The kinetics of algal photoadaptation in the context of vertical mixing

The responses of phytoplankton to turbulent motions in the surfacemixed layer can be measured to estimate the rate of verticalmixing. If the time scale for the response (photoadaptation)is shorter than that for vertical mixing, phytoplankton willexhibit a vertical gradient associated with adaptation to ambientlight, whereas if mixing occurs with a time scale shorter thanthat of photoadaptation, the surface mixed layer will be uniformwith respect to the photoadaptive parameter. To examine thephysiological bases for a model of vertical mixing and photoadaptation,we grew the marine diatom Thalassiosira pseudonana (clone 3H)at three photon flux densities and subjected the cultures toreciprocal light shifts, measuring physiological and chemicalchanges over the following 10 h. Several parameters, easilymeasured in nature and attributable primarily to phytoplankton,responded to fluctuating light on different time scales. Aftercultures were exposed to relatively bright light, both the initialslope of the photosynthesis-irradiance curve and in vivo fluorescencewere depressed on a time scale of less than an hour. Photosyntheticcapacity was also reduced transiently, but recovered over manyhours to a high level characteristic of an adapted state. First-orderkinetics (the current model of choice for describing photoadaptation)reasonably described the rapid responses of phytoplankton tobright light, but other parameters (i.e. cellular chemical compositionand photosynthetic capacity) changed as a result of unbalancedgrowth and required much longer to adapt from low to high lightas compared to from high to low light. A logistic model of thisadaptation is presented. The model suggests that hysteresisof adaptation during vertical mixing may have important consequences.The vertical distributions of photoadaptive properties in mixedlayers not only reveal the rate of vertical mixing, but showhow phytoplankton integrate environmental fluctuations.     

Interaction between wind-induced seiches and convective cooling governs algal distribution in a canyon-shaped reservoir

1. Wind is considered the dominant factor controlling phytoplankton distribution in lentic environments. In canyon‐shaped reservoirs, wind tends to blow along the main axis generating internal seiches and advective water movements that jointly with biological features of algae can produce a heterogeneous phytoplankton distribution. Turbulence generated by wind stress and convection will also affect the vertical distribution of algae, depending on their sinking properties. 2. We investigated the vertical and horizontal distribution of phytoplankton during the stratification period in Sau Reservoir (NE Spain). Sites along the main reservoir axis were sampled every 4 h for 3 days, and profiles of chlorophyll‐a and temperature were made using a fluorescent FluoroProbe, which can discriminate among the main algal groups. Convective and wind shear velocity scales, and energy dissipation were calculated from meteorological data, and simulation experiments were performed to describe non‐measured processes, like vertical advection and sinking velocity of phytoplankton. 3. Wind direction changed from day to night, producing a diel thermocline oscillation and an internal seiche. Energy dissipation was moderate during the night, and mainly attributed to convective cooling. During the day the energy dissipation was entirely attributed to wind shear, but values indicated low turbulence intensity. 4. The epilimnetic algal community was mainly composed of diatoms and chlorophytes. Chlorophytes showed a homogeneous distribution on the horizontal and vertical planes. Diatom horizontal pattern was also homogeneous, because the horizontal advective velocities generated by wind forcing were not high enough to develop phytoplankton gradients along the reservoir. 5. Diatom vertical distribution was heterogeneous in space and time. Different processes dominated in different regions of the reservoir, due to the interaction between seiching and the daily cycle of convective‐mediated turbulence. As the meteorological forcing followed a clear daily pattern, we found very different diatom sedimentation dynamics between day and night. Remarkably, these dynamics were asynchronous in the extremes of the seiche, implying that under the same meteorological forcing a diatom population can show contrasting sedimentation dynamics at small spatial scales (approximately 10³ m). This finding should be taken into account when interpreting paleolimnological records from different locations in a lake. 6. Vertical distribution of non‐motile algae is a complex process including turbulence, vertical and horizontal advection, variations in the depth of the mixing layer and the intrinsic sinking properties of the organisms. Thus, simplistic interpretations considering only one of these factors should be regarded with caution. The results of this work also suggest that diatoms can persist in stratified water because of a synergistic effect between seiching and convective turbulence.     

The role of spatial scale and area in determining richness-altitude gradients in Swedish lake phytoplankton communities

Lake phytoplankton richness data were analyzed to reveal the effects of area and scale on the richness-elevation relationship. Lakes provide a unique opportunity to accomplish this because of their well-defined boundaries, which clearly define local communities and their habitat area. Local phytoplankton richness (alpha diversity) was found to decrease with increasing elevation, even when the effect of lake area was accounted for. This decrease coincided with a decrease in lake productivity with increasing elevation. Additionally, pairwise dissimilarity calculations suggested that isolation by distance was less important in structuring local phytoplankton richness than isolation by either elevation or environmental distance. In contrast, phytoplankton richness calculated for elevation bands (gamma diversity) showed a hump-shaped dependence on elevation, with a mid-elevation maximum, consistent with the predictions of a mid-domain null model. Moreover, mean pairwise dissimilarity within elevation bands shows compositional dissimilarity to be highest at high elevations and low environmental distances, emphasizing the isolated character of high-elevation lakes. We suggest that the form of the phytoplankton richness-elevation relationship is scale-dependent, and that geometric constraints, differences in the possibility of horizontal and vertical dispersal, environmental heterogeneity and an underlying monotonic trend in productivity, are likely to be responsible for the patterns in alpha and gamma diversity observed along elevation gradients.     

Changes in vertical and horizontal diversities mediated by the size structure of introduced fish collectively shape food-web stability

Species introductions can alter local food-web structure by changing the vertical or horizontal diversity within communities, largely driven by their body size distributions. Increasing vertical and horizontal diversities is predicted to have opposing effects on stability. However, their interactive effects remain largely overlooked. We investigated the independent and collective effects of vertical and horizontal diversities on food-web stability in alpine lakes stocked with variable body size distributions of introduced fish species. Introduced predators destabilize food-webs by increasing vertical diversity through food chain lengthening. Alternatively, increasing horizontal diversity results in more stable food-web topologies. A non-linear interaction between vertical and horizontal diversities suggests that increasing vertical diversity is most destabilizing when horizontal diversity is low. Our findings suggest that the size structure of introduced predators drives their impacts on stability by modifying the structure of food-webs, and highlights the interactive effects of vertical and horizontal diversities on stability.     

The spatial distribution of nutrients in the South Basin of Windermere

SUMMARY. The vertical and horizontal distribution of electrical conductivity, soluble reactive phosphorus (SRP), total phosphorus, ammonia-nitrogen and nitrate-nitrogen in the South Basin of Windermere is described and related, where possible, to spatial variations in phytoplankton and zooplankton. For most variables, the maximum range of horizontal variation on a single day was greater than the maximum range of seasonal variation measured at a single station over a full year. Horizontal variations in SRP and ammonia were particularly high, with coefficients of variation often exceeding 100%. The errors associated with sampling at a single station were most pronounced when local accumulations of zooplankton or phytoplankton occurred in the lake. Horizontal variations in conductivity were primarily influenced by the discharge of treated sewage effluent into the central region and the mass transport of water from the more oligotrophic North Basin. Occasionally, more widespread variations in conductivity appeared to be related to spatial variations in photosynthetic activity. The major factor influencing the horizontal distribution of SRP was the discharge of treated effluent into the central region. Despite the intensive recycling of phosphorus, SRP concentrations were nearly always 10–30% higher near the sewage works than elsewhere in the basin. On a few occasions, significant horizontal differences in SRP concentration were also detected within downwind accumulations of crustacean zooplankton. Horizontal variations in total phosphorus were produced by spatial differences in SRP concentration or by local accumulations of phytoplankton or zooplankton. Horizontal differences in ammonia concentration appeared to be produced, both by the effluent discharge and by the turbulent transfer of nutrients from sediments in shallow water. Observations of effluent movement and dispersion demonstrate that wind-induced water movements tend to recirculate nutrient-rich water in the central region and limit mixing along the axis of the basin. The statistical implications of nutrient heterogeneity are discussed in relation to sampling strategy and the possible effects of persistent nutrient concentration gradients on phytoplankton patch formation are assessed.     

闽粤近岸夏季上升流区浮游植物群落组成及其影响因素

基于2009年6月11—16日闽粤近岸(21.6°—24.3°N,115.7°—118.7°E)30个站位133个样品的调查资料,对闽粤近岸上升流区浮游植物群落的物种组成、丰度变化进行了三维结构(水平、垂直、断面)研究,并探讨其与下层水涌升、营养盐补充的关系.共记录浮游植物4门85属159种,以及未定种9种.其中,硅藻为优势类群,甲藻次之,以束毛藻为主要组分的固氮蓝藻也占有较大比例,而金藻仅在近岸10 m上层检出.细长翼根管藻、菱形海线藻、尖刺伪菱形藻、中肋骨条藻、佛氏海线藻、具槽帕拉藻、斯氏几内亚藻、铁氏束毛藻、纺锤角藻和旋沟藻为群落的优势种.调查区内浮游植物以广温种为主,其次是暖水种,而热带高盐和外海广温种较少.浮游植物细胞丰度平均为每升67.59×102个.浮游植物垂直分布的总体特点是丰度在表层最大,随着水深增加逐渐减小.浮游植物细胞丰度的平面和断面分布不均匀,密集区出现在南澳岛邻近海域,与上升流中心重合.上升流强度较弱或在涌升早期阶段,浮游植物细胞丰度增长不明显,密集区位于或邻近上升流中心.南澳岛至漳浦一线海域的4条断面(B、C、D、E)浮游植物细胞丰度值较高,存在经由台湾浅滩的陆架海流向近岸的上涌现...     

Factors influencing the spatial distribution of zooplankton and fish in Loch Ness, UK

• 1 The vertical and horizontal distribution of phytoplankton, zooplankton and fish in Loch Ness, Scotland, were monitored during one day‐time and one night‐time survey in July 1992. The vertical samples were collected at a site located at the northern end of the loch and the horizontal samples along a longitudinal transect.
• 2 The vertical distribution surveys demonstrated that the phytoplankton, the zooplankton and the fish were concentrated in the top 30 m of water above the seasonal thermocline. Within this layer, Cyclops stayed much closer to the surface than Eudiaptomus but both species moved towards the surface at night.
• 3 The most important factor influencing the horizontal distribution of the phytoplankton was the north‐ south gradient in productivity. The sub‐catchments surrounding the north basin contain a greater proportion of arable land than those to the south and the concentrations of nitrate‐nitrogen and phytoplankton chlorophyll increased systematically from south to north.
• 4 Zooplankton distribution patterns were influenced by wind‐induced water movements and the dispersion of allochthonous material from the main inflows. The highest concentrations of Cyclops were recorded in the north, where there was more phytoplankton, and the highest concentrations of Eudiaptomus in the south, where there were higher concentrations of non‐algal particulates.
• 5 There was no spatial correlation between total zooplankton and total fish abundance but the highest concentrations of small (1–5 cm) fish were recorded in the south where there was a large patch of Eudiaptomus. The number of Eudiaptomus at specific locations within this patch were, however, negatively correlated with the numbers of small fish. These results suggest that the fish were actively foraging within the patch and were depleting their zooplankton prey in the areas where they were most abundant.

     

中国蜡梅属种质资源的分布及其特点

根据对中国蜡梅属种质资源的调查,结合已有资料,重点阐述了中国蜡梅属植物的地理分布、水平和垂直分布特点及其生境特点。现知中国蜡梅属植物主要分布于我国的13个省,其水平分布很广,很连续,主要分布于秦岭以南、横断山脉以东的广大地区。垂直分布跨度很大,但垂直分布的上下限与经纬度无显著的相关性。蜡梅属植物对水热条件要求较严格,土壤基质多为沙壤土,在群系组成中,蜡梅属植物多为林木层和灌木层的优势成分。蜡梅属植物跨有5个植被类型,主要生长在常绿落叶阔叶混交林和常绿阔叶林地带。     

Diurnal dynamics of the vertical distribution of zooplankton in an oligotrophic lake

The diurnal dynamics of the vertical distribution of zooplankton was studied in an oligotrophic lake with a high water transparency. Those sedentary species which occupy the upper water layers in waterbodies with low water transparency shift to a border between epy- and metalimnion and stay there during most of the day in Koskovskoye Lake, which has a high water transparency. Active diurnal vertical migrations are characteristic of large organisms. Increased water transparency weakly affects large zooplankters that occupy metalimnial layers in mesotrophic waterbodies. The relationship between the zooplankton’s vertical distribution and the distribution of phytoplankton and fish is analyzed.     

Diel variation in the vertical distribution of fish and plankton in Lake Kinneret: a 24-h study of ecological overlap

Diel vertical migration (DVM) behaviour is a predator avoidance mechanism observed within many zooplankton species in the presence of zooplanktivorous fish. A 24-h survey was carried out in June 1998 to investigate diel variation in the vertical distribution of fish, zooplankton and phytoplankton (chlorophyll) in Lake Kinneret, Israel. Fish revealed diel variation in vertical distribution but had no spatial overlap with zooplankton, and consequently no apparent influence on zooplankton dispersal. Zooplankton revealed some diel variation in distribution being affected by thermocline and oxycline position and movement of the internal the internal seiche wave. Cyclopoid species closely follow the movement of the seiche wave implying that, due to their greater motility, they are following conditions that are suitable to them. The Cladocera species and small rotifers only partly, which may be part of their phototaxic behaviour. Physical forces like convection, horizontal and vertical forcing probably have a role in contributing to a homogeneous distribution of the plankton by preventing stratification or interfering with the more motile zooplankton which may be attempting to migrate.     

Relationship between Chlorophyll a Concentration,Light Attenuation and Diving Depth of the Southern Elephant Seal Mirounga leonina

Recently, a number of Antarctic marine environmental studies have used oceanographic parameters collected from instrumented top predators for ecological and physical information. Phytoplankton concentration is generally quantified through active measurement of chlorophyll fluorescence. In this study, light absorption coefficient (K_0.75) was used as an indicator of phytoplankton concentration. This measurement, easy to obtain and requiring low electric power, allows for assessing of the fine scale horizontal structuring of phytoplankton. As part of this study, Southern elephant seals (SES) were simultaneously equipped with a fluorometer and a light logger. Along the SES tracks, variations in K_0.75 were strongly correlated with chlorophyll, a concentration measured by the fluorometer within the euphotic layer. With regards to SES foraging behaviour, bottom depth of the seal’s dive was highly dependent on light intensity at 150 m, indicating that the vertical distribution of SES’s prey such as myctophids is tightly related to light level. Therefore, change in phytoplankton concentration may not only have a direct effect on SES’s prey abundance but may also determine their vertical accessibility with likely consequences on SES foraging efficiency.     

Phytoplankton development and turbulent mixing in Lake Kinneret (1992-1996)

We have utilized data from a recently developed three-dimensionalvelocity fluctuation meter to compute the dissipation of turbulentkinetic energies (TKE) and the intensity of turbulent mixingin horizontal and vertical planes in the pelagic, epilimnicwater of Lake Kinneret, Israel. These characteristics of wind-inducedturbulent movement have been monitored from January 1992 throughDecember 1996. The turbulence parameters were strongly correlatedto wind energy inputs, calculated daily as 5 day cumulativeinputs. There have been dramatic changes in the annual and seasonaldevelopment of phytoplankton, together with unusually high levelsof primary production in this lake since 1994. We observed differentpatterns of vertical and horizontal turbulent movement and ofTKE dissipation rates during the years when ‘unusual’phytoplankton development occurred (1994–1996) comparedto ‘normal’ years (1992, 1993). The first appearanceof the filamentous cyanobacterium Aphanizomenon in this lakein August–September 1994 coincided with a period of markedlylower rates of TKE dispersion and a shift from vertical to horizontaldominance of the turbulent eddy spins. The absence of a regularwinter-spring bloom of the dinoflagellate, Peridinium, in 1996occurred when dissipation rates of TKE were extremely high,while record high amounts of dinoflagellates (1994, 1995) appearedwhen dissipation rates were very low. Correlations were shownbetween phytoplankton parameters (chlorophyll, primary productionand the ratio of primary production to chlorophyll) and boththe dissipation rate of TKE and the intensity of water turbulentmixing in the vertical plane. We suggest that the changes inthe ‘turbulence climate’ of Lake Kinneret were animportant factor in determining shifts in phytoplankton successionand the population composition of the algal assemblage.     

Environmental forcing on the interactions of plankton communities across a continental shelf in the Eastern Atlantic upwelling system

To investigate whether phytoplankton is the main factor determining mesozooplankton distribution in a continental shelf affected by upwelling, oceanographic surveys were conducted off NW Portugal in 2002 and 2003. During four different seasons, we investigated how the mesoscale relationship between these two communities was forced by environmental conditions across the shelf. The horizontal and vertical distribution of phytoplankton was shaped by wind stress over the water. Diatoms dominated mixed and upwelled waters, whereas dinoflagellates prevailed with thermal stratification. Mesozooplankton was less influenced by wind forcing and concentrated mostly at mid-shelf, on the outer margin of main phytoplankton patches. We found that this pattern, under strong thermal stratification conditions, can be associated with localized grazing “hot spots”. Copepods were dominant, contributing to the mesozooplankton community variability between cruises whereas phytoplankton presented a clearer seasonal pattern. Nevertheless, the distribution and abundance of mesozooplankton were directly correlated with all phytoplankton groups at the inner-mid-shelf, while no correlation was observed offshore the outer-shelf. The relative composition of mesozooplankton did not vary between depth strata, whereas a cross-shelf separation occurred between nearshore and widespread clusters of species. This reflected a dependence on phytoplankton and reflected the high variability of oceanographic conditions of the study area.     

不同叶幕形对设施葡萄叶幕微环境、叶片质量及果实品质的影响

以3年生‘贝达’砧木设施栽培‘京蜜’葡萄为试材,研究直立、V形和水平3种叶幕形处理下葡萄叶幕微环境、叶片质量及果实品质的差异.结果表明: 直立叶幕的总孔隙度和开度显著高于V形叶幕和水平叶幕,叶面积指数、光能截获率和叶幕昼夜温差均显著低于V形叶幕和水平叶幕,后两者间无显著差异.V形叶幕葡萄叶片的栅栏组织厚度显著大于直立叶幕,水平叶幕居中,叶绿素和类胡萝卜素含量显著高于直立叶幕和水平叶幕,后两者间无显著差异.果实品质以V形叶幕最佳,水平叶幕其次,直立叶幕最差.通过GC-MS分析发现,V形叶幕挥发性香气化合物种类最多,为29种,直立叶幕与水平形叶幕分别为17和16种.V形叶幕中‘京蜜’葡萄的特征香气组分除乙醇、反式-2-己烯-1-醇、仲辛酮和甲酸己酯含量较低外,其余含量均较高.芳樟醇(里那醇)含量在直立叶幕和V形叶幕中显著高于水平叶幕,橙花醇含量在V形叶幕中显著高于直立叶幕和水平叶幕,叶醇含量在V形叶幕和水平叶幕中显著高于直立叶幕,香茅醇仅在V形叶幕中检出.V形叶幕设施栽培葡萄的果实香气更浓,更能体现其品种特性.     

The Consequences of Internal Waves for Phytoplankton Focusing on the Distribution and Production of Planktothrix rubescens

Consequences of internal wave motion for phytoplankton and in particular for the distribution and production of the harmful and buoyant cyanobacterium Planktothrix rubescens were investigated based on data from two field campaigns conducted in Lake Ammer during summer 2009 and 2011. In both years, P. rubescens dominated the phytoplankton community and formed a deep chlorophyll maximum (DCM) in the metalimnion. Internal wave motions caused vertical displacement of P. rubescens of up to 6 m and 10 m, respectively. Vertical displacements of isotherms and of iso-concentration lines of P. rubescens from the same depth range coincided, suggesting that P. rubescens did not or could not regulate its buoyancy to prevent wave-induced vertical displacements. Diatoms dominated the phytoplankton community in the epilimnion and were vertically separated from P. rubescens. The thickness of the diatom layer, but not the diatom concentrations within the layer, changed in phase with the changes in the thickness of the epilimnion caused by internal wave motions. Seiche induced vertical displacements of P. rubescens caused fluctuations in the light intensity available at the depth of the P. rubescens layer. The interplay between seiche induced vertical displacements of the P. rubescens layer and the daily cycle of incident light lead to differences in the daily mean available light intensity between lake ends by up to a factor of ∼3. As a consequence, the daily mean specific oxygen production rate of P. rubescens differed by up to a factor of ∼7 between lake ends. The horizontal differences in the specific oxygen production rate of P. rubescens were persistent over several days suggesting that the associated production of P. rubescens biomass may lead to phytoplankton patchiness. The effect of internal seiches on the spatial heterogeneity and the persistence of horizontal differences in production, however, depend on the timing and the synchronization between internal wave motion and the daily course of incident light intensity. Vertical displacements caused by internal waves could be distinguished from other factors influencing the distribution of P. rubescens (e.g. active buoyancy control, production, vertical mixing) by a temperature-based data transformation. This technique may be of general use for separating wave-induced transport from other processes (e.g. sedimentation, vertical mixing) that affect the distributions of dissolved substances and suspended particles.     

Host growth conditions regulate the plasticity of horizontal and vertical transmission in Holospora undulata,a bacterial parasite of the protozoan Paramecium caudatum

Abstract.— A parasite might be prohibited from investing simultaneously in horizontal (infection of new hosts) and vertical (infection of the current host's offspring) transmission because of developmental, physiological, or evolutionary costs and constraints. Rather, these constraints may select for adaptive phenotypic plasticity, where the parasite uses the transmission pathway that maximizes transmission in the current ecological and epidemiological conditions. By varying environmental conditions for the host's replication, we investigated the plasticity of vertical and horizontal transmission of Holospora undulata , a micronucleus-specific bacterial parasite of the protozoan Paramecium caudatum . We observed a negative correlation between the host's growth rate and the parasite's investment in horizontal transmission. In rapidly dividing hosts, the parasite remained in the reproductive stage and was passed on vertically to the daughter nuclei during mitotic division of the Paramecium . In contrast, at low or negative growth rates of the host, the parasite's reproductive forms differentiated into infectious forms, the agents of horizontal transmission. Furthermore, in treatments that were initiated with a high proportion of individuals harboring horizontally transmitted infectious forms, rapid replication resulted in a switch back from predominantly horizontal to almost exclusively vertical transmission. These results suggest a trade-off between the efficacies of vertical and horizontal transmission, with the parasite switching to horizontal transmission only if conditions for host replication, and thus vertical transmission, deteriorate.     

Temporal organization of phytoplankton communities linked to physical forcing

The performance of individual phytoplankton species is strongly governed by the thermal stratification’s impact on vertical mixing within the water column, which alters the position of phytoplankton relative to nutrients and light. The present study documents shifts in phytoplankton structure and vertical positioning that have accompanied intensified long-term stratification in a natural ecosystem. Ordination analysis is used to extract gradients in phytoplankton composition in Lake Tahoe, an extremely nutrient-poor lake, over a 23-year period of records. Community structure in the 1980s was associated most strongly with resource availability (low nitrogen to phosphorus ratios, deeper euphotic zone depth), while intensified stratification dominated the phytoplankton structure since the late 1990s. Within diatoms, small-sized cells increased with reduced mixing, suggesting that suppressed turbulence provides them with a competitive advantage over large-sized cells. Among the morphologically diverse chlorophytes, filamentous and coenobial forms were favored under intensified stratification. The selection for small-sized diatoms is accompanied by a shoaling trend in their vertical position in the water column. In contrast, the motile flagellates displayed a deeper vertical positioning in recent years, indicating that optimal growth conditions shifted likely due to reduced upwelling of nutrients. As the thermal stratification of lakes and oceans is strongly linked to climate variables, the present study confirms that climate warming will alter phytoplankton structure and dynamics largely through effects on nutrient availability and sinking velocities. Intensified stratification should favor the expansion of small-sized species and species with the capability of buoyancy regulation, which may alter primary productivity, nutrient recycling, and higher trophic productivity. Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users.     

The spatial distribution of different phytoplankton functional groups in a Mediterranean reservoir

A new high-resolution spectrofluorimetric probe and an automatic water-quality monitoring station (AWQMS) have been used to record seasonal variations in the spatial distribution of three functional groups of phytoplankton in a Mediterranean water-supply reservoir. In comparison with classical methods, the combined use of these innovative techniques enables development of faster and less laborious spatial distribution surveys, thus favouring higher-frequency and spatially more detailed measurements, and, consequently, a better understanding of phytoplankton dynamics. The results show that the observed variations can be explained by the interaction between the buoyancy properties of the phytoplankton and the mixing characteristics of the reservoir. During the winter, when the lake was isothermal and the phytoplankton was dominated by diatoms, there was no significant spatial variation. In the spring, when the phytoplankton was dominated by chlorophytes there was also very little variation but some motile species formed patches when the wind speed was low. The most pronounced non-uniform distributions of phytoplankton were observed during the summer when the phytoplankton community was dominated by positively buoyant cyanobacteria. Then there was a very strong link between the vertical and horizontal gradients which were also related to the prevailing meteorological conditions.     

Interaction effects of zooplankton and CO2 on phytoplankton communities and the deep chlorophyll maximum

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Phytoplankton in the surface and chlorophyll maximum off southern California in August, 1978

A synoptic sampling of 30 stations in a 25 km x40 km grid closeto the southern California coast revealed that chlorophyll andphytoplankton biomass were higher nearshore and to the south,where relatively large dinoflagellates dominated. A subsurfacechlorophyll maximum was present at each station, near the nitraclineand 10% light level. Nearshore and to the south, these maximarepresented higher levels of phytoplankton biomass than at thesurface whereas at the other stations, chlorophyll maxima couldbe attributed to physiological changes in chlorophyll contentof small flagellated phytoplankton rather than to the accumulationof phytoplankton at depth. Univariate and multivariate statisticalprocedures were used to demonstrate that phytoplankton assemblagesseparated by tens of meters in the vertical were just as differentas those separated by tens of kilometers in the horizontal.We conclude that residence time of water near the coast is ofgreat importance to the determination of the abundance and taxonomiccharacteristics of phytoplankton, and that advection of offshorewater towards the coast was the major determinant of the patternobserved during our study. ¹Present address: University of Texas, Port Aransas Marine Laboratory,Port Aransas, TX 78373, USA