Are readily culturable bacteria in coastal North Sea waters suppressed by selective grazing mortality?

We studied the growth of six culturable bacterial lineages from coastal North Sea picoplankton in environmental samples under different incubation conditions. The grazing pressure of heterotrophic nanoflagellates (HNF) was reduced either by double prefiltration through 0.8- micro m-pore-size filters or by 10-fold dilutions with 0.2- micro m (pore-size) prefiltered seawater. We hypothesized that those gamma-proteobacterial genera that are rapidly enriched would also be most strongly affected by HNF regrowth. In the absence of HNF, the mean protein content per bacterial cell increased in both treatments compared to environmental samples, whereas the opposite trend was found in incubations of unaltered seawater. Significant responses to the experimental manipulations were observed in Alteromonas, Pseudoalteromonas, and Vibrio populations. No treatment-specific effects could be detected for members of the Roseobacter group, the Cytophaga latercula-C. marinoflava lineage, or the NOR5 clade. Statistical analysis confirmed a transient increase in the proportions of Alteromonas, Pseudoalteromonas, and Vibrio cells at reduced HNF densities only, followed by an overproportional decline during the phase of HNF regrowth. Cells from these genera were significantly larger than the community average in the dilution treatments, and changes in their relative abundances were negatively correlated with HNF densities. Our findings suggest that bacteria affiliated with frequently isolated genera such as Alteromonas, Pseudoalteromonas, and Vibrio might be rare in coastal North Sea picoplankton because their rapid growth response to changing environmental conditions is counterbalanced by a higher grazing mortality.     

Mixing, stratification and the fate of primary production in an oligotrophic multibasin lake system (Quebec, Canada)

Impacts of mixing and stratification on the fate of primaryproduction were studied in an oligotrophic lake by comparingthe size-distributions of phytoplankton standing stock and productionin two basins, only one of which experiences seasonal thermalstratification. In both basins, the phytoplankton was dominatedby small cells (pico- and nanoplankton). The contribution ofpicoplankton to both biomass and production remained relativelyconstant throughout the season in both basins. Seasonal variationsin the size structure of phytoplankton communities do not agreewith the paradigm of dominance by small cells during summerstratification and dominance of larger cells during spring andfall mixing events. Nutrient control of productivity throughmixing and stratification is unlikely to affect the structureof phytoplankton communities when nutrients (allochthonous)derived from the catchment basin or sediments are in short supply.In such environments, nutrients (autochthonous) are largelyderived in the lake through heterotrophic food web processessuch as grazing, excretion and decomposition. Maximum ratesof production and losses in July and August in both basins areconsistent with increased regeneration and may represent a responseof larger-sized cells to higher nutrient availability resultingfrom enhanced grazing on picoplankton. The high correlationbetween the rates of loss and of potential growth for the phytoplanktoncommunity during all sampling periods, and the relative constancyof the picoplankton biomass, leads us to propose a long-term,steady-state equilibrium in the phytoplankton community underthe control of grazing by herbivores and/or other loss processes.     

Nutrients associated with terrestrial dissolved organic matter drive changes in zooplankton:phytoplankton biomass ratios in an alpine lake

相似文献   

Microflow Cytometer for optical analysis of phytoplankton

Analysis of the intrinsic fluorescence profiles of individual marine algae can be used in general classification of organisms based on cell size and fluorescence properties. We describe the design and fabrication of a Microflow Cytometer on a chip for characterization of phytoplankton. The Microflow Cytometer measured distinct side scatter and fluorescence properties of Synechococcus sp., Nitzschia d., and Thalassiosira p.; measurements were confirmed using the benchtop Accuri C6 flow cytometer. The Microflow Cytometer proved sensitive enough to detect and characterize picoplankton with diameter approximately 1 μm and larger phytoplankton of up to 80 μm in length. The wide range in size discrimination coupled with detection of intrinsic fluorescent pigments suggests that this Microflow Cytometer will be able to distinguish different populations of phytoplankton on unmanned underwater vehicles.     

Mixotrophic phytoplankton is enhanced by UV radiation in a low altitude, P-limited Mediterranean lake

UV radiation promotes harmful effects on phytoplankton populations, but it is influenced by the degree of sensitivity of different populations to the ultraviolet:photosynthetically active radiation ratio (UVR:PAR), part of which is P-dependent. Given the expected increase of UV radiation along with global change, one may ask if phytoplankton populations are able to adapt to the expectedly higher UVR:PAR ratio. If so, how would phytoplankton communities be affected? The main goal of this study is to answer these questions. Field and laboratory experiments were carried out with phytoplankton populations of an oligotrophic, low altitude lake in Central Spain. No changes were observed in abundance of phytoplankton fractions after UVR removal in the lake. However, autotrophic picoplankton underwent lower growth and contribution to total phytoplankton biomass when UVR increased. Phytoplankton biomass under enhanced UVR was one-third lower than the biomass reached under only PAR. UV-related growth changes were species-specific and linked to cell size and metabolism. An UVR increase would then promote phytoplankton assemblages who resulted from a trade-off between competitive advantages of picoplankton in a P-limited system and selected larger algae. Under these circumstances, the mixotrophic character of these larger species happened to be an evolutionary advantage.     

Demonstration of extraction and PCR amplification of DNA from phytoplankton of lakes with high humic acid content

Lakes with high levels of dissolved organic matter are common in northern temperate regions. These habitats are sensitive to environmental and climate change, but the molecular ecology and eco-physiology of their phytoplankton have been under studied, in part because the DOM interferes with molecular and biochemical analyses of these populations. We developed a procedure which uses polyvinylpyrrolidone to adsorb interfering material during the extraction of nucleic acids from these populations. This procedure does not depend on enzymatic lysis and yields DNA of sufficient quality to serve as a template for PCR amplification of specific genetic sequences. In particular, we detected fragments of the conserved rbcL gene encoding the large subunit of the Rubisco enzyme from the phytoplankton of lakes with high DOM. Our extraction procedure may be useful to other workers studying similar populations.     

Picoplankton photosynthesis and diurnal variations in photosynthesis-irradiance relationship in a eutrophic and meso-oligotrophic lake

The abundance and relative importance of autotrophic picoplankton were investigated in two lakes of different trophic status. In the eutrophic lake, measurements of primary production were performed on water samples in situ and in a light incubator three times during the day whereas for the oligotrophic lake, only one measurement of primary production was performed on water samples in the incubator. Dark-carbon losses of phytoplankton from Lake Loosdrecht were investigated in time series. Cell numbers of autotrophic picoplankton in eutrophic Lake Loosdrecht (3.2 × 10⁴ cells ml^–1) were lower than in meso-oligotrophic Lake Maarsseveen (9.8 and 11.4 × 10⁴ cells ml^–1 at the surface and bottom respectively). In the phytoplankton of both lakes the ratio of picoplankton production increased with decreasing light intensity. In Lake Loosdrecht depth-integrated contribution of picoplankton to total photosynthesis was less than 4%. The P-I-relationship showed diurnal variations in light saturated photosynthesis, while light limited carbon uptake remained constant during the day. Dark carbon losses from short-term labelled phytoplankton during the first 12 hours of the night period accounted for 10–25% of material fixed during the preceeding light period.     

Size-dependent phytoplankton responses to atmospheric forcing in Lake Biwa

Size-dependent changes in chlorophyll a and uptake of inorganiccarbon (C) and nitrogen (N) by phytoplankton were measured inthe shallow South Basin of Lake Biwa, before and during a periodof typhoons (high winds). The latter period was characterizedby complete mixing of the water column, a major decline in underwaterirradiance, and a transient increase in dissolved reactive Nand phosphorus (P). Nutrient concentrations, seston N:P ratiosand uptake rates indicate that P and not N limited phytoplanktonover the whole study period. The typhoon-induced increase inphosphorus supply resulted in Blackman-type (increased C- andN-specific growth rates) and Liebig-type (increased biomassyield) responses by the phytoplankton. Picoplankton were dominantin the relatively stable and clear water column prior to thetyphoons, but were rapidly outgrown by larger cells during andafter wind-induced mixing. The slower response of picoplanktonindicates lower maximum intrinsic growth rates and photosyntheticefficiency. These observations are contrary to the view thatpicoplankton have higher light-harvesting abilities and growthrates than larger cells. Typhoon-induced mixing stimulated theshift to fast-growing, dim light-adapted larger cells. The resultsquestion the allometric paradigm of increasing growth ratesand light-capturing efficiency with decreasing cell size, butare consistent with the oceanographic view that large-celledphytoplankton control the major fluctuations in biomass andprimary productivity, while picoplankton account for a comparativelystable background productivity.     

Net production and consumption of fluorescent colored dissolved organic matter by natural bacterial assemblages growing on marine phytoplankton exudates

An understanding of the distribution of colored dissolved organic matter (CDOM) in the oceans and its role in the global carbon cycle requires a better knowledge of the colored materials produced and consumed by marine phytoplankton and bacteria. In this work, we examined the net uptake and release of CDOM by a natural bacterial community growing on DOM derived from four phytoplankton species cultured under axenic conditions. Fluorescent humic-like substances exuded by phytoplankton (excitation/emission [Ex/Em] wavelength, 310 nm/392 nm; Coble's peak M) were utilized by bacteria in different proportions depending on the phytoplankton species of origin. Furthermore, bacteria produced humic-like substances that fluoresce at an Ex/Em wavelength of 340 nm/440 nm (Coble's peak C). Differences were also observed in the Ex/Em wavelengths of the protein-like materials (Coble's peak T) produced by phytoplankton and bacteria. The induced fluorescent emission of CDOM produced by prokaryotes was an order of magnitude higher than that of CDOM produced by eukaryotes. We have also examined the final compositions of the bacterial communities growing on the exudates, which differed markedly depending on the phytoplankton species of origin. Alteromonas and Roseobacter were dominant during all the incubations on Chaetoceros sp. and Prorocentrum minimum exudates, respectively. Alteromonas was the dominant group growing on Skeletonema costatum exudates during the exponential growth phase, but it was replaced by Roseobacter afterwards. On Micromonas pusilla exudates, Roseobacter was replaced by Bacteroidetes after the exponential growth phase. Our work shows that fluorescence excitation-emission matrices of CDOM can be a helpful tool for the identification of microbial sources of DOM in the marine environment, but further studies are necessary to explore the association of particular bacterial groups with specific fluorophores.     

Size-related photosynthetic characteristics of phytoplankton during periods of seasonal mixing and stratification in an oligotrophic multibasin lake system

Phytoplankton photosynthetic responses were studied in two basinsof an oligotrophic lake (Québec, Canada). which are characterizedby the absence (shallow Basin 1) and presence (deeper Basin2) of seasonal thermal stratification. Size-fractionated photosynthesiswas used to characterize changes in phytoplankton characteristicsduring periods of seasonal mixing and stratification. Seasonalvariations of P _max showed size-related differences, with maximumvalues in July for the picoplankton and in November for thenanoplankton. Similar patterns of variability in     

Seasonal Changes in Chlorophyll-containing Picoplankton Populations of Ten Lakes in Northern England

Key features of photosynthetic picoplankton populations were compared during 1988 in ten lakes in northern England ranging from oligotrophic to slightly eutrophic; two of the three eutrophic lakes were shallow and lacked a thermocline. Measurements were made at 0.5 m depth of temperature, total chlorophyll a, chlorophyll-containing picoplankton cell density, mean picoplankton cell volume and percentage of phycoerythrin-rich cells in the total picoplankton population. All lakes showed maxima for total chlorophyll concentration and picoplankton cell density in mid- to late summer. The maximum value for picoplankton density ranged from 3.4 × 10³ (Esthwaite Water) to 1.3 × 10⁶ cells ml⁻¹ (Ennerdale Water). There was a significant negative relationship (p < 0.05) between log₁₀ of maximum picoplankton cell density and maximum total chlorophyll, the latter being taken as an indicator of lake trophic status. The ratio of maximum to minimum picoplankton density during the year in a particular lake ranged from 39 to 2360 and showed no obvious relationship to lake type. Overall, the seasonal range in picoplankton density was about one order of magnitude greater than the range in total chlorophyll a, but there were considerable differences between lakes. Phycoerythrin-rich picoplankton as a percentage of total picoplankton reached a maximum in summer in all lakes. Values were always very low (<5%) in the two shallow eutrophic lakes, but reached 97% and over in the four most oligotrophic lakes. In two of the oligotrophic lakes, Wast-water and Ennerdale Water, phycoerythrin-rich picoplankton was a major component of the summer phytoplankton biomass.     

Cell-specific beta-N-acetylglucosaminidase activity in cultures and field populations of eukaryotic marine phytoplankton.

It is widely appreciated that eukaryotic marine phytoplankton can hydrolyze a variety of compounds within the dissolved organic matter (DOM) pool in marine environments. Herein, cultures and field populations of marine phytoplankton were assayed for beta-N-acetylglucosaminidase activity, a terminal enzyme of chitin degradation. A traditional bulk assay, which can assess hydrolytic rate, but is not cell-specific, was complemented with a cell-specific assay that images the activity associated with single cells using an enzyme labeled fluorescence (ELF) substrate. beta-N-acetylglucosaminidase activity was widespread across various taxa of marine phytoplankton, and activity was observed both under controlled culture conditions and in field populations. The number of cells with enzyme activity varied with the nutritional physiology of the test species in three of the 17 cultures tested. In these three cases the number of cells with activity in the low nutrient medium was higher than in nutrient replete medium. Taken together, these data suggest that a broad group of marine phytoplankton may be a relevant part of chitin-like DOM degradation and should be incorporated into conceptual models of chitin cycling in marine systems.