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1.
软海绵属海绵Halichondria sp.甾体类化学成分研究   总被引:1,自引:0,他引:1       下载免费PDF全文
为了系统研究中国南海软海绵属海绵 Halichondria sp.的化学成分,文章采用多种色谱方法分离纯化,从其氯仿萃取部位中分离得到了9个甾体类化合物,依据理化性质、波谱数据和文献对照的方法鉴定其结构.其结构分别鉴定为:1)3β-羟基-5,8,22-麦角甾三烯-7-酮;2)3β,5α-二羟基-7,22-麦角甾二烯-6-酮;3)3β,5α,6β-胆甾三醇;4)3β,5α,9α-三羟基-7,22-胆甾二烯-6-酮;5)3β-羟基-5-胆甾烯-6-酮;6)5α,8α-环二氧-6,22-麦角甾二烯-3β-醇;7)5α,8α-环二氧-6-胆甾烯-3β-醇;8)7,22-麦角甾二烯-3β,5α,3β-三醇;9)胆甾醇.本研究结果不仅丰富了软海绵属海绵的化学成分研究,而且将为软海绵属海绵的化学分类及甾体类化合物的进一步研究提供有利的理论依据.  相似文献   

2.
应用色谱-质谱(GC-MS)方法分别鉴定了从广西海涠洲岛水域和海南省陵水县水域采集的莳萝曲网海绵Sigmadocia cymiformis的甾醇类化合物,涠洲岛水域的莳萝曲网海绵所含的旮醇类化合物主要是:胆甾-4,6-二烯3β-醇(1),27-降麦角甾5,22-二烯-3β-醇,(2),胆甾醇(3),(24S)-麦角甾5,22-二烯3β-醇(40,麦角甾5-烯C-3β-醇(5),麦角甾-2,22-二烯-3β-醇(6),豆甾醇(7),β-谷甾醇(8),麦角甾-4,24(28)-二烯-3-酮(9),柳珊瑚甾醇(10);而陵水县水域的莳萝曲网海绵所含甾醇类化合物主要是:(3),(4),(5),(6),(8),胆甾-2,55-二烯-3β-醇(11),胆旨-3,5-二烯-7-酮(12),这是莳萝曲网海绵中甾醇类化合物组成的首次报道。  相似文献   

3.
滨海湿地耐盐植物二色补血草化学成分研究   总被引:5,自引:0,他引:5  
采用硅胶柱层析,Sephedex-LH-20凝胶层析,HPLC等方法,从滨海湿地耐盐植物二色补血草中分离得到了10个单体化合物。运用NMR,MS以及与文献对照,鉴定它们的结构分别为豆甾烷-3,6-二酮(1),豆甾-4烯-3,6-二酮(2),6β-羟基-豆甾-4-烯-3-酮(3),5α,8α-环二氧-24-甲基-胆-甾6,22E-二烯-3β-醇(4),5,α8α-环二氧-24-甲基-胆甾-6,9,22E-三烯-3β-醇(5),麦角-甾4,6,8(14),22E?四烯-3-酮(6),植醇(7),正十六烷酸(8),亚油酸(9),亚油酸单甘油酯(10)。化合物1~7和10为首次从该植物中分离得到。  相似文献   

4.
本实验采用群体感应抑制(quorum sensing inhibitory, QSI)活性导向法, 对分离自山东威海近海底泥的真菌WH7-2开展代谢产物研究。综合菌落形态和转录间隔区 (Internal Transcribed Spacer, ITS)全序列分析, 菌株WH7-2鉴定为腐皮镰刀菌Fusarium solani。综合运用多种色谱方法, 从该真菌大米发酵产物的活性部位中分离得到11个化合物。分别鉴定为 (2E, 5E)-3, 5, 7-三甲基-2, 5-辛二烯酸 (1)、不饱和脂肪酸酯混合物 (2—4)、镰红菌素-3-甲醚 (5)、脱水镰红菌素 (6)、(22E)-5α, 8α-过氧化麦角甾-6, 22-二烯-3β-醇(7)、(22E)-5α, 8α-过氧化麦角甾-6, 9 (11), 22-三烯-3β-醇(8)、3β-羟基-胆甾-5-烯-7-酮 (9)、6β-羟基-胆甾-4-烯-3-酮 (10)和(22E)-胆甾-5, 22-二烯-3β-醇 (11)。其中不饱和脂肪酸酯混合物(2—4)具有QSI活性, 其他化合物无QSI活性。除5和6外, 其他化合物均为首次从腐皮镰刀菌F. solani中发现。  相似文献   

5.
对采自海南文昌红树林根际土壤样品中分离到的真菌Penicillium sp. MA-37的次生代谢产物的化学成分进行了研究.利用硅胶柱层析、葡聚糖凝胶Sephadex LH-20柱层析、制备薄层层析以及重结晶等分离方法并通过现代波谱技术共分离、鉴定了8个天然产物,分别为:氮-(2-甲氧基-4-羟基苯)-丙酰胺酸(1),氮-(2,4-二甲氧基苯)-丙酰胺酸(2),氮-(2,4-二甲氧基苯)-丙酰胺酸甲酯(3),(22E,24R)-麦角甾-5,7,22-三烯-3β-醇(4),(22E,24R)-麦角甾-4,6,8(14),22-四烯-3-酮(5),(22E,24R)-5α,8α-环二氧麦角甾-6,22-双烯-3β-醇(6), asperamide B (7), cis-4-hydroxy-6-deoxyscytalone (8);其中化合物1为新化合物,化合物2和3为新天然产物.  相似文献   

6.
海洋红藻多管藻内生真菌EN-22 的化学成分研究   总被引:4,自引:0,他引:4       下载免费PDF全文
对采自广西涠州岛近海多管藻(Poiysiphonia urceolata)分离到的一株内生真菌EN-22的次生代谢产物的化学成分进行了研究.利用正相硅胶柱层析、葡聚糖凝胶Sephadex LH-20柱层析、制备薄层层析(PTLC)以及重结晶等分离手段从该菌发酵液中分离得到15个化合物,通过一维、二维核磁共振技术、质谱技术等鉴定了所有化合物的结构,分别为:4-(4-喹啉)-4-羟基-2-丁酮(1),3-羟基-3-(2-氧丙基)吲哚-2-酮(2),3-吲哚乙醇(3),3-吲哚甲酸(4),2-羟基-3-吲哚丙酸(5),2-酮-3-吲哚乙醇(6),3,3-二吲哚-2-羟基-丙醇(7),β-咔啉(8),尿嘧啶(9),环-(S-脯氨酸-S-异亮氨酸)(10),(22E,24R)-3β,5α,9α-三羟基麦角甾-7,22-二烯-6-酮(11),(22E,24R)-5α,6α-环氧麦角甾-8,22-二烯-3β,7α-二醇(12),5α,6α-环氧-24(R)-甲基胆甾-7,22-二烯-3β-醇(13),胡萝卜苷(14),过氧化麦角甾醇(15);其中化合物1和2为新天然产物,并首次报道化合物1的碳谱数据.  相似文献   

7.
运用^1HNMR,^13CNMR,MS,IR等波谱方法和GC-MS及计算机数据库检索技术从厚节仙掌藻Halimeda incrassata的乙醇提取物中分离鉴定出十六烷酸,十八烷酸,24-甲基-胆甾-5-烯-3β-醇,24-乙基-胆甾-5,22-烯-3β-醇,胆甾-5,24-二烯-3β-醇,胆甾-7-烯-3β-醇,胆甾-5-烯-3β醇和胆甾烷-3β-醇。  相似文献   

8.
综合运用正相和反相硅胶柱层析、Sephadex LH-20凝胶柱层析以及制备HPLC等分离方法,从1种中国南海海绵Xestospongia testudinaria中追踪分离抗肿瘤活性次级代谢产物。从95%乙醇提取物中分离获得8个单体化合物,通过NMR,MS等波谱技术鉴定其结构分别为:E-18,18-二溴-9,17-二烯-5,7-二炔硬脂酸甲酯(1),E-18,18-二溴-9,17-二烯-5,7-二炔硬脂酸乙酯(2),麦角甾-5,7,22-三烯-3-醇(3),麦角甾-4,6,8(14),22-四烯-3-酮(4),胆甾-4-烯-3-酮(5),3-吲哚醛(6),3-吲哚酸(7)和5-吲哚醛(8)。其中,化合物2-5和8为首次从该属海绵中分离得到。化合物1对肿瘤细胞株HCT116和A549显示较强的抑制活性。  相似文献   

9.
从南海圆裂短足软珊瑚(Cladiella krempfi)中分离出12个甾体化合物,分别鉴定为:1,2-[1',3',4']oxodithiin-pregna-20-en-3-one(1);19-nor-4-methylpregna-1,3,5(10),20-tetraen-1-ol(2);pregna-1-en-3-one-20-ol(3);pregna-1,7-dien-20-ol-3-one(4);pregna-5,20-dien-3-O-α-fucopyranoside(5);pregna-20-en-3-O-α-fu-copyranoiside(6);孕甾-1,20-二烯-3-酮(7);孕甾-1,4,20-三烯-3-酮(8);24-甲基-5α-胆甾-7,22-二烯-3β,5,6β-三醇(9);26-甲基-24-亚甲基胆甾-5烯-3β-醇(10);胆甾-5-烯-3β醇(11);β-谷甾醇(12).化合物1~6系首次从Cladiella属软珊瑚中获得的孕甾类化合物.对所获得化合物的生源途径进行了初步讨论.  相似文献   

10.
鸭毛藻内生真菌Hypocreales sp.的化学成分研究   总被引:2,自引:0,他引:2       下载免费PDF全文
从采自大连近海的红藻鸭毛藻(Symphyocladia latiuscula)中分离到一株肉座菌目真菌(Hypocreales sp.),对其发酵代谢产物的化学成分进行了研究。利用正相硅胶柱层析、葡聚糖凝胶Sephadex LH-20柱层析、制备薄层层析(PTLC)以及重结晶等分离手段,并通过一维、二维核磁共振技术、质谱技术等从该菌发酵液中分离鉴定了10个化舍物:双酚A(1);邻羟基苯甲酸(2);吲哚甲酸(3);吲哚乙酸(4);N-乙酰色胺(5);(22E,24R)-麦角甾-7,9,22三烯-3β-醇(6);过氧化麦角甾醇(7);(22E,24R)-5α,6α-环氧麦角甾-8,22-二烯-3β,7α-二醇(8);(22E,24R)-麦角甾-7,22-二烯-6β-甲氧基-3β,5α-二醇(9);啤酒甾醇(10)。这些化合物均为首次从该菌中分离得到,其中化合物1为首次作为天然产物分离得到。  相似文献   

11.
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.
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。  相似文献   

13.
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   

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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   

17.
A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria ( 〉 99% ), but also between polar marine bacteria and bacteria from other aquatic environments ( ≥ 98.8% ), including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.  相似文献   

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《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   

20.
Sediment properties, such as water content and density, have been used to estimate the dry and wet weights, as well as the volume of sediment recovered and discharged, during benthic impact experiments conducted in the Pacific and Indian Oceans. The estimates show that the weights of dry (355-1332 t) and wet sediment (1651-4888 t) recovered during the experiments, are not only a function of the total duration and distance covered during the experiment, but also depend on water content and density of the sediment. Estimation of dry sediment and its volumetric ratio in the discharge, are key parameters for calculating the discharged volume. The estimated volume of wet sediment recovered (1427-4049 m 3 ) as well as discharged (2693-6951 m 3 ) during the experiments, provide important inputs to evaluate the sediment resettlement and migration. Using these estimates, the average depth of excavation on the seafloor, can also been calculated. However, the stages of sediment recovery and discharge are expressed differently in some of the experiments. In order to standardize these, different stages have been identified, and definitions of certain terms have been suggested, for use in the future. The methods of calculating different properties, as well as weight and volume of discharged sediment are described in the paper for use in other applications concerning deep-sea discharges.  相似文献   

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