Composition and distribution of ciliates inner and outer of Daya Bay, China

Daya Bay was undergoing eutrophication process by increased nutrient loading, and the changes in nutrients have strongly influenced the phytoplankton community structure. Ciliates are common component of planktonic community, what role do ciliates play in Daya Bay was still unknown. In this study, ciliates were enumerated and identified from the inner and outer Daya Bay during three seasons. Thirty-one species belong to 16 genera of ciliates were recorded, and Cyclotrichida, Strombidiida, Tintinnida were most common. In spring, ciliates abundance of D2 was lower than D1 and D3, abundance in the surface of D1 and D3 were higher than in the bottom, while D2 showed the opposite character. The lowest ciliate abundance was found in the E1 in summer. In fall, Ciliates abundance of D3 was lower than in fall, and abundance in the surface was lower than in the bottom, which was different compared to in spring. Different hydrographic character was shown between the surface (high temperature, low salinity and nutrients) and bottom layer (low temperature, high salinity and nutrients) at E1 in summer. Ciliate abundance had no significant variation between the surface and bottom at E1 in summer, but ciliates community structure changed a lot.     

大亚湾表层水中溶解无机碳的时空分布

于2010 年12 月～2011 年11 月分4 个季度,对大亚湾海域进行了采样调查,分析了大亚湾表层水体中溶解无机碳(Dissolved inorganic carbon, DIC)含量的时空分布特征,并讨论了大亚湾表层水DIC 与pH、盐度、水温和叶绿素a 等环境因子之间的关系。大亚湾海域表层水DIC 含量的变化范围为19.49～23.20 mg·L^-1,均值为21.13±1.07 mg·L^-1,较黄海及东海水域的DIC 含量低。DIC 的水平分布大致呈现出西部及西北部海域高于东部及湾口海域的趋势。大亚湾表层水DIC 含量呈现出冬季>夏季>秋季>春季的季节变化趋势,但春、夏及秋季差异不大。大亚湾海域表层水的DIC 含量除与盐度呈现了显著的正相关关系外,与pH 值、水温及叶绿素a 显示出负相关,但不显著。大亚湾海域DIC 的时空分布特征是多种因素综合作用的结果,其同时受季风、水温、盐度、水动力、生物地球化学和生物等因子的影响。     

大亚湾大辣甲水域溶解无机碳垂直分布特征及季节动态

于2007年10月～2008年9月进行了4个季节的垂直采样监测,对大亚湾大辣甲水域溶解无机碳(DIC)的垂向分布和季节动态特征进行了研究,分析了大亚湾溶解无机碳与各环境要素(pH、水温、溶解氧和叶绿素a等)的相关性。结果表明:在春、秋和冬季,大亚湾大辣甲水域DIC含量在垂直分布上差异较小,但夏季(2008年7月)变化较为显著,DIC含量的变化范围为16.79～26.52mg·L^-1;DIC高值基本集中在中、底层水域(8～16m),尤以底层水域(13～16m)为甚;DIC含量基本呈现出春、夏季较高,秋、冬季较低的分布趋势;DIC含量与pH值和水温含量显示出了负相关关系,而与盐度呈正相关关系。     

春季和秋季东海陆架区浮游纤毛虫的丰度和生物量

于2011年春季(5月)和秋季(11月)在东海陆架区进行浮游纤毛虫丰度和生物量的调查.春季和秋季纤毛虫的平均丰度分别为(614±861)和(934±809) ind·L^-1,平均生物量分别为(1.70±3.91)和(0.93±0.99) μg C·L^-1.表层纤毛虫丰度和生物量的高值区春季主要分布在近岸及远岸海区,秋季主要分布在远岸海区.春季纤毛虫的丰度和生物量在水体上层较高;秋季纤毛虫主要分布在水体上层,有时在水体底层也会出现丰度和生物量的高值.春季无壳纤毛虫群落的粒级较大,秋季较小.砂壳纤毛虫占纤毛虫丰度的平均比例春季和秋季分别为(26.9±34.3)%和(44.9±25.2)%.两个季节共鉴定出砂壳纤毛虫27属52种,春季丰度较大的种为原始筒壳虫、橄榄领细壳虫及筒状拟铃虫,秋季丰度较大的种为原始筒壳虫、小领细壳虫及矮小拟铃虫.纤毛虫丰度与温度、叶绿素a(Chl a)浓度呈显著正相关.砂壳纤毛虫丰度与盐度呈显著负相关,群落结构变化与温度显著相关.     

大亚湾浮游植物群落特征

于2002年冬、春、夏和秋季对大亚湾浮游植物进行采样调查,分析了浮游植物的种类组成、丰度、优势种、多样性及群落结构的季节变化特征和平面分布特征。并讨论了浮游植物与营养盐、水温及环流等环境因子之间的关系。2002年大亚湾浮游植物共鉴定出48属114种(包括变型和变种),丰度范围在5.79×104~5.37×106cells/m3之间,平均值为1.14×106cells/m3。其中硅藻共37属84种,其种数和细胞丰度都占绝对优势,平均丰度为1.08×106cells/m3,其次为甲藻,9属23种,平均丰度为9.91×104cells/m3。此外还鉴定出蓝藻和金藻。大亚湾浮游植物丰度变化呈单一周期型,春夏季高,秋冬季节低。虽然硅藻的丰度占优势,但秋季硅藻丰度降低(占总丰度75.8%)使甲藻和蓝藻所占比例上升。研究得出春夏季大亚湾浮游植物主要以沿岸暖水性种类为主,秋季和冬季除沿岸暖水种之外,广布种和大洋种也较多,尤其在冬季后者占优势。大亚湾浮游植物优势种类多,不同季节既有交叉又有演替。与以往调查资料相比,部分优势种发生变化,优势程度顺序和细胞丰度发生了一定改变,个体较大的细胞丰度优势逐渐增加。另外,受季风、潮流、地理位置及人类活动影响,大亚湾浮游植物丰度和群落结构有一定的季节和平面分布特征。大亚湾浮游植物的多样性在夏季偏低,尤其在大亚湾核电站和大鹏澳养殖区附近表现明显。大亚湾浮游植物的丰度、种数、优势种演替及群落结构等其它群落特征与营养盐尤其是氮、磷和N/P、水温、环流等环境因子密切相关。     

Dynamic analysis of phytoplankton community characteristics in Daya Bay, China

Daya Bay is a large bay along the southern coast of China. The composition, abundance, community structure and diversity of phytoplankton in Daya Bay were investigated to assess its status in different seasons in 2002, and a total of 48 genera and 114 species of phytoplankton were identified. The cell abundance of phytoplankton varied from 5.79 × 10⁴ cells/m³ to 5.37 × 10⁶ cells/m³ with an average of 1.14×10⁶ cells/m³. The largest community was Bacillariophyta containing 84 taxa, and its average abundance was 1.08 × 10⁶ cells/m³. Annual abundance variations show a typical one-peak cycle, with the highest peak recorded during summer and the lowest recorded during autumn. The ecotypes of phytoplankton were mostly alongshore warm-water species; however, marine warm-water species and eurytopic species during winter and autumn are more abundant than during the other seasons. The dominant species were diverse and varied with seasons. The species diversity index of phytoplankton in Daya Bay was low during summer, especially near the nuclear power station (NPS) and the aquaculture farms during summer and autumn. Community structure and cell abundance were categorized in relation to monsoon, current and anthropological activities. It is presented that the temperature and hydrodynamics in conjunction with the pattern of nutrients (DIN, DIP and N/P) availability and depletion affect the composition, abundance, community structure, community succession and diversity of phytoplankton.     

Dynamic analysis of phytoplankton community characteristics in Daya Bay, China

Daya Bay is a large bay along the southern coast of China. The composition, abundance, community structure and diversity of phytoplankton in Daya Bay were investigated to assess its status in different seasons in 2002, and a total of 48 genera and 114 species of phytoplankton were identified. The cell abundance of phytoplankton varied from 5.79 × 10⁴ cells/m³ to 5.37 × 10⁶ cells/m³ with an average of 1.14×10⁶ cells/m³. The largest community was Bacillariophyta containing 84 taxa, and its average abundance was 1.08 × 10⁶ cells/m³. Annual abundance variations show a typical one-peak cycle, with the highest peak recorded during summer and the lowest recorded during autumn. The ecotypes of phytoplankton were mostly alongshore warm-water species; however, marine warm-water species and eurytopic species during winter and autumn are more abundant than during the other seasons. The dominant species were diverse and varied with seasons. The species diversity index of phytoplankton in Daya Bay was low during summer, especially near the nuclear power station (NPS) and the aquaculture farms during summer and autumn. Community structure and cell abundance were categorized in relation to monsoon, current and anthropological activities. It is presented that the temperature and hydrodynamics in conjunction with the pattern of nutrients (DIN, DIP and N/P) availability and depletion affect the composition, abundance, community structure, community succession and diversity of phytoplankton.     

大亚湾澳头水域浮游植物群落结构及周年数量动态

对1997年至1998年广东省大亚湾澳头水域的浮游植物群落进行调查和分析。结果发现浮游植物65属198种;硅藻在种类组成和数量上都比甲藻占有优势,存在春季和秋季高峰,主要优势类群依次是角毛藻、骨条藻、拟菱形藻等;甲藻只存在春季高峰,代表种类有裸甲藻、原甲藻等。主要优势种类的生长与调查水域的盐度没有明显关系,但全年水温的季节性变化对优势种类的消长影响显著。Simpson多样性指数、Shannon-Weaver多样性指数、均匀度的年平均值分别是0.611、2.107、0.557,多样性指数没有明显的季节变化规律和水平分布规律。       

大亚湾鱼类群落嵌套分布格局

为保护大亚湾渔业资源,2015年4月(春季)、8月(夏季)、10月(秋季)和12月(冬季)对大亚湾进行了4航次底拖网渔业资源调查,结合距最近大陆距离、距最近大岛距离、水深、水温、盐度、叶绿素a、总氮、总磷、鱼类的最大体长和捕捞努力量(CPUE)这些参数,研究了大亚湾鱼类的群聚特征。结果表明,大亚湾鱼类呈嵌套分布格局,鱼类最大体长对嵌套格局的形成具有显著影响;大亚湾鱼类群落嵌套格局的形成支持选择性迁入假说;大亚湾鱼类全年与四季的嵌套最友好位点均在湾口杨梅坑和大辣甲北部海域,此两海域为大亚湾鱼类的主要群聚区,大辣甲北部海域是鱼类的产卵场繁殖区,杨梅坑海域是鱼类的主要育肥区,均应优先进行保护和管理,是开展大亚湾鱼类增殖放流的最适宜海域。     

Observations on the hydrography and inshore plankton of the bay of Bengal of Balasore

The hydrographical features and the inshore plankton of the northern part of the Bay of Bengal was studied from the Balasore coast. The hydrology is mainly governed by the monsoons and river systems flowing into the bay. The surface temperature showed a bimodal pattern with a summer and autumn maximum. The salinity was below the oceanic average with the lowest value during October. The coastal water was found to be rich in nutrients, with peak values during the southwest monsoon. Three phytoplankton blooms followed by zooplankton maxima were observed between early spring and late fall.     

Annual variability in ciliate community structure, potential prey and predators in the open northern Baltic Sea proper

Biomass of ciliates, bacteria and mesozooplankton, as well asbiomass estimates of phytoplankton from chlorophyll a values,were studied in the mixed layer of the northern Baltic Sea proper,between February and December 1998. Production of phytoplanktonand bacteria was measured, and production of ciliates and mesozooplanktonwas estimated. The phytoplankton spring bloom in late Marchwas dominated by diatoms and dinoflagellates. Ciliates had abiomass peak shortly after the spring bloom, while mesozooplanktonpeaked in July. Thus, the predation pressure on ciliates waslow in spring, and ciliates were major predators, potentiallyconsuming up to 15% of the primary production. In summer, therewas a shift from larger to smaller ciliates coinciding witha shift from larger to smaller primary producers, an increasein bacterial production, and also an increase in mesozooplanktonabundance, mainly copepods. Elevated mesozooplankton predationand selective removal of larger ciliate species and/or a shiftto smaller prey size presumably caused these changes. The potentialcarbon consumption from ciliates and mesozooplankton was highestin summer and autumn, reaching 55 and 40% of the primary productionin summer and autumn, respectively. Ciliates consumed twiceas much as mesozooplankton, thus acting as important regenerators.     

太平湖浮游动物动态演替与环境因子的相关性研究

2012年11月至2014年10月, 对太平湖浮游动物群落进行了为期两年的调查研究。共鉴定出浮游动物45属89种, 其中轮虫 29属69种、枝角类5属7种、桡足类2属4种和原生动物9属9种; 优势种主要来自于轮虫异尾轮虫属(Trichocereca)和龟甲轮虫属(Keratella)。浮游动物的丰度值存在明显的季节变化, 表现为夏季最大, 平均达1326 ind./L, 秋季春季次之, 分别为608和605 ind./L, 冬季最小为216 ind./L; 垂直分布表现为春夏季太平湖表层浮游动物丰度最高, 中间层次之, 底层最小, 秋冬季则表现为中间层最高。浮游动物群落Shannon-Wiener多样性指数和Margalef丰富度指数中间层普遍高于表层和底层, Pielou均匀度指数表现为底层要高于表层和中间层, 季节变化表现为夏秋季显著高于冬春季的现象, 水质评价表明夏秋季水质好于春冬季。聚类和多维尺度分析表明: 太平湖浮游动物可分为夏秋季类群与春冬季类群, 两类群均表现为湖心与上下游区域群落结构差异较大, 其中春冬季类群差异较明显; 相关和逐步回归分析表明: 透明度和水温为太平湖浮游动物群落结构变化的主要环境影响因子; 依据结构方程模型(SEM)和冗余分析(RDA)的结果显示, 在溶解氧和水温较高的水环境中浮游动物丰度值表现为较大, 其中水温对轮虫的影响高于对枝角类和桡足类的影响。     

Community characteristics and of zooplankton in Qinzhou Bay

Qinzhou Bay, the biggest bay in Guangxi Province, is very species-rich and is developing a robust marine economy. In recent years, as human impact has increased, problems associated with the environment have become more complicated. Measuring zooplankton diversity and abundance is a way to monitor environmental conditions. According to the data from four ecological surveys of the zooplankton in Qinzhou Bay during 2008 and 2009, a total of 134 species of zooplankton were identified, including 52 Copepoda species, 27 Medusa species, 14 Planktonic larvae, 9 Chaetognatha species, 8 Pteropoda species, 5 Amphipoda species, 4 Cladocera species, 4 Ostracoda species, 3 Thaliacea species, 2 Appendiculata species, 2 Sergestdae species, 2 Protlsta species, 1 Rotiera species and 1 Cumacea species. The fauna was clearly characterized as tropical population. The total species number was highest in autumn, followed by spring, winter and summer. Zooplankton species diversity in Qinzhou Bay has increased compared with the results obtained in 1983–1985 (83 species). However, compared with other bays, the number of zooplankton species in Qinzhou Bay is close to Daya Bay (128), higher than in Zhilin Bay (60), Jiaozhou Bay (81) and Luoyuan Bay (70), and far lower than in the north South Sea (709). We adopted the dominant index Y > 0.02 as the distinguishing standard of dominant species. The number of dominant species in spring, summer, autumn and winter were six, nine, eight and five. There was only one common dominant species (Penilia avirostris) appeared in different seasons, For summer and autumn, the shared dominant species numbered about four. Between other seasons, the shared dominant species varied between two and three. The number of uniquely dominant species was four in summer, three in autumn and one in both spring and winter. The dominant species in different seasons have some overlaps and some differences. The average biomass of zooplankton was 378 mg/m³ at all times of year. The average biomass was largest in autumn, followed by winter, and was the least in spring and summer. The average density of zooplankton for the entire year was 805.11 ind/m³. The average density was largest in summer, followed by winter, and was least in autumn and spring. Copepoda and Planktonic larvae were the major components of zooplankton in spring and summer at Qinzhou Bay, with the other species’ densities under 10%. In autumn, Copepoda, Planktonic larvae and Chaetognatha were the major components of the biomass, and in winter, the major species were Copepoda and Cladocera, with the others species’ density under 10%. The average value of the Shannon–Wiener diversity index (H′) was 3.84 and the evenness index (J′) was 0.77. The zooplankton diversity index and community evenness overall were good and the community organization had a complete and stable state, but the status of the community was relatively weak. The relationship between biomass/density of zooplankton and environmental factors is remarkable. Biomass and density are positively correlated with temperature and nutrient concentration, and are negatively correlated with salinity.     

Seasonal pattern of zooplankton communities and their environmental response in subtropical maritime channels systems in the Bay of Bengal,Bangladesh

Zooplankton are a primary component of aquatic food chain and play an important role in the functioning of aquatic food webs. Seasonal variation in community structures of zooplankton and potential environmental drivers were studied, during a 1-year cycle (summer 2015 – spring 2016) in subtropical maritime channels systems in the Bay of Bengal, coastal waters in Bangladesh. A total of 32 species representing 25 families, 13 orders and 15 taxonomic groups were identified. Of these species, 23 distributed in all four season of which 8 were dominant species with high contributions of the total communities. Species number was peaked in autumn and fell in summer while maximum abundance was in the winter and minimum in summer. Multivariate analyses showed that there was a clear seasonal shift in zooplankton community structures in relation with environmental conditions. Species diversity and evenness peaked in summer while the high value of species richness was found in autumn. Multivariate correlation (RELATE) and BIO-ENV analysis demonstrated that seasonal variation in community patterns was significantly correlated with temporal shift of environmental conditions and that variation mainly driven by water transparency, salinity, DO, TSS and nutrients. Thus, this finding implies that the zooplankton community represented a clear seasonal shift shaped by environmental drivers in subtropical channels systems.     

象山港春、夏季大中型浮游动物空间异质性

为探明象山港大中型浮游动物空间分布特征及主要影响因素,分别于2010年4月、7月大、小潮期对浮游动物群落和相关环境因子进行调查。四个航次共检出浮游动物成体14大类64种、浮游幼体10大类14种,春、夏季群落结构差异极显著(P=0.001),物种更替率为66.7%,优势种差异明显,共同优势种仅有短尾类溞状幼虫(Brachyura zoea)和仔鱼(Fish larvae)两类幼体;同一季节大、小潮物种相似度约为60%,群落结构差异较小(P=0.031);春季生物量和丰度高于夏季,但物种多样性低于夏季。温度是浮游动物群落季节变化的主导因素。方差分析、聚类和多维尺度分析显示:浮游动物群落空间异质性分布方式受潮流影响,群落结构在大潮期梯度分布特征明显,小潮期通常呈斑块性分布;生物量、丰度和多样性等参数的空间分布取决于群落的分布特征,并受影响于该参数在狭湾口内外的差异。典范对应分析及环境参数统计分析表明:梯度分布主要由盐度、悬浮物的梯度性特征决定;主导斑块性分布的因素多样,不同情况下可能为水深、叶绿素a、营养盐和内外水团相互作用;梯度性和斑块性分布均受到潮流影响。总体来看,象山港浮游动物空间分布主要受水文因素控制,受化学和生物因素影响较弱,其中叶绿素a浓度仅在春季与浮游动物丰度有一定相关性,溶解氧、酸碱度和营养盐等水质参数对浮游动物空间分布几乎无直接影响。     

大亚湾亚历山大藻种群周年变动与环境因子的关系

于1997年7月至1998年6月,在大亚湾澳头海域设立6个监测站位,连续监测亚历山大藻(Alexandrium sp.)种群周年变动规律及其与环境因子的关系。大亚湾亚历山大藻种群的密度高峰出现在春季(4月至5月),最高密度达到20.4cells·mL^-1,其它季节则密度较低。亚历山大藻密集出现的温度为22.8～30.0℃、盐度范围为25～30。在亚历山大藻种群密度高峰期里,N/P都较高,DIN含量维持较高水平,有利于亚力山藻的生长,DIP含量却很低,使得此藻比其他藻更具竞争优势。可溶性Fe含量可能成为亚历山大藻增殖的限制性因子。     

大亚湾基础生物生产力及潜在渔业生产量评估

通过对大亚湾海域初级生产力及浮游动物次级生产力的现场调查数据,对该海域潜在渔业生产量及最大可持续渔获量进行了评估。结果表明,大亚湾春季及秋季初级生产力平均值分别为765.23 mgC.m-2.d-1和1786.33 mgC.m-2.d-1,浮游动物次级生产力春季及秋季平均值分别为175 mgC.m-2.d-1和679 mgC.m-2.d-1。采用Tait模式和Cushing模式估算的大亚湾潜在渔业产量分别为3.30万吨和4.78万吨。数据分析结果表明,基于基础生物生产力的评估方法很可能高估了该海区的实际渔业产量,这与基础生物群落结构的改变密切相关;高生物多样性及生态系统结构与功能的健康性是维持渔业资源产量与质量的重要基础。     

Monsoonal and lunar variability in microzooplankton abundance and community structure in the Terusan mangrove creek (Malaysia)

This study documents the monsoonal and lunar effects on species composition and abundance of microzooplankton in a tropical estuary. We investigated microzooplankton abundance in relation to the various environmental and biotic parameters, sampled in the Matang mangrove (Malaysia) from April 2013 to February 2014. A total of 39 microzooplankton taxa comprising four major groups, i.e. loricate ciliates (37.72%), aloricate ciliates (29.46%), dinoflagellates (24.33%) and meroplanktonic nauplii (8.49%) were identified. The loricate ciliates were the most diverse group with 31 taxa recorded. Four major species of loricate ciliates were identified, i.e. Tintinnopsis beroidea, Tintinnopsis rotundata, Stenosemella avellana and Tintinnidium primitivum, while Strombidiidae and Strobilidiidae dominated the aloricate ciliates. Although small loricate ciliates were ubiquitous, redundancy analysis shows marked shifts in microzooplankton community structure, from one that was dominated by loricate ciliates during the drier SW monsoon, to aloricate ciliates at the onset of the wet NE monsoon, and then to dinoflagellates towards the end of the drier NE monsoon period. These shifts were associated with rainfall, dissolved inorganic nutrients, salinity, temperature and microbial food abundance. There was no clear lunar effect on abundance of microzooplankton except for Favella ehrenbergii and copepod nauplii, which were more abundant during neap than spring tides.     

Comparative population ecology of Ephydra hians Say (Diptera: Ephydridae) at Mono Lake (California) and Abert Lake (Oregon)

The population dynamics of Ephydra hians Say final instar larvae and pupae were compared over a two year period in rocky littoral habitats of two alkaline saline lakes in the western Great Basin. Relative abundance increased from 1983 to 1984 at Mono Lake (California), during dilution from ca. 90 to 80 g 1^-1 TDS (total dissolved solids). In contrast, relative abundance decreased over the same period at Abert Lake (Oregon), accompanied by a dilution of salinity from ca. 30 to 20 g l^-1 and a marked increase in the number and abundance of other benthic macroinvertebrate species. These observations are consistent with a hypothesis that proposes biotic interactions limit E. hians abundance at low salinity, and physiological stress limits abundance at high salinity.Oviposition extends from early spring to early fall. Mixed instars present throughout this period indicates multivoltine population dynamics with overlapping generations. The standing stock biomass of final instars increases exponentially in late spring and peaks in late summer or early fall. Pupae increase in proportional representation and abundance from a spring minimum to a fall maximum. The body size of adults and pupae cycle seasonally from a spring maximum to a fall minimum, and may be related to either or both food limitation, or water temperature.     

The distribution and temporal dynamics of the estuarine macroalgal community of San Francisco Bay

Long-term sampling of intertidal macroalgae along permanently marked transects within San Francisco Bay has shown a marked decline in overall species number along the estuarine gradient from the ocean to the river, presumably as a result of decreasing salinity and a progressive lack of hard substrata in the upstream direction. Green algae penetrated further landward than either brown or red species. Seasonally, macroalgal species diversity is lowest during the winter-spring months when salinity, temperature, and irradiance are at yearly minima. Macroalgal abundance as measured by percent cover was maximum during the late spring near the mouth of the estuary and during late summer towards the head. The seasonal increase in algal abundance is related to increasing salinity, temperature, and light availability to the bottom. The summer increase in irradiance is due to the longer photoperiod, increased frequency of day-time low tides, and reduced levels of suspended sediments. The aperiodic occurrence of algal blooms in San Pablo Bay may be caused by a combination of physical factors which are ultimately associated with the river inflow. A hypothesis based on interannual differences in river inflow and the contribution of phytoplankton to nutrient cycles in the benthos is presented to explain the occurrence of nuisance algal blooms.