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1.
近年来白色霞水母(Cyaneanozakii)在我国近海出现数量波动,在其暴发年份严重影响了暴发区域的社会、经济和生态。本文通过观察不同饵料密度下白色霞水母触手丝的长度变化、游动状态来研究其摄食行为,同时对白色霞水母消化时间进行研究,结果表明:饵料密度较低时,霞水母触手丝完全伸展;密度过量时(500ind./L),周围饵料较充足,触手丝处于收缩状态;饵料密度对霞水母游动状态无显著影响,表明霞水母在水体中通过不断调整触手丝伸长与收缩来对周围饵料进行感知,达到一种高效的摄食状态,而非调整其游动状态。饵料种类、大小对霞水母消化时间具有显著影响:温度为18.5°C环境下,胶质类生物(水螅水母和海月水母碟状体)在霞水母胃中平均存留时间为(0.8±0.2)h,平均比大小无差异的桡足类短2.3h,比鱼类短3.7h,相比而言,胶质类生物较易消化,鱼类最难消化;随桡足类、海月水母、鱼类的体长增加,霞水母对其消化时间显著增长;随着霞水母伞径增大(2.2—14.5cm),以卤虫为饵料消化时间呈显著线性下降,以桡足类为饵料消化时间无显著差异,表明霞水母伞径大小对消化时间的影响因饵料种类不同而有差异。本文的研究结果为野外环境中定性与定量研究霞水母摄食率提供基础。 相似文献
2.
基于脂肪酸标记法和碳氮稳定同位素比值法的东海水母常见种的食性分析 总被引：1，自引：0，他引：1
采用脂肪酸标记法和碳氮稳定同位素比值法研究了东海6个水母常见种的食性。结果表明,6种水母的总脂肪酸含量都不高,说明作为饵料,水母不能够给捕食者提供较多的脂类营养物质。蝶水母(Ocyropsis crystallina)、瓜水母(Bero cucumis)和四叶小舌水母(Liriope tetraphylla)的脂肪酸组成较为相近,它们更多地通过捕食食物链获得有机质。同时,这几种小型水母摄食浮游植物(主要是硅藻和甲藻)比其它几种水母多;另外,它们对植食性桡足类也有一定的摄食。4月份墨绿多管水母(Aequorea coerulescens)主要通过腐生食物链获取有机质;另外,其对植食性桡足类也有一定的摄食。双生水母(Diphyidae spp.)参与腐生食物链也较多;另外,20:1+22:1含量较低指示了其对植食性桡足类几乎不摄食。蝶水母、瓜水母、四叶小舌水母和沙海蜇(Nemopilema nomurai)的δ13C更接近于陆源的C4植物的δ13C,说明其受陆源影响较大。δ15N特征结果表明,蝶水母、瓜水母和四叶小舌水母(Liriope tetraphylla)在浮游食物网中均处于较高营养级,沙海蜇虽个体较大,但由于其摄食器官较小,故其与这3种小型水母的营养地位相近。并且相对于其它几种水母,沙海蜇细菌脂肪酸标记更为明显。 相似文献
3.
在海洋食物链中,浮游动物联系着生产者浮游植物和鱼类等高层消费者,处于中枢的地位。它的摄食决定了食物链的能量传递效率,从而影响鱼类的产量。浮游动物的摄食也是影响海洋碳通量的重要因素。本文介绍4种估计浮游动物现场摄食压力的方法,并进行评价。1 饵料浓度差减法培养实验动物,根据培养前和培养后饵料浓度的变化估计动物的摄食率,这就是饵料浓度差减法。海上调查时,用现场的海水培养浮游动物,就可以估计现场的摄食率。Frost(1972)首先提出了这种方法并给出了计算方法:对照瓶中饵料浓度的变化为C2=C1ek(t2-t1)。C1,C2为培养前和培养… 相似文献
4.
基于脂肪酸标记的长江口海区浮游动物常见种食性分析 总被引：5，自引：0，他引：5
脂肪酸不仅是浮游动物的重要组分,也被作为生物标记来指示动物的食物组成及其之间的营养关系。本文运用脂肪酸标记法对长江口附近海区6个浮游动物常见种的食性进行了分析。研究结果表明,中华哲水蚤(Calanus sinicus)雌体和桡足幼体都表现出明显的植食性。但雌体中16:1ω7的含量要明显高于18:4ω3,表明雌体对硅藻的摄食较多;桡足幼体的18:4ω3要高于雌体,说明桡足幼体对甲藻的摄食较多。磷虾(Euphausia spp.)的多不饱和脂肪酸(PUFA)和ω3系列脂肪酸的含量很高,说明其作为饵料可以给摄食者提供较多的脂类营养物质。中华哲水蚤和磷虾较低的22:6ω3/20:5ω3比值说明他们的营养地位较低。箭虫(Sagitta spp.)的20:1和22:1脂肪酸含量很高,指示了其对植食性桡足类的摄食。蝶水母(Ocyropsis crystallina)、瓜水母(Bero cucumis)和四叶小舌水母(Liriopetetraphylla)的20:1+22:1脂肪酸所占比例较高,指示了其对植食性桡足类的摄食,但是水母类的总脂肪酸含量都很低。几种水母和箭虫的22:6ω3的含量要明显高于20:5ω3的含量,说明它们在浮游食物网中具有较高的营养地位。 相似文献
5.
水母类在自然海区的食物组成是摄食生态学研究的核心问题,本研究利用高通量测序技术分析了管花萨氏水母(Sarsia tubulosa)和八斑芮氏水母(Rathkea octopunctata)的现场食物组成。结果表明:管花萨氏水母和八斑芮氏水母现场摄食食物具有较高的多样性,管花萨氏水母摄食食物31种,八斑芮氏水母29种;两种水母从食物组成上看,属于杂食性生物,其食物包括浮游动物、真菌、浮游植物、陆地植物碎屑等;管花萨氏水母和八斑芮氏水母二者互为捕食对象;二者摄食的食物类群具有相似性,主要来源于节肢动物门和颚足纲,均以太平真宽水蚤为摄食优势种,分别贡献两者食物总量的45.14%和42.42%。高通量测序技术是深入探究水母现场食物组成新的技术手段,两种水母的现场食物组成结果为水母摄食生态学的研究提供了重要参考。 相似文献
6.
为了探究不同种类水母对浮游食物网的摄食影响,采用碳氮稳定同位素和脂肪酸标记法,研究分析了渤海红沿河海域常见的4种小型水母(伞径直径5 cm:卡玛拉水母Malagazzia carolinae、球形侧腕水母Pleurobrachia globosa、帽铃水母Tiaricodon coeruleus、半球美螅水母Clytia hemisphaerica和3种大型水母(伞径10—200cm:沙海蜇Nemopilema nomurai、海月水母Aurelia aurita)和白色霞水母Cyanea nozakii)的食物组成。结果表明,不同种类水母的食物组成存在差异。其中卡玛拉水母、球形侧腕水母、帽铃水母、半球美螅水母和白色霞水母均偏肉食食性,食物组成中动物性食物所占比例更高,高于海月水母与沙海蜇。在食物粒径谱上,帽铃水母和半球美螅水母较大粒径的食物比例均高于小粒径的悬浮有机物(POM)比例。卡玛拉水母和球形侧腕水母各个粒径食物比例接近。大型水母中,白色霞水母的食物中大粒径的浮游动物的比例高于海月水母,更高于沙海蜇。由此看来,小型水母和大型的白色霞水母的暴发会直接影响大中型浮游动物数量,海月水母的暴发对不同大小的浮游生物均会产生一定的影响。而沙海蜇的暴发会大量摄食1 mm的小型浮游生物和POM,对大中型浮游动物以及更高营养层生物(鱼类等)的影响可能是通过蜇伤以及饵料竞争导致的。因此,不同种类水母暴发对浮游生物的影响存在差异。本研究从摄食角度初步探究了水母对海洋生态系统物质循环和能量流动的影响,为水母暴发的灾害防治提供了数据支持。 相似文献
7.
一种钵水母—黄金水母(Chrysaora pacifica)被怀疑是海月水母(Aurelia aurita)碟状幼体的潜在捕食者,为了验证这一假设,在实验室可控条件下进行了以黄金水母幼水母为捕食者、海月水母碟状幼体为猎物的捕食实验。实验结果表明黄金水母幼水母(伞径:9-15mm)能够以海月水母碟状幼体(ca. 2mm)为食。在2 h的实验中,黄金水母幼水母最多摄食了15只海月水母碟状幼体(实验容器容积为450mL)。黄金水母幼水母对海月水母碟状幼体的摄食率在44ind./L和111ind./L的密度下分别为0.8±0.6/ind.·h和1.3±1.0/ind.·h。滤水率在两个密度下分别为0.029±0.024和0.051±0.041L/ind.·h。滤水率随着饵料密度的降低显著提高。实验结果证实黄金水母是海月水母碟状幼体的重要潜在捕食者,并且其对海月水母碟状幼体的捕食可能是影响天然海域中海月水母碟状幼体成活率的重要因素。 相似文献
8.
近几年来,随着各方面研究的进展,人们认识到水母类在生态系统体制转换(Regimeshift)中扮演着重要的角色。水母类在海洋生态系统中的作用正成为新兴的研究热点,但目前,这方面的研究才刚起步,对水母类在生态系统中的作用及机制仍然众说纷纭,在很多观点上难以达成一致看法。本文根据近年来的研究资料,对与水母类相关的食物网结构进行了综述,并初步探讨了水母类在海洋食物网中的作用。1 与水母类相关的营养关系1.1 捕食关系1.1.1 水母类的食物范围 水母类的食性很广,几乎无选择地摄食一切可获得的浮游动物,还包括许多海洋动物的卵和幼虫(包… 相似文献
9.
传统研究结果表明水母的捕食者很少,认为它是海洋食物网的死胡同,但是越来越多的研究表明水母存在于很多生物的胃中。为研究生态系统中水母的上层营养级状况以及水母种群动态变化的捕食性影响机制,以黑鲷为研究对象,通过室内实验,研究了黑鲷对海月水母不同发育期的摄食情况。研究结果表明：黑鲷对海月水母各发育期的摄食情况不尽相同,黑鲷无法直接摄食附着在波纹板上的水螅体;黑鲷对碟状体的摄食是吞食性的,15℃条件下黑鲷对碟状体的摄食率最大可达到（15.487±1.150）ind./（g·d）;黑鲷对小水母体的摄食是吞食性的,对较大水母体的摄食是蚕食性的,这种摄食能力受自身体长大小和水母伞径大小的双重影响,随着体长的增加,黑鲷能摄食更大伞径的海月水母;黑鲷对给定伞径海月水母的摄食能力存在阈值,增大水母密度,不会导致黑鲷摄食量的增加;高密度下黑鲷更倾向于摄食水母体口腕部分。研究结果为理解海月水母碟状体的高死亡率提供了可能性新认知,为理解胶质类在海洋生态系统中的消亡提供了理论。 相似文献
10.
厦门港中华哲水蚤碳氮收支的研究 总被引：2，自引：0，他引：2
本文在分析厦门港中华哲水蚤元素组成基础上,研究其各项生理速率并估算碳氮收支.结果表明:摄食率与饵料含量呈线性相关,未发现饱和摄食.同化效率介于92％～96％之间,与饵料含量及摄食率无关.呼吸率与摄食率及同化率均呈线性相关,其SDA系数介于摄入碳量的9.3％(m/m)或同化碳量的9.9％(m/m).总氮排泄率随摄食率与同化率的提高而呈线性增加.随着摄食率的提高,分配给卵生产的能量也增多,二者呈线性相关.饵料中N含量是厦门港中华哲水蚤生长的主要限制因子,当其对N的摄食率低于10.5×10~(-3)(m/m)/d时,动物“负”生长. 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.
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
13.
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
14.
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
15.
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
16.
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
17.
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
18.
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
19.
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
20.
An Improved Calibration of Satellite Altimetric Heights Using Tide Gauge Sea Levels with Adjustment for Land Motion 总被引：2，自引：0，他引：2
Gary T. Mitchum 《Marine Geodesy》2000,23(3):145-166
Several major improvements to an existing method for calibrating satellite altimeters using tide gauge data are described. The calibration is in the sense of monitoring and correcting temporal drift in the altimetric time series, which is essential in efforts to use the altimetric data for especially demanding applications. Examples include the determination of the rate of change of global mean sea level and the study of the relatively subtle, but climatically important, decadal variations in basin scale sea levels. The improvements are to the method described by Mitchum (1998a), and the modifications are of two basic types. First, since the method depends on the cancellation of true ocean signals by differencing the altimetric data from the tide gauge sea level time series, improvements are made that produce a more complete removal of the ocean signals that comprise the noise for the altimetric drift estimation problem. Second, a major error source in the tide gauge data, namely land motion, is explicitly addressed and corrections are developed that incorporate space-based geodetic data (continuous GPS and DORIS measurements). The long-term solution, having such geodetic measurements available at all the tide gauges, is not yet a reality, so an interim solution is developed. The improved method is applied to the TOPEX altimetric data. The Side A data (August 1992?February 1999) are found to have a linear drift component of 0.55 + / 0.39 mm/yr, but there is also a significant quadratic component to the drift that is presently unexplained. The TOPEX Side B altimeter is estimated to be biased by 7.0 + / 0.7 mm relative to the Side A altimeter based on an analysis of the first 350 days of Side B data. 相似文献