Polychlorinated biphenyl (PCB) uptake by marine phytoplankton

The time-courses of uptake for 2,4,5,2,5-pentachlorobiphenyl (PCB) by 11 marine phytoplankton species were measured and found to be rapid, with equilibration occurring within 0.5 to 2.0 h. These data were described with the empirical Freundlich adsorption isotherm. The relationship between cell density and accumulation of PCBs was also investigated. Concentration factors on a volume per volume basis ranged from 1.23x10⁴ to 2.41x10⁶ for the 11 algal species examined. These values are comparable in magnitude to factors reported previously for phytoplankton in natural marine systems.     

The effects of three oils on marine phytoplankton photosynthesis

The effects of 3 oils (Venezuelan crude, No. 2 fuel, and No. 6 fuel) on the photosynthesis of natural phytoplankton communities from Bedford Basin, Nova Scotia (Canada), and the northwest Atlantic Ocean between Halifax and Bermuda were examined using a radiocarbon method. The 3 oils can inhibit photosynthesis, and the degree of inhibition depends upon oil type and concentration. The No. 2 fuel oil was the most toxic. Under certain conditions, low concentrations of Venezuelan crude oil can stimulate photosynthesis. On the basis of these results, it is concluded that present levels of oil contamination in Bedford Basin could be inhibiting photosynthesis by a few percent, while present levels in open ocean water have no apparent deleterious effect on photosynthesis.Bedford Institute of Oceanography Contribution.     

Polychlorinated biphenyl (PCB) residues in European roe deer (Capreolus capreolus) and red deer (Cervus elaphus) from north-western Poland

The purpose of this study was to evaluate polychlorinated biphenyls (PCBs) contamination levels in roe and red deer from north-western Poland and to assess environmental pollution in this area. A quantitative analysis was conducted using a capillary gas chromatography/mass spectrometry method. The mean concentrations of ΣPCBs (sum of PCBs: 28, 52, 101, 138, 153, 180) in liver samples were 30.24±12.35 ng·g^?1 of lipid weight (l.w.) in roe deer and 60.13±14.23 ng·g^?1 l.w. in red deer, compared with 24.21±10.02 and 45.22±9.77 ng·g^?1 in the lungs of roe and red deer, respectively. PCBs 138, 153 and 180 were the dominant congeners in the liver samples of the analysed animals, whereas PCB 138 and 153 in the lungs. TEQs levels calculated for only dioxin-like PCBs were low: 0.32 and 0.29 pg WHO-PCB-TEQ·g^?1 fat in liver of red deer and roe deer, respectively. The mean PCB concentrations obtained in our study for organs of roe deer and red deer were several times lower than those reported elsewhere. These findings show that the investigated roe and red deer originated from an area with low levels of PCB contamination.     

Diel periodicity of photosynthesis in marine phytoplankton

Short-term changes in photosynthesis were documented for 17 of 24 marine phytoplankton species, representing a range of taxonomic groups. Periodicity in phytoplankton photosynthesis on light-dark cycles (diel periodicity) was widespread but not universal for the species studied. The centric diatoms Lauderia borealis, Ditylum brightwellii, Stephanopyxis turris, Coscinodiscus rex, Chaetoceros gracile, and Biddulphia mobiliensis had strong diel periodicity in photosynthetic capacity (P _max). Amplitudes of the daily variations ranged from 2.9 to >50, with maxima in the morning or near midday, and with minima during the dark period, and these variations were not dependent on changes in cell pigmentation. There was some evidence for sustained photosynthetic periodicity in constant conditions in several diatoms, and an endogenous rhythm may have been present. The photosynthesis-irradiance (P-I) relationship was time-dependent for representative marine diatoms, with both the initial slope () and the asymptote (P _max) of P-I curves exhibiting significant synchronous diel oscillations. Moreover, detailed studies of the amplitude and timing of photosynthetic periodicity for the diatoms L. borealis and D. brightwellii demonstrated large temporal variations in photosynthesis with morning maxima. These P-I oscillations are discussed with reference to models of primary production which use the relationship between photosynthesis and light as a component of predictive equations for phytoplankton growth in the sea.     

Short-term variability of photosynthesis in natural marine phytoplankton populations

Harmonic regression analysis has been used to determine the short-term variability in the photosynthetic rate (mgC/mg chlorophyll a/h) of phytoplankton in three inlets of Japan. In natural water without large zooplankton present, the photosynthetic rate [log P=log (100xmgC/mg chlorophyll a/h)] can be expressed as (B+A cos T). Factor B represents the average photosynthetic rate, of which the maximum is usually designated as P _max, and Factor A corresponds to the slope of the regression line. The phase of the periodicity, represented by T, is adjusted to give the highest correlation: usually T is expressed as [360/24 x (local time + 4)] in degrees. The correlation between Factors A and B is very high (r=0.95, P<0.001), indicating that Factor A may depend upon Factor B (potential activity of chlorophyll a). Both Factors A and B decrease with decreasing irradiance, but the slope of each regression between Factor A and irradiance varies with season. Continuous darkness reduces the phase of the periodicity to one cycle a day when phytoplankton has multiple cycles of photosynthetic rate per day. Adequate nutrient supply from zooplankton regeneration may cause an increase in Factor B; however, excess density of zooplankton decreases Factor A.     

Iron-mediated effects on nitrate reductase in marine phytoplankton

The potential activity of nitrate reductase was determined in uni-algal cultures in the laboratory and in natural marine phytoplankton assemblages. In the laboratory bioassays, distinct differences in nitrate reductase activity were observed in iron replete versus depleted cultures for Emiliania huxleyi, Isochrysis galbana and Tetraselmis sp. Cells from iron-depleted cultures had 15 to 50 percent lower enzyme activity than those from iron-replete cultures. Upon addition of iron, nitrate reductase activity was enhanced in depleted cells up to levels comparable to those of the replete cells. Bioassays in the northern North Sea conducted in 1993, under low iron conditions, demonstrated similar results. Upon addition of 2.5 nM iron, a distinct enhancement, to a maximum of three times, of nitrate reductase activity was observed within 32 h after addition. Therefore, iron can stimulate nitrate reductase activity. In spite of the clean techniques used, some nitrate reductase activity was always observed. Iron deficiency was shown to impair nitrate reductase activity, but it is unlikely that nitrate reduction would cease completely.     

Effects of light intensity on photosynthesis and dark respiration in six species of marine phytoplankton

Using an oxygen polarographic electrode, the shapes of photosynthetic curves and the effects of light on dark respiration in 6 species of marine phytoplankton wer examined. The species used were Skeletonema costatum, Ditylum brightwellii, Cyclotella nana (Thalassiosira pseudonana) (all Bacillariophyceae), Dunaliella tertiolecta (Chlorophyceae), Isochrysis galbana (Haptophyceae), and Gonyaulax tamarensis (Dinophyceae). A hysteresis was observed in all species examined with respect to increasing and decreasing light. Compensation light intensities varied by over 4 orders of magnitude, suggesting that the 1% light depth is an ambiguous measure of the euphotic zone. The data suggest that dark respiration accounts for ca. 25% of gross photosynthesis, but is species-dependent. In addition, respiration versus cell size does not describe an inverse exponential function over the size scales examined.This research was performed under the auspices of the United States Energy Research and Development Administration under Contract No. EY-76-C-02-0016.     

The effect of intensity and quality of illumination on the photosynthesis of some tropical marine phytoplankton

Using solar energy as a source of illumination, photosynthesis in 11 species of marine plankton algae was studied as a function of light intensity. From the photosynthesis-light curve for each organism, the saturation points (I _k ) in different organisms were determined. Among the diatoms and flagellates, the highest I _k (saturation point) values were found in Rhizosolenia styliformis and Dinophysis miles respectively. When the organisms were exposed to a portion of the visible spectrum starting from 700 m, the photosynthesis was found to be related to the radiant energy. The missing portions of the spectrum produced no significant change in the rate of photosynthesis. The photosynthetic response shown by the different organisms was strikingly similar, which signifies that, despite the qualitative dissimilarities which the organisms may possess in their pigment composition, they are capable of much chromatic adaptation.     

Products of photosynthesis in natural populations of marine phytoplankton from the Gulf of Maine

We have measured the photosynthetic assimilation of ¹⁴C-carbon dioxide into (1) ethanol-soluble, (2) hot-trichloroacetic acid (TCA)-soluble (polysaccharide), and (3) protein fractions of natural populations of marine phytoplankton. Diurnal studies showed a continuing incorporation of carbon-14 into the protein fraction during hours of darkness. This was accompanied by a concomitant decrease in the proportion assimilated into polysaccharide. When incorporation was measured under constant experimental conditions, the pattern of photosynthesis did not vary from one time of day to another. At one station approximately 12 km south of Boothbay Harbor, the proportion of carbon entering protein showed marked seasonal changes. During the winter, approximately 10 to 20% of the fixed carbon was incorporated into protein. During the summer the value increased to 22 to 35%. Between these times, a transient high value of 37 to 47% of the fixed carbon entering protein coincided with the spring bloom. The increases in proportion incorporated into protein were largely paralleled by equivalent decreases in the polysaccharide fraction. The proportion of carbon incorporated into protein during photosynthesis also increased markedly at reduced light intensities. This increase occurred both when populations were incubated in neutral-density filters and when incubated at increasing depths in the photic zone. There was little consistent and significant difference between the neutral-density filters and depth in the water column, suggesting a minimal role for light quality. The extent of the increased relative rate of protein synthesis at the lower light intensities depended on the nutritional state of the phytoplankton. For example, summer populations from water containing low concentrations of inorganic nutrients responded less dramatically to reduced light intensities than did populations from nutrient-rich waters.     

Effects of cadmium and low magnesium on cell division and calcification in the marine coccolithophorid Cricosphaera (Hymenomonas) carterae

Cadmium (Cd) added to normal media and to magnesium (Mg)-deficient media produced inhibitory effects on cell division and cell calcification in the marine coccolithophorid alga Cricosphaera (Hymenomonas) carterae. Compared with controls in normal media (with 25 mM Mg), cell growth decreased progressively with Cd at concentrations of 5–20 M. In Mg-deficient media (with 6 mM and 0.08 mM Mg) the inhibitory effects were more pronounced with complete arrest of cell division at 20 M Cd. The greatest Cd inhibition occurred in media with the lowest Mg concentration (0.08 mM). Cadmium (5–40 M) also decreased recalcification (coccolith formation) in cells previoasly decalcified with CO₂ with complete inhibition at 40 M Cd. Inhibition of recalcification in various Cd concentrations (5–40 M) was more pronounced in low-Mg medium (with 6 mM and 0.08 mM Mg) compared with normal medium (25 mM Mg). Partial or complete reversal of the inhibitory effects of Cd and low Mg media on cell division and calcification occurred following a wash and resuspension of the cells in normal control medium (25 mM Mg).     

Products of photosynthesis by marine phytoplankton: the effect of environmental factors on the relative rates of protein synthesis

A method is presented by which the gross pattern of photosynthetic carbon-dioxide fixation in marine phytoplankton can be determined. It depends on differential solvent extraction yielding an ethanol-soluble, a hot TCA-soluble (polysaccharide) and a residue (protein) fraction. Using this fractionation technique, the effects of various environmental factors on the pattern of photosynthesis by the marine diatom Phaeodactylum tricornutum (Bohlin) have been investigated. Low light intensities and increasing degrees of nitrogen limitation in a chemostat increase markedly the relative rates of protein synthesis. Growth of the alga at lower temperatures also increases the proportion of carbon incorporated into the protein fraction. This increased protein syntheses is generally at the expense of the polysaccharide fraction. Preliminary experiments have established the suitability of this fractionation method for natural populations of phytoplankton and have shown similar effects of light intensity on the relative rates of protein synthesis.     

Climate change effects on phytoplankton depend on cell size and food web structure

We investigated the effects of warming on a natural phytoplankton community from the Baltic Sea, based on six mesocosm experiments conducted 2005–2009. We focused on differences in the dynamics of three phytoplankton size groups which are grazed to a variable extent by different zooplankton groups. While small-sized algae were mostly grazer-controlled, light and nutrient availability largely determined the growth of medium- and large-sized algae. Thus, the latter groups dominated at increased light levels. Warming increased mesozooplankton grazing on medium-sized algae, reducing their biomass. The biomass of small-sized algae was not affected by temperature, probably due to an interplay between indirect effects spreading through the food web. Thus, under the higher temperature and lower light levels anticipated for the next decades in the southern Baltic Sea, a higher share of smaller phytoplankton is expected. We conclude that considering the size structure of the phytoplankton community strongly improves the reliability of projections of climate change effects.     

Impact of osmolytes on buoyancy of marine phytoplankton

Marine phytoplanktonic cells can achieve neutral buoyancy only if the excess density of their relatively heavy structural materials (proteins, carbohydrates, silicate) is compensated for by the incorporation of materials that have densities less than seawater. We have calculated densities and osmotic concentrations for several marine algae, based on published values of structural materials and concentrations of inorganic ions and other osmolytes. The calculations, incorporating the partial molal volume, molecular mass, concentrations and osmotic coefficients, indicate that most published listings of intracellular osmolytes in marine algae are insufficient to provide the turgor known to exist. Similarly, the density of phytoplanktonic cells, calculated on the basis of known or estimated concentrations of cellular components, generally exceeds the density of seawater, which would cause negative buoyancy (sinking) throughout. We use models of osmotic concentration and cellular density in which we supplement known concentrations of osmolytes with proxy osmolytes. In particular, concentrations of some 100 mol m^-3 of quaternary ammonium derivatives can explain the deficits of both osmotic concentration and buoyancy.     

Effects of power-plant cooling systems on marine phytoplankton

The large quattities of marine phytoplankton passing through the cooling systems of two Southern California coastal power plants were found to be greatly reduced in numbers (41.7%) and in volume (33.7%). The biomass killed from June, 1972 to May, 1973 amounted to approximately 1,700 tons of organic carbon. Phytoplankton mortalities were most pronounced from October to December when intake waters of 17° to 20°C were subjected to temperature elevations of 9 to 11C°, and were lowest from January to March when cooler ambient temperatures prevailed. There was no apparent reduction in phytoplankton stocks when the intake water was cooler than 15°C. Surviving cells in 25° and 26.5°C effluent waters were growing three times faster than influent populations, which suggests that power-plant effects on phytoplankton stocks are often short-lived. However, entrainment effects appear very disruptive, in changing the structure of phytoplankton communities and in constantly reducing species diversity (H′). Passage through the condenser tubes affected algal species differentially, killing diatoms in greater numbers (45.7%) than dinoflagellates (32.8%), and reinforcing the dominance of the two major species, Asterionella japonica and Gonyaulax polyedra, that were the most tolerant. The severity of the impact appears to be controlled by two interacting factors: intake water-temperature and magnitude of temperature increase. On this basis, use by coastal power plants of deep-sea water for cooling is strongly advocated.     

Feeding of marine planktonic copepods on mixed phytoplankton

The feeding of juveniles and adults of the copepods Eucalanus pileatus, Temora stylifera and T. turbinata fed a mixture of the phytoplankton Skeletonema costatum, Leptocylindrus danicus and Rhizosolenia alata f. indica was studied at 20°C. E. pileatus nauplii, copepodids and adult females ingest similar percentages of the 3 algae in terms of carbon. Temora juveniles younger than CII ingest mainly S. costatum; at more advanced developmental stages, the ingestion rate on S. costatum remains constant whereas feeding on L. danicus and R. alata f. indica increases with increasing body weight. Feeding on high concentrations of large particles reduces the grazing pressure on small particles, thus favoring zooplankton which require small-sized food.     

Influence of inter- and intra-daily light-field variability on photosynthesis by coastal phytoplankton

An investigation was carried out to determine the relationships between the principal photosynthetic parameters of natural marine phytoplankton and the properties of the irradiance of the preceding five days and the intra-daily ambient irradiance. Samples used in the study were collected from Strangford Lough, Northern Ireland during both winter and summer between 1979 and 1981. Photosynthetic parameters were determined for both constant and ambient incubation light fields. The fluctuation properties of the irradiance field exerted little influence on the photosynthetic parameters. In summer populations, the parameters obtained from morning samples were strongly influenced by the total irradiance recorded on the fourth day previous to experimentation, irrespective of the incubation irradiance. In contrast, the corresponding parameters from afternoon samples were most influenced by the total irradiance received during incubation. The influence of these two separate factors over a day may contribute to variability in the magnitude of diel changes in marine phytoplankton photosynthesis.     

Influence of high temperature and residual chlorine on marine phytoplankton

Marine phytoplankton forms are frequently exposed to sudden biological changes such as rapid rise in water temperature and chlorine content of their environment, resulting from the use of sea water for cooling purposes by electric generators. The direct influence of these effluents, i.e. inhibitory effects of high temperature and residual chlorine on growth and photosynthesis of Chlamydomonas sp. and Skeletonema costatum, were investigated experimentally. Chlamydomonas sp. and S. costatum exposed to high temperatures were affected in their growth from 43° and 35°C, respectively, by immersion of the respective cultures in a warm bath for 10 min. Treatment at high temperatures of 40 °C and 30° 35°C for 10 min, influenced their photosynthetic activities, which were completely inhibited immediately after 10 min exposure at 42° and 37 °C, respectively. S. costatum was killed by chlorine at a concentration of 1.5 2.3 ppm when exposed for exactly 5 or 10 min, while Chlamydomonas sp. was not irreversibly damaged even at 20 ppm chlorine or more with the same exposure period. These results lead to the conclusion that the high temperature of, and residual chlorine in, effuents from a power plant discharging into the open sea, should not cause great damage to marine phytoplankton in that area.     

Cycling of selenite and selenate in marine phytoplankton

The marine phytoplankton Dunaliella tertiolecta, Cachonina niei, Thalassiosira nordenskioldii, Phaeodactylum tricornutum, and Chaetoceros sp. were incubated with a range of molar concentrations of sodium-selenite (Na₂-SeIVO₃) and sodium-selenate (Na₂-SeVIO₄) to examine further their role in metabolic cycling of selenium in ocean waters. At low selenium concentrations, approaching those found naturally in seawater (10^-10 to 10^-9 M), all species distinguished between selenite and selenate, and actively concentrated selenite from the incubating medium while only marginally accumulating selenate. At much higher concentrations (10^-8 to 10^-6 M), selenate was also taken up. At the highest concentration tested, i.e., 10^-5 M with C. niei, after an immediate rapid uptake in the first 24 h, the intracellular selenite and selenate levels dropped to about 35 to 50% of the initial peak values. These observations suggest an uptake mechanism in these algae which, at normal ambient concentrations of selenium (10^-9 M), preferentially selects selenite and excludes selenate. At much higher concentrations (10^-8 M), the mechanism becomes overloaded and both selenium species enter the cells. Intracellularly, selenite became associated primarily with protein and amino acid fractions, in approximately equal proportions, while only ca. 4% of total intracellular selenium was found in the lipid fraction. Trace amounts of selenate that entered the cells, mainly during the first minutes of exposure, also entered the protein and amino acid components, but over time were increasingly associated with the protein fraction only. At the end of a 10-d incubation of algal cells in selenite-spiked medium, less than 25% of total Se in the medium could in fact be identified analytically as selenite. This suggests the presence of a non-selenite metabolite, possibly released back into the medium from the algae.     

Coagulation efficiency and aggregate formation in marine phytoplankton

Flocculation of phytoplankters into large, rapidly sinking aggregates has been implicated as a mechanism of vertical transport of phytoplankton to the sea floor which could have global significance. The formation rate of phytoplankton aggregates depends on the rate at which single cells collide, which is mainly physically controlled, and on the probability of adhesion upon collision (=coagulation efficiency, stickiness), which depends on physico-chemical and biological properties of the cells. We describe here an experimental method to quantify the stickiness of phytoplankton cells and demonstrate that three species of diatoms grown in the laboratory (Phaeodactylum tricornutum, Thalassiosira pseudonana, Skeletonema costatum) are indeed significantly sticky and form aggregates upon collision. The dependency of stickiness on nutrient limitation and growth was studied in the two latter species by investigating variation in stickiness as batch cultures aged. In nutrient repleteT. pseudonana cells stickiness is very low (< 5 × 10^?3), but increases by more than two orders of magnitude as cell growth ceases and the cells become nutrient limited. Stickiness ofS. costatum cells is much less variable, and even nutrient replete cells are significantly sticky. Stickiness is highest (> 10^?1) forS. costatum cells in the transition between the exponential and the stationary growth phase. The implications for phytoplankton aggregate formation and subsequent sedimentation in the sea of these two different types of stickiness patterns are discussed.     

Size structure of phytoplankton biomass and photosynthesis in subtropical Hawaiian waters

In a subtropical Hawaiian ecosystem, phytoplanton size structure analyses (November–December, 1980) showed that ultraplankton (>3μm), nanoplankton (>20μm) and netplankton (>20μm) accounted for ca. 80, 98, and 2% of total chlorophyll standing stock, respectively, on the basis of chlorophyll. Similar trends were evident, for other biomass indices (e.g. cell numbers, total cell volume, ATP, particulate organic carbon, particulate organic nitrogen). The ultraplankton fraction consisted primarily of small flagellates (1 to 3 μm diam) and coccoid cells (?1 μm diam); the 3 to 20 μm fraction was represented by dinoflagellates, coccolithophores, diatoms, and chrysophytes; and the netplankton fraction consisted principally of dinoflagellates and centric diatoms. Community photosynthesis had a size distribution similar to that of biomass. Sinking rates for the 3 μm, 3 to 20 μm, and >20 μm fractions averaged 0.0, 0.09, and 0.29m d^?1, respectively. The absence of measurable sinking rates for the ultraplankton, together with the relative abundance of biomass in this fraction, result in very small phytoplankton losses due to sinking in such subtropical surface waters.