南麂列岛海洋自然保护区浮游植物的种类多样性及其生态分布

于2006年5月至2007年2月之间,对南麂列岛海域的浮游植物类群进行了4个季节的调查,分析了该海域浮游植物的种类组成、优势种类、群落结构以及水平分布等特征参数的季节变化。共鉴定浮游植物80种,隶属于4个门,硅藻种类最多,甲藻其次。浮游植物可划分为3个生态类群,以广温类群为主。春季和夏季分别以三角棘原甲藻和中肋骨条藻为绝对优势种,秋冬季的优势种类组成多样化。共鉴定57种赤潮生物,占浮游植物种类数的71.25%。调查期间,三角棘原甲藻和中肋骨条藻分别于春季和夏季形成赤潮。浮游植物的物种丰富度呈现春、夏、秋、冬递减的趋势。浮游植物细胞丰度的年平均值为1.03×106cells/L,春夏季显著高于秋冬季。春季和夏季时,浮游植物高值区集中在南麂岛西北近岸海域;秋季和冬季时,浮游植物高值区相对集中在南麂岛东南近岸海域。浮游植物群落的多样性指数(H')以秋季最高,冬季最低。春季的三角棘原甲藻赤潮期间,水体中N/P值显著升高;夏季的中肋骨条藻赤潮期间,水体中N/P值显著降低。     

春季东海中华哲水蚤对有害藻华物种的选择性摄食

2005年4月27日—6月5日在东海有害藻华高发区的6个典型站位采样,分析了浮游植物的群落结构,并采用现场实验研究了中华哲水蚤(Calanus sinicus)的选择性摄食.结果表明,中华哲水蚤对浮游植物的选择性摄食具有食物密度依赖性.低浮游植物细胞丰度下中华哲水蚤具有明显的选择性摄食行为,高浮游植物细胞丰度下中华哲水蚤摄食选择性由偏好转变为排斥,浮游植物细胞丰度329 cells·ml^-1是中华哲水蚤由偏好趋于排斥摄食的阈值.中华哲水蚤的选择性摄食还与食物组成有关,对于食物中的微型浮游动物,中华哲水蚤无选择性或排斥摄食.有害藻华发生区中华哲水蚤对具齿原甲藻(Prorocentrum dentatum)的偏好摄食以及对米氏凯伦藻(Karenia mikimotoi)的排斥摄食,促使藻华的物种演替最终向米氏凯伦藻水华方向发展.     

2006年春夏期间浙江南麂海域浮游植物群落结构特征

研究了2006年春夏期间(4~6月)浙江省南麂列岛海域的浮游植物群落结构,共观察到68种浮游植物,其中硅藻53种,甲藻13种,金藻和蓝藻各1种。调查期间,该海域浮游植物群落结构变化明显,原甲藻赤潮的形成和持续是最显著的特征,三角棘原甲藻和东海原甲藻分别在5月中、下旬先后引发赤潮。原甲藻赤潮的形成与水温有密切关系,其生消引起海水中营养盐结构的相应变化。     

1996年德国石荷西部沿岸水域浮游植物种群变动及其整齐圆筛藻赤潮

1996年早春至初夏,德国石荷州西海岸水域尤其是在易白河河附近海区发生了数次赤潮事件,河口区的高叶绿素浓度总是与低盐、高营养盐浓度的分布区吻合。从早春3月至5月底,发生了持续时间很长的大规模赤潮事件,其引发赤潮原因种为整齐圆筛藻,6月份对浮游植物生物量的贡献主要来自几种硅藻如微小细柱藻、聚生角毛藻、远洋角毛灌以及属于鞭毛藻类的棕囊藻群体,7月中旬,自养的纤毛虫类Myrionecta rubra (Mesodinium rubrum）达到数量高峰。从7月下旬至8月中旬,以梭形角藻、叉状角藻占优势的甲藻类几科贡献了全部的浮游植物生物量,8月中旬至9月上旬为甲藻和硅藻等类别的混合期,9月中旬以后,硅藻重新占据浮激植物 数量的绝对优势,主要优势种为浮动弯角藻、复瓦根管藻等,该海域浮游植物种群的演替反映了温带海域的特征。在早期发生的大规模赤潮期间,整齐圆筛藻的细胞密度达到2180cells dm^-3,与之相对应的生物量为758.1μg C dm^-3,占浮游植物生物量的94.2%,整齐圆筛藻的爆发性增殖所产生的大量油膜覆盖了黑尔果兰岛和东Frisian群岛周围的海域,这一现象有史以来第一次被卫星所观测到。     

藻华发生过程中胶州湾水体颗粒有机物脂肪酸的组成与动态

胶州湾在2005年夏季发生了中肋骨条藻(Skeletonema costatum ( Grev.) Cleve)藻华,该优势种占细胞总量的比例在两个研究站位(C3站及A5站)分别达到59%和86%.对藻华发生过程中(7月,8月及9月份)的颗粒有机物进行了采样分析,测定了脂肪酸、叶绿素(Chl-a)和颗粒有机碳(POC)的浓度,分析了藻华发生过程中浮游植物和脂肪酸的组成特征,并通过标志脂肪酸对藻华发生过程中颗粒有机物组成的动态变化进行了分析.总脂肪酸浓度同叶绿素和颗粒有机碳浓度一样,在藻华发生期达到最高,两个采样站位(C3站及A5站)分别为29.0μg·L-1及185.5μg·L-1,比藻华发生前和消退后高2～3倍及20倍.胶州湾悬浮颗粒脂肪酸主要包括16:0,14:0,18:0等直链饱和脂肪酸(SSFA),16:1ω7、16:1ω5+ω9、18:1ω9,18:1ω7等单不饱和脂肪酸(MUFA)及以 20:5ω3(DHA)和22:6ω3(EPA)为主的多不饱和脂肪酸(PUFA)和以i-15:0及ai-15:0为主的支链饱和脂肪酸(BSFA).藻华期与发生前相比,脂肪酸中的不饱和组分(MUFA,PUFA)所占比例在两个取样站位均有提高.随着藻华的消退,藻华区域中心的A5 站的SSFA及BSFA比例有大幅提高,而在非藻华中心区域的C3站,不饱和脂肪酸尤其是ω3系列多不饱和脂肪酸(DHA, EPA等)比例的上升非常显著.藻华发生时浮游植物在颗粒有机物中的比重提高.藻华消退后,A5站颗粒有机物中碎屑有机物及细菌所占比重提高,而C3站颗粒有机物中浮游植物的比重仍然很高.浮游植物大量死亡是A5站藻华消退的主要形式,而C3站藻华的消退则可能与浮游动物的摄食有关.     

涠洲岛海域球形棕囊藻藻华过程中营养盐及浮游植物群落组成分析

球形棕囊藻(Phaeocystis globosa)是近年来北部湾常见的有害藻华原因种,涠洲岛海域作为广西沿海藻华的高发区之一,目前仍缺乏关于该海域球形棕囊藻藻华过程的相关研究。为探究涠洲岛海域球形棕囊藻藻华过程中营养盐的状况及藻华的发生对浮游植物群落组成的影响,对2017年3月下旬涠洲岛周边发生的球形棕囊藻藻华区域进行取样调查。结果表明,藻华期间水体中溶解有机磷含量与细胞及囊体密度呈显著正相关。本次藻华主要受水体中溶解态无机氮含量影响,多个调查站点的无机氮/无机磷(DIN/DIP)<10,且硅酸盐/无机氮(SiO₃^2–/DIN)>1,表明这些站点存在氮限制现象,而氮限制可能是本次藻华消亡的主要因素。调查区域共鉴定出浮游植物4门58种,球形棕囊藻细胞密度最高可达1.04×10⁸ cells/L,占浮游植物总细胞密度的98.28%。球形棕囊藻细胞密度与物种多样性指数存在显著的负相关关系。在营养缺乏条件下,有利于球形棕囊藻成囊的链状硅藻种类具有相对较大的细胞密度。     

辽宁近岸浑浊海域网采浮游生物的粒径结构特征

河口及近岸海域环境复杂,浮游生物反馈调节频繁,粒径结构极不稳定.本文对辽宁近岸河口区和港口区浑浊带海域的浮游生物粒径结构进行研究.结果表明:在无机氮含量高的浑浊带海域,浮游植物生物量主要集中在20 μm＜ESD(等效球径,equivalent sphere diameter) ＜100μm小粒径区域;而在低营养盐的清洁海域,浮游植物生物量主要集中在ESD＞100 μm大粒径区域.表明浮游植物群落对高浓度悬浮物的响应可能通过小粒径生物进行反馈调节,使圆筛藻(Coscinodiscus sp.)等大粒径浮游植物生物量组成降低,将影响以摄食这些饵料为主的各种鱼虾幼体资源量.另外,本文构建了标准生物量谱,它符合北方近岸浅海、富营养化水域生态系统的特征,谱线斜率表明,研究海域浮游生物群落的生物量随着粒级的增加而逐渐增大.探讨了甲藻和枝角类作为评估悬浮物污染的指示生物的可行性.     

舟山海域春季浮游植物生物量及东海原甲藻赤潮频发机制初探

通过2002和2003年春季2个航次对东海舟山群岛及其邻域大面站的浮游植物及期间爆发的大规模东海原甲藻(Prorocentrum donghaiense)赤潮的综合调查,研究了调查海区浮游植物叶绿素a和营养盐的分布特性,分析了赤潮高发区域的生态环境特征,探讨了诱发和控制海域赤潮发生的环境因子.结果表明,2002和2003年春季大面站表层平均叶绿素a浓度分别为1.09±1.63和4.21±5.33 mg·m^-3,调查海区平均为0.70±0.48和2.60±2.99 mg·m^-3,叶绿素a浓度的高值区基本上位于122.5°～123°E间冲淡水形成的锋面区域,此区域营养盐可以得到充分补充,光照条件适宜,也是浮游植物生产力的高值带.2002和2003年东海原甲藻赤潮跟踪期间,表层平均叶绿素a浓度分别高达18.45±11.04和12.47±8.15 mg·m^-3.赤潮发生海域盐度在26～30,赤潮藻生长易受磷的限制.光照条件适宜、营养盐(特别是磷酸盐)能得到较快的补充及锋面辐聚带的形成是赤潮形成的重要条件.     

南麂列岛砂质潮间带底栖硅藻多样性与群落结构的时空变化

为了解南麂列岛国家级海洋自然保护区砂质潮间带底栖硅藻多样性与群落结构的现状及近20多年来的变化,于2013年11月至2014年8月,对南麂列岛火焜岙砂质潮间带的底栖硅藻进行了4个季节的采样和研究,并与1981–1993年有关的历史资料进行了比较分析。本研究共鉴定底栖硅藻49属120种,海岸曲解藻(Fallacia litoricola)、史氏双壁藻(Diploneis smithii)、稀疏双壁藻(D.parca)等17种为目前的优势种。Shannon多样性指数在2.388–3.445之间,以春季最高,秋季最低;在空间分布上依次为:中潮区低潮区高潮区。相似性分析(analysis of similarities,ANOSIM)表明底栖硅藻群落在不同潮区间差异显著,而季节差异不显著。BIOENV分析显示盐度与底栖硅藻群落结构的相关性最高。本研究结果表明,南麂列岛砂质潮间带的底栖硅藻群落结构近几十年来已发生了明显变化。与1981–1993年南麂列岛的3次调查数据相比,目级阶元减少了2个,科级阶元增加了7个,而属级和种级阶元较过去的29属55种有了显著增加,这可能是分类研究强度增加所致。但分类学多样性降低,平均分类差异指数Δ+由过去的79.79降至71.41;且过去记录的大个体固着类群被现今的小个体固着类群和间隙运动类群(epipelon)所取代,这可能是火焜岙过去人类活动频繁、有机质过量排放的长期效应所致。     

南麂列岛海洋保护区浮游动物调查

主要研究南麂列岛海洋保护区浮游动物种类组成、数量分布、多样性指数、浮游动物与浮游植物动态变化及浮游动物数量变化与营养盐的关系。经鉴定共发现,浮游动物98种,主要有2个生态类群:(1)暖温带近海类群,优势种有中华哲水蚤(Calanus sinicus)、中华假磷虾(Pseudeuphausia sinicas)、五角水母(Muggiaea atlantica)、百陶箭虫(Sagitta bedoti)、拿卡箭虫(S.nagae)等;(2)暖水性外海类群,代表性种类有肥胖箭虫(S.enflata)、精致真刺水蚤(Euchaeta concinna)等。结果表明,8月份南麂列岛浮游动物生物量和丰度出现最高值,9、10月份逐渐减少,多样性指数变化范围1.78~4.38,平均3.99;保护区内浮游动物数量与浮游植物细胞密度呈良好的正相关关系,与氮含量呈负相关关系。     

Phytoplankton growth rates in the freshwater tidal reaches of the Schelde estuary (Belgium) estimated using a simple light-limited primary production model

During the course of 1996, phytoplankton was monitored in the turbid, freshwater tidal reaches of the Schelde estuary. Using a simple light-limited primary production model, phytoplankton growth rates were estimated to evaluate whether phytoplankton could attain net positive growth rates and whether growth rates were high enough for a bloom to develop. Two phytoplankton blooms were observed in the freshwater tidal reaches. The first bloom occurred in March and was mainly situated in the most upstream reaches of the freshwater tidal zone, suggesting that it was imported from the tributary river Schelde. The second bloom occurred in July and August. This summer bloom was situated more downstream in the freshwater tidal reaches and appeared to have developed within the estuary. A comparison between phytoplankton growth rates estimated using a simple primary production model and flushing rate of the water indicated that no net increase in phytoplankton biomass was possible in March while phytoplankton could theoretically increase its biomass by 20% per day during summer. Chlorophyllaconcentrations at all times decreased strongly at salinities between 5–10 psu. This decline was ascribed to a combination of salinity stress and light limitation. Phytoplankton biomass and estimated annual net production were much higher in the freshwater tidal zone compared to the brackish reaches of the estuary (salinity > 10 psu) despite mixing depth to euphotic depth ratios being similar. Possible reasons for this high production include high nutrient concentrations, low zooplankton grazing pressure and import of phytoplankton blooms from the tributary rivers.     

Student's tutorial on bloom hypotheses in the context of phytoplankton annual cycles

Phytoplankton blooms are elements in repeating annual cycles of phytoplankton biomass and they have significant ecological and biogeochemical consequences. Temporal changes in phytoplankton biomass are governed by complex predator–prey interactions and physically driven variations in upper water column growth conditions (light, nutrient, and temperature). Understanding these dependencies is fundamental to assess future change in bloom frequency, duration, and magnitude and thus represents a quintessential challenge in global change biology. A variety of contrasting hypotheses have emerged in the literature to explain phytoplankton blooms, but over time the basic tenets of these hypotheses have become unclear. Here, we provide a “tutorial” on the development of these concepts and the fundamental elements distinguishing each hypothesis. The intent of this tutorial is to provide a useful background and set of tools for reading the bloom literature and to give some suggestions for future studies. Our tutorial is written for “students” at all stages of their career. We hope it is equally useful and interesting to those with only a cursory interest in blooms as those deeply immersed in the challenge of understanding the temporal dynamics of phytoplankton biomass and predicting its future change.     

Phytoplankton distribution patterns in the northwestern Sargasso Sea revealed by small subunit rRNA genes from plastids

Phytoplankton species vary in their physiological properties, and are expected to respond differently to seasonal changes in water column conditions. To assess these varying distribution patterns, we used 412 samples collected monthly over 12 years (1991–2004) at the Bermuda Atlantic Time-Series Study site, located in the northwestern Sargasso Sea. We measured plastid 16S ribosomal RNA gene abundances with a terminal restriction fragment length polymorphism approach and identified distribution patterns for members of the Prymnesiophyceae, Pelagophyceae, Chrysophyceae, Cryptophyceae, Bacillariophyceae and Prasinophyceae. The analysis revealed dynamic bloom patterns by these phytoplankton taxa that begin early in the year, when the mixed layer is deep. Previously, unreported open-ocean prasinophyte blooms dominated the plastid gene signal during convective mixing events. Quantitative PCR confirmed the blooms and transitions of Bathycoccus, Micromonas and Ostreococcus populations. In contrast, taxa belonging to the pelagophytes and chrysophytes, as well as cryptophytes, reached annual peaks during mixed layer shoaling, while Bacillariophyceae (diatoms) were observed only episodically in the 12-year record. Prymnesiophytes dominated the integrated plastid gene signal. They were abundant throughout the water column before mixing events, but persisted in the deep chlorophyll maximum during stratified conditions. Various models have been used to describe mechanisms that drive vernal phytoplankton blooms in temperate seas. The range of taxon-specific bloom patterns observed here indicates that different ‘spring bloom'' models can aptly describe the behavior of different phytoplankton taxa at a single geographical location. These findings provide insight into the subdivision of niche space by phytoplankton and may lead to improved predictions of phytoplankton responses to changes in ocean conditions.     

Timing of blooms,algal food quality and Calanus glacialis reproduction and growth in a changing Arctic

The Arctic bloom consists of two distinct categories of primary producers, ice algae growing within and on the underside of the sea ice, and phytoplankton growing in open waters. Long chain omega‐3 fatty acids, a subgroup of polyunsaturated fatty acids (PUFAs) produced exclusively by these algae, are essential to all marine organisms for successful reproduction, growth, and development. During an extensive field study in the Arctic shelf seas, we followed the seasonal biomass development of ice algae and phytoplankton and their food quality in terms of their relative PUFA content. The first PUFA‐peak occurred in late April during solid ice cover at the onset of the ice algal bloom, and the second PUFA‐peak occurred in early July just after the ice break‐up at the onset of the phytoplankton bloom. The reproduction and growth of the key Arctic grazer Calanus glacialis perfectly coincided with these two bloom events. Females of C. glacialis utilized the high‐quality ice algal bloom to fuel early maturation and reproduction, whereas the resulting offspring had access to ample high‐quality food during the phytoplankton bloom 2 months later. Reduction in sea ice thickness and coverage area will alter the current primary production regime due to earlier ice break‐up and onset of the phytoplankton bloom. A potential mismatch between the two primary production peaks of high‐quality food and the reproductive cycle of key Arctic grazers may have negative consequences for the entire lipid‐driven Arctic marine ecosystem.     

Increased intrusion of warming Atlantic water leads to rapid expansion of temperate phytoplankton in the Arctic

The Arctic Ocean and its surrounding shelf seas are warming much faster than the global average, which potentially opens up new distribution areas for temperate‐origin marine phytoplankton. Using over three decades of continuous satellite observations, we show that increased inflow and temperature of Atlantic waters in the Barents Sea resulted in a striking poleward shift in the distribution of blooms of Emiliania huxleyi, a marine calcifying phytoplankton species. This species' blooms are typically associated with temperate waters and have expanded north to 76°N, five degrees further north of its first bloom occurrence in 1989. E. huxleyi's blooms keep pace with the changing climate of the Barents Sea, namely ocean warming and shifts in the position of the Polar Front, resulting in an exceptionally rapid range shift compared to what is generally detected in the marine realm. We propose that as the Eurasian Basin of the Arctic Ocean further atlantifies and ocean temperatures continue to rise, E. huxleyi and other temperate‐origin phytoplankton could well become resident bloom formers in the Arctic Ocean.     

The phytoplankton community of a eutrophic reservoir

The dynamics of the phytoplankton community of a eutrophic reservoir are described for a two year period. Fifty-eight species were recorded, 25 of them common. Bacillariophyta dominated during the winter and early spring and Chlorophyta during late spring, to be replaced by a bloom of Cyanophyta. The mean and peak biomass of phytoplankton was 8.6 mg 1^–1 and 40.8 mg 1^–1 in 1981, and 8.3 mg 1^–1 and 37.6 mg 1^–1 in 1982. Temperature accounted for 67.3% and pH for 8% of the variation in total phytoplankton biomass over the two year period, using a multiple regression technique.Both horizontal and vertical patchiness, measured as an index of mean crowding, were recorded in the reservoir. Horizontal aggregations were associated with spring blooms of Chlorophyta and summer blooms of Cyanophyta, while vertical aggregations were most marked during the summer bloom of Cyanophyta. Concentrations of phytoplankton were influenced by wind, the prevailing southwesterly wind accumulating algae in the northeasterly arm of the reservoir during much of the year.     

Changes to the phytoplankton assemblage of Lake Kinneret after decades of a predictable, repetitive pattern

1. Phytoplankton abundance and species composition in Lake Kinneret, Israel, have been monitored at weekly or fortnightly intervals since 1969. This paper summarises the resulting 34‐year phytoplankton record with a focus on the last 13 years of new data, and reassesses an earlier conclusion that the lake phytoplankton shows remarkable stability despite a wide range of external pressures. 2. The Kinneret phytoplankton record can be split into two major periods. The first, from 1969 till 1993, was a period of distinct stability expressed by a typical annual pattern revolving around a spring bloom of the dinoflagellate Peridinium gatunense that repeated each year. The second period, starting around 1994 and ongoing, is characterised by the loss of the previously predictable annual pattern, with both ‘bloom years’ and ‘no‐bloom years’. 3. In the second period, deviations from the previous annual pattern include: the absence of the prevailing spring P. gatunense blooms in some years and increased variability in the magnitude of the bloom in others; intensification of winter Aulacoseira granulata blooms; higher summer phytoplankton biomass with replacement of mostly nanoplanktonic, palatable forms by less palatable forms; new appearance and establishment of toxin‐producing, nitrogen fixing cyanobacteria in summer; increase in the absolute biomass and percentage contribution of cyanobacteria to total biomass; and fungal epidemics attacking P. gatunense. 4. The 34‐year record serves to validate Schindler's (1987) assessment that phytoplankton species composition will respond to increased anthropogenic stress before bulk ecosystem parameters.     

Short-term variations in the physiological state of phytoplankton [2pt] in a shallow temperate estuary

Short-term changes in the photosynthetic carbon metabolism and physiological state of phytoplankton were studied over a summer fortnight-long period in the Urdaibai estuary (Bay of Biscay) and related to observed environmental patterns. Day-to-day variability in the hydrographical and biological features of the estuary during the study period was due to changes in meteorological and tidal conditions. Phytoplankton biomass and primary production increased with the improvement of weather, i.e., light conditions, during neap tides. Thus a mixed bloom of cryptophyceans, Euglena sp., and the dinoflagellate Peridinium foliaceum developed in the middle and upper estuary. Photosynthetic responses of phytoplankton were related to the time-scale of changes in light regime. Allocation of photosynthate to major macromolecular classes (LMWM, lipid, polysaccharide, and protein), like phytoplankton biomass and primary production, showed strong spatio-temporal variability. High carbon fixation into low molecular weight metabolites was associated with growth limitation by low light. The relative incorporation of photosynthetic carbon into proteins increased at the beginning of the phytoplankton bloom but overall, it was rather constant. However, carbon allocation into storage products such us lipid or polysaccharide increased when carbon and energy produced under optimal growth conditions exceeded what could be assimilated into protein. These patterns are explained by both spatio-temporal changes in the environmental conditions and species-specific differences. In general, daily variability appeared to be more important than diurnal periodicity in the physiological responses of phytoplankton. Results from this study show that phytoplankton photosynthesis and carbon metabolism are simultaneously affected by biotic and abiotic factors, although short-term light fluctuations may have a major influence on the physiological state of phytoplankton in the Urdaibai estuary.     

中国近海生物固碳强度与潜力

通过现场调查和数据分析,首次探讨了中国近海浮游植物的固碳强度与潜力以及近海人工养殖大型藻类的固碳能力.结果表明,渤、黄、东海的浮游植物固碳强度约为2.22亿t a-1,固碳量的季节变化从大到小的顺序依次为春季、夏季、秋季、冬季,其中春夏季的固碳量占全年的65.3%.南黄海1999～2005年10～11月间浮游植物固碳强度有较大的年际变化,10～11月份7a间其浮游植物最低固碳量为3.54万t d-1,最高为16.58万t d-1,平均为10.50万t d-1,没有明显的年际变化趋势,磷对浮游植物固碳强度的影响最为明显,次之的影响因素是Chl a和亚硝氮 (NO2-N)的含量.南海的固碳能力约为渤黄东海的2倍,为4.16亿t a-1,其季节变化和渤黄东海不同,南海浮游植物在冬季的固碳能力最强,在夏季最弱.整个中国近海浮游植物年固碳量达6.38亿t,可占全球近海区域浮游植物年固碳量的5.77%.实际外海龙须菜的养殖发现,龙须菜每年固定的碳为8.18 t,养殖密度与方式对其产量和固碳量影响巨大.近几年,我国大型经济藻类养殖产量每年在120～150万t左右,换算为固碳量为36～45万t,平均每年40万t,如果海藻养殖产量每年增加5%,到2010年,我国大型经济藻类养殖的固碳量可达57万t a-1,海藻养殖是海洋增加碳汇有多重价值的重要措施.