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2014年9月和2015年5月,分别在泉州湾北岸布设3条潮间带断面进行大型底栖生物群落研究.共计采获潮间带大型底栖生物样品166种,其中泥沙滩有80种,岩相有96种.其中环节动物、软体动物和节肢动物有145种,构成该区域潮间带大型底栖生物的主要类群,调查的3条断面中,泥沙滩断面的平均栖息密度和生物量分别为133 ind./m~2和24.48 g/m~2,岩相断面的平均栖息密度和生物量分别为1 412 ind./m~2和958.78 g/m~2.数量垂直分布,泥沙滩断面和岩相断面平均栖息密度和生物量均以中潮区低潮区高潮区.数量季节变化,泥沙滩断面平均栖息密度和生物量均为春季(170 ind./m~2和32.04 g/m~2)大于秋季(96 ind./m~2和16.92g/m~2),岩相断面平均栖息密度为春季(1 360 ind./m~2)小于秋季(1 464 ind./m~2),而平均生物量为春季(1 122.83 g/m~2)大于秋季(794.75 g/m~2),数量季节变化显著.丰度/生物量曲线显示,泉州湾北岸潮间带大型底栖生物群落群落结构较为稳定,受到干扰较小. 相似文献
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大亚湾红树林区底相大型动物的群落 总被引：6，自引：2，他引：6
本文据1987～1989年实地调查资料,研究了大亚湾红树林区底栖生物的种类组成与数量分布。结果表明,分布于湾顶5种红树林内的底栖生物70种,主要由多毛类(23种)、软体动物(23种)、甲壳动物(12种)和星虫动物(8种)组成;平均生物量219.77g/m~2,平均栖息密度281个/m~2;在数量上以软体动物的腹足类占优势。文中应用群落结构指数进行分析,并与九龙江口的作了比较。 相似文献
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渔山列岛夏季潮间带大型底栖生物群落结构研究 总被引：4，自引：0，他引：4
于2014年8月,在浙江宁波渔山列岛布设4个岩礁断面开展潮间带大型底栖生物调查,分析其种类组成、丰度、生物量、优势种、生物多样性和群落结构特征等。该调查共采集到潮间带大型底栖生物98种,包括大型底栖动物70种和大型底栖藻类28种;其中优势种有9种,分别为小结节滨螺[Echinolittorina radiata(Souleyet)]、条纹隔贻贝[Septifer virgatus(Wiegmann)]、厚壳贻贝[Mytilus coruscus(Gould)]、带偏顶蛤[Modiolus comptus(Sowerby)]、栗色拉沙蛤[Lasaea nipponica(Keen)]、日本笠藤壶[Tetraclita japonica(Pilsbry)],刺巨藤壶[Megagbalanus volcano(Pilsbry)],以及珊瑚藻[Corallina officinalis(Linnaeus)]和小石花菜[Gelidium divaricatum(Marteus)]。潮间带大型底栖生物平均生物量为8 515.50 g/m~2,平均丰度为6 841.63个/m~2;各断面Shannon-wiener指数(H′)、Pielou均匀度指数(J)和Margalef丰富度指数(d)平均值分别为1.89±0.14、0.38±0.01和3.66±0.52。ABC曲线分析表明,4个断面受到一定扰动。与历史资料相比,该区域物种数减少明显,生物量和丰度有所增加,优势种被个体较小的日本笠藤壶、条纹隔贻贝等物种所演替。上述结果可为渔山列岛潮间带开发保护管理及其生物资源的可持续利用提供重要参考。 相似文献
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福清核电站邻近潮间带大型底栖生物数量分布与群落结构 总被引：3，自引：0，他引：3
于2006年2、4、7和10月在福清核电厂运行前对其邻近潮间带不同底质断面的大型底栖生物进行采样,以了解该潮间带大型底栖生物的种类及资源分布.结果表明,该核电站附近潮间带大型底栖生物总共为146种,以多毛类、软体动物和甲壳动物为主.以季节和底质为因素对取样获得物种数进行双因素方差分析显示:种类获得数的季节变化无显著差异,底质间呈边缘性显著.4季的大型底栖生物平均生物量为1 446.11 g/m2、平均栖息密度为972个/m2.大型底栖生物生物量平均值为春季＞夏季＞冬季＞秋季,栖息密度平均值为夏季＞春季＞冬季＞秋季.以季节和底质为因素的双因素方差分析显示:大型底栖生物生物量和栖息密度季节间无显著差异但底质间差异极显著.底质和季节间大型底栖动物的Shannon-Weiner指数、Margalef种类丰度、Pielou均匀度和Simpson优势度指数均无显著差异.利用Bray-Curtis相似性聚类对福清核电站邻近潮间带大型底栖生物进行分析后得出,该潮间带大型底栖生物可划分为两个群落:岩礁群落和泥沙滩群落.分析表明,底质是影响大型底栖生物分布的主要环境因子,季节对大型底栖生物分布的影响不显著. 相似文献
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硇洲岛潮间带不同生境底栖软体动物物种多样性研究 总被引：13，自引：0，他引：13
对硇洲岛潮间带（岩石、砾石、泥沙滩）3种不同生境的11个样方的底栖软件动物进行了生物多样性调查，共鉴定底栖软体动物21科41种。研究结果表明，硇洲岛潮间带底栖软体动物动物种丰富度指数砾石滩最大（平均为9.236)，岩石滩次之（平均为6.494)，泥沙滩最小（平均为3.788)，多样性指数砾石滩（平均为2.154)大于泥沙滩（平均为1.506）大于岩石滩（平均为1.334)。对上述样方进行聚类分析的结果表明，底栖软体动物的种类及数量分布受底质、浪击、污染等因素的影响。 相似文献
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本文根据大亚湾50个站底栖生物生态调查资料,对孔径1mm和0.5mm筛网中多毛类的种类数、主要种、平均密度、平均生物量进行比较分析。结果表明,孔径1mm的为14种/站、9种、110个/m~2和8.03g/m~2,而0.5mm为22种/站、12种、216个/m~2和0.71g/m~2;1mm筛网多毛类密度(X)与0.5mm的密度(Y)呈线性正相关关系,其回归方程为:Y=0.93X+113.77;在估算海域生产力中,应当使用0.5mm孔径筛网。 相似文献
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珠江口东南部海域大型底栖生物群落特征研究 总被引：4，自引：0，他引：4
根据2006年的3月和7月在珠江口东南部海域进行的大型底栖生物调查,初步鉴定出大型底栖生物共156种,其中多毛类种类最多(79种),其次是甲壳动物(37种)。7月(116种)比3月(92种)种类多。3月大型底栖生物平均生物量和平均密度分别为6.703g/m2和679.4ind/m2,7月分别为22.436g/m2和576.3ind/m2。大型底栖生物种类数、生物量、密度和多样性指数(H’和J’)在调查海区东南部相对较低。采用Bray-Curtis相似性系数聚类分析和多维排序尺度(MDS)分析了3月和7月大型底栖生物群落的相似性,认为相同季节各站大型底栖生物相似性系数较高,大型底栖生物群落季节性差异相对较大。大型底栖生物群落在40%相似性以上,3月和7月分别可以划分出2个和3个生物群落。3月大型底栖生物群落Ⅱ和7月群落Ⅰ受到中等程度的扰动,其它生物群落处于轻微扰动状态。大型底栖生物种类数、密度、种类均匀度和种类丰富度与水深和沉积物特征相关性显著。 相似文献
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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
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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
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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
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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
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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
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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
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Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations. 相似文献
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Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans 总被引：1，自引：0，他引：1
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