Catastrophic transition in vertical distributions of phytoplankton: alternative equilibria in a water column

We showed a catastrophic transition between a surface maximum pattern and a subsurface maximum pattern of phytoplankton in a water column by a mathematical model considering the vertical distribution of phytoplankton and two resources, light and a limiting nutrient. In our model, we assumed that a water column consists of two layers: a complete mixing layer above a seasonal thermocline and an incomplete mixing layer below it. From numerical calculation of the model, we obtained that there are two stable vertical patterns of phytoplankton over a certain range of parameters of the model: a pattern having its maximum below the thermocline and another having its maximum above the thermocline. As other models having multiple stable equilibria, our model also exhibits a hysteresis effect and catastrophic transition when one of the parameters of the model changes continuously. These results indicate the possibility of the existence of alternative equilibria of vertical patterns of phytoplankton even if the trophic status and physical condition of the water column are similar. Moreover, the catastrophic transition between the steady states suggests one of the possible mechanisms of autumn algal blooms.     

Seasonal cycle of nitrogen and phytoplankton biomass in a well-mixed coastal system (Eastern English Channel)

The hydrological structure of the French coastal part of the eastern English Channel is strongly linked with tidal regimes and riverine input. Two distinct water masses are separated by a frontal area and drift along the coast in SW–NE direction. These two water masses are well-mixed during the entire year. We studied the seasonal dynamic of nitrogenous nutrients, chlorophyll a and organic particulate carbon and nitrogen at two stations, characteristic of these water masses, during the year 1994. Results show (i) a winter stock of nitrate and ammonium, (ii) a pre-bloom period corresponding to the use of ammonium, (iii) a high bloom period of short duration using nitrate, (iv) a post-bloom period with little phytoplanktonic activity probably limited by nutrients other than nitrogen and (v) an autumnal period of reconstitution of stock. The essential difference between the two stations is the importance of winter stock of nutrients and of bloom chlorophyll a concentration, with the coastal station richer than the offshore one. An assumption about the nitrogen available for new production in this area gives a value of 57% of the winter stock of inorganic nitrogen.     

The effect of water column mixing on phytoplankton succession, diversity and similarity

The lake number was used to describe the mixing condition forthree consecutive years (1992–1994) in Lake Tegel, Berlin,and compared to the successions of diatoms, dinoflagellatesand cyanobacteria, the main phytoplankton groups in the lake,as well as to diversity and similarity indices. Using both diversityand similarity indices in juxtaposition provides an indicationof the growth type of prevailing species (r- or K-strategists)and the degree of competition in the aqua-ecological system.A genera] pattern of these indices can be recognized as threephases: (i) high diversity—during spring, summer and autumn,interrupted by (ii) phases of low diversity during the latespring clear-water phase as the number of spring species plummeted,and (iii) during the late summer, climax populations of K-strategists.On a smaller time scale, similarity and diversity proved toreact sensitively to disturbances at frequencies intermediatein relation to the generation times of the phytoplankton. Thissupports the ‘intermediate disturbance hypothesis’,as proposed for phytoplankton by Padisak et al. [(eds) IntermediateDisturbance Hypothesis in Phytoplankton Ecology. Kluwer Academic,1993]. Diversity may remain quite high even for extended periodsduring summer climax situations, in conjunction with a highdegree of similarity, if deeper mixing of the epilimnion occursat time intervals of 2–3 weeks, as during the summer of1993. This enables the prevalence of ‘ruderal’ species,together with some motile K-strategists who actively seek optimaldepths for photosynthesis. During such summer situations describedby frequent occurrences of lower lake numbers, the epilimnionof Lake Tegel is mixed deeply enough to support ruderals, butnot too vigorously to counteract competitive advantages of motilespecies. Thus, vertical niche separation enhances diversity.     

The effect of elevated CO2 on growth and competition in experimental phytoplankton communities

We report an experiment designed to identify the effect of elevated CO₂ on species of phytoplankton in a simple laboratory system. Major taxa of phytoplankton differ in their ability to take up CO₂, which might lead to predictable changes in the growth rate of species and thereby shifts in the composition of phytoplankton communities in response to rising CO₂. Six species of phytoplankton belonging to three major taxa (cyanobacteria, diatoms and chlorophytes) were cultured in atmospheres whose CO₂ concentration was gradually increased from ambient levels to 1000 parts per million over about 100 generations and then maintained for a further 200 generations at elevated CO₂. The experimental design allowed us to trace a predictive sequence, from physiological features to the growth response of species to elevated CO₂ in pure culture, from the growth response in pure culture to competitive ability in pairwise mixtures and from pairwise competitive ability to shifts in the relative abundance of species in the full community of all six species. CO₂ altered the dynamics of growth in a fashion consistent with known differences among major taxa in their ability to take up and use CO₂. This pure‐culture response was partly successful in predicting the outcome of competition in pairwise mixtures, especially the enhanced competitive ability of chlorophytes relative to cyanobacteria, although generally statistical support was weak. The competitive response in pairwise mixtures was a good predictor of changes in competitive ability in the full community. Hence, there is a potential for forging a logical chain of inferences for predicting how phytoplankton communities will respond to elevated CO₂. Clearly further extensive experiments will be required to validate this approach in the greater complexity found in diverse communities and environments of natural systems.     

Nutrient competition and division synchrony in phytoplankton

In the Gulf Stream in October of 1968, division of at least nine species of dinoflagellates occurred between 03.00 h and 06.00h indicating a high level of developmental synchronization. Whereas light-dark and temperature cycles act independently on each species, the synchronizing agent in the Gulf Stream apparently couples the development of many species of the dinoflagellate community. It is proposed that diurnal fluctuation in nutrients, acting through interspecific competition, is the coupling and synchronizing agent in this environment. A mathematical model of interspecific competition shows that regular, short-term changes in nutrient levels are extremely sffective in synchronizing the development of several species. Calculations also suggest that division eynchrony is an indicator of the occurrence of competition for nutrients and that the degree of synchronization increases with the severity of nutrient limitation on the phytoplankton.     

Kinetics and bioenergetics of light-limited photoautotrophic growth of Spirulina platensis

Blue-green algae, Spirulina platensis, is cultivated under photoautotrophic growth conditions designed to have nearly uniform growth rate throughout the fermentor by illumination both sides of a rectangular vessel. The results show that growth rate and bioenergetic yield are a function of light intensity. Several kinetic models are considered to express the relationship between growth rate and light intensity.     

The relationship between phytoplankton distribution and water column characteristics in North West European shelf sea waters

Phytoplankton underpin the marine food web in shelf seas, with some species having properties that are harmful to human health and coastal aquaculture. Pressures such as climate change and anthropogenic nutrient input are hypothesized to influence phytoplankton community composition and distribution. Yet the primary environmental drivers in shelf seas are poorly understood. To begin to address this in North Western European waters, the phytoplankton community composition was assessed in light of measured physical and chemical drivers during the "Ellett Line" cruise of autumn 2001 across the Scottish Continental shelf and into adjacent open Atlantic waters. Spatial variability existed in both phytoplankton and environmental conditions, with clear differences not only between on and off shelf stations but also between different on shelf locations. Temperature/salinity plots demonstrated different water masses existed in the region. In turn, principal component analysis (PCA), of the measured environmental conditions (temperature, salinity, water density and inorganic nutrient concentrations) clearly discriminated between shelf and oceanic stations on the basis of DIN:DSi ratio that was correlated with both salinity and temperature. Discrimination between shelf stations was also related to this ratio, but also the concentration of DIN and DSi. The phytoplankton community was diatom dominated, with multidimensional scaling (MDS) demonstrating spatial variability in its composition. Redundancy analysis (RDA) was used to investigate the link between environment and the phytoplankton community. This demonstrated a significant relationship between community composition and water mass as indexed by salinity (whole community), and both salinity and DIN:DSi (diatoms alone). Diatoms of the Pseudo-nitzschia seriata group occurred at densities potentially harmful to shellfish aquaculture, with the potential for toxicity being elevated by the likelihood of DSi limitation of growth at most stations and depths.     

The interaction of components controlling net phytoplankton photosynthesis in a well-mixed lake (Lough Neagh, Northern Ireland)

The homogeneous distribution of the phytoplankton in a shallow (mean depth 8·6 m) unstratified lake, L. Neagh, Northern Ireland, facilitated the study of the interaction of components controlling gross photosynthesis per unit area. These included the photosynthetic capacity, the phytoplankton content of the euphotic zone, and a logarithmic function describing the effective radiation input. These factors were analysed for two sites, the open lake and Kinnego Bay, which respectively had standing crops of up to 90 and 300 mg chlorophyll a m^?3 and maximum daily rates of gross integral photosynthesis of 11·7 and 15·6 g O₂ m^?2 day^?1. Values are reduced by the high contribution to light attenuation by non-algal sources, which increases at low standing crops particularly in winter, when values of integral photosynthesis decrease to 0·5 g O₂ m^?2 day^?1. This relative change is the result of self-shading behaviour of the phytoplankton altering the crop content of the euphotic zone at different population densities. Changes in the irradiance function, incorporating day length, are largely responsible for the changes in daily rates of integral gross photosynthesis; as daily irradiance is also a determinant of water temperature, it exerts further influence through the photosynthetic capacity which was strongly correlated with temperature. Much of the gain in gross photosynthesis resulting from higher photosynthetic capacity may not be reflected in a higher net column photosynthesis, because of the greater proportional rise in respiration with temperature. The balance in the water column between respiration losses and photosynthetic input may frequently alter since the ratio of illuminated to dark zones is between 1/4 to 1/5 in the open lake, and small shifts in any of the controlling features may result in conditions unfavourable for growth. This is analysed especially for the increase of diatoms in spring, when small modifications of the underwater light field can delay growth.     

Seasonal fluctuations in the biomass and metabolic activity of bacterioplankton and phytoplankton in a well-mixed estuary: the Ems-Dollard (Wadden Sea)

The biomass and metabolic activity of bacterioplankton weremeasured over 1 year in the Ems Dollard Estuary, a part of theDutch-German Wadden Sea. Very productive phyzoplankton blooms,composed mainly of diatoms and the haptophycean alga Phaeocystispouchetii, are a feature of the estuarine section studied. Theproduction of bacterial populations, as measured using the [³H]thymidinemethod broadly followed the phytoplankton density during bloomsin spring and late summer. There was no indication of a disproportionateincrease in bacterial production during the bloom or declineof particular algal species. The rate at which ¹⁴C-labelledglucose, glutamate and leucine were incorporated by bacterialpopulations, measured as a metabolic potential, varied seasonally,but did not precisely follow the rate of [³H]thymidine incorporation.The utilization of the absorbed ¹⁴C substrates for respirationor for cellular synthesis was constant over a prolonged periodof bacterial growth; apparent yields of 0.7, 0.4 and 0.8 weremeasured for glucose, glutamate and leucine, respectively. Inthe colder season most of the absorbed substrate was respired.The production by pelagic bacteria was 60 gC m^–2 y^–1,a value that amounted to 12% of the pelagic primary production.A preliminary experiment with a mixed culture of the abundantlyoccurring diatom species Thalassiosira excentrica and a marinespirillum, indicated that part of the algal exudates were rapidlyconverted by the bacteria, but another part resisted degradation.The incomplete bacterial degradation of algal exudates togetherwith the short residence time of the estuarine phytoplanktonmay contribute to the apparently incomplete mineralisation ofthe primary production in the water.     

Temperature-influenced species competition in mass cultures of marine phytoplankton

Five marine phytoplankton species (Phaeodactylum tricornutum, Thalassiosira pseudonana, Skeletonema costatum, Monochrysis lutheri, and Dunaliella tertiolecta) were grown in enriched laboratory continuous cultures and natural populations were mass cultured outdoors for 16 months. Competition among the species was shown to be highly dependent on temperature, although the actual production of plant organic matter at the low growth rates used was relatively independent of this variable. Control of marine species in mass cultures does not appear economically feasible, but this drawback may be overcome by selecting herbivorous shellfish that are capable of assimilating those temperature-dependent phytoplankton species dominating in a particular locale.     

Seasonal shifts in ice edge phytoplankton blooms in the Barents Sea related to the water column stability

The development of the phytoplankton bloom and its relation to water column stabilisation during the transition from early to high summer (of 1991) in the seasonally ice-covered zone of the Barents Sea were studied from a meridional transect of repeated hydrographic/biological stations. The water column stabilisation is described in detail with the aid of vertical profiles of the Brunt-Väisälä frequency squared (N²). The contributions of seasonal warming and ice melting to stabilisation are elucidated by determining the effects of temperature and salinity on N². The spring bloom in 1991 migrated poleward from June to July by about 400 km, associated with the retreat of the ice edge. The spring bloom culminated with maximum chlorophyll concentrations in the mixed layer about 100–300 km north of the centre of the meltwater lens, at its northern edge, where the ice cover was still substantial. From the distribution of N² it becomes obvious that the bloom starts at the very beginning of stabilisation, which results solely from the release of meltwater. The increase in temperature due to the seasonal warming does not contribute to the onset of vernal blooming; temperature starts to contribute to the stratification later, when the spring bloom has ceased due to the exhaustion of nutrients in the mixed layer. By that time a deep chlorophyll maximum has formed in the seasonal pycnocline, 20–30 m below the base of the mixed layer. The effect of the seasonal ice cover on the mean areal new primary production is discussed.     

Steady-State growth of budding yeast populations in well-mixed continous-flow microbial reactors

A population-balance mathematical model of microbial growth in a flow reactor is formulated which incorporates an asymmetric-division, budding-cycle model of coordinated cell and nuclear division cycles for the budding yeast Saccharomyces cerevisiae. Analytical solutions are obtained for limiting nutrient and cell-number concentrations in the reactor as functions of basic cell cycle parameters. Frequency functions for cell mass and DNA content in the resident yeast population are also derived under different assumptions concerning cell mass and DNA synthesis and bud scar accumulation. These results, which correspond to experimentally observable medium and population variables, provide new bases for evaluating budding-yeast-cell cycle models and for deducing kinetics of mass and DNA synthesis in single cells growing in steady-state, asynchronous populations.     

Comparison of the light-limited growth of the nitrogen-fixing cyanobacteria Anabaena and Aphanizomenon

The effect of simultaneous N₂ fixation and light limitation on the growth of two strains of Anabaena sp. Bory de St. Vincent and Aphanizomenon flos-aquae (L.) Ralfs was investigated using continuous cultures. Under severely light-limited conditions, Aphanizomenon showed a broader absorption spectrum (due to the presence of phycoerythrin), a higher maximum efficiency of photosynthesis, a higher steady-state N₂ fixation activity and a higher growth affinity for light than did Anabaena . On the other hand, under light saturation, Anabaena showed a higher maximum rate of O₂ production and a higher maximum specific growth rate than Aphanizomenon . These monoculture results characterize Anabaena and Aphanizomenon , in relative terms, as a 'sun' and a 'shade' species respectively, and are in accordance with field observations. The difference between the two species in their acclimatory response is discussed in terms of a species-specific alteration of the PSI:PSII stoichiometry. Besides the species-specific modulation of the accessory pigments, such an acclimation would provide a biochemical basis for the observed physiological differences. The monoculture results were used to differentiate the niches of the two species and suggested that Aphanizomenon would competitively displace Anabaena under N₂-fixing, light-limited conditions. However, when both species were grown together, Anabaena became dominant and seemed to be the superior competitor for light. In order to explain this finding, the possible effects of release of allelopathic compounds, or dynamic aspects of light supply, are discussed.     

Energy requirements for growth and maintenance of Scenedesmus protuberans Fritsch in light-limited continuous cultures

Scenedesmus protuberans Fritsch was grown in light-limited continuous cultures with a light-dark cycle, at temperatures of 20° and 28° C. At 20° irradiances of 12 and 38 W m^–2 were used, at 28° 38 W m^–2.The relationships between growth rate and light uptake rate were of diphasic linear character. With the lower growth rates the relationships were defined with the parameters _e , i.e. the specific maintenance rate constant, and c, the true efficiency of light energy conversion into biomass. The _e -value was dependent on temperature, the c on irradiance.In cultures, incubated in prolonged darkness, decrease rates of biomass were comparable to the derived _e -values.Both diphasic linear relationships between growth rate and light uptake rate and the same order of magnitude of _e -values could be derived from literature data on other green algae.     

Size-asymmetric competition and size-asymmetric growth in a spatially explicit zone-of-influence model of plant competition

Size-asymmetric competition among plants is usually defined as resource pre-emption by larger individuals, but it is usually observed and measured as a disproportionate size advantage in the growth of larger individuals in crowded populations (“size-asymmetric growth”). We investigated the relationship between size-asymmetric competition and size-asymmetric growth in a spatially explicit, individual-based plant competition model based on overlapping zones of influence (ZOI). The ZOI of each plant is modeled as a circle, growing in two dimensions. The size asymmetry of competition is reflected in the rules for dividing up the overlapping areas. We grew simulated populations with different degrees of size-asymmetric competition and at different densities and analyzed the size dependency of individual growth by fitting coupled growth functions to individuals. The relationship between size and growth within the populations was summarized with a parameter that measures the size asymmetry of growth. Complete competitive symmetry (equal division of contested resources) at the local level results in a very slight size asymmetry in growth. This slight size asymmetry of growth did not increase with increasing density. Increased density resulted in increased growth asymmetry when resource competition at the local level was size asymmetric to any degree. Size-asymmetric growth can be strong evidence that competitive mechanisms are at least partially size asymmetric, but the degree of size-asymmetric growth is influenced by the intensity as well as the mode of competition. Intuitive concepts of size-asymmetric competition among individuals in spatial and nonspatial contexts are very different.