Advantages from diel vertical migration can explain the dominance of Gonyostomum semen (Raphidophyceae) in a small, steeply-stratified humic lake

In late summer, a large flagellated alga, Gonyostomum semen(Raphidophyceae), constituted most of the phytoplankton biomassin a small steeply-stratified humic lake. Its diel verticalmigration (DVM) was very distinct and extended at night intothe anoxic hypolimnion. After midsummer, the depletion of hypolimneticoxygen led to a gradual release of soluble reactive phosphorus(SRP) from the sediment, but one month later, irrespective ofcontinuing stratification, the concentrations again returnedto undetectable levels down to the bottom. As this coincidedwith the rapid increase in G.semen population, the latter wasprobably responsible for the depletion of SRP. The flux of SRPfrom the sediment to the epilimnion was virtually interrupted,making non-migrating phytoplankton dependent only on regeneratedand inflowing inorganic phosphorus. Besides nutrient availability,DVM also benefited G.semen in the reduction of metabolic andgrazing losses. In this lake, the remarkable multiple advantagesof DVM probably explain the dominance of the large G.semen inthe late summer phytoplankton biomass over much smaller algae.     

Effects of Light and Wind Speed on the Vertical Distribution of Microcystis aeruginosa Colonies of Different Sizes during a Summer Bloom

Different dynamics, of the vertical distribution of Microcystis aeruginosa colonies of different sizes, were examined in a large shallow lake (Taihu Lake) during a summer bloom. During the observation the Microcystis colonies, larger than 120 μm, were mainly concentrated in the upper layer both under calm and windy conditions. Colonies from 36 μm to 120 μm showed a clear relationship to wind conditions whereas colonies less than 36 μm showed a nearly uniform vertical distribution at the different depths. There was no clear relationship between the vertical distribution of colonies larger than 36 μm and light intensity. However, at solar noon, colonies less than 36 μm were mainly distributed in the middle layers of the water column. The results indicate that small colonies are easily affected by the wind‐induced mixing, and they show an ability for active movement in response to light intensity under calm conditions. In contrast, large colonies tend to show little diurnal repositioning to light intensity and thereby are mainly concentrated in the surface layer. (© 2009 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

Factors controlling pelagic populations of ciliates and heliozoans-- late summer investigations in an acidic lake before and after liming

Ciliates and heliozoans were studied in a small oligotrophicSwedish lake with the objective of investigating what controlledthe community structure and population dynamics. Enclosure experimentswere performed with five levels of inorganic nutrient concentrationsand the presence or absence of crustacean zooplankton. The experimentswere performed during the summers immediately preceding andfollowing liming of the lake. The responses of protozooplanktonto these manipulations were investigated and compared with theresponses of bacterioplankton, phytoplankton and metazooplankton.In contrast to most studies on protozoan zooplankton, ciliateswere determined to the lowest taxon possible, and biomassesand abundances were calculated for the different taxa. The protozooplanktonbiomass of the lake, expressed as summer average, did not changebetween the years. However, the community composition changedfrom smaller to larger species as the small prostomatid ciliatesUrotricha and Balanion were largely replaced by oligotrichsof the genera Strombidium and Strobilidium. The experimentssuggested that the protozooplankton community in the lake wascontrolled by metazooplankton in the acidic environment, whilefood limitation was the most important controlling factor afterliming. Before liming, Urotricha and Balanion were unaffectedby nutrient additions as well as by metazooplankton, while otherciliates and Heliozoa showed a significantly negative responseto metazooplankton. After liming, Urotricha and Balanion showeda significant positive response to nutrient addition as wellas to bacterioplankton biomass. A possible explanation for thisresponse in these algivore genera is that the response was indirectand mediated through small chrysoflagellates.     

The IJsselmeer and its phytoplankton--with special attention to the suitability of the lake as a habitat for Oscillatoria agardhii Gom

The IJsselmeer (surface area 1200 km², mean depth 4.5 m, residencetime 0.4 year, phosphorus load 7 g m^–2 year^–1) isa very important conservation area. Regular summer bloomingof Oscillatoria spp. can depreciate this value, so the boundsof possibility of this kind of blooming have been investigated.Therefore samples were taken along the shore and in the openwater from 1974 to 1982, continuous temperature profile measurementswere made in the same period in the middle of the lake and insitu primary production was measured in 1976 and 1977. The phytoplanktonconsists of green algae throughout the year, diatoms in spring,and blooms of Microcystis aeruginosa in summer. Blooming ofOscillatoria agardhii Gom occurs regularly in summer along theFrisian shore. In 1976, however, a heavy bloom of this algaoccurred in the whole lake. Comparing the IJsselmeer with shallowerOscillatoria-lakes in the Netherlands distinct differences arepresent concerning biomass, chlorophyll a content, relativevolume of the euphotic zone and light-dark cycle. Not only thelarger depth and extensiveness of the IJsselmeer are unfavourablefactors for Oscillatoria, but also the separation by land reclamationof many of the shallow littoral regions from the main body ofthe lake. High temperature and microstratification are neededto develop a bloom in the whole lake.     

Phytoplankton and periphyton responses to in situ experimental nutrient enrichment in a shallow subtropical lake

Experiments were performed in situ in shallow, subtropical LakeOkeechobee (Florida. USA) to quantify and compare the responsesof phytoplanklon (in 20 I clear polycarbonate carboys) and periphyton(on nutrient-diffusing clay substrates) to additions of nitrogenand/or phosphorus. During early and late summer. 1994, bothassemblages were nitrogen limited or co-limited by nitrogenand phosphorus, indicating the potential for competition betweenbenthic and planktonic communities. During late summer, therewas evidence that high phytoplankton biomass reduced light penetrationthrough the water column and may have suppressed periphytongrowth. The similar phytoplankton and periphyton taxonomic structures,both dominated by Lyngbya sp. and pennate diatoms, suggestedthat in shallow regions of this lake, resuspended meroplanktonmight account for a large portion of phytoplankton biomass.This phenomenon has been observed in other shallow, wind-drivenFlorida lakes.     

The calanoid copepod Acartia italica Steuer, phenomenon in the small saline Lake Rogoznica (Eastern Adriatic coast)

Lake Rogoznica, near ibenik, Croatia, is a salt coastal lakewith a maximum depth of about 15 m. During most of the year,this small, naturally eutrophied lake is highly stratified,with hypoxia/anoxia occurring in the bottom layer. Total anoxia,with the presence of hydrogen sulphide, was recorded on September27, 1997. At that moment, massive mortality of all planktonicand benthic organisms was observed. After the anoxia, Acartiaitalica, the only planktonic copepod species of the lake, re-establishedquickly. Before anoxia, the population dynamics of the A.italicapopulation depended primarily on predator/prey relationships.However, in the post-anoxic period, nutrient–phytoplankton–copepodrelationships became more important, as there was no longerany predation pressure. From all accounts, it would appear thatonly A.italica is adapted to the extreme conditions which appearfrom time to time in the lake, and that this species has animportant role in the functioning of the lake ecosystem. Acartiaitalica was very important for the gradual normalization oflife in the lake after total anoxia.     

Effect of summer weather on internal loading and chlorophyll a in a shallow lake: a modeling approach

The effect of weather on the eutrophication of a shallow lake was estimated by a hydrodynamic lake model coupled with a simple water quality module. The model was applied to Lake Villikkalanjärvi in southern Finland. This shallow, agriculturally loaded lake may stratify during warm and calm periods in summer and as a result oxygen is often consumed from the hypolimnion, causing high internal loading of phosphorus. Vertical mixing and temperature distribution in the lake were simulated by a one-dimensional, horizontally integrated hydrodynamic model. State variables included in the water quality model were dissolved reactive phosphorus, chlorophyll a and dissolved oxygen. The model was first calibrated against observations from 1989 and 1990. Thereafter, simulations were carried out using weather data from the years 1961 to 1988. The results indicated that warm summer periods may cause high chlorophyll a concentrations due to high internal loading. In four years with exceptionally warm summers the model predicted maximum chlorophyll a concentrations almost twice as high as in years without remarkable internal loading. The model simulates accurately temperature and mixing but the reliability of water quality predictions could be improved by adding more factors regulating algal biomass and sediment phosphorus release.     

Overwintering of Microcystis aeruginosa Kutz. in a shallow lake

The standing crop and photosynthetic activity of Microcystisaeruginosa Kütz. in both the plankton and sediment wereinvestigated from November 1979 to May 1982 in Lake Kasumigaura,Japan. The number of planktonic colonies of this species decreasedfrom early autumn to early spring, but increased in the sedimentduring late summer and autumn. The overwintering colonies inthe sediment were –100–1000 times greater per unitarea than those in lake water. No photoinhibition of photosynthesiscould be observed in overwintering Microcystis. The values ofthe initial slopes of photosynthesis-light (P-I) curves weresimilar to those of the summer population, although the maximumphotosynthetic rate (P_max) measured at 20°C was lower thanthat of the summer planktonic population. In winter the valuesof initial slope of the P-I curve, and the ratio of phycobilinto chlorophyll a sorted from sediment were higher than in coloniesfrom the plankton.     

The impact of year-to-year changes in the weather on the dynamics of Daphnia in a thermally stratified lake

The factors influencing the seasonal dynamics of Daphnia in a thermally stratified lake (Esthwaite Water) are described and related to long-term changes in the weather. The Daphnia produced three cohorts in the year and the strength of the cohorts was determined by year-to-year variations in the physical characteristics of the lake and the abundance of edible algae. Food was most abundant in early summer when small, fast-growing flagellates were particularly common. In late summer, the phytoplankton community was dominated by large, inedible species but edible forms re-appeared when nutrients were entrained by wind mixing. Examples are presented to demonstrate the effect that year-to-year variations in the weather have on the growth of the phytoplankton and the dynamics of the Daphnia. In ‘good’ years, when the lake stratifies early and there are periods of episodic mixing in summer, there are two ‘pulses’ of edible algae and two strong cohorts of Daphnia. In ‘bad’ years when stratification is delayed and there is little episodic mixing, the growth of the edible algae is suppressed and the Daphnia produce two weak cohorts. The results are discussed in relation to the impact of intermediate disturbances on growth of phytoplankton and current theories of population regulation in Daphnia. The evidence suggests that the dynamics of the Daphnia in the lake are strongly influenced by seasonal variations in the mixing regime, the recycling of nutrients and the episodic growth of edible algae.     

Ctenophore-zooplankton-phytoplankton interactions in Narragansett Bay, Rhode Island, USA, during 1972-1977

Plankton dynamics at a station in lower Narragansett Bay, RIare compared for six summer and fall seasons, 1972–1977.In four of these years, initiation of the summer pulse of thectenophore Mnemiopsis leidyi was accompanied by a rapid declinein zooplankton abundance and a summer phytoplankton bloom. Terminationof the phytoplankton bloom coincided with depleted ctenophoreabundance and increased zooplankton biomass in two of the years.Yearly variations in the summer abundance of the diatom Skeletonemacostatum were positively related to the magnitude of the ctenophorepulse. The magnitude of ctenophore population was related tothe zooplankton biomass present at the start of the pulse. Theserelationships, the timing and magnitude of the plankton eventssuggest that M. leidyi regulated summer zooplankton and phytoplanktondynamics. Ctenophores may control phytoplankton blooms indirectlythrough their predation on herbivorous zooplankton and directlyby the nutrient excretion accompanying such grazing. This evidencethat a planktonic carnivore two trophic steps removed from thephytoplankton regulates the latter's dynamics in NarragansettBay is analogous to reported regulation of benthic algal (kelp)dynamics by the sea otter, lobster and various crabs throughtheir predation on herbivorous sea urchins. The factors responsiblefor the seasonal decrease in ctenophores remain unresolved;ctenophore predators on Mnemiopsis are absent in NarragansettBay. Infection by the vermiform larval anemone, Edwardsia lineata,grazing by the butterfish, Peprilus triacanthus, and changesin food availability, temperature and salinity likewise do notexplain this disappearance.     

DENSITY-DEPENDENT SELECTION ON CONTINUOUS CHARACTERS: A QUANTITATIVE GENETIC MODEL

A quantitative genetic model of density-dependent selection is presented and analysed with parameter values obtained from laboratory selection experiments conducted by Mueller and his coworkers. The ecological concept of r- and K-selection is formulated in terms of selection gradients on underlying phenotypic characters that influence the density-dependent measure of fitness. Hence the selection gradients on traits are decomposed into two components, one that changes in the direction to increase r, and one that changes in the direction to increase K. The relative importance of the two components is determined by temporal fluctuations in population density. The evolutionary rate of r and K (per-generation changes in r and K due to the genetic responses of the underlying traits) is also formulated. Numerical simulation has shown that with moderate genetic variances of the underlying characters, r and K can evolve rapidly and the evolutionary rate is influenced by synergistic interaction between characters that contribute to r and K. But strong r-selection can occur only with severe and continuous disturbances of populations so that the population density is kept low enough to prevent K-selection.     

Hyperscums and the population dynamics of Microcystis aeruginosa

Conceptual models, based on 7 years of data, are constructedto simulate the annual cycle and population dynamics of Microcystisaeruginosa in hypertrophic, warm monomictic Hartbees-poort Dam,South Africa in order to assess the role of hyperscum formation.In Hartbeespoort Dam the large summer planktonic population(mean epilimnion biovolumes of 20–50 mm³ I^–1) andthe low wind speed resulted in the formation of hyperscums (thick,crusted accumulations of floating cyanobacteria at wind-protectedsites) containing up to 50% of the total standing crop for 2–3months in 4 out of 5 years. In years in which hyperscums formedthe post-maximal summer population maintained itself throughoutautumn and into late winter before declining to the annual nadir(>1000 cells ml^–1). When hyperscums did not form, orwere artificially removed, the population fell to similarlylow levels as early as May (autumn) and remained small untilthe spring growth phase began. Microcystis cells decompose inthe upper layers of a hyperscum, but this is not a major lossto the planktonic population. Hyperscums are refuges which helpmaintain large planktonic standing crops during winter whengrowth is not possible but have no effect on the long-term (perennial)survival of Microcystis.     

Niche width and variation within and between populations in colonizing species (Carex flava group)

Summary Taxa of the Carex flava group in Switzerland show a trend towards increased colonizing ability (r-selection). High colonizing ability is correlated with a large fundamental but a small and discontinuous realized niche. It is argued that r-selected species with wide niches should be monomorphic with generalists rather than polymorphic with specialists since they have small effective population sizes in which high genetic variability cannot be maintained. The most r-selected taxon of the group, C. viridula spp. viridula, has indeed the lowest genetic variability within populations but, in ecologically important characters, expresses the highest plasticity. The taxonomically important characters (inflorescences) have high heritability and differences between populations of C. viridula ssp. viridula are probably much affected by genetic drift.     

Life history, biomass and production of two planktonic cyclopoid copepods in a shallow subtropical reservoir

Two planktonic cyclopoid copepods (Tropocyclops prasinus andMesocyclops longisetus) were raised in the laboratory to obtainlife history information (duration of embryonic and post-embryonicdevelopment, reproductive performance, longevity, and stage-specificlength and weight values). Animals were maintained at 20 and25°C, and fed ad libitum. Development times were temperaturedependent when food was not limiting, with shorter periods ofembryonic and post-embryonic development and decreased longevityat 25°C. Laboratory data on the duration of developmentand biomass, together with population dynamics data obtainedin the field, were used to estimate summer and winter biomassand production of these species in a shallow reservoir, LagoaDourada, Brazil. The maximum production rate of T. prasinus,attained during summer, was 2.8 mg dry weight (DW) m^–3day^–1 and the highest daily production:biomass (P:B) ratiowas 0.29, whereas for M. longisetus the maximum production ratewas 1.4 mg DW m^–3 day^–1 and the highest daily P:Bratio was 0.39, in the winter. Over short time intervals (everyother day), there was great variability of the species productionrates. Species production rates were low compared to valuesreported in the literature for the same or other species ofequivalent sized copepods from both tropical and subtropicalregions.     

A model of the population dynamics of salps in coastal waters of the Ligurian Sea

A model of the population dynamics of saips is presented. Thismodel is unique in that its parameters (reproduction, transferand mortality rates) are based on physiological functions (feeding,excretion) determined experimentally in previous studies. Ittakes into account the simultaneous effects of temperature andfood concentration. It shows the mean trend of the annual variationand population dynamics of Salpa fusiformis (Cuvier) in thecoastal shallow waters of Villefranche-sur-Mer (Mediterranean).It can also be used as a tool to plan further studies: the resultsof its dynamics allow us to define better sampling programsin the field, and a sensitivity analysis suggests the experimentsto be performed in the laboratory.     

Population dynamics in variable environments. III. Evolutionary dynamics of r-selection

The boundary dynamics of a genetic model for an age-structured population in a temporally fluctuating environment are analyzed. The condition for invasion by a new allele identifies the logarithmic growth rate a of each life history phenotype as the fitness measure relevant to “r-selection.” An analytical formula is obtained for fitness a when temporal variance in life history characters is small. This formula reveals the major qualitative and quantitative effects of the average life history, fluctuations, and temporal autocorrelation on fitness. A similar approximation is obtained for the log-variance of population number so that the statistical distribution of population size can be estimated.     

Benthic–pelagic coupling in the population dynamics of the harmful cyanobacterium Microcystis

1. In eutrophic lakes, large amounts of the cyanobacterium Microcystis may overwinter in the sediment and re‐inoculate the water column in spring. 2. We monitored changes in pelagic and benthic populations of Microcystis in Lake Volkerak, The Netherlands. In addition, sedimentation rates and the rate of recruitment from the sediment were measured using traps. These data were used to model the coupling between the benthic and pelagic populations and to calculate the contribution of overwintering benthic and pelagic populations to the magnitude of the pelagic summer bloom. 3. Changes in the benthic Microcystis population showed a time lag of 3–14 weeks compared with the pelagic population. This time lag increased with lake depth. The largest amount of benthic Microcystis was found in the deepest parts of the lake. These observations suggest horizontal transport of sedimented Microcystis from shallow to deep parts of the lake. 4. Recruitment from and sedimentation to the sediment occurred throughout the year, with highest recruitment and sedimentation rates during summer. Model simulations indicate that the absence of benthic recruitment would reduce the summer bloom by 50%. 5. In spring, the total pelagic population was three to six times smaller than the total benthic population. Yet, model simulations predict that the absence of this small overwintering pelagic population would reduce the summer bloom by more than 64%. 6. Reduction of the overwintering pelagic populations, for instance by flushing, may be a useful management strategy to suppress or at least delay summer blooms of Microcystis.     

Factors regulating cladoceran dynamics in a Venezuelan floodplain lake

Five cladoceran zooplankton species in a Venezuelan floodplainlake, Laguna la Orsinera, were analyzed to identify factorscontrolling their dynamics over a period encompassing isolation,inundation by the Orinoco River and drainage. The abundanceof each species increased rapidly to a maximum associated withflooding of the lake by the Orinoco River. We calculated birth,death and population growth rates, and developed a method forestimating uncertainty in these parameters, in order to interpretobserved cladoceran abundance patterns. Rapid increases in populationsizes resulted both from high birth rates associated with decreasingturbidity following inundation and from the hatching of restingeggs. Birth rates remained high throughout the study, but highdeath rates restricted each population to a brief maximum andthen maintained small population sizes throughout the remainderof the study. Our demographic analyses suggest that high mortalityresulted from intense predation by fish and by Chaoborus larvae,rather than from resource limitation, and that this mortalitywas the major factor regulating cladoceran abundance duringinundation and drainage in this tropical floodplain lake.     

Seasonal variations of size-fractionated phytoplankton along the salinity gradient in the York River estuary, Virginia (USA)

The dynamics of phytoplankton size structure were investigatedin the freshwater, transitional and estuarine zones of the YorkRiver over an annual cycle. The contribution of large cells(microplankton, >20 µm) to total concentrations ofchlorophyll a increased downstream during winter, whereas thatof small cells (nanoplankton, 3–20 µm; picoplankton,<3 µm) increased downstream during summer. In the freshwaterregion, the contribution of micro phytoplankton to total concentrationsof chlorophyll a was significant during warm seasons (springand summer) but not during colder seasons (winter), whereasthe contribution of small-sized cells (especially picoplankton)increased during cold seasons. Temperature, light and high flushingrate appear to control phytoplankton community structure inthe freshwater region. In the transitional region, nano-sizedcells dominated the phytoplankton population throughout allseasons except during the spring bloom (April) when the chlorophylla concentration of micro phytoplankton increased. Size structurein the transitional region is most likely regulated by lightavailability. In the mesohaline region, nano- and pico-sizedcells dominated the phytoplankton population during the summerbloom, whereas micro-sized cells dominated during the winterbloom. Factors controlling phytoplankton community size structurein the mesohaline zone may be riverine nitrogen input, temperatureand/or advective transport from up-river. Based on these results,the spatial and seasonal variations in size structure of phytoplanktonobserved on the estuarine scale may be determined both by thedifferent preferences for nutrients and by different light requirementsof micro-, nano- and picoplankton. The results suggest thatanalyses of phytoplankton size structure are necessary to betterunderstand controls on phytoplankton dynamics and to bettermanage water quality in river-dominated, estuarine systems.     

DENSITY-DEPENDENT EVOLUTION OF LIFE-HISTORY TRAITS IN DROSOPHILA MELANOGASTER

Populations of Drosophila melanogaster were maintained for 36 generations in r- and K-selected environments in order to test the life-history predictions of theories on density-dependent selection. In the r-selection environment, populations were reduced to low densities by density-independent adult mortality, whereas populations in the K-selection environment were maintained at their carrying capacity. Some of the experimental results support the predictions or r- and K-selection theory; relative to the r-selected populations, the K-selected populations evolved an increased larval-to-adult viability, larger body size, and longer development time at high larval densities. Mueller and Ayala (1981) found that K-selected populations also have a higher rate of population growth at high densities. Other predictions of the thoery are contradicted by the lack of differences between the r and K populations in adult longevity and fecundity and a slower rate of development for r-selected individuals at low densities. The differences between selected populations in larval survivorship, larval-to-adult development time, and adult body size are strongly dependent on larval density, and there is a significant interaction between populations and larval density for each trait. This manifests an inadequacy of the theory on r- and K-selection, which does not take into account such interactions between genotypes and environments. We describe mechanisms that may explain the evolution of preadult life-history traits in our experiment and discuss the need for changes in theories of density-dependent selection.