Nutrient and phytoplankton dynamics in the Queen Charlotte Islands (Canada) during the summer upwelling seasons of 2001-2002

The Queen Charlotte Islands, Canada, lie at the northern extremeof the coastal upwelling system of the eastern North PacificOcean (51–54°N). In this study, the first observationsof spatial and inter-annual patterns in nutrient inventories,chlorophyll (Chl) a and phytoplankton assemblages are reportedand related to oceanographic conditions in near-shore watersof the island archipelago. Stronger and more persistent upwellingin 2002 coincided with higher nutrient and Chl a standing stockscompared to 2001 and a higher proportion of diatoms. Dinoflagellateswere more prevalent in 2001, including several potentially harmfulspecies. At sub-seasonal scales, Chl a concentrations were greatestduring downwelling conditions and smallest during upwellingconditions. On the west coast, weak water column stratification,high relative proportions of diatoms and large nutrient inventoriesaccompanied upwelling-favourable conditions, whereas on theeast coast, there was no direct relationship between the BakunUpwelling Index and water column stability. According to redundancyanalysis, variability in species composition was best explainedby sea surface temperature, the depth of the euphotic zone andnutrient inventories. The east coast supported blooms of coccolithophoreswithin protected bays, confirming previous satellite observationsthat showed bright patches in these areas. The data illustratethat moderate upwelling can have an important influence on near-shorealgal standing stocks and species composition at the northernextreme of the upwelling system off the west coast of NorthAmerica, and that topographical complexity may be importantfor the development of phytoplankton blooms.     

Growth of harmful marine algae in multispecies cultures

Mixtures of harmful and harmless algae were grown in discontinuouslydiluted batch cultures under ammonium, nitrate and phosphatelimitation, and at different irradiances (20–500 µjnolquanta m^–2 s^–1). The species used were Chrysochromulinapolylepis, Emiliania huxleyi type B, Rhodomonas sp., the dinoflagellalesFibrocapsa japonica, Gymnodinium simplex, Gyrodinium aure-olum,Heterocapsa triquetra, Heterosigma carterae, Prorocentrum micansand Alexandrium tamarense, the diatoms Chaetoceros socialis,Cymatosira belgica, Ditylum brightwellii, Laudcria borealis,Odon-telta aunla, Pseudonitzschia pungens, Streptotheca tamesis,and the cyanobacterium Synechococcus. Their growth responsein the mixed algal cultures is discussed in relation to theirabundance in different natural habitats. In comparison withthe other non-diatoms, the mixotrophic C.polylepis grew fastunder all tested nutrient and light limitations.Emiliania huxleyigrew well under nitrogen (N) limitation (with nitrate as N source)and at irradiance levels from 15 up to 500 µmol quantam^–2 s^–1. No growth of calcifying cells could bedetected under N limitation when ammonium was used as N source.Rhodomonas grew reasonably well under ammonium-N limitationand grew fast at the highest irradi-ance. The dinoflagellateswere poor competitors compared to the Prymnesiophyceae. Theenvironmental fitness of the Prymnesiophyceae appears to beclosely related to the reproductive capacity of the vegetativestage, whereas the natural distribution of dinoflagellates seemsmore closely dependent on the generative reproduction-relatedspecific life cycle characteristics of the individual species.The marine diatoms include a mixture of both types of species.Some marine diatom species clearly have the capability to outcompetenon-diatoms under different types of nutrient and light limitationswhen silicate is in excess. Other diatoms seem to be poor competitors.     

The distribution of the dinoflagellate Ceratium in relation to environmental factors along 28N in the eastern North Pacific

The distribution of the species of the dinoulagellate Ceratiumare related to the oceanographic conditions observed in January1983 across the eastern North Pacific central gyre, the CaliforniaCurrent and the transition zone between them. A change in dominanceoccurs in the central gyre not accompanied by Concomitant changesin the observed physical or chemical features.Ceratium ‘recognized’the edge of the California Current although it seems unaffectedin its abundance and species structure by a major warm temperatureanomaly.     

Changes in the growth rate of phytoplankton in local upwelling around the Izu Peninsula, Japan

The composition and temporal changes in phytoplankton populationswere evaluated in local upwelling off the Izu Peninsula. Japan.in May. 1982. Phytoplankton in the upwelled water was dominatedby diatoms and that in the surrounding water by various flagellatesand monads. Phytoplankton started logarithmic growth almostimmediately after subsurface nutrient-rich water was upwellinginto the euphotic zone and nutrients were depleted within afew days. Growth enhancement was most striking among diatoms.As a result >50% of the total phytoplankton biomass of cells>2 µm was from a centric diatom. Leptocylindrus danicus.The results confirmed many past observations of the dominanceof diatoms in upwelled water. Such dominance is explained bythe rapid growth of diatoms when nutrient concentrations areenhanced.     

'St Martin's Summer': the case of an autumn phytoplankton bloom in the Gulf of Naples (Mediterranean Sea)

Phytopiankton abundance. species composition and primary productionof the Gulf of Naples were investigated during an autumn bloomin November 1985. Hydrographic data and surface phytoplanktonsamples were collected during a 3 day cruise, whereas investigationson in situ primary production and phytoplankton vertical distributionwere conducted from a second boat on three different dates.A coast-offshore gradient was recorded for most of the chemicaland biological parameters analysed. At stations closer to thecoast, which were affected by land run-off, phytoplankton populationsattained concentrations of 2.5 10⁶ cells l^–1 with amarked dominance of diatoms belonging to the genera Thalassiosiraand Chaetoceros. The most striking character of the system wasa remarkably high carbon assimilation rate (up to 1.04 g C m^–2day^–2) at stations closer to the coast. The causativemechanism for this bloom appeared to be land-derived nutrientenrichment, possibly enhanced by autumn rains, followed by aperiod of favourable meteorological conditions, which occursrecurrently in the region for a brief period around November,known locally as ‘St Martin's Summer’. We hypothesizethat a similar mechanism can stimulate phytoplankton growthmore than once every year. since high-stability penods followingmeteoro logical perturbations can occur several times in temperateregions of the northern hemisphere in autumn.     

Bicapitate Nitzschia species: abundant nanoplankton in aggregates during November-December (l992) in the equatorial Pacific

From 12°S to 9°N-140°W on the benthic cruise ofthe US Joint Global Ocean Flux Studies (JGOFS), horizontal near-surfacenet tows (n = 18) and vertical net hauls (n = 15, 200-0 m) yieldedhigh relative abundances of small, bicapitate, intact Nitzschiavalves (average 59.0 and 56.0% of total diatoms, respectively),although >90% of them were too small to have been caughteffectively with the net used. This complex was much less common(average 3.2% of diatoms) in the surface sediment samples (n= 7, 12°S-9°N, below water depths of 4269-4991 m). Examinationunder the light microscope showed concentrations of cells associatedwith organic detritus, planar and cylindrical membranous structures,fecal pellets, and occasionally on other diatoms (e.g. Asterolampra),i.e. on or within particles large enough to be collected inthe net. Although Nitzschio bicapitato Cleve has been consideredto have a characteristic range of shapes, and has often beencited from open-ocean habitats in nano- and microplanktonicstudies, a scanning electron microscopic study revealed severalspecies in our material. Examples of larger and smaller speciesare given, and Nitzschia ikeanae G.Fryx. & H.Lee, sp. nov.,is described here. Ecologically, these observations indicatethat although some are grazed and have been seen aggregatedin fecal pellets, these small pennate diatoms can affix to andgrow on substrates, termed ‘pseudo-benthic habitats’in the open ocean, resulting in unexpected concentrations thathave implications for their life histories and sexual cycles,selection or avoidance by grazers, sinking on substrates, androles in the recycling of nutrients in near-surface waters.     

A comparative study of the size-dependent organic composition of marine diatoms and dinoflagellates

Cellular chlorophyll a, protein, carbohydrate and lipid contentwas determined for eleven clones of centric marine diatoms (volume89–1.47 x 10⁷ µ³) and eight species of marine dinoflagellates(597–4.45 x 10⁴ µ³) cultured under continuous illuminationat 18°C and 20°C, respectively. In both groups the logof cellular concentrations of each constituent was directlyrelated to the log of cell volume; diatoms generally had lowercellular concentrations than dinoflagellates of an equivalentvolume. Diatom chlorophyll a, protein and lipid concentrationsnormalized to a unit cell volume (pg µ^–3) decreasedexponentially with increasing cell size; this decrease is aconsequence of the diatoms' unique morphology restricting cellcytoplasm to a thin parietal layer within the frustule. Althoughdinoflagellates yield a wide range of cytoplasm concentrations,small dinoflagellates contained up to 3-fold higher cytoplasmconcentrations of all constituents than diatoms of equal volume.The log of cellular caloric values, summed from the caloricequivalents of cellular protein, carbohydrate and lipid, wasa linear function of log volume. Diatoms contained ca. halfthe caloric value of dinoflagellates of an equivalent volume.Although the evaluation of caloric content provides a basisfor comparing the "nutritional value" of phytoplankton groups,evidence from the literature suggests subjective factors suchas taste and digestibility are equally important in determiningnutritional values of individual species.     

Composition and distribution of the pelagic and sympagic algal assemblages in the Laptev Sea during autumnal freeze-up

The phytoplankton and ice algal assemblages in the SiberianLaptev Sea during the autumnal freeze-up period of 1995 aredescribed. The spatial distribution of algal taxa (diatoms,dinoflagellates, chrysophytes, chlorophytes) in the newly formedice and waters at the surface and at 5 m depth differed considerablybetween regions. This was also true for algal biomass measuredby in situ fluorescence, chlorophyll (Chl) a and taxon-specificcarbon content. Highest in situ fluorescence and Chl a concentrations(ranging from 0.1 to 3.2 µg l^–1) occurred in surfacewaters with maxima in Buor Khaya Bay east of Lena Delta. Thealgal standing stock on the shelf consisted mainly of diatoms,dinoflagellates, chrysophytes and chlorophytes with a totalabundance (excluding unidentified flagellates <10 µm)in surface waters of 351–33 660 cells l^–1. Highestalgal abundance occurred close to the Lena Delta. Phytoplanktonbiomass (phytoplankton carbon; PPC) ranged from 0.1 to 5.3 µgC l^–1 in surface waters and from 0.3 to 2.1 µg Cl^–1 at 5 m depth, and followed the distribution patternof abundances. However, the distribution of Chl a differed considerablyfrom the distribution pattern shown by PPC. The algal assemblagein the sea ice, which could not be quantified due to high sedimentload, was dominated by diatom species, accompanied by dinoflagellates.Thus, already during the early stage of autumnal freeze-up,incorporation processes, selective enrichment and subsequentgrowth lead to differences between surface water and sea icealgal assemblages.     

Under-storey Nutrient Content in an Age Sequence of Douglas-fir Stands

The nutrient concentrations and contents of the under-storeyspecies were estimated for a series of Pacific North-west Douglas-fir[Pseudotsuga menxiessii (Mirb.) Franco] stands ranging in agefrom 9 to 95 years. Analyses were carried out for ash, N, P,K, Ca, Mg, Mn, Fe, Zn and Na and significant differences innutrient concentrations were found to exist between species;species rejecting certain nutrients and accumulating others.General trends for mean concentrations of some nutrients areassociated with stand maturity in that ash, K and Mg decline,P and Mn increase and N and Ca reaches a peak at 20–30years and then declines. The nutrient contents (kg ha^–1)of the under-storey component of the stands are presented andtrends discussed. Mineral nutrient content, under-storey vegetation, Pseudotsuga menziessii stands, Douglas-fir     

Structure and Function of an Age Series of Poplar Plantations in Central Himalaya. II Nutrient Dynamics

This paper elucidates nutrient dynamics in 5- to 8-year-oldpoplar (Populus deltoides) clone D₁₂₁ plantations previouslyinvestigated for dry matter dynamics. The nutrient concentrationin different layers of the vegetation were in the order: tree> shrub > herb, whereas the standing state of nutrientswere in the order: tree > herb > shrub. Soil, litter andvegetation, respectively, accounted for 80-89, 2-3 and 9-16%of the total nutrients in the system. Considerable reductions(trees 42-54, shrubs 31-37 and herbs 15-23%) in concentrationof nutrients in leaves occurred during senescence. The uptakeof nutrients by the vegetation and also by the different components,with and without adjustment for internal recycling, has beencalculated separately. Annual transfer of litter nutrient tothe soil by vegetation was 113·7-137·6 N, 11·6-14·6P and 80·1-83·2 K kg ha^-1 year^-1. Turnover rateand time for different nutrients ranged between 0·72-0·89year^-1 and 1·12-1·39 years, respectively. Thehigh turnover rate of litter on the forest floor indicates thegreater productivity of the stands, which was due to the higherdry matter dynamics and nutrient release for the growing vegetation.The nutrient use efficiency in poplar plantations ranged from159-175 for N, 1405-1569 for P and 295-332 for K. Compared withEucalyptus, there was a higher proportion of nutrient retranslocationin poplars largely because of higher tissue nutrient concentrations;this indicates lower nutrient use efficiency as compared tothe eucalypt plantation. Compartment models for nutrient dynamicshave been developed to represent the distribution of nutrientpools and net annual fluxes within the system.Copyright 1995,1999 Academic Press Populus deltoides plantations (Clone D₁₂₁), nutrient retranslocation, net nutrient uptake, nutrient use efficiency, nutrient cycling, nutrient pool, nutrient fluxes     

An immunofluorescent survey of the brown tide chrysophyte Aureococcus anophagefferens along the northeast coast of the United States

Surveys were conducted along the northeast coast of the USA.between Portsmouth, NH, and the Chesapeake Bay in 1988 and 1990,to determine the population distribution of Aureococcus anophagefferens,the chrysophyte responsible for massive and destructive ‘browntides’ in Long Island and Narragansett Bay beginning in1985. A species-specific immunofluorescent technique was usedto screen water samples, with positive identification possibleat cell concentrations as low as 10–20 cells ml^–1.Both years.A.anophagefferens was detected at numerous stationsin and around Long Island and Barnegat Bay, NJ, typically athigh cell concentrations. To the north and south of thus ‘center’,nearly half of the remaining stations were positive for A.anophagefferens,but the cells were always at very low cell concentrations. Manyof the positive identifications in areas distant from Long Islandwere in waters with no known history of harmful brown tides.The species was present in both open coastal and estuanne locations,in salinities between 18 and 32 practical salinity units (PSU).The observed population distributions apparently still reflectthe massive 1985 outbreak when this species first bloomed, giventhe number of positive locations and high abundance of A.anophagefferensin the immediate vicinity of Long Island. However, the frequentoccurrence of this species in waters far from this population‘center’ is disturbing. Aureococcus anophagefferensis more widely distributed than was previously thought. Numerousareas thus have the potential for destructive brown tides suchas those associated with the sudden appearance of the speciesin 1985.     

On the trophic fate of Phaeocystis pouchetii (Harlot). III. Functional responses in grazing demonstrated on juvenile stages of Calanus finmarchicus (Copepoda) fed diatoms and Phaeocystis

The objective of this study was to quantify the functional responsein feeding rate in the various developmental stages of Calanusfinmarchicus to different concentrations of the diatoms Thalassiosiranordenskioeldii and Porosira glacialis, and the haptophyseanPhaeocystis pouchetii. Grazing of copepodite stage I–VC.finmarchicus was measured using two different approaches.Feeding rates were obtained from either incubation experiments,estimating the rate of removal of particles from suspension,or by quantifying the turnover rate of the plant pigments inthe gut. Clearance as a function of algal concentration (1–30µg plant pigment 1^–1) was described in juvenilestages of C.finmarchicus fed the diatoms T.nordenskioeldii [20µm equivalent spherical diameter (ESD)], P.glacialis (40µm ESD), and two size categories (30–100 µmand >100 µm ESD) of the gelatinous alga P.pouchetii.When the copepodite stages were fed T.nordenskioeldii, the gutcontent of plant pigments was in general higher than when fedP.glacialis. Rates obtained were variable when the same copepoditestages were offered the two size categories of P.pouchetii,but within the same order of magnitude as those obtained forthe larger diatom. At unialgal diets, diatoms were more readilyconsumed than the larger size fraction among colonies of P.pouchetiiby copepodite stage I–III C.finmarchicus. But given anappropriate prey size, C.finmarchicus grazed both diatoms andcolonies of gelatinous algae at equal rates. A linear relationshipbetween gut content and food concentrations <10 µgchlorophyll 1^–1 was found. This indicates that the ingestionrate in C.finmarchicus is directly proportional to the ambientfood concentration during the most productive period in Mayand June in high latitudes irrespective of algal species present. ¹Present address: Marine Biological Laboratory, University ofCopenhagen, Strandpromenaden 5, DK-3000 Helsingør, Denmark ²Present address: Greater Copenhagen Council, Gl. KøgeLandevej 1–3, DK-2550 Valby, Denmark     

Growth and decline of a diatom spring bloom phytoplankton species composition, formation of marine snow and the role of heterotrophic dinoflagellates

During the spring of 1994, we determined the factors responsiblefor the decline of the seasonal diatom bloom in the Gullmarfjord, on the west coast of Sweden. Four species constituted>75% of the biomass—Detonula confervacea, Chaetocerosdiadema, Skeletonema costatum and Thalassiosira nordenskioeldii—reachingconcentrations of 4900, 350, 8200 and 270 cells ml^–1,respectively. Growth of phytoplankton was exponential (growthrate = 0.12 day^–1) from 3 to 21 March, after which a galewith winds >15 m s^–1 caused massive aggregation. Amaximum of 130 p.p.m. (v/v) of marine snow aggregates was observedby in situ video at the peak of the bloom. Critical concentrations(Jackson, Deep-Sea Res., 37, 1197–1211, 1990) were similarto observed showing that coagulation theory could explain thesudden decline of the bloom. The heterotrophic dinoflagellateGyrodinium cf. spirale increased exponentially after the peakof the bloom with maximum (temperature-adjusted) growth rates.After the rapid aggregation and sedimentation of the bloom,they were able to control any further growth of diatoms. Nitrateand silicate were never depleted, but phosphate may have beenlimiting by the end of the study period. We conclude that massaggregation during a gale marked the end of the bloom, and thatintense grazing by heterotrophic dinoflagellates prevented anysubsequent increase of diatoms.     

Inverse Correlation of Thiol Proteinase with Nitrate Reductase Activities in Barley Leaves

Experiments conducted to determine the effects of leupeptin,a specific inhibitor of thiol proteinase, on extractable nitratereductase (NR) activity in leaves of Hordeum distichum duringdarkness revealed that leupeptin (0.01 mg.ml^–1) appliedto detached leaves significantly reduced the loss of NR activity.At the same time it also reduced the formation of small cytochromec reductase species, which is a degradation product of NR complex,Upon nitrate induction, extractable NR activity increased butthe content of thiol proteinase decreased. This inverse correlationwas also observed upon transfer of nitrate-grown barley seedlingsto nitrate-free nutrient solution. Furthermore, cycloheximide(0.1 mg.ml^–1) treatment of barley seedlings reduced thecontent of thiol proteinase and retarded the loss of NR activityunder noninducing conditions. These results suggest that invivo changes in NR content in leaves of Hordeum distichum arethe result of proteolysis by an endogenous thiol proteinase. (Received May 16, 1985; Accepted July 22, 1985)     

Phytoplankton distribution in a floodplain lake and river system. II Seasonal changes in the phytoplankton communities and their control by hydrology and nutrient availability

Phytoplankton community development and water chemistry werestudied for 2 years in the lowland R.Bure and most of the Broads(shallow lakes) associated with it. The data were analysed interms of ‘time for development’, which is the minimumestimated time that an average parcel of water takes to reacha site plus that it spends in it before it moves on downstream.This allows to some extent for the delaying effects that theBroads have on downriver water movement. Regressions of meanchlorophyll a on time for development were linear and suggestedthat the upstream Broads, where phytoplankton first developsin quantity in the system, have retained the water for longerthan anticipated from hydrological measurements. They effectivelyadded several weeks to the time for development. Available phosphateand nitrate concentrations decreased with time for development.Those for silicate increased. Seasonal changes in the upperpart of the study area were largely in centric diatom species.Pennate diatoms and cyanophytes became predominant in the lowerstretches. All major species were present at the extreme upperend of the stretch. With increasing development time, in a watermass dominated by water entering at the head of the study area,a succession of Cyclotella meneghiniana, Stephanodiscus hantzschiiand Melosira species was followed by Oscillatoria species thenDiatoma elongatum, Synedra ulna and Anabaena planctonica. Possiblereasons for these changes are discussed. Over 80 other taxawere present though none were so abundant as the above species.The succession is interpreted in terms of nutrient physiologyand algal growth rates to generate hypotheses for experimentaltesting.     

Uptake and regeneration of inorganic nitrogen in coastal waters influenced by the Mississippi River spatial and seasonal variations

The Mississippi and Atchafalaya Rivers introduce large amountsof nutrients to surface waters of the northern Gulf of Mexico.This paper reports the most complete data to date on inorganicnitrogen uptake and regeneration in a broad range of coastalenvironments influenced by the river water, along with informationon nutrient concentrations and including pico-, nano-, and microplanktonspecies composition. Nitrate in surface waters is greatly reducednear the river plume, at salinities between 5 and 25 PSU, wherethe largest variance in uptake rates was observed, and was coincidentwith peaks in surface chlorophyll. Despite the depletion ofnitrate, nitrogen limitation was a rare event during the study,because of relatively high ammonium concentrations (>1 µmolNH₄⁺ I^–1 and regeneration rates. Two contrasting situationscharacterize the seasonal nitrogen dynamics in surface shelfwaters. High nitrate input during the spring caused a largebloom in which the cells were well adapted to use nitrate.Thedominant phytoplankton species were chain forming diatoms, alsoreported in sediment-trap studies in the area. Ammonium regenerationonly accounted for a small fraction of the nitrogen requirementsduring the bloom. In contrast, the low flow of river water duringsummer resulted in low nitrate concentrations in surface water.In this case phytoplankton productivity was highly reduced andmay depend greatly on ‘in sita’ ammonium regeneration.     

Fluxes of diatoms in the Dona Paula Bay, west coast of India

Sediment traps were deployed at a station in the Dona PaulaBay to collect sedimenting particles at weekly intervals fromNovember to May during 1995–1997. Sedimented particleswere analysed for total diatom flux, chlorophyll a (Chl a) andparticulate organic carbon (POC). The highest diatom flux wasrecorded in April–May for both the years. Fluxes of diatomsvaried from0.6 x 10⁴ cells m^–2 day^–1 (November 1995)to 121.47 x 10⁴ cells m^–2 day^–1 (December 1996).In all, 19 diatom genera were identified in the sedimented material.Navicula, Nitzschia, Pleurosigma, Licmophora, Coscinodiscus,Rhizosolenia and Surirella were the most abundant genera inthe sedimented material throughout the sampling period. Meanflux of POC and diatom carbon was 251 and 0.39 mg C m^–2day^–1, respectively. The diatom carbon accounted for 0.15%of the POC flux. Mass flux of diatoms showed significant negativecorrelation with the concentration of nitrate and phosphate.This suggests that the nutrient concentration played an importantrole in influencing the sedimentation of diatoms at this coastalstation.     

A 91-year record of seasonal and interannual variability of diatoms from laminated sediments in Saanich Inlet, British Columbia

Diatom seasonal succession and interannual variability werestudied using laminated sediments from Saanich Inlet, BritishColumbia, for the years 1900–1991. Frozen sediment coresallowed fine-scale sampling of laminae for each year. Thus,three ‘seasons’ for each year were identified basedon species composition. Thalassiosira species were indicatorsof spring deposition. Skeletonema costatum was abundant in samplesfollowing Thalassiosira, probably deposited in late spring andsummer. Rhizosolenia sp. was most abundant in fall/winter samples.Diatom stratigraphies were related to sea surface temperature,salinity, sea level and the Pacific North American Index (PNA)using canonical correspondence analysis (CCA). CCA showed thatspecies of a particular season generally had optima for temperatureand salinity characteristic of that time. Interannual changesin diatom species composition and abundance were most prevalentin the decades 1920–1940, with the exception of S.costatumwhich showed cyclic changes in abundance. Skeletonema was moreabundant during periods of cool temperatures, while littoraldiatoms were more abundant during times of heavy winter rains.Sea level was an important variable in CCA and while its relationshipto diatoms is not clear, it may be related to variations innutrient supply to diatoms in surface waters.     

Phytoplankton species and abundance in response to eutrophication in coastal marine mesocosms

In a mesocosm nutrient enrichment experiment the species (orcategories) and abundances of diatoms, dinoflagellates, flagellates,monads and ciliates were identified and counted over a 16-monthperiod. Diatoms and ciliates increased with increasing nutrienttreatment while monads and flagellates, <10 µm in size,did not. By contrast, in the field diatoms sometimes appearedto decrease while small phytoplankton µ10 µm appearedto increase under eutrophic conditions. In the experiment, insome instances, grazing controlled abundances to low levelsin nutrient-enriched treatments. Self-shading by phytoplanktonlimited upper levels of abundance when nutrients were excessive.While nuisance species were occasionally present in variousnutrient treatments, the intensity and frequency of their presencedid not tend to increase with nutrient treatment. Generallyspecies (or categories) did not appear to change with nutrienttreatment.     

Pico-, nano- and microplankton communities in hydrothermal marine coastal environments of the Eolian Islands (Panarea and Vulcano) in the Mediterranean Sea

This paper reports the relationship among pico-, nano- and microplanktoniccommunities observed in two different shallow marine hydrothermalenvironments. Seawater samples from five stations in the coastalarea of the ‘Porto di Levante’ (Vulcano Island)and from three stations off the Island of Panarea (Eolian Islands,Italy) were collected in May and July of 1989, respectively.Microbiological investigations were carried out in order todetermine the density of: (i) the total picoplankton (both autotrophicand heterotrophic): (ii) the total picophytoplankton (autofluorescentpicoplanktonic cells); (iii) the larger phytoplankton (>2µm): (iv) the ‘metabolically active’ cellsof total picoplankton and cyanobacteria; (v) the heterotrophicaerobic bacteria. The peak values of picoplankton and picophytoplanktoncomponents, with an order of magnitude of 10⁹ and 10⁷ cells1¹, respectively, were registered in the wannest water samples(30–75°C) collected from the Vulcano area. At Panarea.eukaryotic picophytoplankton and ‘metabolically active’coccoid cyanobacteria showed an opposite trend. A possible competitionbetween the two groups is to be considered. Cyanobacteria, diatomsand the genus Licmophora. in particular, were prevalent in thewarmest hydrothermal vents of Vulcano. Nano- and microphytoplanktoniccommunities in the offshore waters of the Island of Panareashowed more variability than in Vulcano. Moreover, in the Panareawaters the prevalence of phytoflagellates above the thermoclinewas observed, whereas diatoms were predominant below this layer.