低的Fucoidan水解产物除O2.-的活性较好,其中15%H2O2降解得<5KD的低聚糖清除O2.-的活性明显高于肌肽(IC50为0.65mg/mL),IC50为0.17mg/mL。 相似文献
5.
为比较大型藻抑制赤潮藻的能力,研究了孔石莼、羊栖菜、长浒苔、马尾藻、蜈蚣藻和裙带菜的干粉末海水浸提液对中肋骨条藻的化感抑制作用并从长浒苔中分离出具有强抑制作用的组分。分析6种大型藻浸提液对中肋骨条藻的生长抑制率(Inhibitory rate,IR%)和120 h的半效应浓度(Effect concentration,EC50,120 h)发现,孔石莼、羊栖菜、长浒苔、马尾藻和蜈蚣藻的浸提液在浓度达到2.4 g/L时可在实验周期内使中肋骨条藻全部致死,抑制率达到100%,全部致死所需时间分别为96、120、96、144和144 h,当浓度达到4.8 g/L时,6种大型藻均可全部杀死中肋骨条藻,6种大型藻对中肋骨条藻的EC50,120 h分别为1.0、1.0、1.1、1.4、1.5和4.7 g/L。从长浒苔浸提液中分离的乙酸乙酯萃取组分具有强抑藻效果,受试条件下,其EC50值为0.08 mg/L。乙酸乙酯相气相色谱-质谱分析表明,组分至少包含14种物质,其中9-十八炔和邻苯二甲酸二异丁酯是含量最大的2种物质,各物质的抑藻活性尚需进一步研究。长浒苔具有很强的抑藻效果,具有应用于赤潮藻控制的潜力,研究结果为分离鉴定抑制中肋骨条藻的化感物质奠定了基础。 相似文献
6.
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%。 相似文献
7.
岩藻聚糖硫酸酯体外抗氧化特性的研究 总被引：2，自引：2，他引：0
采用化学发光分析法研究岩藻聚糖硫酸酯清除超氧阴离子自由基 (O· -2 )及羟基自由基(· OH)的作用 ,并以高效液相色谱法研究对卵磷脂 (PC)过氧化的抑制能力。结果显示 :(1)三种岩藻聚糖硫酸酯组分均有清除活性氧自由基的能力 ,但清除超氧阴离子自由基的能力高于清除羟基自由基的能力。其中糖醛酸含量高和硫酸酯含量低的组分 清除自由基的能力最强 ,它对 O· -2 的IC50 为 0 .0 4 4 mg/m L,对· OH的 IC50 为 0 .0 6 2 mg/m L。 (2 )岩藻聚糖硫酯具有抑制 PC过氧化的能力。岩藻聚糖硫酸酯组分受活性氧损伤后 ,它们的抗氧化能力均降低。研究表明 ,岩藻聚糖硫酸酯具有较强的体外抗氧化的功能。 相似文献
8.
海洋褐藻羊栖菜(Sargassum fusiforme)中马尾藻甾醇、岩藻甾醇的分类纯化及抗菌、抗氧化活性研究 总被引：1，自引：0，他引：1
本文评价海洋褐藻羊栖菜(Sargassum fusiforme)中分离纯化的总甾醇、马尾藻甾醇(Saringosterol)和岩藻甾醇(Fucosterol)抗菌和抗氧化活性。马尾藻甾醇和岩藻甾醇化合物采用红外光谱、核磁共振光谱和高分辨质谱确定其结构。实验结果显示,总甾醇含量在30、60和80mg/m L对金黄色葡萄球菌(Staphylococcus aureus)和变形链球菌(S.mutans)具有抑制作用。马尾藻甾醇和岩藻甾醇对金黄色葡萄球菌和变形链球菌具有高活性,最小抑制浓度范围为4—32mg/m L。总甾醇还显示出对大肠杆菌(Escherichia coli)菌株1924和1356的抗菌作用。而马尾藻甾醇和岩藻甾醇在4—32mg/m L浓度范围内体外对大肠杆菌的抗菌作用不明显。马尾藻甾醇和岩藻甾醇对耐药性革兰氏阳性临床分离菌株具有显著的抑菌活性。另外,药理实验结果显示,总甾醇、马尾藻甾醇和岩藻甾醇的抗氧化活性与它们清除DPPH、ABTS、超氧化物和羟基自由基的能力有关。 相似文献
9.
紫球藻胞外多糖抗氧化和免疫调节活性的研究 总被引：1，自引：0，他引：1
采用密闭微波法降解紫球藻胞外多糖。通过测定多糖对羟自由基OH·、超氧阴离子O2-·和二苯代苦味酰基自由基DPPH·的清除效果及对小鼠单核-巨噬细胞RAW264.7和淋巴细胞的增殖效果,考察低分子量紫球藻多糖的体外抗氧化活性和免疫调节活性。结果表明,在一定的浓度范围内,降解后的紫球藻多糖对OH·、O2-·和DPPH·的清除能力与浓度呈正相关性,它们的半抑制率IC50分别为0.619,0.114和0.015mg/mL,表明紫球藻胞外多糖具有体外抗氧化活性。溶液浓度在50～200μg/mL的多糖都表现出体外免疫促进作用,与对照组相比,100μg/mL的多糖对巨噬细胞RAW264.7的促进作用最大,其增值指数为1.72。200μg/mL的多糖对脾淋巴细胞的增值指数为2.11。 相似文献
10.
重金属镉对斜生栅藻光合作用的影响 总被引：1，自引：0，他引：1
本文研究了斜生栅藻(Scenedesmus obliquus)对重金属镉(Cd)的吸附情况及不同浓度的镉处理和恢复处理下斜生栅藻的光合活性。研究表明:斜生栅藻对镉有高达97%的吸附率,Cd2+对斜生栅藻的生长半抑制浓度(IC50-96h)为119.04μmol/L。浓度高于50μmol/L的Cd2+不仅会抑制叶绿素a的合成,还会明显抑制斜生栅藻的光合活性,并且这种抑制作用对于光系统Ⅱ更显著。添加新鲜培养基的处理方式,不仅不能恢复其光合活性,反而导致其实际光合量子产量和最大光合量子产量几乎为零。而浓度为1—10μmol/L的Cd2+对斜生栅藻的损伤并不大,尚能保持较高的光合活性。因此,我们初步认为斜生栅藻作为治理镉污染水体的吸附材料有着良好的发展前景。 相似文献
11.
12.
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. 相似文献
13.
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. 相似文献
14.
15.
16.
17.
P.N. Froelich L.W. Kaul J.T. Byrd M.O. Andreae K.K. Roe 《Estuarine, Coastal and Shelf Science》1985,20(3):239-264
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 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. 相似文献
18.
E. Wolanski P. Colin J. Naithani E. Deleersnijder Y. Golbuu 《Estuarine, Coastal and Shelf Science》2004,60(4):705-716
Three years of temperature data along two transects extending to 90 m depth, at Palau, Micronesia, show twice-a-day thermocline vertical displacements of commonly 50–100 m, and on one occasion 270 m. The internal wave occurred at a number of frequencies. There were a number of spectral peaks at diurnal and semi-diurnal frequencies, as well as intermediate and sub-inertial frequencies, less so at the inertial frequency. At Palau the waves generally did not travel around the island because there was no coherence between internal waves on either side of the island. The internal waves at a site 30 km offshore were out-of-phase with those on the island slopes, suggesting that the waves were generated on the island slope and then radiated away. Palau Island was thus a source of internal wave energy for the surrounding ocean. A numerical model suggests that the tidal and low-frequency currents flowing around the island form internal waves with maximum wave amplitude on the island slope and that these waves radiate away from the island. The model also suggests that the headland at the southern tip of Palau prevents the internal waves to rotate around the island. The large temperature fluctuations (commonly daily fluctuations ≈10 °C, peaking at 20 °C) appear responsible for generating a thermal stress responsible for a biologically depauperate biological community on the island slopes at depths between 60 and 120 m depth. 相似文献
19.
20.
Klaus Kremling 《Marine Chemistry》1983,13(2):87-108
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 O2H2S 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. 相似文献