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1.
福建红树林上钻孔动物的生态 总被引：1，自引：0，他引：1
福建红树林上的钻孔动物共发现了５种，其中软体动物的龙骨节铠船蛆Ｂａｎｋｉａ ｃａｒｉｎａｔａ、裂铠船蛆Ｔｅｒｅｄｏ ｍａｎｎｉ和甲壳动物的光背团水虱Ｓｐｈａｅｒｏｍａ ｒｅｔｒｏｌａｅｖｉｓ是破坏红树林的主要的钻孔动物。钻孔动物钻凿红树茎的基部和裸露的根部，垂直分布受潮汐水位制约，在红树林区的纵深分布与水流畅通程度有关。 相似文献
2.
福建九龙江口红树林上大型底栖动物的群落生态 总被引：10，自引：1，他引：10
热带和亚热带海湾、河(?)的红树林海岸是个特殊的生态环境。近几年来,红树林生态系的研究日益受到人们的重视。目前,对红树植物方面的研究较多,而红树区动物方面的报道很少。Macnae,W.(1968)定性地综合报道过印度-西太平洋红树区动物的种类、分布和某些底相动物的个体生态。红树上底栖动物群落生态的研究至今未见专题报道。 相似文献
3.
广西防城港东湾红树林污损动物的种类组成与数量分布特征 总被引：5，自引：0，他引：5
对白骨壤(Avicennia marina)树上的污损动物进行了定性和定量调查。共采得污损动物9种。以白条地藤壶(Euraphia withersi)和潮间藤壶(Balanus littoralis)在多数采样点的附着密度最高，但二者在树上的分布有明显的差异；团聚牡蛎(Ostrea glomerata)分布最广，是惟一～种在各采样点均能采到的污损动物；黑养麦蛤(Xenostrobus atraus)主要分布在树干和较粗的枝条上，其密度在向海林缘达到最大，超过牡蛎和藤壶的附着密度。污损动物附着高度与树高的比值(h：H)，主干、枝条和叶片上附着的污损动物总量均随林带离岸距离增大而增大，呈明显的变化趋势。 相似文献
4.
罗源湾大官坂围垦区附着生物生态研究 总被引：13，自引：1，他引：13
通过罗源湾大官坂围垦区水域附着生物碉 年挂板试验，共鉴定动物39种，藻类8种，统计分析显示，主要附着期在5-10月，生物量及覆盖面积率的高峰期在6-9月，网纹藤壶（Balanus reticulatus)、总合草苔虫（Bugula neritina)、乳突皮海鞘（Molgula manhattensis)、中胚花筒螅（Tubulari a mesembryanthemum)和肠浒苔（Enteromopha intesinalis)是附着生物群落的优势种，测定群落的种类多样性指数、种类丰度、均匀度，以及进行环境因子分析的结果表明，水流畅通程度是影响附着生物群落种类及数量组成的最主要因子，对于围垦区水域的养殖生产来说，6-9月是生物污损危害的主要月份。 相似文献
5.
藤壶亚目是目前为止海洋生物群落中种类最丰富和最重要的类群之一,也是海洋污损生物的重要组成部分,主要分布于岩石潮间带栖息地、深海热液口,有的物种会附着在红树林植物、动物和人工构筑物上。文章综述了藤壶亚目的起源以及分类系统的建立和发展,认为藤壶亚目在下白垩纪从有柄目分化而来,其中篱藤壶科(小藤壶总科)是最早分化出的一支,而后逐渐分化为星板藤壶总科、厚藤壶总科、鲸藤壶总科、笠藤壶总科、小藤壶总科和藤壶总科6支;总结了国内藤壶亚目的研究进展;比较了藤壶亚目系统发育学的研究方法;展望了未来的研究方向,即结合形态学方法与分子系统学方法研究藤壶亚目物种的系统发育关系,为今后研究藤壶亚目物种的分类及防治等工作提供借鉴和帮助。 相似文献
6.
互花米草Spartina alterniflora自1979年引入至今,已在我国海岸带大范围扩张并对盐沼湿地生态系统产生了很大影响.本研究以附着生物藤壶为例,研究了互花米草扩张对附着生物的影响.通过对5个断面共28个样方的米草植株、附着藤壶以及藤壶在互花米草上的最大附着高度调查,获得结果如下:藤壶在互花米草滩上的附着范围位于潮沟两侧,且呈宽度约为5 m的带状分布;潮沟规模越大,其向陆方向的延伸范围越宽;每个站位藤壶附着的相对最大高度都位于同一水平.附着藤壶均为白脊管藤壶Fistulobalanus albicostatus,平均干重237±69g·m-2,大部分藤壶直径在2～10mm之间.互花米草的平均干重为981±81g·m-2,潮沟附近互花米草高壮但密度较小,远离潮沟互花米草矮小但密度较大.分析表明,互花米草为藤壶提供了附着基质,并影响藤壶在潮间带的平面分布格局(尽管藤壶的生态位保持不变).影响白脊管藤壶分布特征的原因主要是海水浸没时间的差异;负地形的浸没时间更有利于藤壶的附着和生存;另外潮沟较高的潮水流速除了利于白脊管藤壶幼体的附着外,还可以通过水流的涨、落为其带来充足的食物. 相似文献
7.
舟山枸杞水域的污损生物生态 总被引：1，自引：0，他引：1
本文系１９８８年９月～１９８９年９月在舟山枸杞乌里西岙水域进行挂板试验的结果。共获污损生物１３５种，其中，近岸的油库码头获７７种，远岸的养殖筏获１１０种。动物以亚热带高盐性种类为主，三角藤壶Ｂａｌａｎｕｓｔｒｉｇｕｎｕｓ、小海葵Ａｃｔｉｎｉａ、柯氏分胞孔苔虫Ｃｅｌｌｅｐｏｒｉｎａｃｏｓｔａｚｉｉ、西方三胞苔虫Ｔｒｉｃｅｌａｒｉａｏｃｃｉｄｅｎｔａｌｉｓ、艾氏美熄Ｃｌｔｉａｅｄｗａｒｄｓｉ、广口小桧叶螅Ｓｅｒｔｕｌａｒｅｌｌａｍｉｕｒｒｅｎｓｉｓ等占优势，藻类常见的有长石莼Ｕｌｖａｌｉｎｚａ、肠浒苔Ｅｎｔｅｒｏｍｏｒｐｈｙｉｎｔｅｓｔｉｎａｌｉｓ和日本多管藻Ｐｏｌｙｓｉｐｈｏｎｉａｊａｐｏｎｉｃａ。枸杞污损生物的附着期主要在夏季，附着量也以夏季最大。不同地点附着量的差异极大。夏季由于近岸三角藤壶大量附着，故生物量明显大子远岸，其他季节均是远岸大于近岸。夏季近岸三角藤壶的覆盖面积达１００％，生物量达１８１１９ｇ／ｍ２，占污损生物总生物量的９８％。故夏季是污损生物防除的主要季节，三角藤壶是防除的主要对象。与１９７５～１９７６年嵊山污损生物进行比较，发现两地污损生物的种类组成和群落结构极为相似，说明１０多年以来嵊山 相似文献
8.
北部湾大风江与南流江河口红树林空间分布格局研究 总被引：1，自引：1，他引：0
生长在潮间带的红树植物在河口植物群落构成、海岸防风消浪中具有重要价值。本文基于本地种桐花树胚胎浸泡下沉实验与北部湾南流江和大风江河口段水体盐度、沿线潮间带植物群落结构与地貌分析，探讨红树林在河口空间分布及影响因素。结果主要表明:南流江河口和大风江河口红树林自海向陆基本展现“红树林纯林(桐花树、秋茄、无瓣海桑种类混生)→红树植物与半红树植物(黄槿、苦朗等)混生→红树植物、半红树植物与非红树植物混生→红树植物镶嵌→稀疏红树林小苗”的分布格局，但大风江河口向陆界限主要以红树、红树幼苗及半红树混生为主。此外，红树被浸淹时长是控制河口红树空间分布结构的主要因素。潮水上溯时长影响红树向陆生长的极限位置，宜林滩地是红树发育生长的必要条件。 相似文献
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沙筛贝(Mytilopsis sallei)属于软体动物门(Mollusca)双壳纲(Bivalvia)帘蛤目(Veneroida)饰贝科(Dreissenidae),也称萨氏仿贻贝.20世纪90年代初作为鱼虾饵料被引到厦门马銮湾,逐渐成为附着生物的优势种,严重影响贝类养殖.在厦门马銮湾水域设计挂板实验和采集沉积物中大型底栖动物,获得了外来物种沙筛贝与其他大型底栖动物的时空分布数据.SPSS统计软件回归分析表明,沙筛贝与网纹藤壶(Balanus reticulatus)在挂板的垂直分布上呈负相关,沙筛贝高密度(大于105个/m2)时能导致网纹藤壶死亡,其主要原因是沙筛贝附着在网纹藤壶壳壁上,抢夺网纹藤壶食物而导致其饿死.无论是在挂板上还是在沉积物中,小头虫(Capitella capitata)、凿贝才女虫(Polydoraciliata)的数量有随沙筛贝数量增加而增加的趋势,这是因为成团的沙筛贝有利于小头虫和凿贝才女虫的栖息. 相似文献
11.
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
12.
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
13.
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
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《海洋学报(英文版)》2014,(9):F0003-F0003
<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology, 相似文献
16.
The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance. 相似文献
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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
19.
Rahul Sharma 《Marine Georesources & Geotechnology》2000,18(3):237-250
Observations on seafloor features from subbottom profiling and seabed photography data show that the undisturbed and natural conditions before the benthic disturbance undergo a substantial change after operation of the disturber. The effects can be seen in the form of deep trenches and grooves, formed by the action of the sleds and the pumping of the sediment along its path, as well as sediment piles on either side of the track. Biological traces such as fecal coils, casts, tubes, burrows, and trails get obliterated in the areas of disturbance and resedimentation. The smooth, uniform nature of the seafloor observed in predisturbance phase shows microtopographic changes in and around the disturbed area as a result of sediment excavation and resettlement. Vertical mixing as well as lateral transport of sediment alter the geological, biological, physical, and chemical conditions on the seafloor, which need to be monitored over time to assess the process and the time taken for restoration of environmental conditions. 相似文献
20.
Vance P. Vicente 《Marine Ecology》1989,10(2):179-191
Abstract. Long-term changes in the distributional patterns of commercial sponges ( Spongia spp. and Hippospongia spp.) within the West Indian Region indicates that: 1) commercial sponges had a widespread distribution throughout the whole West Indian Region and were ubiquitous in very shallow water until about the first half of the present century; 2) they were fished commercially not only in the traditional northern Caribbean sites (Florida, Gulf of Mexico, Bahamas) but also in the Greater ( e. g. , Hispaniola, Jamaica) and Lesser Antilles; and 3) they became extinct throughout most of the Lesser Antilles ( e. g. , Puerto Rico, Vieques, St. Thomas) sometime during the first half of this century. Mortalities of spongiids within the Antilles were found to differ from other marine mortalities in that: 1) species disappeared from a large region; 2) species vanished from different habitats and depths; and 3) natural populations never recovered. Species richness patterns suggest that commercial sponge genera ( Spongia and Hippospongia ) evolved under slightly cooler elimatic conditions than those found at present, and that these extinctions occurred as a direct or indirect effect of positive thermal anomalies in sea surface and atmospheric temperatures between 1900–1950. The concept that species diversity is stable on a regional scale is questioned. 相似文献