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1.
利用编码线粒体细胞色素氧化酶I(COI)的基因片段序列,对泰国近海有毒水母69个样本进行遗传多样性研究,并探讨该片段作为DNA条形码对泰国近海有毒水母类进行快速分类鉴定的可行性,以期为后续有毒水母的监测和预警、生物学和生态学等的研究提供技术支撑。基因碱基组成分析表明,立方水母COI序列GC含量为42.1%,明显高于钵水母(37.1%)和水螅水母(36.9%)。COI基因编码氨基酸的密码子第3位点GC含量(30.2%)显著低于第1,2位点(分别为47.4%,42.1%),且该位点碱基替换频率最高,转换/颠换比值为1.0,表明该位点碱基突变趋于饱和;但去除密码子第3位点,对系统进化树的构建无显著影响。根据COI序列计算3个纲水母的K2P(Kimura 2-parameter)遗传距离,得出种内遗传差异为0.000~0.151,均值为0.036,同纲种间遗传差异为0.167~0.321,均值为0.263,纲间遗传差异为0.246~0.385,均值为0.334。该COI基因片段能够快速有效区分这些有毒水母种类。研究表明,泰国沿岸水母多样性较高,所获69个样品可以分为13个种,包括5种钵水母、6种立方水母和2种水螅水母,其中Carukiidae科存在新属新种。立方水母的地理分布具有明显的区域特征,马来半岛东西两岸存在物种和遗传多样性差异,其产生原因还有待于进一步研究。 相似文献
2.
长江口及其邻近海域水螅水母纲新种和新记录记述 总被引：6，自引：2，他引：4
长江口及其邻近海域水螅水母纲有49种,隶属于26科,34属,其中有2个新种:瓣高手水母(Bougainvillia lamellata n.sp.)、单管玛拉水母(Malagazzia monocanalis n.sp.)和2种我国新记录:橙黄高手水母(Bougainvillia aurantiaca Bouillon,1980)、玫瑰太阳水母[Solmaris rhodolma(Brandt,1838)],此外,我国记载的束状高手水母[Bougainvillia ramosa(van Beneden,1844)]订正为鳞茎高手水母(B.muscus(Allman,1863)). 相似文献
3.
环境因子对海蜇生长发育影响的研究进展 总被引：1，自引：0，他引：1
<正>海蜇(Rhopilema esculenta Kishinouye)隶属于刺胞动物门(Cnidaria),钵水母纲(Scyphozoa),根口水母目(Rhizostomeae),根口水母科(Hizostomadae),海蜇属(Rhopilema)[1]。海蜇为进化比较保守的两胚层动物[2]。丁耕芜等[3]首次报告了海蜇的整个生活史。海蜇生活史具有刺胞动物门典型的世代交替特征,分为两个世代:水螅体世代和水母体世代。在水螅体世代整个过程中,海蜇螅状体于海底基质上营固着生活,以无性生殖 相似文献
4.
泰国近海习见有毒立方水母和钵水母的遗传分析 总被引：2，自引：0，他引：2
本研究利用线粒体16S rDNA和核基因18S rDNA片段,对泰国沿海常见的有毒水母进行遗传分析,并比较了2个基因片段作为通用分子标记,在研究水母类多个纲的遗传多样性中的应用。研究发现,泰国近海的有毒水母存在较高的遗传多样性,所获得的32个样品可以分为9个种,包括4种钵水母、4种立方水母和1种水螅水母。然而,完全确定各种的分类地位,还需要更多的形态、生活史等方面信息。两个基因片段均能明确区分各种类,但核基因18S序列比线粒体基因片段更为保守。根据16S基因片段序列计算水母种内和种间的K2P(Kimura 2-parameter)遗传距离,发现所研究的9个水母种类,种内遗传距离在0~0.050之间,其中94%的种内遗传距离小于0.040,同纲种间的遗传距离为0.204~0.474,其中91%的种间遗传距离大于0.250;而利用18S基因,种内距离在0~0.002之间,同纲种间距离为0.008~0.066(平均为0.038,SE=0.006)。16S的AT碱基含量明显高于核基因18S,且16S的碱基含量在不同纲之间有显著差异,进一步表明水母线粒体16S基因的突变率相对较高,适合研究水母较低分类阶元以及种下的遗传差异。 相似文献
5.
《中国海洋大学学报(自然科学版)》2016,(9)
为进一步丰富水螅水母的多样性记录,同时为海洋生物学和生物海洋学研究提供水母分类学资料,本文对2011年9月采自南海中西部水域的2个疑似水母新种进行了详细研究,通过显微观察、绘图和分类学特征分析,并与其它相似种类进行比较,确定其为2个新种,隶属于花水母亚纲(Anthomedusae Haeckel)、丝螅水母目(Filifera Kühn)、高手水母科(Bougainvillidae Lütken)、单肢水母属(Nubiella Bouillon,1980),将其分别命名为锥形单肢水母(N.conica Li,Huang et Liu.sp.nov.)和半球单肢水母(N.hemisphaerica Li,Lin et Chen,sp.nov.)。模式标本保存于中国海洋大学环境科学与工程学院。 相似文献
6.
九龙江口的水螅水母类、管水母类、钵水母类和栉水母类 总被引：5，自引：0，他引：5
有关九龙江口水母类的研究,早期有Vanhoffen(1913)在厦门港记载了2种水螅水母;徐锡藩(1928)在厦门港发现了1个新种;Stia(?)ny(1933)和金德祥(1936、1948)在厦门港记载了1种钵水母和2科管水母。解放后,先是丘书院(1954a—b、1957)在厦门港记载了19种水母,其中栉水母3种;接着,许振祖、金德祥(1962)在福建沿海水母类的调查研究一文中,又记载了厦门港的水母类12种;许振祖、张金标(1974)在厦门又记录了20种水母;丘书院(1962、1980)在厦门港又记载了2种栉水母;最近,张金标、吴玉清(1981)在厦门港的锺宅又发现了一个新属新种。以上所记录的种类共有62种。这些种类绝大部分是在厦门港采集的,而在九龙江口中,低盐区的鸡屿以东、海(?)、玉枕洲采集很少,仅报导6种。上述这些研究,为九龙江口水母类的分类打下良好的基础,也为今后生态系的进一步研究提供基本 相似文献
7.
厦门海域鱼类群落分类学多样性的研究 总被引：5，自引：2，他引：3
根据厦门海域鱼类种类组成历史资料和调查资料,系统整理了厦门海域的鱼类总名录和现有名录,并应用分类学等级多样性指数和分类差异变异指数分析了厦门海域鱼类群落分类学多样性的时空变化。结果表明:厦门海域有记录鱼类共649种;现有鱼类有331种,隶属2纲22目90科181属,其中软骨鱼纲共5目9科9属15种,辐鳍鱼纲共17目81科172属316种。厦门海域鱼类总名录的等级多样性指数Δ+和分类差异变异指数Λ+分别为79.267和220.96;现有鱼类群落分类多样性指数Δ+和分类差异指数Λ+分别为77.504和245.34。分类多样性指数Δ+在冬、春季较高,秋季次之,而夏季最低;而分类差异指数Λ+夏季较高,秋季次之,冬春季较低。秋季和冬季鱼类组成的相似度最高,其次为夏季,最后为春季。与历史总名录相比,厦门海域的现有鱼类群落分类学范围较小,生态幅变窄,群落稳定性较差。 相似文献
8.
广义上说,水母是多种生物的统称,包括水母、海葵、珊瑚、水螅等。水母在地球上出现的时间比恐龙还早,大约6.5亿万年前就存在了,不过现在它们仍然属于较低等的生物,目前地球上被称为"水母"的生物大约有200多种。在分类上有些属于水螅纲,有些属于钵水母纲,其生活史中,几乎所有种类都有两型,即水螅型和水母型,并有两型在有性生殖与无性生 相似文献
9.
10.
胶州湾水母类生态研究Ⅰ.种类组成与群落特征 总被引：11，自引：5，他引：6
根据2003年5月-2004年9月胶州湾浮游生物浅水Ⅰ型网中水母的调查资料,分析了胶州湾水母类的种类组成和群落特征.共记录水母34种,其中水螅水母类31种,管母类2种,钵水母类1种,属胶州湾首次报道的有3种;订正并列出了到目前为止的胶州湾水母种属目录,累计共60种,其中水螅水母类52种,管水母3种,钵水母4种,栉水母1种.分析其群落特征结果表明,全年共有9种优势种,各月份水母的优势种类不尽相同,薮枝螅水母和半球美螅水母为春季和夏季的主要优势种,五角水母为秋季的主要优势种,八斑芮氏水母为冬季的主要优势种;水母的总丰度在调查时期内有3个高峰,分别为2003年6、9月份、2004年3月份,3月份作为最高峰丰度高达120.42ind/m^3;总种类数以2003年5、6月份为最多,共14种;1年中,5-11月份的群落多样性指数较12-4月份高;2003年12月到2004年3月各月优势种到下个月的更替基本是完全的（更替率为100%）,其它月份优势种的更替或者部分更替（0〈更替率〈100%）,或者没有更替（更替率为0）.本文中作者对80年代以来水母类的优势种、总种数及总丰度的变化进行了讨论,总种数比90年代有所增加,但未达到1984、1985年的水平;水母的总丰度水平也较80、90年代要高.本文中作者把胶州湾水母生态类群分为近岸低盐生态类型和大洋暖水性生态类型. 相似文献
11.
Chandralata Raghukumar G. Sheelu P. A. Loka Bharathi Shanta Nair C. Mohandass 《Marine Georesources & Geotechnology》2001,19(1):1-16
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. 相似文献
12.
Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
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
13.
Derek V. Ellis 《Marine Georesources & Geotechnology》2001,19(1):51-63
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. 相似文献
14.
G. Parthiban 《Marine Georesources & Geotechnology》2000,18(3):223-235
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. 相似文献
15.
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
16.
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. 相似文献
17.
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. 相似文献
18.
Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
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
19.
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
20.