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1.
核酸探针原位杂交检测白斑综合症病毒的组织特异性 总被引：3，自引：0，他引：3
从白斑综合症病毒（ｗｈｉｔｅ ｓｐｏｔ ｓｙｎｄｒｏｍｅ ｖｉｒｕｓ,简称ＷＳＳＶ）部发基因组库中得到核酸探针,采用原位杂交检测方法检测对虾甲壳下表皮、胃、后肠、鳃、触角腺的上皮细胞、淋巴器官的基质细胞、肌细胞、心肌细胞及结缔组织细胞,原位杂交结果均为阳性。对虾甲壳下表皮的上皮细胞、胃的上皮细胞对病毒较其它部位敏感,感染程度高;中肠上皮细胞、肝胰腺上皮细胞、淋巴器官内皮细胞未发现感染病毒,原位杂 相似文献
2.
核酸探针原位杂交检测白斑综合症病毒的组织特异性 总被引：2，自引：0，他引：2
从白斑综合症病毒 (whitespotsyndromevirus ,简称WSSV)部分基因组文库中得到核酸探针 ,采用原位杂交检测方法检测对虾甲壳下表皮、胃、后肠、鳃、触角腺的上皮细胞、淋巴器官的基质细胞、肌细胞、心肌细胞及结缔组织细胞 ,原位杂交结果均为阳性。对虾甲壳下表皮的上皮细胞、胃的上皮细胞对病毒较其它部位敏感 ,感染程度高 ;中肠上皮细胞、肝胰腺上皮细胞、淋巴器官内皮细胞未发现感染病毒 ,原位杂交用于WSSV检测 ,比组织切片HE染色更准确、更敏感。在同一组织的同一部位 ,原位杂交所得到的阳性细胞个数比HE多。探针大小不同 ,敏感性也有变化。短的探针 41 3bp敏感性较高 ,长的探针敏感性降低。 相似文献
3.
本文对东方对虾消化道及肝胰脏进行大体解剖和组织学观察,并将其结构与功能同其它主要十足动物作比较。 前肠和后肠内壁有几丁质层覆盖,中肠则没有。食道壁向四个角落内褶,在其表皮层之下的结缔组织中充满皮肤腺,环肌层连续,纵肌成束分散排列:胃的组织学结构除没有皮肤腺分布外,大体与食道相似。中肠从胸部延伸到第六腹节前区,约占消化道总长的60％,其上皮是一层柱状细胞,环肌层薄,纵肌成束分散排列;中肠前,后盲囊分别从中肠的前端和后端发出。后肠是一短管,内壁突出四个大的垫状隆脊,肛门开口于尾节腹面,和食道一样后肠壁分布大量皮肤腺:后肠上皮由单层柱状细胞组成,环肌层连续,纵肌在后肠前段成束分散排列于环肌之下,在后段则在环肌层之上。肝胰脏由许多分支肝小管构成,肝小管内壁为单层柱状上皮,中央为管腔:肝管细胞分为分泌细胞、吸收细胞、纤维细胞和原始细胞四种。原始细胞是一种未分化的细胞,分布于肝小管末端。 相似文献
4.
东方对虾消化系统解剖和组织学的研究 总被引：13，自引：0，他引：13
本文对东方对虾消化道及肝胰脏进行大体解剖和组织学观察．并将其结构与功能同其它主要十足动物作比较。前肠和后肠内壁有几丁质层覆盖，中肠则没有，食道壁向四个角落内褶．在其表皮层之下的结缔组织中充满皮肤腺．环肌层连续．纵肌成束分散排列；胃的组织学结构除没有皮肤腺分布外．大体与食道相似。中肠从胸部延伸到第六腹节前区．约占消化道总长的60％．其上皮是一层柱状细胞．环肌层薄．纵肌成束分散排列：中肠前、后盲囊分别从中肠的前端和后端发出，后肠是一短管．内壁突出四个大的垫状隆脊，肛门开口于尾节腹面．和食道一样后肠壁分布大量皮肤腺：后肠上皮由单层柱状细胞组成，环肌层连续，纵肌在后肠前段成束分散排列于环肌之下，在后段则在环肌层之上。肝胰脏由许多分支肝小管构成．肝小管内壁为单层柱状上皮．中央为管腔；肝管细胞分为分泌细胞．吸收细胞、纤维细胞和原始细胞四种。原始细胞是一种未分化的细胞．分布于肝小管末端。 相似文献
5.
以凡纳滨对虾（Litopenaeus vannamei）为研究对象，运用Western—blotting和免疫组织化学等现代免疫学方法，对对虾中的类Ig（immunoglobulin，免疫球蛋白）蛋白进行定性和定位研究。结果发现，虾血清中有两种分子质量约为70ku和62ku的蛋白可与抗人Ig发生特异性的结合。同时，虾血细胞——无颗粒细胞的外膜及虾类淋巴器、肝胰脏、心脏、胃和肠等5种组织器官的石蜡切片与抗人Ig反应呈不同程度的阳性，其中类淋巴器和肝胰脏显色较深。提示，虾体内确实存在能与抗人Ig发生特异性结合的类Ig蛋白，其不仅存在于虾血清中，还存在于无颗粒细胞、类淋巴器和肝胰脏等组织中，为对虾的免疫系统的研究和疾病的防治奠定基础。 相似文献
6.
造血激素（astakine）是一种具有促进造血组织细胞分化和增殖作用的甲壳动物细胞因子,参与甲壳动物的造血活动,对于只依赖于非特异性免疫的甲壳动物抗感染能力有重要的意义。本实验室前期成功克隆凡纳滨对虾造血激素（LvAST）的基因Lvast。为了进一步了解其功能,本文通过实时荧光定量PCR技术检测了Lvast表达的组织分布,同时还用Dlight标记抗LvAST抗体进行了LvAST在对虾细胞和组织中的免疫荧光定位分析。荧光定量PCR测定结果说明,Lvast主要在肝胰腺、鳃和肌肉中大量表达,而淋巴器官和血淋巴细胞中表达量较低;免疫荧光结果显示,LvAST可同时存在于血淋巴细胞内和血淋巴细胞膜表面,不同的血淋巴细胞表面的LvAST分布呈现出明显差异,可能具有重要的血细胞分类意义。LvAST的蛋白在肝胰腺、鳃、肌肉、淋巴器官等组织中均有分布,并且肝胰腺组织中分布较多,淋巴器官组织中分布较少。 相似文献
7.
造血激素(astakine)是一种具有促进造血组织细胞分化和增殖作用的甲壳动物细胞因子,参与甲壳动物的造血活动,对于只依赖于非特异性免疫的甲壳动物抗感染能力有重要的意义。本实验室前期成功克隆凡纳滨对虾造血激素(LvAST)的基因Lvast。为了进一步了解其功能,本文通过实时荧光定量PCR技术检测了Lvast表达的组织分布,同时还用Dlight标记抗LvAST抗体进行了LvAST在对虾细胞和组织中的免疫荧光定位分析。荧光定量PCR测定结果说明,Lvast主要在肝胰腺、鳃和肌肉中大量表达,而淋巴器官和血淋巴细胞中表达量较低;免疫荧光结果显示,LvAST可同时存在于血淋巴细胞内和血淋巴细胞膜表面,不同的血淋巴细胞表面的LvAST分布呈现出明显差异,可能具有重要的血细胞分类意义。LvAST蛋白在肝胰腺、鳃、肌肉、淋巴器官等组织中均有分布,并且肝胰腺组织中分布较多,淋巴器官组织中分布较少。 相似文献
8.
卵黄蛋白原和血蓝蛋白是凡纳滨对虾(Litopenaeusvannamei)卵巢和/或肝胰腺合成的重要蛋白。利用半定量和荧光定量PCR技术分别检测了亲虾卵巢不同发育期卵黄蛋白原和血蓝蛋白mRNA在卵巢和肝胰腺的相对表达量。结果显示,卵黄蛋白原mRNA在卵巢和肝胰腺中均有表达,其相对表达量随着卵巢发育持续增加,在第五期达到最高,在恢复期迅速下降。根据卵巢和肝胰腺质量的综合计算,凡纳滨对虾的卵黄蛋白中,卵巢的贡献率占主导地位,约占80%,而肝胰腺仅为卵巢的四分之一。血蓝蛋白mRNA主要在肝胰腺中表达,随着卵巢的发育,表达量呈增加趋势,至第三期达到高峰,其后稍有下降,但仍然维持在较高水平,在第六期恢复到初始水平。血蓝蛋白是否直接或间接参与了卵黄发生和卵巢发育有待进一步探讨研究。 相似文献
9.
对虾一种无包涵体杆状病毒病原的PCR检测 总被引：4，自引：0，他引：4
为建立对虾无包涵体杆状病毒的快速诊断技术,应用PCR技术分别对暴发性流行病发生前、流行中和发病后的对虾样品进行了检测.根据已克隆的对虾杆状病毒部分基因组序列而设计的引物能特异性地扩增出靶DNA片段,最低可以检测1pg的病素DNA.由典型发病症状对虾的胃、腮、肝胰腺、中肠、游泳足、肌内和心脏等器官和组织中成功地检测到病毒.不同组织和器官经扩增得到的信号强弱不同:病虾的胃扩增得到的信号最强,中肠、肌肉、心脏和游泳足次之,腮和肝胰腺信号最弱,说明病毒在不同组织和器官中数量及感染程度不同.在对虾发病前及发病后,用二次PCR还能检测表面不发病呈隐性感染状态的对虾携带的病毒;而对野生健康虾的检测结果为阴性.研究表明,PCR是检测对虾暴发性流行病快速、灵敏而准确的方法,对病毒病的早期诊断、防治和高健康对虾品种的选育具有指导意义. 相似文献
10.
实验室条件下测定盐度突变对凡纳滨对虾(Litopenaeus vannamei)血淋巴渗透压、血蓝蛋白、血糖、己糖激酶(HK)以及丙酮酸激酶(PK)活力的影响。以蜕皮间期对虾为实验材料(初始湿体重为(2.485±0.303)g),设盐度30为对照组,4个不同的盐度突变幅度(为2、4、6、8)为处理组(用S2、S4、S6和S8表示),于降低盐度和恢复盐度至30的不同时间点采样,实验持续7d。结果表明:(1)凡纳滨对虾血淋巴渗透压会随盐度变化而变化,S4组对虾血淋巴含量在整个实验过程中处于较低水平;(2)随着盐度突变幅度的增加,血蓝蛋白含量与对照组呈现显著性差异(P<0.05)的采样点增多;(3)S4组对虾血糖含量整个实验过程中一直处于较低水平,而S6、S8组对虾血糖含量相对较高;(4)整个实验过程中,S4组对虾肝胰脏中HK活力处于较低水平,而S6与S8组对虾肝胰脏中HK活力处于较高水平;(5)S2、S4组对虾肝胰脏中PK活力与对照组没有显著性差异(P<0.05),而S6和S8组对虾肝胰脏PK活力在盐度突变后与对照组肝胰脏PK活力表现出显著性差异(P<0.05)。 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.
Hoi-Soo Jung Kap-Sik Jeong Yong-Shik Chu Sung-Hyun Park Ki-Hyune Kim 《Marine Georesources & Geotechnology》2001,19(3):181-195
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.
Shigehisa Nakamura 《Marine Geodesy》2001,24(1):27-33
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.
Andrzej Chybicki 《Marine Geodesy》2018,41(1):1-23
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.
N. H. Khadge 《Marine Georesources & Geotechnology》2000,18(3):251-258
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.
J. N. Pattan Ch. M. Rao A. A. Migdisov S. Colley N. C. Higgs L. Demidenko 《Marine Georesources & Geotechnology》2001,19(3):155-165
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.
Lori E. Fenstermacher Gregory B. Crawford Jeffry C. Borgeld Tristan Britt Douglas A. George Meredith A. Klein Neal W. Driscoll Larry A. Mayer 《Marine Georesources & Geotechnology》2001,19(2):135-145
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