石油污染对海洋浮游生物的影响

从浮游植物和浮游动物两方面分析了海洋石油污染对海洋浮游生物的影响。石油污染影响多种海洋浮游生物的生长、分布、营养吸收、光合作用及浮游植物参与DMS的产生和循环的过程,可以引发赤潮。石油污染对浮游生物的生长可以表现出促进作用也可表现出抑制作用。由于石油的遮光作用,浮游生物的光合作用受到抑制,进而影响垂直分布及昼夜移动情况。石油污染可由浮游生物经食物链对其它海洋生物产生的影响。     

以色列Kinneret湖多甲藻水华期间浮游植物的P-I曲线

在水域生态系统中,浮游植物的光合作用在很大程度上决定水体可更新资源的丰度以及碳在生物地球化学过程中的通量。为了描述光合作用与光辐射强度的关系,很多作者进行了有益的探索。通过不同的P－I曲线对观察值的拟会,得到了反映光合作用特征的参数。事实上,很多环境因子影响着光合作用的强度和效率,如光强、光周期、温度、营养盐以及浮游植物群落结构等。本研究采用不同的WI曲线模型对以色列kirmeret湖P-I观察值进行拟合,阐明该湖泊夏季浮游植物群落光合作用的特点,并对湖泊中浮游植物的光适应规律作一探讨。1材料和方法1．1湖泊…     

闽南-台湾浅滩近岸上升流区浮游植物碳同化速率的研究

本文采用~(14)C同位素示踪法,测定了浮游植物光合作用速率,结合浮游植物细胞含碳量,计算了不同季节、不同深度下浮游植物碳同化速率常数,讨论了不同环境条件对浮游植物碳同化速率常数的影响。结果表明,闽南-台湾浅滩近岸上升流的形成,是该海域高生产力的主要原因,上升流期间浮游植物复制时间要比非上升流期间浮游植物复制时间缩短1.8倍。同时还表明,温度,光照强度、营养盐是控制浮游植物生长的主要因子。上升流期间营养盐始终保持在较高的水平。是上升流区具有较大的浮游植物碳同化速率常数(3.3d~(-1))的原因之一。适宜该海域浮游植物生长的光照强度在3 000—15 000lx之间,温度的影响可用Goldman和Carpenter模式近似表示。     

浮游动物

不论海水或淡水中,都漂浮着许多微小的生物,叫做浮游生物.这类生物没有运动的能力,或游泳能力很弱,只能随波逐流,因而得名.浮游生物包括浮游植物和浮游动物两大类.浮游植物的种类组成较单纯,常见的如各种硅藻、绿藻和蓝藻,一般能通过光合作用制造有机质,是水中的物质生产者.浮游动物的种类组成较复杂,通常以浮游植物为食,是初级消费者或其他级消费者,因而是水域食物链中重要的一环.     

春季季风转换期间孟加拉湾的初级生产力

2010年中国科学院东北印度洋科学考察期间,对孟加拉湾水域初级生产力展开了研究.孟加拉湾表层水体的水温较高,盐度变化范围较大,且上层水体营养盐含量较低,在真光层底部营养盐浓度突然增加.表层叶绿素a浓度较低(＜0.1 mg/m3),叶绿素a最大值常出现在75 m水深处,上层水体浮游植物的生长受氮限制明显.表层潜在初级生产力低于0.2mgcm-3h-1,且初级生产速率在50-75 m出现最大值.水柱中初级生产力变化范围为199-367 mgCm-2d-1,高值出现在88°-89°(E)附近.浮游植物固碳的主要贡献者是微微型浮游生物(＜3 μm),其次是小型浮游生物(＞20 μm)和微型浮游生物(3-20 μm),但表层与75 m水深处固碳浮游植物的结构有一定差异.将孟加拉湾与阿拉伯海初级生产力进行对比,孟加拉湾水体初级生产力显著低于阿拉伯海,且初级生产力的影响因素有着显著的差异.     

南海北部浮游植物生长对营养盐的响应

2004年夏季作者在南海北部海域研究了浮游植物生长的营养动力学,结合物理-化学过程对浮游植物生物量分布的影响与机制进行了研究,阐明了水平对流和中尺度涡对营养盐分布的影响及浮游植物生长和现存生物量对其的响应。受西南季风和东向沿岸流作用所形成的Ekman输送的影响,南海北部海岸带表层海水作离岸运动,使深层富含营养盐的冷水爬坡涌升到表层来补充,激发浮游植物生物量迅速增长。海区反气旋涡使海水辐聚下沉,造成水体具高温、低盐、高溶解氧浓度、低营养盐浓度和低浮游植物生物量。同时通过现场营养盐加富试验,发现该海域营养盐是浮游植物生长的主要限制因子,而且是多种营养元素共同限制了浮游植物的生长,添加单一的营养盐并不能促进浮游植物的生长。在生物量出现增长的试验组中,营养盐添加不仅促使浮游植物生物量的增长,而且也改变了浮游植物的粒级结构和群落结构。例如,在站S1008,培养前叶绿素a浓度为0.28 mg.m-3,加富培养60 h后浮游植物生物量在NP和NPSi的试验组中有显著的增加,叶绿素a浓度分别达1.07 mg.m-3和1.19 mg.m-3;培养前粒度分级叶绿素a主要以Pico级份占优势,而加富试验结束后,在NP和NPSi的试验组以Nano级份占优势,其它试验组仍以Pico级份占优势;同时,在培养后生物量出现增长的试验组,浮游植物群落的优势类群从甲藻向硅藻演替。     

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.     

深层海洋浮游植物研究综述

对深层海洋(200 m)浮游生物的研究是我国海洋浮游生物研究的前沿,已有的深层海洋浮游生物知识是我国相关研究的基础。浮游植物需要阳光进行光合作用,大多数浮游植物沉降到深海中会死亡,但有些浮游植物却能在深海中生存。综述深层海洋中存活的浮游植物的研究进展,为我国的研究提供参考。在深层海洋发现的浮游植物(2"m)种类不多,共有18种,最深分布在4000 m,颗石藻的丰度大于硅藻和甲藻,最大丰度为2220个/L,出现在500 m。在1911—1985年期间,曾经发现橄榄绿细胞,由于研究手段有限,一直没有对其进行分类学研究。1985年以后的研究怀疑这些橄榄绿细胞就是聚球藻蓝细菌,聚球藻蓝细菌在太平洋、大西洋和地中海的几个站位能分布到2750 m,在深层海洋的最大丰度为3.5×105个/mL,出现在800 m。在许多海区200—700 m发现有浮游植物色素荧光的高值,但对引起高值的原因尚不清楚。浮游植物生物量在深层海洋的垂直剖面研究不多,已有的研究表明浮游植物生物量在300 m以深为0.001—0.1"g C/L,且其随深度增加而降低。     

罗非鱼对盐碱池塘围隔浮游生物群落的影响

本文报道了单养尼罗罗非鱼 (Orecohromisniloticus)对施肥处理下盐碱池塘围隔生态系统浮游生物群落的影响。结果表明 ,罗非鱼的放养使浮游植物丰度、叶绿素a含量和初级生产力增大 ,浮游植物小型化 ,生物量以小型硅藻和绿藻占优势 ,裸藻占有相当比重 ;浮游动物生物量也增大 ,桡足类占优势 ,枝角类小型化 ,原生动物密度增大。施肥特别是施有机肥能显著地提高浮游植物生物量 ,使透明度降低 ,但施无机肥对初级生产力和浮游动物生物量影响不大。施有机肥围隔浮游植物和浮游动物密度、浮游动物生物量和浮游生物多样性指数高于其他有鱼围隔 ,罗非鱼的生长最好。文后讨论了罗非鱼滤食和施肥对浮游生物群落结构的影响 ,并与鲢鱼的实验结果 (赵文 ,1999)进行了比较     

黄海和东海营养盐分布及其对浮游植物的限制

根据1997～1999年黄海和东海4个季节的现场调查资料,分析探讨了黄海、东海的营养盐分布特征及其对浮游植物生长的限制状况．结果表明,在长江口以东及其东北部海域终年存在一个范围很大的营养盐高值区．分析表明,这些营养盐主要来自长江冲淡水的扩展及苏北沿岸流的输送．此外,还获得了1998年长江流域特大洪水期间,迄今被观测到的长江冲淡水中营养盐的最大扩展范围,计算并研究了黄海、东海上层水中Si／N／P比值,结果表明,黄东海上层水中Si／N比值较高,Si不会成为黄东海浮游植物生长的限制因子;但在南黄海南部尤其是西南部、东海近岸及长江口以东海域,N／P比值很高(>30),说明与一般海洋环境的情况不同,黄海、东海有很大一部分海域浮游植物的生长受磷限制,而不是受氮限制．     

The effects of abrupt topography on plankton dynamics

Plankton population dynamics in the upper layer of the ocean depends on upwelling processes that bring nutrients from deeper waters. In turn, these depend on the structure of the vertical velocity field. In coastal areas and in oceanic regions characterized by the presence of strong submarine topographic features, the variable bottom topography induces significant effects on vertical velocities and upwelling/downwelling patterns. As a consequence, large plankton and fish abundances are frequently observed above seamounts, canyons and steep continental shelves. In this work, the dynamics of an NPZ (nutrient-phytoplankton-zooplankton) system is numerically studied by coupling the ecosystem model with a quasi two-dimensional (2D) fluid model with topography. At variance with classical 2D approaches, this formulation allows for an explicit expression of the vertical motions produced when fluid columns are squeezed and stretched as they experience changes of depth. Thus, input or output of nutrients at the surface are associated with fluid motion over the bottom topography. We examine the dynamics of a cyclonic vortex over two basic topographies: a steep escarpment and a submarine mountain. We show that plankton abundance over the escarpment is modulated by the passing of topographic Rossby waves, generated by the vortex-topography interaction. In such configuration, advection effects driven by the flow over the escarpment are of limited relevance for the dynamics of biological fields. By contrast, we find that the flow resulting from the interaction of a vortex with a seamount is sufficiently strong and persistent to allow for a remarkable increase of nutrients, and a corresponding enhancement of phytoplankton and zooplankton concentrations. Over the seamount, advection effects associated with trapped flow perturbations around the summit play an essential role.     

Plankton-toxin interaction with a variable input nutrient

A simple model of phytoplankton–zooplankton interaction with a periodic input nutrient is presented. The model is then used to study a nutrient–plankton interaction with a toxic substance that inhibits the growth rate of plankton populations. The effects of the toxin upon the existence, magnitude, and stability of the periodic solutions are discussed. Numerical simulations are also provided to illustrate analytical results and to compare more complicated dynamical behaviour.     

Nitrogen subsidies to pelagic food webs through profundal methane-oxidising bacteria in oligotrophic fresh water

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Nutrient dynamics and pelagic food web interactions in oligotrophic and eutrophic environments: an overview

The concept of limiting nutrients is a cornerstone of theories concerning the control of production, structure and dynamics of freshwater and marine plankton. The current dogma is that nitrogen is limiting in most marine environments while freshwater ecosystems are mostly phosphorus-limited, although evidence of phytoplankton limitation by either N or P has been found in both environments.However, the same considerations apply to the availability of phosphorus in freshwater as to nitrogen in oceans. In resource-limited environments the plankton dynamics depend mostly on the internal mechanisms which act to recycle the limiting nutrient many times over within the surface waters. As the overall productivity increases, this dependence on nutrient regeneration decreases.The relationship between the stock of limiting nutrient, rates of supply and plankton dynamics must therefore be seen in the light of the processes operating within the entire food chain over quite different time scales. There is strong evidence that process-rates are mostly size-dependent and that food web interactions at the microbial level (picophytoplankton, bacteria, microheterotrophs) strongly effect the production of carbon and the regeneration of nutrients in the pelagic zone.     

Interaction among Non-toxic Phytoplankton,Toxic Phytoplankton and Zooplankton: Inferences from Field Observations

We explore the mutual dependencies and interactions among different groups of species of the plankton population, based on an analysis of the long-term field observations carried out by our group in the North–West coast of the Bay of Bengal. The plankton community is structured into three groups of species, namely, non-toxic phytoplankton (NTP), toxic phytoplankton (TPP) and zooplankton. To find the pair-wise dependencies among the three groups of plankton, Pearson and partial correlation coefficients are calculated. To explore the simultaneous interaction among all the three groups, a time series analysis is performed. Following an Expectation Maximization (E-M) algorithm, those data points which are missing due to irregularities in sampling are estimated, and with the completed data set a Vector Auto-Regressive (VAR) model is analyzed. The overall analysis demonstrates that toxin-producing phytoplankton play two distinct roles: the inhibition on consumption of toxic substances reduces the abundance of zooplankton, and the toxic materials released by TPP significantly compensate for the competitive disadvantages among phytoplankton species. Our study suggests that the presence of TPP might be a possible cause for the generation of a complex interaction among the large number of phytoplankton and zooplankton species that might be responsible for the prolonged coexistence of the plankton species in a fluctuating biomass.     

鲤鱼种和鲢鳙对池塘浮游生物的影响

本文根据１９９０年－９月对９个鱼池的研究,报道鲤鱼种和鲢鳙对浮游生物的影响,结果表明：鲤鱼种使浮游植物和浮游动物生物量增加,浮游植物大型化,浮游动物小型化,并使浮游植物多样性增加,浮游动物多样性下降;鲢鳙密度增加,浮生物小型明显,微型藻类和超微在在浮植物中所占比重显著增加,小型浮游动物（原生动物和轮虫）在浮游动物中比重也明显增;鲢鳙密度对浮游生物多样性和浮游生物量的影响具有阶段性,当鲢鳙密度低时,     

Effects of silver carp (Hypophthalmichthys molitrix) and nutrients on the plankton community of a deep,tropical reservoir: an enclosure experiment

1. An in situ enclosure experiment was conducted in a deep reservoir of southern China to examine (i) the effects of a low biomass (4 g wet weight m^?3) of silver carp (Hypophthalmichthys molitrix) and nutrients on the plankton community and (ii) the response of Daphnia to eutrophication. 2. In the absence of fish, Daphnia galeata dominated the zooplankton community, whereas calanoids were dominant in the fish treatments, followed by D. galeata. Silver carp stocking significantly reduced total zooplankton biomass, and that of D. galeata and Leptodorarichardi, but markedly increased the biomass of smaller cladocerans, copepod nauplii and rotifers. In contrast, nutrient enrichment had no significant effect on the plankton community except for cyclopoids. 3. Chlorophyta, Cryptophyta and Bacillariophyta were dominant phytoplankton groups during the experiment. Chlorophyta with high growth rates (mainly Chlorella vulgaris in the fish enclosures and Ankyra sp. in the fishless enclosures) eventually dominated the phytoplankton community. Total phytoplankton biomass and the biomass of edible phytoplankton [greatest axial linear dimension (GALD) < 30 μm], Chlorophyta, Cryptophyta, Bacillariophyta and Cyanobacteria showed positive responses to fish stocking, while inedible phytoplankton (GALD ≥ 30 μm) was significantly reduced in the fish enclosures. However, there was no significant effect on the plankton community from the interaction of fish and nutrients. 4. Overall, the impact of fish on the plankton community was much greater than that of nutrients. High total phosphorus concentrations in the control treatment and relatively low temperatures may reduce the importance of nutrient enrichment. These results suggest it is not appropriate to use a low biomass of silver carp to control phytoplankton biomass in warmer, eutrophic fresh waters containing large herbivorous cladocerans.     

The effects of abrupt topography on plankton dynamics

Plankton population dynamics in the upper layer of the ocean depends on upwelling processes that bring nutrients from deeper waters. In turn, these depend on the structure of the vertical velocity field. In coastal areas and in oceanic regions characterized by the presence of strong submarine topographic features, the variable bottom topography induces significant effects on vertical velocities and upwelling/downwelling patterns. As a consequence, large plankton and fish abundances are frequently observed above seamounts, canyons and steep continental shelves. In this work, the dynamics of an NPZ (nutrient-phytoplankton-zooplankton) system is numerically studied by coupling the ecosystem model with a quasi two-dimensional (2D) fluid model with topography. At variance with classical 2D approaches, this formulation allows for an explicit expression of the vertical motions produced when fluid columns are squeezed and stretched as they experience changes of depth. Thus, input or output of nutrients at the surface are associated with fluid motion over the bottom topography. We examine the dynamics of a cyclonic vortex over two basic topographies: a steep escarpment and a submarine mountain. We show that plankton abundance over the escarpment is modulated by the passing of topographic Rossby waves, generated by the vortex-topography interaction. In such configuration, advection effects driven by the flow over the escarpment are of limited relevance for the dynamics of biological fields. By contrast, we find that the flow resulting from the interaction of a vortex with a seamount is sufficiently strong and persistent to allow for a remarkable increase of nutrients, and a corresponding enhancement of phytoplankton and zooplankton concentrations. Over the seamount, advection effects associated with trapped flow perturbations around the summit play an essential role.