A seasonal study of the distributions of surface state variables in Liverpool Bay. II. Nutrients

Distributions of dissolved inorganic nitrate, phosphate, and silicate observed in the surface waters of Liverpool Bay during a seasonal cycle of cruises in 1975 are presented. Winter distributions were influenced by the proportion of waters from various sources, their chemistry, and the mode of circulation, all of which were temporally variable. Non-winter distributions were additionally influenced by in situ biological activity. Principal component analysis provided a preliminary means of separating and assessing the relative importance of these factors and depicting the centres of biological activity during the non-winter cruises. Different circulation modes in January and December produced distributions with little visual similarity, and patchy nutrient distributions accompanied the spring and autumn phytoplankton blooms. Nitrogen-rich industrial and domestic effluents modified the nutrient availability ratios in the receiving waters so that silicon limited diatom growth over large areas of the Bay in spring. Nitrogen became ‘bio-limiting’ in summer and autumn. The direction of the surface residual circulation before the spring bloom is proposed as the major influence governing subsequent nutrient distributions and phytoplankton populations.     

A seasonal study of the distributions of surface state variables in Liverpool Bay. I. winter data

The physical, chemical, and biological characteristics of the surface waters of Liverpool Bay were investigated during six seasonal cruises in 1975. The winter data has been analysed to provide criteria by which spatial and temporal changes in the distributions of surface state variables during the seasonal production cycle may be judged. Surface distribution maps observed during two winter cruises (January and December) were markedly dissimilar. This temporal variability is attributed to changing circulation patterns within the Bay induced by variations in magnitude and direction of wind stress. Despite the ‘visual’ dissimilarity in spatial distributions observed on the two cruises, principal component analysis demonstrates a similar general background which is dominated by conservative physical mixing of sea and fresh waters. During winter, the spatial variability in water characteristics originated at the boundaries of the cruise path and spread internally, primarily as a consequence of the differing composition of the source waters, to the sea area. No internal sources or sinks, either anthropogenically or biologically induced, were encountered during the winter cruises.     

A seasonal study of the distributions of surface state variables in Liverpool Bay. III. An offshore front

Variously orientated transects through Liverpool Bay in December, 1976, revealed a narrow but steep density discontinuity running north to south through the surface waters. Surface distribution maps from cruises during the winter of 1976–1977 showed that the density discontinuity provided a sharp line of demarcation between the physical and chemical characteristics of the offshore and coastal waters. Over the winter, an accumulation of river discharged nutrients in the waters bounded by the front and the coast generated a large nutrient reservoir in the inshore waters and propagated a difference in the nutrient availability ratios across the front. As a consequence, by March the inshore waters were characterized by lower salinities and temperatures, higher dissolved inorganic nutrient concentrations and lower silicon to total nitrogen ratios than the offshore waters. Prior to the 1977 spring phytoplankton bloom in Liverpool Bay, these two contrasting water types were in juxtaposition along the length of the front.     

The flowers that bloom in the spring: RNA processing and seasonal flowering

Seasonal flowering in plants responds to hormonal and environmental cues that lead to expression of genes for flowering and growth. A new paper in this issue of Cell describes how one regulatory gene controls its own expression at the level of mRNA polyadenylation, adding an exciting new model for both the RNA processing and plant gene expression fields.     

Filtration rate of zooplankton community during spring bloom in Akkeshi Bay

The filtration rate of a natural Zooplankton community at the time of the spring bloom in Akkeshi Bay was estimated using changes in concentration of chlorophyll a, of particulate carbon, and changes in cell numbers. The size range of phytoplankton cells utilized indicated that the maximum length of chain consumed depended upon the size-range of the Zooplankton community. Evidence for size-selection of food by animals is presented. The possible explanation of relation between the filtration efficiency — the ratio of respiration rate to the product of filtration rate and dissolved oxygen — and the quantity and quality of food is discussed. When there is a wide range of phytoplankton sizes or a small amount of phytoplankton, the filtration efficiency decreases.     

Bacterial dynamics and distribution during a spring diatom bloom in the Hudson River plume, USA

Bacterial abundance and [³H]thymidine incorporation rates wereused to characterize bacterial distributions and dynamics duringa spring diatom bloom in the coastal plume of the Hudson Riverduring March, 1981. Bacterial abundance did not decline significantlyaway from the plume or across the continental shelf. However,a pronounced gradient was observed for [³H]thymidine incorporation. Following a northeast gale, a bloom of Skeletonema costatumdeveloped in response to coastal upwelling. As the plume becamesaltier, warmer and larger, bacterial abundance averaged 1.3x 10⁹ cells 1^–1. Bacterial incorporation of [³H]thymidineinto cold 5% TCA insoluble materials, bacterial production andspecific growth rates averaged 80–120 pmol 1^–1 d^–1,1.4–2.0 x 10⁹ cells 1^–1 and 1.2–1.5 d^–1.respectively. The mean density of bacteria in the plume didnot change even though growth rates were higher than expectedlosses from sinking, mixing and export. The abundance and production levels of attached bacteria inthe plume were significantly higher than they were in coastalwater outside the plume. In contrast, free bacterial levelswere similar in all regions of the shelf and plume. Bacterialparameters in the plume were not correlated with phytoplanktonpigment concentrations, while significant positive correlationswere found in shelf waters >33 salinity. Thus bacteria werecoupled to phytoplankton in shelf waters but not in the plumewhere allochthonous dissolved matter was probably supportingthe bacteria. ^*Lamont-Doherty Geological Observatory Contribution No. 3459²Present address: Department of Microbiology, University ofGeorgia, Athens, GA 30602, USA.     

A multi-lake study of seasonal variation in lake surface evaporation using MODIS satellite-derived surface temperature

Knowledge of the evaporative loss from lakes and reservoirs is critical to water resources managers as well as to the overall understanding of the water balance in a given basin, geographical region, or continent. Existing methods for ascertaining evaporation from lakes and reservoirs include point measurements, water balance and mass transfer calculations, and proxy measurements using a pan. Point measurements using the eddy flux covariance method can be accurate, but are resource intensive and unsuited for determining spatial variation over a lake, or for obtaining measurements over many lakes. Mass balance methods cannot provide spatial variability and their accuracy depends on other portions of the water balance that can be challenging to obtain, such as leakage. Similarly, relatively recently deployed scintillation methods provide only an average for a strip across a lake and are also resource intensive and not suited for multi-lake studies. Evaporation pan measurements can also be used, though their accuracy is poor. Herein, we use a combination of Moderate Resolution Imaging Spectroradiometer (MODIS) satellite measurements of water surface temperature, measurements of wind speed, air temperature, and relative humidity from local NWS stations, and a mass transfer method, to demonstrate multi-lake evaporation measurements. Specifically, the seasonal variation in evaporation is obtained for the five major lakes in the Savannah River Basin (in South Carolina, USA): Lakes Jocassee, Keowee, Hartwell, Russell, and Thurmond. Since this approach requires only an existing satellite resource with global coverage and existing NWS stations, this method can potentially be ported to any lake where there is a nearby meteorology station. Hence, this method could be used by both water resource managers and limnologists alike. The possibility is discussed of extending this approach beyond a single basin to encompass an entire geographical region or continent.     

Vertical distribution and cyst production of Peridiniella catenata (Dinophyceae) during a spring bloom in the Baltic Sea

Vertical distribution and cyst production of the chain-forming,spring dinoflagellate Peridiniella catenata were studied throughoutthe spring season of 2000 in the coastal Gulf of Finland. Numbersof cells were monitored in the water column, and cyst sedimentationwas recorded using multiple sediment traps moored at three discretedepths. At the onset of the spring bloom, most of the populationwas situated in the euphotic zone. When the bloom progressed,the population was more evenly dispersed throughout the watercolumn. Coinciding with the decline of the spring bloom, afternitrogen depletion, a general reduction of cell size of P. catenataand a break-up of chains were observed. Resting cysts startedto appear shortly after the peak of the bloom, in sedimentationtraps moored at 30 and 40 m depth. Cysts were only retrievedfrom the uppermost sediment trap on three of the six samplingoccasions, constituting only a small proportion of all cystsproduced by P. catenata during spring. Our results suggest thatcyst production of this vertically migrating organism takesplace to a large extent in deep water layers and emphasizesthe necessity of whole water column monitoring in studies aimingto understand in situ life-cycle transformations of verticallymigrating dinoflagellates.     

Observation and simulation of the spring bloom in the northwestern Irish Sea

A two-layer, coupled physical-biological model was used to investigatephytoplankton dynamics in the north-western Irish Sea. The modelwas parameterized with values obtained from the published literature,and predicted the concentration of chlorophyll and dissolvedinorganic nitrogen in an upper and lower layer. Simulationswere driven with measured hourly values of meteorological data.The timings of the spring bloom predicted by the model at asummer thermally stratified site and a vertically mixed sitewere compared with observations made during 1992. At the mixedsite, good agreement was found between the model and observations.At the stratified site, the results are less satisfactory andshow that the model predicted a spring bloom 13 days later thanobserved. The difference was probably due to overestimationof the surface mixed-layer depth leading to underestimationof upper-layer irradiance. A simple numerical experiment demonstratedthat the timing of the spring bloom was best simulated usingthe maximum theoretically justifiable value for photosyntheticefficiency.     

Dynamics in bacterial surface properties of a natural bacterial community in the coastal North Sea during a spring phytoplankton bloom

The hydrophilic and hydrophobic properties of single cells of natural bacterioplankton communities were determined using a recently developed staining method combined with confocal laser scanning microscopy and advanced image analysis. On an average, about 50% of the bacterial cell area was covered by hydrophobic and only 16% by hydrophilic properties, while about 72% was covered by the genome. However, the size of these properties was independent of the bacterial cell size. Bacterial hydrophobicity was positively correlated with ambient NH(4)(+) concentrations and negatively correlated with overall bacterial abundance. The expression of hydrophilicity was more dynamic. Over the spring phytoplankton bloom, the bacterioplankton ratio(phil/phob) repeatedly reached highest values shortly before peaks in bacterioplankton abundance were observed, indicating a direct and fast response of bacterial surface properties, especially hydrophilicity, to changing environmental conditions. Compared to bacterial strains, recently studied with the same method, cells of marine bacterioplankton communities are much smaller and less frequently covered by hydrophobic or hydrophilic properties. While the percentage area covered by the genome is essentially the same, the percentage area covered by hydrophobic or hydrophilic properties is much smaller.     

Three-year study of benthic algal spring bloom development in a small, Danish lowland stream

Seasonal development of benthic algae was studied over a three-year period in a small, nutrient-rich lowland stream to investigate inter-annual variation in the algal spring bloom and differences in algal biomass regulation on two different substrata: fine-grained sediments and stones. The algal spring bloom was initiated when irradiance at the sediment surface exceeded 7 mol photons m^-2 d^-1 and mean water velocity was concomitantly below the threshold for bed load transport in the stream. Large inter-annual and substratum-dependent differences in peak algal biomass were observed, thus suggesting that different parameters regulate algal biomass development on the two substrata. On fine-grained sediments algal biomass development was predominantly coupled to light availability, while on stony substrata algal composition and peak biomass might be affected by invertebrate grazing.     

A daily study of the diatom spring bloom at Roscoff (France) in 1985. III. Free amino acids composition studied by HPLC analysis

The growth of a natural phytoplankton population was studiedduring a monospecific spring bloom of the diatom Rhizosoleniadelicatula at Roscoff (western English Channel). Direct examinationof the intracellular pool of 19 free amino acids (FAA) was usedas an index of the physiological status of the cells. TotalFAA in the particulate matter shows a general decrease duringthe bloom, and FAA cell content varies from 200 mM 1 cell volume^–1to 10 mM at the time of maximum biomass. FAA-N/particulate Nis <3% during the study, slightly decreasing at the timeof maximum biomass. Individual free amino acids appear reliablefor the development of the diatom biomass and good indicatorsof the growing population. At maximum biomass, major compoundsare glutamic acid (30.8 mol%), glutamine (11.7%), alanine (9.9%),isoleucine (6.6%) and lysine (6.4%). Serine, glycine, arginineand aspartic acid appear also as major components during otherperiods of the study. We suggest that the observed changes arean indication of the physiological state of the cells duringthe bloom. In particular glutamine (GLN), glutamic acid (GLU)and the GLN/GLU ratio allow the metabolic evolution of the naturalpopulation to be characterized. GLN is strictly linked to theliving biomass (Chla) while GLU is present at high percentagethroughout the study. The ecological significance of ß-alanine(BALA) is also revealed during this study, being strongly correlatedto degraded matter represented by phaeopigments. These resultsdemonstrate the validity of using individual free amino acidsas an aid in understanding the physiological status of algaein natural bloom conditions.     

The influence of integral solar radiation on the spring bloom of phytoplankton in the Ucha Reservoir

The results of the study of the quantitative relationships between solar radiation (integral radiation and PAR), the content of nutrients, and the spring bloom parameters in the Ucha Reservoir are presented. Positive significant correlations between the date of peak bloom and the sum of light intensity over the period from the 35the to the 40th days (the upper reaches of the reservoir, station Pestovo) and the period from the 44th to the 49th days (the lower reaches of the reservoir, station Listvyanka) were determined on the basis of a retrospective analysis of the data from the period of 1993–2003. Regression equations were derived, which permit forecasting the start of phytoplankton growth in spring according to the results of solar radiation measurements. The sum of light intensity over the course of 50 calendar days in each years correlate positively with the phytoplankton abundance in spring (the highest daily number of algae and integral estimation of algae number in spring).     

Changes in the elemental composition of Asterionella formosa during the diatom spring bloom

Changes in the elemental composition of the diatom Asterionellaformosa within mixed phytoplankton samples were determined overthe spring bloom period using energy dispersive X-ray microanalysis.Using a 10 kV electron microprobe, X-ray information from thetop 1–2 µm of the cell revealed overall mean concentrationsof: Si (4636 mmol kg^–1 dry wt), P (82), S (54), Cl (71)K (94) and Ca (90). Concentrations of all elements showed widevariation within each date sample, with unimodal frequency distributionsapproximating to a Normal distribution. Correlation of the entiredata set demonstrated clear statistical associations betweenelements, including Si, P and K. Uptake of Si during the courseof the diatom bloom led to a major fall in lake water concentration(1.0 to 0.07 mg l^–1), which correlated with a decreasein the mean cell Si concentration (6735 to 3107 mmol kg^–1dry wt) during the final phase of the bloom. Mean cell concentrationsof P and K also showed marked decreases with time, in closeparallel with cell Si. These changes in P and K were attributedto the high level of internal correlation with Si and not toany significant decrease in P and K availability in the environment.     

A toxic dinoflagellate bloom of Alexandrium tamarense (Lebour) Balech in Tokyo Bay

We report here, for the first time, the occurrence of the toxigenicdinoflagellate species. Alexandrium tamarense, in Tokyo Bay.It suggests the possibility of human intoxication (paralyzingshellfish poisoning) upon consuming local shellfish.     

Decadal-scale changes of dinoflagellates and diatoms in the anomalous baltic sea spring bloom

The algal spring bloom in the Baltic Sea represents an anomaly from the winter-spring bloom patterns worldwide in terms of frequent and recurring dominance of dinoflagellates over diatoms. Analysis of approximately 3500 spring bloom samples from the Baltic Sea monitoring programs revealed (i) that within the major basins the proportion of dinoflagellates varied from 0.1 (Kattegat) to >0.8 (central Baltic Proper), and (ii) substantial shifts (e.g. from 0.2 to 0.6 in the Gulf of Finland) in the dinoflagellate proportion over four decades. During a recent decade (1995-2004) the proportion of dinoflagellates increased relative to diatoms mostly in the northernmost basins (Gulf of Bothnia, from 0.1 to 0.4) and in the Gulf of Finland, (0.4 to 0.6) which are typically ice-covered areas. We hypothesize that in coastal areas a specific sequence of seasonal events, involving wintertime mixing and resuspension of benthic cysts, followed by proliferation in stratified thin layers under melting ice, favors successful seeding and accumulation of dense dinoflagellate populations over diatoms. This head-start of dinoflagellates by the onset of the spring bloom is decisive for successful competition with the faster growing diatoms. Massive cyst formation and spreading of cyst beds fuel the expanding and ever larger dinoflagellate blooms in the relatively shallow coastal waters. Shifts in the dominant spring bloom algal groups can have significant effects on major elemental fluxes and functioning of the Baltic Sea ecosystem, but also in the vast shelves and estuaries at high latitudes, where ice-associated cold-water dinoflagellates successfully compete with diatoms.     

Microbial dynamics during the decline of a spring diatom bloom in the Northeast Atlantic

The microbial dynamics during a spring diatom bloom declinewas monitored in the Northeast Atlantic during a 5-day Lagrangianstudy (8–12 April 2002). Phytoplankton abundance, compositionand health status were related to viral and bacterial abundance,zooplankton abundance and grazing rates, as well as bacterialproduction. Phytoplankton reached maximum concentration on Day3 (Chl a >5 µg L^–1) and declined on Day 5 (Chla 2 µg L^–1) and was dominated (70% of Chl a) bydiatoms. Bacterial production increased substantially to >20µg C L^–1 day^–1 on Day 3 and concomitantlylarge viruses decreased in number by half to <10 x 10³ mL^–1.This was followed by a 5-fold increase in large viruses on Day5, indicating infection and subsequent lysis on Days 3 and 5,respectively. Micro- and mesozooplankton grazing were not theprincipal cause for the decline of the bloom and pheophorbide-ashowing little variation in concentration from Days 1–4(100 ng L^–1) although doubled on Day 5. The poor physiologicalstatus of the diatoms, indicated by the high chlorophyllide-aconcentrations (50–480 ng L^–1), likely promoteda series of closely interrelated events involving bacteria andviruses leading to the demise of the diatom bloom.     

Vertical distribution and seasonal variation of eelgrass beds in Iwachi Bay,Izu Peninsula,Japan

The vertical distribution and population structure of eelgrass beds were surveyed in Iwachi Bay, along the Pacific coast of central Japan. Samplings were conducted from May through November 1977 by SCUBA. Eelgrass was distributed between 3 and 11 m in depth. The relative light intensity at 12 m depth was 11% at the lower range. The highest population density was 290 shoots/m² in September and the fresh weight of biomass was 888 g/m² in July at 7 m depth. The maximum mean leaf area index was about 3 at 10 m depth in July. The ratio of reproductive shoots to the total shoots was about 36% at 7 m depth in June. Eelgrass showed good growth at 7–10 m depth, which is comparatively deeper than other eelgrass habitations. The high values of water transparency and sunshine duration, as well as solar radiation compared with other localities was believed to contribute to the growth of eelgrass in deeper waters in Iwachi Bay.     

Influence of seasonal environmental variables on the distribution of presumptive fecal Coliforms around an Antarctic research station

Factors affecting fecal microorganism survival and distribution in the Antarctic marine environment include solar radiation, water salinity, temperature, sea ice conditions, and fecal input by humans and local wildlife populations. This study assessed the influence of these factors on the distribution of presumptive fecal coliforms around Rothera Point, Adelaide Island, Antarctic Peninsula during the austral summer and winter of February 1999 to September 1999. Each factor had a different degree of influence depending on the time of year. In summer (February), although the station population was high, presumptive fecal coliform concentrations were low, probably due to the biologically damaging effects of solar radiation. However, summer algal blooms reduced penetration of solar radiation into the water column. By early winter (April), fecal coliform concentrations were high, due to increased fecal input by migrant wildlife, while solar radiation doses were low. By late winter (September), fecal coliform concentrations were high near the station sewage outfall, as sea ice formation limited solar radiation penetration into the sea and prevented wind-driven water circulation near the outfall. During this study, environmental factors masked the effect of station population numbers on sewage plume size. If sewage production increases throughout the Antarctic, environmental factors may become less significant and effective sewage waste management will become increasingly important. These findings highlight the need for year-round monitoring of fecal coliform distribution in Antarctic waters near research stations to produce realistic evaluations of sewage pollution persistence and dispersal.