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实验室混合藻种的光谱分解方法研究 总被引：1，自引：0，他引：1
颗粒物吸收是海洋水色的重要因子.现有的规范方法将颗粒吸收分成浮游植物色素吸收与非色素颗粒物吸收两部分,没有对浮游植物色素吸收作进一步的分离.然而,自然界海水中存在多种藻类都会影响浮游植物的吸收.不同藻类包含的色素种类和组成比例各不相同,实际上,海水中浮游植物色素吸收是多种藻类吸收的综合反映.从不同藻种的吸收光谱特征研究入手,分析了小球藻、扁藻、裸甲藻的吸收光谱特征,研究了多藻种自然混合状态下的光谱分解方法.研究结果表明,混合藻种吸收光谱分解技术是水体藻类信息提取的一种有效方法. 相似文献
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西赤道太平洋暖池区光合色素分布及其对浮游植物群落的指示作用 总被引：2，自引：0，他引：2
利用光合色素的生物标志性可以在"纲"水平上表征浮游植物群落结构。依托大洋科学考察第20航次和21航次,通过对西赤道太平洋不同区域5个站位的HPLC藻类色素分析及CHEMTAX程序因子分析,获取了暖池区光合色素及浮游植物群落的垂直分布信息。结果显示在寡营养的暖池区,玉米黄素(Zeaxanthin)及乙二烯叶绿素a(DV Chl a)与叶绿素a浓度呈显著的正相关,浮游植物群落结构以蓝细菌、原绿球藻及定鞭金藻为优势藻纲,按对生物量的贡献率原绿球藻大于蓝细菌大于定鞭金藻的。蓝细菌和原绿球藻分布在真光层不同深度,而在营养盐丰富的次表层优势浮游藻类为定鞭金藻。 相似文献
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浮游藻类对溶解态氮的吸收同化是湖泊氮生物循环和水体富营养化发生机制探讨的关键环节。本文通过~(15)N稳定同位素添加实验以铜绿微囊藻(Microcystis aeruginosa)、海链藻(Thalassiosira sp.)、卡德藻(Tetraselmis sp.)、剧毒卡尔藻(Karlodinium veneficum)以及盐水隐藻(Rhodomonas salina)为研究对象,从浮游藻类氮素吸收时间、营养盐基质以及藻种差异三个方面研究五种藻类对铵氮(NH_4~+-N)、硝氮(NO_3~--N)、尿素氮(Urea-N)三种形态氮的吸收特征。研究发现:(1)浮游藻类对三种形态氮的吸收均在1h时吸收速率最高,其氮素吸收过程为快速吸收。(2)浮游藻类优先吸收还原态氮,其中NH_4~+-N吸收速率最高,当培养周期为1d和4d时浮游藻类对NH_4~+-N吸收速率的均值分别为4.05和4.15μmol/(L·h);浮游藻类对Urea-N吸收相对偏好系数为25.18—713.42,表现出对小分子溶解态有机氮的特定偏好性。(3)不同藻种对氮素吸收具有不同特征,其中,剧毒卡尔藻对三种形态氮的吸收速率均为最高,而铜绿微囊藻的吸收速率均为最低;不同藻种不同培养时间氮素吸收速率差异与浮游藻类生长周期等特性有关。不同浮游藻类对不同形态氮素表现出吸收特异性,对水体氮负荷和浮游藻类水华优势种形成将产生重要影响。 相似文献
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基于诊断色素分析的胶州湾浮游藻功能类群研究 总被引：2，自引：0，他引：2
分析了2003年12月至2004年10月胶州湾18个站位7个航次的浮游藻色素组成(包括叶绿素和类胡萝卜素)。使用岩藻黄素、多甲藻黄素、色素组合(别黄素+19'-丁酰氧基岩藻黄素+19'-己酰氧基岩藻黄素+青绿藻黄素)和玉米黄素作为特定功能类群的诊断色素指标定义了四个浮游藻功能类群(PFTs), 即硅藻、甲藻、微型鞭毛藻和蓝细菌, 并根据各浮游藻功能类群的诊断色素(组合)占诊断色素总量的比例研究了各功能类群在胶州湾的时空分布特点, 结果表明硅藻是胶州湾的优势类群(平均占65.8%), 微型鞭毛藻次之(26.0%), 甲藻和蓝细菌最低(分别为6.3%和1.9%)。基于诊断色素指标的浮游藻功能类群分析是一种简便的判断优势浮游藻类群组成和丰度的方法。 相似文献
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《中国海洋湖沼学报》 《海洋科学》2012,36(6):127-129
Pigment characterization for the 2011 bloom in Qin-huangdao implicated"brown tide"events in China孔凡洲,于仁成等:渤海秦皇岛沿岸海域近年来发生大规模藻华,对贝类养殖业构成巨大危害,但藻华原因种(一种细胞大小约2μm的微藻)一直未能鉴定。通过对2011年该海域藻华期间浮游植物色素的分析发现,高含量的19-丁酰氧基岩藻黄素是最为突出的特征色素,据此判断藻华原因种应为海金藻类 相似文献
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杭州西湖浮游藻类的种类组成和数量变动 总被引：3，自引：0，他引：3
本文根据1985年2月至1986年2月对西湖浮游藻类所作的周年调查资料,就西湖浮游藻类的种类组成、数量变动及其与环境因子的关系作了研究。在20个测站260余号样品中,共鉴定出浮游藻类7门92属229种、变种和变型。优势种类为水华束丝藻、螺纽鞘丝藻、大螺旋藻、铜绿微囊藻、弯曲尖头藻、微小平裂藻、球胞鱼腥藻、克罗脆杆藻、连结脆杆藻和颗粒直链藻。西湖浮游藻类年均值为614×10~5个/升,并且以蓝藻占绝对优势,绿藻、硅藻次之。浮游藻类密度与透明度的(?)变化成负相关。 相似文献
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1998年春季珠江口海域大规模赤潮原因生物的形态分类和 … 总被引：15，自引：11，他引：4
对１９９８年４月１５日采集于广东珠江口万山群岛网箱养殖区的赤潮新鲜水样和福尔马林固定样品进行赤潮原因生物的形态分类和生物学特征的研究。结果发现,此次赤潮共有７种原因生物,全部属于裸甲藻类,其中最占优种三宅甲藻（Ｇｙｍｎｏｄｉｎｉｕｍ ｍｉｋｉｍｏｔｏｉ）和优势种斯氏多沟藻（Ｐｏｌｙｋｒｉｋｏｓ ｓｃｈｗａｒｔｚｉｉ）。螺旋螺沟藻（Ｇｙｒｏｄｉｎｉｕｍ ｓｐｉｒａｌｅ）的形态分类及生物学特征研究结果 相似文献
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对一种海洋浮游藻色素高效液相色谱分析方法进行了有效性验证。该方法使用反相C8色谱柱,以甲醇、乙腈和丙酮为流动相,并在流动相中添加吡啶/醋酸溶液作为修饰剂改善色素峰的分离效果。结果表明,4种色素标准在一定的浓度范围内线性关系良好,叶绿素a的线性范围为189.6~18 960μg/L,叶绿素b为89.2~8 920μg/L,β,β-胡萝卜素为7.77~777.2μg/L,叶黄素为15.28~1 528μg/L。除β,β-胡萝卜素外各色素标准的回收率在不同浓度下均在90%以上,相对标准偏差也普遍低于5%。在4个参考藻种和123个胶州湾现场样品中共检测出37种色素,一些关键的特征色素均获得了良好的分离效果。该方法操作简便,具有分离度好、灵敏度高、重复性好、回收率高等优点,适用于培养的藻种和现场样品中的海洋浮游藻色素分析。 相似文献
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Dilution experiments were conducted to investigate microzooplankton grazing impact on phytoplankton of different taxonomic groups and size fractions (< 5, 5–20, 20–200 μm) during spring and summer bloom periods at two different sites (inner Tolo Harbour and Tolo Channel) in the Tolo Harbour area, the northeastern coastal area of Hong Kong. Experiments combined with HPLC pigment analysis in three phytoplankton size fractions measured pigment and size specific phytoplankton growth rates and microzooplankton grazing rates. Pigment-specific phytoplankton growth rates ranged between 0.08 and 3.53 d− 1, while specific grazing rates of microzooplankton ranged between 0.07 and 2.82 d− 1. Highest specific rates of phytoplankton growth and microzooplankton grazing were both measured in fucoxanthin in 5–20 μm size fraction in inner Tolo Harbour in summer, which coincided with the occurrence of diatom bloom. Results showed significant correlations between phytoplankton growth and microzooplankton grazing rates. Microzooplankton placed high grazing pressure on phytoplankton community. High microzooplankton grazing impact on alloxanthin (2.63–5.13) suggested strong selection toward cryptophytes. Our results provided no evidence for size selective grazing on phytoplankton by microzooplankton. 相似文献
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《Estuarine, Coastal and Shelf Science》2006,66(1-2):135-146
The dynamics of phytoplankton diversity constitute crucial data in environmental monitoring, food-web studies and ecosystem modeling. Proper assessment of phytoplankton community composition requires large investments in offshore sampling and taxonomic competence because these communities can change fundamentally on a weekly scale. Cheap and high-frequent offshore phytoplankton sampling can be achieved by using ships-of-opportunity, and in the present study we used the Alg@line facilities onboard a passenger ferry during its regular route between Finland and Sweden in the northern Baltic Sea. The first aim was to test if pigment analysis, as a cheaper alternative to cell counts, can be used to detect environment-correlated variation in phytoplankton communities. It has been shown that spatial variation (salinity differences) and variation throughout one annual cycle (changes in temperature and nutrients) were strongly reflected by pigment composition. The second aim was to test if pigment analyses and cell counts detect environment-correlated variation in phytoplankton communities equally well. It has been shown that spatial and seasonal variations were reflected by pigment composition while cell counts reflected seasonal variation only. This suggests that the pigment analyses detected aspects of the phytoplankton that were neglected or misinterpreted by cell counts. It is advocated that available resources of long-term studies, such as environmental monitoring, can be used more efficiently by utilizing the high ecological resolution of pigment composition in combination with high-frequent ships-of-opportunity sampling. To assess heterotrophic and/or toxic species, such programs could also include sampling for cell counts in a complementary manner, with actually performing counts only for crucial samples (e.g. between large community changes) as indicated by multivariate statistical analysis of pigment composition. Some aspects of analyzing phytoplankton data with multivariate statistics are also discussed. 相似文献
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Readman JW Devilla RA Tarran G Llewellyn CA Fileman TW Easton A Burkill PH Mantoura RF 《Marine environmental research》2004,58(2-5):353-358
Characterisation of natural phytoplanktonic communities is currently being advanced through flow cytometry and high resolution pigment analyses. To date, toxicological methods to assess impacts of herbicides on natural phytoplankton populations are lacking. Here, we report the novel use of these techniques in combination to study changes in phytoplankton populations exposed to 2-methylthio-4-tertiary-butylamino-6-cyclopropylamino-s-triazine (Irgarol 1051), a herbicide used in antifouling paints. Flow cytometry results revealed that following a 72-h exposure to approximately 100 ngL(-1), eukaryote abundance was less than half that in the controls. High performance liquid chromatographic analyses of pigments demonstrated that 19'-hexanoyloxyfucoxanthin was selectively lost relative to the control. This carotenoid is specific to the prymnesiophytes which are key constituents of phytoplanktonic communities within temperate marine waters. Values of EC(50) (72 h) as low as 70 ngL(-1) were calculated from the selective reduction in this compound. Concentrations substantially exceeding this level have been reported in UK and other European coastal waters. 相似文献
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稀释法(dilution technique)是研究微型浮游动物摄食和浮游植物生长的常用方法之一,负值浮游植物生长率是稀释实验中常见的现象。分析了造成负值生长率出现的因素,以及这些因素对实验结果的影响,并提出了防止不利影响产生的措施。负值生长率的出现不能简单地视为实验失败的标志,培养光照和温度条件、取样误差、无颗粒水污染、营养盐污染和限制等都可能造成负生长率的出现,且对实验结果的影响不同。同时,根据实验结果,演示浮游植物光适应、取样误差、无颗粒水污染和加富营养盐对稀释实验的影响。结果显示,光照条件可以改变细胞色素含量,且不同浮游植物类群对光照条件的响应不同,从而导致基于色素分析的稀释实验结果出现误差;取样混合不均,可造成取值偏低,导致浮游植物生长率估值偏低,甚至为负值,但可能不影响对摄食率的估算。另外,实验污染(无颗粒水和加富营养盐污染)往往会抑制浮游植物生长,甚至造成浮游植物死亡。因此,培养条件模拟和人为干扰控制是稀释实验成功的关键。 相似文献
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R.K. Naik A.C. Anil D.D. Narale R.R. Chitari V.V. Kulkarni 《Journal of Sea Research》2011,65(4):435-441
Spatial and temporal variations in surface water phytoplankton pigment distribution in the Bay of Bengal were studied during the spring intermonsoon (SpIM, February–April) and the commencement of the summer monsoon (CSM, May–June), using pigment and diagnostic indices. The Prokaryotic pigment index (ProkDP) was dominant at all the oceanic stations whereas the Flagellate pigment index (FlagDP) was dominant at the near coastal stations. However, during the commencement of summer monsoon, an oscillation in the dominance of ProkDP and FlagDP was observed in the central oceanic bay, whereas flagellates and diatoms were dominant at the near coastal stations. This change in pigment pattern is possibly related to the influence of rainfall. Comparison of pigment data with microscopic cell counts indicated a significant relationship between the diatom pigment index (DiatDP) and diatom abundance. However, the relationship between the dinoflagellate pigment index (DinoDP) and dinoflagellate abundance was not significant. Studies coupling pigment composition analysis with microscopic analysis of phytoplankton in natural conditions should thus be a prerequisite in establishing valid biogeochemical and ecosystem models. 相似文献
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Selective transmission of light in the ocean waters and its relation to phytoplankton photosynthesis
Occurrence of the depth differences in pigment composition and photosynthetic properties of marine phytoplankton were examined in relation to the spectral changes of light with depth. Phytoplankton were taken from various depths in the northwestern North Pacific, and their absorption spectra were determined with intact cells and in 90% acetone extract. The photosynthetic activities of phytoplankton were concurrently measured under blue, green, red and white light. The difference in absorption spectra for the surface and deeper samples was considerably small, indicating that the prevailing green or blue light in the deeper layers may have little significance for depth-variations of the pigment composition in marine phytoplankton. The depth differentiation in the shape of the light-photosynthesis curve was marked in a well stratified water column but no active response of deeper phytoplankton to green light could be confirmed. The photosynthetic efficiencies of phytoplankton for blue and green light were approximately 105–115 % and 80–90 % of white light, respectively, irrespective of sampling depth.Contribution No. 261 from Shimoda Marine Biological Station 相似文献
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浮游植物吸收光谱已逐渐成为高光谱水色遥感的可获取参量。文章采用了多层感知器模型, 由珠江口担杆群岛附近水体的浮游植物吸收光谱进行了色素浓度的反演, 感知器的输入量是浮游植物吸收光谱, 输出量分别对应叶绿素a、叶绿素b、叶绿素c、光保护类胡萝卜素和非光保护类胡萝卜素五大类主要色素的浓度。分析结果表明, 叶绿素a和叶绿素c估算结果的平均相对偏差比较低, 在测试数据集中两者的偏差分别为19.06%和15.90%; 光保护类胡萝卜素和非光保护类胡萝卜素的估算浓度的相对偏差比较高, 对于测试数据而言, 分别为37.62%和36.96%; 叶绿素b浓度在测试数据集中的估算相对偏差约为27.47%。五大类色素在测试数据集和训练数据集的估算偏差比较接近, 已训练好的多层感知器可用于担杆岛水体中色素信息的反演。同时, 此色素反演方法也为遥感监测水体浮游植物种群动态提供了重要的手段。 相似文献
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尝试利用放射性同位素14C示踪方法测定浮游植物不同类群的光合速率和生长速率,并通过实验室和现场海域的培养实验来初步评估该技术的可行性.通过高效液相色谱法分离光合色素,手动收集并测定各对应光合色素峰的放射性活度,依据Redalje-Laws法并结合类胡萝卜素标记法计算出各大类群浮游植物的光合速率和生长速率.实验结果表明,在实验室纯种培养的4株藻光合速率范围为347.73~678.98 mg/（dm3.d）,最高的为绿藻的小球藻,最低的为定鞭金藻的球石藻.其生长速率范围为0.12~0.24 d-1,最高的为球石藻,最低的为小球藻.在现场海域各类群的光合速率相对较低,变化范围为0.63~68.78 mg/（dm3.d）,生长速率在0.07~1.68 d-1之间.本研究首次在我国海域通过现场原位测定得到不同类群浮游植物的光合速率和生长速率.但在测定过程中存在的样品含量和放射活度较低等问题还有待于进一步解决. 相似文献
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The study was carried out from April 30 until July 13 of 1997 in Adventfjorden (Spitsbergen). Formation of less saline and warmer surface water (～1 m thick) caused by melting of the fast ice was observed in the fjord during the first days of May. In summer a less saline surface layer was about 3 m thick. Euphotic depth measured under ice sheet reached 12 m, whereas load of mineral matter brought with riverine discharge in summer (the content of total particulate matter in the fjord reached 1.66 kg m?2) dramatically reduced euphotic zone depth to 0.35 m. By pigment measurement three phases of phytoplankton development in Adventfjorden were distinguished: (1) spring bloom that has started under fast ice and reached maximum in the mid of May, (2) stagnation period in June, (3) increase of pigment concentration in July, what could indicate a start of the next algae bloom. Analyses of chlorophylls and carotenoids revealed that diatoms (chl c, fucoxanthin), and green algae (chl b, lutein) dominated phytoplankton community in the fjord. Moreover, the presence of peridinin indicates the presence of Dinophyta and alloxanthin—the occurence of Cryptophyta. In May and June 1997 phytoplankton appeared mainly in the surface of water, while in July, as a result of inflow of turbulent riverine waters into Adventfjorden, algae cells were pushed down and the highest numbers were observed at the depth ～20 m. Great phaeopigments to chl a ratio (= 0.54) found in the fjord seston in June and July probably shows strong impact of zooplankton grazing on phytoplankton development. High contribution of chlorophyllide a in porphyrin a poll in samples collected under fast ice (chlorophyllide a/chl a ratio = 0.18) reflects the final stage of algal communitie succession in ice, just before spring ice melt and release of biota to oceanic water. Chloropyllide a content during summer was minor or not detectable, demonstrating that diatom cells were in good physiological condition. High chl a allomer/chl a ratio (average = 0.11 for the period investigated) confirms high oxygen concentration in environment of Adventfjorden. 相似文献