鲍鱼幼苗培养池附板上的危害性纤毛虫及其优势类群研究   总被引：3，自引：0，他引：3  

黄建荣  徐润林  廖家遗 《热带海洋学报》2002,21(3):1-6

应用纤毛虫的定性和定量方法,研究了人工养殖幼鲍培养池中危害性纤毛虫的种类组成和数量变化过程及优势类群的种群动力学变化。共观察到16目、46属、68种纤毛虫,锐利Shun纤虫Aspidisca lynicaster、钟虫Vorticella sp.和双眉虫Diophrys histrix是优势种。还对幼鲍培养过程中危害性纤毛虫的密度、种类与幼苗附板上藻类密度、鲍苗密度等关系进行了分析。  相似文献   

越冬期鲍养成池中浮游动物密度与种类的变化     

黄建荣  张铸淼  徐润林 《海洋科学》2006,30(3):26-29

研究了杂色鲍(Haliotisdiversicolor)越冬期养殖环境中的浮游动物种类组成和密度变化。共检测到浮游动物33种,其中纤毛虫(Ciliata)23种,鞭毛虫(Mastigophora)5种,轮虫(Rotatoria)4种,桡足类(Copepoda)1种。优势种是奇异猛水蚤(Miraciaefferata)和海洋尾丝虫(Uromenamarinam);钩状狭甲轮虫(Colurellauncinata)和偏体虫(Dysterialancolata)为常见种。砂井水养殖可以减少养殖环境中原生动物以外的各种浮游动物种类。  相似文献   

褶皱臂尾轮虫室外培育池浮游生物的初步研究     

李晓东  吴辉良  张清靖  李永函 《海洋科学集刊》2002,(44):52-60

室外轮虫培育池(简称轮虫池，下同)和养鱼池同是一种人工生态系统。轮虫池具有外来有机质特别丰富、生物生产力极高和食物链短的特点，并不受鱼类下行效应的影响。研究轮虫池的浮游生物，不但有助于提高轮虫池的生产力，而且对探讨水域生态系功能也有一定的理论意义。近年来，利用土池大量培育轮虫正逐步开展(Li Yonghan，1996；李永函等，1993，1997；赵沟等，1993)，但多侧重于培养方法和生产应用，对培育池浮游生物状况的资料甚少。本文作者对辽河三角洲河蟹养殖有限公司的若干培育池的浮游生物种类、数量及其分布进行了测定，以期为土池轮虫的持续高产提供生物学依据。  相似文献   

鲈鱼土池人工育苗研究   总被引：3，自引：0，他引：3  

蔡良候  叶金聪  林向阳  温凭  郑镇安 《海洋科学》1997,21(6):57-60

报道了１９８９－１９９３年鲈鱼土池人工育苗的研究结果，捕自天然海区、围垦内 网箱培育的亲鱼注射ＬＲＨ－Ａ与ＨＣＧ诱导能顺利排卵，产卵率７０－１００％，受精卵卵径１．２５－１．４０ｍｍ，浮性卵、受精率２１－８９．０％，在水温１８．０－２１．２℃、盐度３１．０－３４．０的条件下，一般经５０．６７ｈ孵出仔鱼，孵化率４６．０－９０．０％。人工育苗在室外土池进行，最高成活率１１．７％。初孵仔鱼全长３．５３－  相似文献   

利用盐田卤水池塘养殖卤虫的研究   总被引：6，自引：0，他引：6  

孙世春  孙锡恩 《海洋湖沼通报》1991,(2):70-77

1988年和1989年,作者在山东省盐场利用盐田卤水池进行了卤虫池塘养殖的研究。研究内容包括微藻培养试验、卤虫群体生长能力试验和间捕法养殖卤虫试验。通过试验在6个投饵池塘获得的鲜活卤虫产量为423.5—551.0公斤/亩(平均491.6公斤/亩),在4个不投饵池塘获得的产量为240.5—299.5公斤/亩(平均272.3公斤/亩)。本文报告了以上三个试验的内容和结果,并对卤虫养殖中出现的几个问题进行了讨论。  相似文献   

Salinity-Temperature Relations and Morphotypes of a Mixed Population of Coccoid Cyanobacteria from a Hot, Hypersaline Pond in Israel     

Inka  Dor Miriam  Hornoff 《Marine Ecology》1985,6(1):13-25

Abstract. A mixed population of unicellular and colonial cyanobacteria was transferred into culture from a hypersaline helio-thermal pond in the vicinity of the Dead Sea. The entire complex of strains, incubated in Dead Sea water of varying salinity and temperature, showed a pronounced shift of the maximal growth from a salinity of 72 g l^-1 at 30 ^oC up to 142 g 1^-1 at 50 ^oC. Over the above range of salinities and temperatures, these cyanobacteria were capable of about four divisions per day, providing that any increase in salinity was coupled with the suitable increase in temperature. The above peculiar adaptation can explain the prominent success of this group of microorganisms in the extreme and unstable ecological conditions of hypersaline habitats. Amounts of slime accumulating in the cultures were proportional to the incubation temperature.  相似文献   

The Effect of Salinity and Temperature Gradients on the Distribution of Littoral Microalgae in Experimental Solar Ponds, Dead Sea Area, Israel     

Inka  Dor Aline  Ehruch 《Marine Ecology》1987,8(2):193-205

Abstract. Several species of cyanobacteria, diatoms and one euglenid alga populated the littoral zone of hypersaline solar ponds investigated over a period of three years. The composition of the microalgae community changed with salinity and temperature. In the shallow marginal zone the diatoms predominated in winter and spring, at salinities of 30–72 g-1^-1 and at temperatures not exceeding 30o°C, whereas in summer, cyanobacteria were the most abundant. In the deeper zone, at higher salinities and temperatures, cyanobacteria predominated throughout the year. The depth limit of algal growth was 60-80cm, where salinity and temperature exceeded 211 g-1^-1 and 48°C.
The most euryhaline and eurythermal among cyanobacteria were Aphanolhece halophytica F remy and Phormidium hypolimneticum C ampbell , among diatoms Nitzschia sp. aff. N. rostellata H ustedt , Amphora coffeaeformis (A gardh ) K utzing , and Navicula massadaea E hrlich .  相似文献   

Climatic and topographic limits to the abundance of bog pools     

Lisa R. Belyea 《水文研究》2007,21(5):675-687

On patterned peatlands, open water pools develop within a matrix of terrestrial vegetation (‘ridges’). Regional patterns in the distribution of ridge–pool complexes suggest that the relative cover of these two surface types is controlled in part by climate wetness, but landscape topography must also be an important controlling factor. In this paper, a functional model that relates relative cover of ridges and pools to climate and surface gradient was developed and tested. The model was formulated in terms of a water budget, based on the differential effects of ridges and pools on losses by evapotranspiration and subsurface flow. It predicts a positive relationship between surface gradient and ridge proportion, with a linear effect related to water supply and ridge hydraulic conductivity, modified at high ridge proportion by differences in evapotranspiration between ridges and pools. The limit to patterned peatland distribution occurs where the surface is completely covered by ridges. The model may be sensitive or insensitive to climate differences between localities, depending on whether hydraulic characteristics of ridge peat co‐vary with water supply. To distinguish between these alternative hypotheses, surface gradient and ridge proportion were surveyed along 20 transects in each of three localities in Scotland that differ threefold in net precipitation to pools. The results of the field survey served to reject the climate‐sensitive hypothesis, but were consistent with the climate‐insensitive hypothesis. Analysis of the residuals suggested that variation within localities was related more to topographic control of water supply than to ridge hydraulic conductivity or developmental stage. Hence, within this maritime climate region, the distribution of ridge–pool complexes and the relative abundance of pools are controlled mainly by topographic variables. Field surveys across both maritime and continental regions are required to confirm a subtle climatic effect that allows pools to occur on higher gradients in drier climates than in wetter climates. Further development and testing of the functional model will provide a stronger basis for assessing potential feedback between climate change, peatland surface structure and methane emission from pools. Copyright © 2006 John Wiley & Sons, Ltd.  相似文献   

Assessing optical earth observation systems for mapping and monitoring temporary ponds in arid areas     

Valrie Soti  Annelise Tran  Jean-Stphane Bailly  Christian Puech  Danny Lo Seen  Agnes Bgu 《International Journal of Applied Earth Observation and Geoinformation》2009,11(5):344-351

Remote sensing methods for locating and monitoring temporary ponds over large areas in arid lands were tested on a study site in Northern Senegal. Three main results are presented, validated with field data and intended to highlight different spectral, spatial and temporal characteristics of the methods: (1) Among several water indices tested, two Middle Infrared-based indices (MNDWI—Modified Normalized Difference Water Index and NDWI₁—Normalized Difference Water Index) are found to be most efficient; (2) an objective method is given prescribing the necessary sensor spatial resolution in terms of minimal detected pond area; and (3) the potential of multi-temporal MODIS imagery for tracking the filling phases of small ponds is illustrated. These results should assist in epidemiological studies of vector-borne diseases that develop around these ponds, but also more generally for land and water management and preservation of threatened ecosystems in arid areas.  相似文献   

Recent environmental changes inferred from the sediments of small lakes in Yellowstone's northern range (Engstromet al., 1991)     

Wayne L. Hamilton 《Journal of Paleolimnology》1994,10(2):153-157

Sedimentation rate data of Engstromet al. (1991) were analyzed in relation to the elevation of the eight ponds studied. The ... asynchroneity of the stratigraphic changes among the lakes ... that they noted was transformed into a pattern of time-transgressive change of sedimentation rate with elevation. Sediment units representing increasing (and decreasing) sedimentation rate and accelerating (and decelerating) sediment accumulation were correlated from pond to pond, suggesting that the sediment-producing condition somehow moved upslope over time at a rate of 3.4 to >5 m yr^–1. Climatic data appear not to explain this monotonic pattern, but dendrochronological data and elk population numbers suggest that ungulate foraging patterns might. Engstromet al. (1991) concluded that ...the lake-sediment records in the northern range do not convincingly show systematic direct or indirect effects of ungulate grazing during the history of the Park. Reinterpretation of these sediment data suggests that detailed reanalysis might lead to a different conclusion.  相似文献