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1.
夏季青岛近海浮游动物种类组成、群落结构及多样性 总被引：2，自引：0，他引：2
2006年7月在青岛近海海域(35°19′～36°35′N, 119°50′～121°33′E)进行浮游动物采样调查,研究了青岛近海浮游动物的种类组成、群落结构及多样性.调查共鉴定浮游动物48种,浮游幼虫18类.种类数的平面分布为灵山湾、琅琊台湾附近海区较多,其他海区较少.优势种类有中华哲水蚤(Calanus sinicus)、强壮箭虫(Sagitta crassa)、拟长脚虫戎(Parathemisto gaudichaudi)、长尾类幼虫(Macrura larvae)和短尾类幼虫(Brachyura larvae).调查海区近岸暖温类群、近岸暖水类群、近岸低盐类群、温带外海类群四种生态类群共存,但以近岸暖温类群为主.浮游动物丰度、生物量的水平分布趋势与表层温度、盐度的水平分布趋势相似,都从调查海区的外海区向近岸逐渐降低;Shannon-weiner多样性指数与Pielou均匀度指数水平分布趋势与表层温度、盐度相反,从青岛近岸向调查海区外海逐渐降低.与该区域1959年同月份的调查数据相比,浮游动物主要种类组成、丰度、生物量差别不大,主要种类中华哲水蚤丰度有较大的增加. 相似文献
2.
《海洋湖沼通报》2017,(6)
根据2015年4月(春季)和11月(秋季)珠江口海域南沙段海洋生态调查资料,探讨了该海域浮游动物种类组成、优势种、丰度、均匀度(J)、多样性指数(H')及多样性阈值(Dv)等群落生态特征。共鉴定浮游动物73种(类),其中春季28种(类),秋季57种(类),中华异水蚤(Acartiella sinensis)和长尾类幼体为2季共有优势种(类群)。调查海区的浮游动物可划分为淡水生态类群、河口低盐生态类群、广温广盐生态类群、近岸暖水生态类群和外海暖水生态类群。浮游动物丰度和生物量均为春季高于秋季,而多样性指数、均匀度和多样性阈值则以秋季高于春季。统计分析表明,浮游动物丰度均与水温有关(P0.05),除了水温,盐度成为秋季浮游动物最主要的影响因子,相关性极显著(P0.01)。 相似文献
3.
福建沙埕港浮游动物群落特征及影响因子 总被引：1，自引：0，他引：1
根据沙埕港2006年1月和4月冬、春季2个航次的调查资料,分析了浮游动物种类组成、优势种、丰度和生物多样性的季节变化,并利用PRIMER统计软件中的PCA、BIOENV和RELATE程序探讨了浮游动物与环境因子的关系.经鉴定共有浮游动物77个种类(含浮游幼虫15类 ).中华哲水蚤(Calanus sinicus)和真刺唇角水蚤(Labidocera euchaeta)是2个航次共有的优势种,桡足幼体在2个航次中也都占优势.与1990年调查相比,浮游动物丰度大幅下降,浮游动物种类组成已发生了较大改变.沙埕港的浮游动物大致可分为河口型类群、沿岸型类群和近海型类群.冬季航次浮游动物的平均总丰度为20.6 ind/m3,春季航次为92. 2 ind/m3,低于福清湾浮游动物同期调查结果.浮游动物总丰度分布均为由湾口向湾顶递减的趋势.春季的浮游动物总丰度和香农-威纳多样性指数均高于冬季,冬季浮游动物生物多样性呈现湾中、西部高,湾口、湾顶低的趋势,而春季浮游动物多样性分布比较均匀.经统计分析,影响冬季和春季浮游动物分布的主要环境因子为盐度、温度. 相似文献
4.
福清湾及附近海域浮游动物的数量和分布 总被引：3，自引：0，他引：3
本文分析了2005年10月和2006年5月在福清湾及其附近海域采集的浮游动物样品,结果表明,福清湾已鉴定的浮游动物有64种,10类浮游幼体.分为4个生态类群,包括河口低盐类群,近岸暖温类群,近岸暖水类群和广布外海类群.浮游动物物种多样性指数春季高于秋季.春季浮游动物总个体数均值为(161ind/m3)高于秋季的(83ind/m3),春季生物量均值为(67.7mg/m3)低于秋季的(87.7mg/m3);浮游动物总个体数的平面分布,春季湾内西部水域最高,海坛海峡最少;秋季福清湾东部水域最高,湾内西部水域最少.浮游动物生物量和总个体数的平面分布趋势基本一致.另外还对浮游动物的分布与环境因子的关系进行了分析. 相似文献
5.
胶州湾浮游动物生物完整性指数的建立 总被引：1，自引：0，他引：1
为补充中国海湾环境质量状况评估方法,作者通过整理和综合胶州湾常规监测项目中6年(2003~2008)的监测数据,经数据整理与综合、生境区域划分、评价因子选择、因子阈值确定、指数建立、指数验证与应用6个过程,初步建立了胶州湾浮游动物生物完整性指数(指数存在季节性差异,本实验以夏秋季节为例)。指数建立过程中将生境区域通过溶解性无机氮(DIN)、磷酸盐(PO_4)及透明度3项指标划分为参照区和受损区,低营养盐、高透明度海域划为参照区,相反则划为受损区。通过检验11项浮游动物因子参照区与受损区的差异性,最终确定7项为指数建立的评价因子。对7项评价因子得分加权平均即得胶州湾浮游动物生物完整性指数得分。将指数得分划分为5个等级,分别表征不同的浮游动物要素质量状况。胶州湾浮游动物生物完整性指数的建立为从浮游动物角度评估胶州湾环境质量提供了新的方法,是对胶州湾生态环境质量综合评价的良好补充,能够更全面地反映海区浮游动物的质量状况,同时为发展和完善海湾生态系统质量综合评价体系奠定良好基础。 相似文献
6.
7.
海南岛近岸海域夏初浮游动物与环境因子的关系 总被引：4，自引：1，他引：3
根据2011年夏初在海南岛近岸海域采集的浮游动物样本,分析了该海域浮游动物的种类组成、优势种类、丰度、生态类群,生物多样性及均匀度,并对浮游动物与环境因子之间的关系进行了探讨。海南岛近岸海域共鉴定出终生性浮游动物164种,阶段性浮游幼体11个类群,其中以桡足类的种类最多,40属82种。优势种主要有棘皮动物幼体Echinodermata larva、鸟喙尖头溞Penilia avirostris、异体住囊虫Oikopleura dioica、长尾类幼体Macrura larva、肥胖软箭虫Ferosagitta enflata、羽长腹剑水蚤Oithona plumifera、小齿海樽Doliolum denticulatum、中型莹虾Lucifer intermedius、泡抱球虫Globigerina bulloides、微驼隆哲水蚤Acrocalanus gracilis等。海南岛近岸海域浮游动物丰度平均值为1 348.68ind/m3,东部海域浮游动物丰度最高,由近岸向远岸呈递减趋势,而北部湾海域和南部海域由近岸向远岸则呈先增后减的趋势。夏初由于受沿岸流和南海暖流的影响,海南岛近岸海域的生态类群以暖水沿岸种和广布暖水外海种为主。浮游动物多样性指数和均匀度平均值为3.03和0.72,东部海域的多样性指数和均匀度较低,主要原因是阶段性浮游幼体的偶然性暴发。相关性分析显示,海南岛近岸海域浮游动物丰度与pH值呈极显著负相关(p0.05,r=-0.360);与浮游植物丰度(PA)呈极显著正相关(p0.01,r=0.395);与盐度、DO、CODMn、NO3-N浓度、NH4-N浓度、PO4-P浓度成正相关,与温度、NO2-N浓度、SiO3-Si浓度呈负相关。 相似文献
8.
本研究基于2013年夏季“大洋一号”船大洋第30航次西南印度洋海区科学考察走航线路,对西南印度洋21°S到38°S海域表层浮游动物群落进行连续采样调查,研究了该海域表层中型浮游动物群落结构和物种多样性及空间分布格局。结果显示,研究海域表层中型浮游动物群落组成包括:桡足类、磷虾类、端足类、十足类、介形类、毛颚动物、被囊类、异足类、翼足类、刺胞动物及多毛类等11大类,总计50属69种;优势类群为桡足类(69%)和磷虾类(27%)。多样性指数随经度和纬度的变化特征:H′、D多样性指数及J均匀度指数随纬度的升高均呈下降趋势;在经度梯度上,几种多样性指数也大致呈现出东高西低的趋势。聚类分析表明,研究区可大致以36°S附近为界划分为南部和北部两大类群,分别以北部桡足类(平均粒径小),南部磷虾类(平均粒径大)Euphausia属为优势群落。群落相似性结果反映出,南部类群与南极克罗克海峡和南极长城湾水域群落,北部类群与西北印度洋海域群落的联通性不高。 相似文献
9.
10.
夏季莱州湾浮游动物群落特征 总被引：3，自引：0，他引：3
根据2009 年8 月监测资料, 研究了夏季莱州湾海域浮游动物种类组成、生态分布、群落结构及其环境影响因子。共记录包括浮游幼虫在内的浮游动物38 种(类), 优势种类为长尾类幼虫、强壮箭虫、短尾类溞状幼虫及太平洋纺锤水蚤等。浮游动物丰度101.3～3620.0 个/m3, 平均602.8 个/m3, 丰度平面分布呈现湾西部高, 向中东部逐渐降低趋势; 长尾类幼虫、强壮箭虫、短尾类溞状幼虫出现频率100%,太平洋纺锤水蚤出现频率40.9%; 长尾类幼虫丰度7.8～1747.9 个/m3, 平均96.3 个/m3, 高值区分布于莱州湾西部黄河口以南近岸水域; 强壮箭虫丰度2.5～747.8 个/m3, 平均85.4 个/m3, 偏离近岸趋深水、低温区分布; 短尾类溞状幼虫丰度3.3～271.7 个/m3, 平均20.5 个/m3, 主要分布于莱州湾南部近岸水域; 太平洋纺锤水蚤丰度0～968.3 个/m3, 平均29.0 个/m3, 密集分布区在莱州湾西南部小清河外近岸低盐水域。浮游动物丰度分布与NO2-N、DO、COD 及NO3-N 呈显著正相关关系, 与盐度呈显著负相关关系(P＜0.01)。等级聚类分析(CLUSTER)将莱州湾的浮游动物分为湾西部和湾中东部两个群落。相比于湾中东部群落, 湾西部群落占据着莱州湾西部近岸较狭窄的地理范围, 其所在水域水浅, 盐度低, 无机氮、活性磷酸盐、叶绿素a、浮游动物丰度高及物种多样性高, 群落内生物相似性弱。 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.
Extreme sea levels associated with severe cyclonic storms are common occurrences along the east coast of India. The coastal districts of Orissa have experienced major surges in the past. The recent Paradip super cyclone is one of the most severe cyclones, causing extensive damage to property and loss of lives. Extreme sea levels are major causes for coastal flooding in this region. Damages can be minimized if the extreme sea levels are forecast well in advance. In the present study, we develop a location specific, fine resolution model for the Orissa coast on the lines similar to that of IIT-D storm surge model (Dube et al. 1994). The model runs on a personal computer. The bathymetry for the model is extracted from very fine resolution naval hydrographic charts for the region extending from the south of Orissa to south of West Bengal. A simple drying scheme has also been included in the model in order to avoid the exposure of land near the coast due to strong negative sea surface elevations. An attempt was made in this study to simulate extreme sea levels along the Orissa coast using the data of past severe cyclones. The model results reported in the present study are in good agreement with available observations or estimates. 相似文献
19.
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
20.
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