Structural variations of phytoplankton in the coastal seas of Yucatan,Mexico

A study was done of the relationship between hydrographic variables and the composition, abundance, community structure and biomass spectrums of coastal phytoplankton at scales greater than 100 km on the Yucatan Peninsula (SE Gulf of Mexico). This was done during the season of greatest environmental instability in the region, the northwind season (late fall to winter). Samples were collected at stations in the west (Campeche), north (Yucatan), and east (Quintana Roo) zones of the Peninsula. Measurements were taken of temperature, salinity, dissolved oxygen, dissolved inorganic nutrients (ammonia, nitrite, nitrate and phosphate) and chlorophyll a, and samples were taken for phytoplankton analysis. The hydrographic results showed the Campeche zone as having the lowest salinity (<35 psu) values, as well as the highest inorganic nutrient and chlorophyll a values, all of which are related to continental water contributions. The Yucatan zone had the lowest temperatures and the lowest inorganic nutrient values, indicating influence from the Yucatan Current and the Gulf of Mexico. A total of 159 phytoplankton species were identified, dominated by diatoms (>80%) and dinoflagellates. Phytoplankton exhibited greater concentration, richness, equitability and diversity in Campeche, while the lowest community structure values were had in the Quintana Roo zone. The ordination analysis demonstrated that the dominant genera were the diatoms Chaetoceros, Pseudonitzschia and Thalassionema. The biomass spectrums exhibited the lowest slope in environments of higher heterogeneity, with Campeche being the most disturbed and heterogeneous zone and Quintana Roo that with the least heterogeneity.     

'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.     

Zooplankton assemblages and influence of environmental parameters on them in a Mediterranean coastal area

Temporal dynamics of zooplankton communities and assemblages,as well as the influence of environmental factors on them, werestudied in Saronikos Gulf (Aegean Sea, Greece). Different multivariatetechniques (hierarchical clustering, multidimensional scalingand correspondence analysis) were applied on a 2 year data setof zooplankton species composition, based on samples collectedat five stations of the study area. A clear discrimination oftwo communities was revealed, the first one in the semi-enclosedpolluted northern part (Elefsis Bay) andthe second in SaronikosGulf proper. Within the latter community, five assemblages weredistinguished: (i) the coastal winter assemblage characterizedby Ctenocalanus vanus, Oithona similis, Clausocalanus pergensand Fritillaria pellucida; (ii) the psychrophilic assemblageinfluenced by the open sea and characterized by Oithona plumiferaand Clausocalanus jobei; (iii) the spring assemblage characterizedby Evadne nordmanni and Centropages typicus; (iv) the coastalthermophilic assemblage characterized by Penilia avirostis,Evadne ergesrina and Temora stylifera; (v) the thermophilicassemblage influenced by the open sea and characterized by Clausocalanusfurcatus. Both zooplankton and environmental data were treatedby multiple correspondence analysis which revealed the importanceof some environmental factors on zooplankton community composition(eutrophication-pollution, temperature, water mass circulation,hydrology and topography).     

Phytoplankton distribution and composition off the coast of Galicia (northwest of Spain)

During October 1977, phytoplankton iamples were collected alongwith other hydrographic and biological data from a grid of stationslocated off Galicia (NW of Spain), between the coast and about100 km offshore. Chlorophyll a distribution and phytoplanktoncomposition were studied and related to hydrographic and geographicfeatures of the area. The higher phytoplankton biomasses werefound off the western coast and were conditioned by the presenceof the rias - flooded tectonic valleys of moderate depth functioningas positive estuaries - and the occurrence of coastal upwelling,which allows the injection of nutrient rich water along thebottom of the rias. The qualitative composition of the phytoplanktonreflected principally the influence of the rias but appearedalso to show variability related to the distribution of watermasses. The patterns of circulation of the surface and sub-surfacewaters were likely to reinforce the phytoplankton differencesbetween the northern and western coasts of Galicia.     

Summer phytoplankton distributions in the Weddell Sea

Summary The quantitative composition of phytoplankton was studied along a transect of 14 hydrographic stations, between the southern coast of the Weddell Sea and the Antarctic Peninsula, during the austral summer of 1984–1985. The most apparent feature of the phytoplankton distribution was the presence of a bloom of Phaeocystis at a frontal zone over the shelf break, and the marked contrast between a southern region, with high phytoplankton biomass, and a poorer region north of the shelf break. The most widely distributed diatom genus was Nitzschia (Fragilariopsis section). The phytoplankton assemblage of the southern region included the silicoflagellate Distephanus speculum, the diatom Rhizosolenia alata and several heterotrophic dinoflagellates such as Protoperidinium antarcticum and P. applanatum. The northern assemblage could be characterized by the abundance of flagellates and small dinoflagellates, and by diatoms such as Chaetoceros criophilum, Corethron criophilum Nitzschia kerguelensis and other Nitzschia species of the Fragilariopsis section.     

Species-specific phytoplankton sedimentation in relation to primary production along an inshore--offshore gradient in the Baltic Sea

The temporal and spatial variability in the quality and quantityof settling phytoplankton material in relation to concurrentprimary production was studied using sediment traps at threecoastal stations from a semi-enclosed bay (Pojo Bay) throughthe outer archipelago to the open Gulf of Finland. The fluxof settling phytoplankton was high (9.3 g C m^–2period^–1)in Pojo Bay, especially in spring, and lower in the archipelago(8.1 g C m^–2 period^–1) and open-sea area (5.2 gC m"2 period"1), although the primary production followed theopposite pattern. A large influx of allochthonous material intoPojo Bay in spring brought allochthonous phytoplankton cellsinto the traps, but limited primary production. Diatoms werethe most abundant settled phytoplankton at all stations, butthe species composition varied between Pojo Bay (Aulacoseiraspp., Rhizosolenia minima) and the outer stations (Skeletonemacostatum, Chaetoceros spp.)At the outer stations, migratingdinoflagellates (Peridiniella catenate) comprised part of thesettling material in spring. The high settling flux of the cyanophyteAphanizomenon flos-aquae is discussed. The species compositionof the phytoplankton assemblage influenced the proportion ofthe total organic carbon sedimentation that consisted of phytoplanktoncarbon.     

Composition and seasonality of nocturnal peracarid zooplankton from coastal New Hampshire (USA) waters, 1978-1980

Seasonal changes in the nocturnal peracarid zooplankton froma nearshore area of the Gulf of Maine were studied from January1978 through December 1980 as a requirement of an ecologicalmonitoring program for the Public Service Company of New Hampshire'sSeabrook Generating Stanon. Numerically dominant species includedthe mysids Michteimysis mixta and Neomysis americana. the amphipodsPontogeneia inermis, Themisto gaudichaudi and Monoculodes edwardsi.and the cumaceans Diastylis polita and Lamprops quadriplicata.A general seasonal cycle was documented with a more abundantand speciose assemblage during fall and winter than summer.Peak abundance occurred during spring months prior to emigrationof juvenile M.mixta from the study area. Abiotic and bioticfactors which may affect the structure and composition of thisassemblage are discussed.     

Seasonal variability of phytoplankton populations in the middle Adriatic sub-basin

The seasonal variability of phytoplankton assemblages in themiddle Adriatic sub-basin is described. The investigated areacrossed the middle Adriatic from the Italian to the Croatiancoasts. Hydrographic data, chlorophyll (Chl) a and phytoplanktonwere collected on a seasonal basis from May 1995 to February1996. Highest phytoplankton densities (up to 6 x 10⁶ cells dm^–3)were observed in spring and autumn in the western side, withinthe diluted waters. The vertical distribution of Chl a exhibiteda pronounced subsurface maximum associated, in coastal waters,with micro-planktonic diatoms. Phytoplankton assemblages weredominated by phytoflagellates in all the periods investigated.Diatom maxima were observed in spring and autumn: their verticaldistribution generally reflected the Chl a pattern and in thewestern coastal area peaks are due to large diatom species (Pseudo-nitzschiaspp.). In offshore waters, dinoflagellates strongly prevailover diatoms and provide a relevant contribution to the totalbiomass, especially in highly stratified conditions. Coccolithophoridswere mostly encountered in surface layers and their highestcontribution to the total biomass was observed in the LevantineIntermediate Water.     

The contribution of picophytoplankton to community structure in a Mediterranean brackish environment

The seasonal composition of phytoplankton communities was investigatedin a Mediterranean brackish area (Varano lagoon). Twelve stationswere sampled monthly from March 1997 to February 1998. Numbersof prokaryotic and eukaryotic picophytoplankton cells were estimatedby epifluorescence microscopy, while larger phytoplankton (nanoand micro fractions) were enumerated by the Utermöhl settlingtechnique. Picophytoplankton densities ranged from 0.7 to 448.6cells x 10⁶ l^–1. Nano- and microphytoplankton abundancesvaried between 0.2 and 7.9 cells x 10⁶ l^–1. The picoplanktonfraction was represented mainly by cyanobacteria and the Utermöhlfraction by nano-sized phytoflagellates (56.2%) and diatoms(20.1%). The phytoflagellates had a greater abundance over timewhile diatoms reached the highest densities in summer and fall.In Varano lagoon, phytoplankton development is related to ‘nitrogen-poor'waters and to phosphorus availability. Suspension-feeding bivalves(Mytilus galloprovincialis) are sufficiently abundant to filtera volume equivalent to the volume of Varano lagoon at leastonce daily. These observations suggest that grazing exerts animportant influence on phytoplankton dynamics, mainly on themicro fraction, and that diatoms seem to play an important rolein the food web dynamics of this coastal fishery.     

Symbiotic associations among the microplankton in oligotrophic marine environments, with special reference to the Gulf of Aqaba, Red Sea

Instances of symbiotic consortia in the microplankton of highlyoligotrophic seas are discussed on the basis of case studiesand long-term observations off the Israeli coast of the Gulfof Aqaba, Red Sea, and the inshore and offshore waters of theEastern Mediterranean. Associations described include diatomswith filamentous cyanophytes, diatoms with protozoans, tintinnidswith attached or encrusted diatoms, and acantharians with algalendosymbionts. Noted among the case studies is the frequentoccurrence of the endosymbiont cyanophyte Richelia inrracellularis,capable of molecular nitrogen fixation, in diatoms, includingthree species of Hemiaulus. For one of these associations, seeminglywith Hemiaulus sinensis, this is the first photographic record.The consortia are considered in relation to their seasonal distributionin depth profiles from the northern end of the Gulf of Aqaba,and in relation to their occurrence in the Eastern Mediterraneanand also worldwide in similar environments. These aspects andthe easily identifiable symbiotic nature of the consortia describedherewith make them useful as indicator species of warm wateroligotrophic seas.     

Physiological response of 10 phytoplankton species exposed to macondo oil and the dispersant,Corexit

Culture experiments were conducted on ten phytoplankton species to examine their biological and physiological responses during exposure to oil and a combination of oil and dispersant. The species tested included a range of taxa typically found in the Gulf of Mexico such as cyanobacteria, chlorophytes, and diatoms. Cultures were exposed to Macondo surrogate oil using the water accommodated fraction (WAF), and dispersed oil using a chemically enhanced WAF (CEWAF) and diluted CEWAF, to replicate conditions following the Deepwater Horizon spill in the Gulf of Mexico. A range of responses were observed, that could broadly class the algae as either “robust” or “sensitive” to oil and/or dispersant exposure. Robust algae were identified as Synechococcus elongatus, Dunaliella tertiolecta, two pennate diatoms Phaeodactylum tricornutum and Navicula sp., and Skeletonema grethae CCMP775, and were largely unaffected by any of the treatments (no changes to growth rate or time spent in lag phase relative to controls). The rest of the phytoplankton, all centric diatoms, exhibited at least some combination of reduced growth rates or increased lag time in response to oil and/or dispersant exposure. Photophysiology did not have a strong treatment effect, with significant inhibition of photosynthetic efficiency (F_v/F_m) only observed in the CEWAF, if at all. We found that the effects of oil and dispersants on phytoplankton physiology were species‐dependent, and not always detrimental. This has significant implications on how oil spills might impact phytoplankton community structure and bloom dynamics in the Gulf of Mexico, which in turn impacts higher trophic levels.     

Phytoplankton composition in the Weddell-Scotia Confluence area during austral spring in relation to hydrography

During the EPOS leg 2 cruise of the RV Polarstern, carried out in late austral spring of 1988–1989, the composition of phytoplankton in relation to the distribution of hydrographic parameters was studied in four successive transects carried out along 49°W and 47°W, across the Weddell-Scotia Confluence (WSC) and the marginal ice zone (which overlapped in part). In all transects, a maximum of phytoplankton biomass was found in the WSC, in surface waters stabilized by ice melting. Different phytoplankton assemblages could be distinguished. North of the Scotia Front (the northern limit of the WSC) diatoms with Chaetoceros neglectus, Nitzschia spp. and (Thalassiosira gravida) dominated the phytoplankton community. This assemblage appeared to have seeded a biomass maximum which occupied, during the first transect, an area of the WSC, south of the Scotia Front. The southernmost stations of the first transect and all the stations to the south of the Scotia Front in the other transects were populated by a flagellate assemblage (with a cryptomonad, Pyramimonas spp. and Phaeocystis sp.) and an assemblage of diatoms (Corethron criophilum and Tropidoneis vanheurkii among others) associated to the presence of ice. During the last three transects, the flagellate assemblage formed a bloom in the low salinity surface layers of the WSC zone. The bulk of the biomass maximum was formed by the cryptomonad which reached concentrations up to 4×10⁶ cells l^–1 towards the end of the cruise. Multivariate analysis is used to summarize phytoplankton composition variation. The relationships between the distribution of the different assemblages and the hydrographic conditions indicate that the change of dominance from diatoms to flagellates in the WSC zone was related to the presence of water masses from different origin.Data presented here were collected during the European Polarstern Study (EPOS) sponsored by the European Science Foundation     

Phytoplankton community structure and environment in the Kenyan waters of Lake Victoria

• 1 Phytoplankton species composition, numerical abundance, spatial distribution and total biomass measured as chlorophyll a concentration were studied in relation to environmental factors in September 1994 (dry season) and March 1995 (rainy season), respectively, in the Kenyan waters of Lake Victoria; 103 species were recorded.
• 2 Blue‐green algae (Cyanophyceae) were most diverse, followed by diatoms (Bacillariophyceae), green algae (Chlorophyceae) and dinoflagellates (Dinophyceae).
• 3 Twinspan separated the phytoplankton communities in the Nyanza Gulf and those in the open lake during both seasons. During the dry season, the Nyanza Gulf was strongly dominated by blue‐greens, while diatoms dominated in the open lake. During the rainy season, blue‐greens remained dominant in the Nyanza Gulf although the number of species found was lower than during the dry season; in the open lake, blue‐greens replaced diatoms as the dominant group and there were more species than in the dry season.
• 4 Canonical correspondence analysis indicated that the phytoplankton species distribution was significantly correlated with turbidity during the dry season and with SiO₂ during the rainy season. Chlorophyll a concentrations ranging from 2.0 to 71.5 mg m^‐3 in the dry season and 2.0–17.2 mg m^‐3 in the rainy season confirm earlier reports of increasing phytoplankton biomass in Lake Victoria since the 1960s.

     

Production of dissolved organic carbon in phyloplankton cultures as measured by high-temperature catalytic oxidation and ultraviolet photo-oxidation methods

The production of dissolved organic carbon (DOC) in culturesof the diatoms Chaetoceros gracilis and Phaeodactylum tricornutum,the flagellate Isochrysis galbana, the dinoflagellate Alexandriumtamarense and a natural algal assemblage from the NorthwestArm, Halifax, Nova Scotia, Canada, was followed using a high-temperaturecatalytic oxidation (HTCO) and a UV photo-oxidation method.Molecular weight fractionation of the DOC was performed fortwo cultures: C.gracilis and I.galbana. While the DOC in theculture medium increased significantly during log-phase growthfor all organisms except the dinoflagellate, this increase wasproportional to the increase in cell numbers; the increase inDOC per cell was either small or zero. In all cultures, maximumrelease took place during stationary and senescent phases, usuallyafter cell numbers had started to decrease. In both C.gracilisand I.galbana, a major portion (>65%) of the organic matterreleased to the medium during log-phase growth had mol. wtsof <10 000 Da. The increase in DOC in the I.galbana culturein stationary and senescent phases was due to the release ofhigh-molecular-weight materials. The differences in extracellularrelease of DOC between species and between different growthstages in the same species suggest that both the species compositionand physiological state of phytoplankton populations must beknown before interpretations and predictions based on fielddata can be made. In order to determine whether the differencesin DOC values found by the HTCO and UV oxidation methods arecaused by the resistance to UV oxidation of some compounds producedby phytoplankton, rather than by less than optimum efficiencyof the UV unit used, standards must be based on naturally occurringcompounds, rather than the pure compounds normally used.     

Hydrography and phytoplankton of the Ria de Vigo before and during a red tide of Gymnodinium catenatum Graham

At the end of summer 1986, hydrographic data and phytoplanktonsamples were collected on three occasions in the Ríade Vigo. The phytoplankton composition was studied in relationto the hydrography using principal component analysis and canonicalcorrelation analysis. Upwelling and the response of the planktoncommunity emerge as the main source of variation in the analysesWithin this framework, nutrient regeneration was observed, partlyattributable to ciliates and small flagellates. The second sourceof variation of the phytoplankton was the presence in the latersamples of a Gymnodinium catenatum red tide. Two other phytoplanktonpopulations were clearly differentiated One oceanic, dominatedby Erythropsis sp, Ceratium horridum and Stauroneis membranacea,which practically disappeared when the red Ode was established.The other, dominated by Solenicola setigera, dinoflagellatecysts and elongated diatoms, was a permanent population locatedbelow the populations which responded to upwelling. The penetrationof warm oceanic water into the ría during the secondday of observations altered the distributions of all the planktonicpopulations, isolating them in a downwelling zone. The energyof the oceanic intrusion could have been sufficient to removesediments from the interior of the ría and to stimulatethe formation of the red tide, by confining a water body inthe ría which lost little by mixing. It is likely thatthe resuspension of G.catenatum cysts provided the necessaryinoculum.     

Transport of diatom and dinoflagellate resting spores in ships' ballast water: implications for plankton biogeography and aquaculture

Diatom and dinoflagellate species that are not endemic to aregion can be inadvertently introduced when their resistantresting stages are discharged with the ballast-tank waters andsediments of bulk cargo vessels. A survey of 343 cargo vesselsentering 18 Australian ports showed that 65% of ships were carryingsignificant amounts of sediment on the bottom of their ballasttanks. All of these samples contained diatoms, including speciesthat are not endemic to Australian waters. Diatom resting spores,especially of Chaetoceros, were also detected. Dinoflagellateresting spores (cysts) were present in 50% of the sediment samples.Of the 53 cyst species identified, 20 (including Diplopelta,Diplopsalopsis, Gonyaulax, Polykrikos, Protoperidinium, Scrippsiellaand Zygabikodinium spp.) were successfully germinated to produceviable cultures. Such diversity of diatom and dinoflagellatespecies in ships' ballast water suggests that the apparent cosmopolitanismof many coastal phytoplankton species may be due partly to theglobal transport of seawater ballast. Of considerable concernwas the detection in 16 ships of cysts of the toxic dinoflagellatesAlexandrium catenella, Alexandrium tamarense and Gymnodiniumcatenatum. One single ballast tank was estimated to contain>300 million viable A.tamarense cysts, some of which weresuccessfully germinated in the laboratory to produce toxic cultures.These toxic dinoflagellate species, which can contaminate shellfishwith paralytic shellfish poisons, pose a serious threat to humanhealth and the aquaculture industry. Ballast-water quarantinemeasures recently introduced in Australia are discussed. Mid-oceanexchange of ballast water is only partially effective in removingdinoflagellate cysts which have settled to the bottom of ballasttanks. The present work indicates that the most effective measureto prevent the spreading of toxic dinoflagellate cysts via ships'ballast water would be to avoid taking on ballast water duringdinoflagellate blooms in the water column of the world's ports.     

A 5-year study of the influence of the northeast and southwest monsoons on copepod assemblages in the boundary coastal waters between the East China Sea and the Taiwan Strait

Danshuei River in the northwestern tip of Taiwan dischargesinto the boundary coastal waters between the East China Seaand the Taiwan Strait. We conducted a 5-year study between October1998 and September 2003 to assess the influence of the northeast(NE) and the southwest (SW) monsoons on copepod assemblagesin the area. A total of 110 copepod species were identified.Temora turbinata, Paracalanus aculeatus, Acrocalanus gibber,Parvocalanus crassirostris and Oithona rigida comprised 80%of the copepod assemblages that consisted of coastal speciesfrom the East China Sea and species associated with the KuroshioBranch Current. The effect of the NE monsoon was observed duringa short period of each winter when species such as Calanus sinicuswere transported into the study area by the China Coastal Current.In summer, species such as A. gibber, Acrocalanus gracilis andCanthocalanus pauper may be transported into the study areafrom Southern Taiwan by the combined effect of the SW monsoonand the Kuroshio Current. Influence of the NE monsoon on thecopepod assemblages in terms of introduction of species fromthe Yellow Sea and the East China Sea during winter was observedevery year but was unlikely to represent an important carbonsource into the region due to its short-term nature. Local speciessuch as T. turbinata, P. crassirostris and O. rigida form amajor component of the copepod assemblage. The high copepoddiversity in the area was caused by the year-round presenceof many local species and the aggregation of different speciesfrom subtropical, tropical, and temperate water masses. Monsoon-drivenwater currents and the Kuroshio Branch Current appeared to maskthe effect of river discharge in the region.     

Day-to-day variation in phytoplankton assemblages during spring blooming in a fixed station along the Lebanese coastline

Day-to-day variations in coastal marine phytoplanktonic assemblageswere studied over a 45 day period and related to changing environmentalconditions. Water temperature increased from 17.5 to 23C. Importantfluctuations in water salinity, which normally ranges between37.5 and 39, were recorded. The phytoplankton community sampledwas composed mainly of diatoms, whose numbers increased regularlyover several days. Leptocylindrus danicus was dominant and waspositively correlated to total phytoplankton and total diatomconcentrations. Dinoflagellates did not show regular net variations.Some peaks were recorded which may have been caused by sporadicproliferation of well-known coastal species. Variations in chlorophylla concentration did not parallel increases in total cell numbers,which may have been caused by the introduction of new populationsand contamination of samples by benthic diatoms. In the absenceof thermal stability, changes in meteorological conditions directlyinfluenced phytoplankton populations. Large daily fluctuationsin population numbers and composition were recorded over a shortperiod. Fluctuations were highly significant in successive days.This emphasizes the importance of daily sampling of planktoncommunities. Changes in meteorological conditions appear todisturb the correlation between parameters. Consequently, frequentsampling may be useful in elucidating many secondary phenomenawhich could interfere.     

Oligotrophic waters of the Northwest Atlantic support taxonomically diverse diatom communities that are distinct from coastal waters

Diatoms are important components of the marine food web and one of the most species-rich groups of phytoplankton. The diversity and composition of diatoms in eutrophic nearshore habitats have been well documented due to the outsized influence of diatoms on coastal ecosystem functioning. In contrast, patterns of both diatom diversity and community composition in offshore oligotrophic regions where diatom biomass is low have been poorly resolved. To compare the diatom diversity and community composition in oligotrophic and eutrophic waters, diatom communities were sampled along a 1,250 km transect from the oligotrophic Sargasso Sea to the coastal waters of the northeast US shelf. Diatom community composition was determined by amplifying and sequencing the 18S rDNA V4 region. Of the 301 amplicon sequence variants (ASVs) identified along the transect, the majority (70%) were sampled exclusively from oligotrophic waters of the Gulf Stream and Sargasso Sea and included the genera Bacteriastrum, Haslea, Hemiaulus, Pseudo-nitzschia, and Nitzschia. Diatom ASV richness did not vary along the transect, indicating that the oligotrophic Sargasso Sea and Gulf Stream are occupied by a diverse diatom community. Although ASV richness was similar between oligotrophic and coastal waters, diatom community composition in these regions differed significantly and was correlated with temperature and phosphate, two environmental variables known to influence diatom metabolism and geographic distribution. In sum, oligotrophic waters of the western North Atlantic harbor diverse diatom assemblages that are distinct from coastal regions, and these open ocean diatoms warrant additional study, as they may play critical roles in oligotrophic ecosystems.     

Red tide assemblage formation in an estuarine upwelling ecosystem: Ria de Vigo

Red tides are conspicuous in the upwelling system of Galicia(NW Iberian Peninsula). At present, there are conflicting hypothesesabout the generation site of these phytoplankton assemblages.It is interesting to know whether the rias can be sites of redtide formation or if they act only as accumulation sites ofpopulations advected from shelf waters. A study in the Ra deVigo, carried out during late September 1990, showed the developmentof a red tide assemblage, composed of Alexandrium affinis, Ceraiiumfusus and Gymnodinium catenaium, during a 2 week upwelling-downwellingcycle. Growth occurred at the bottom of the thermocline-topof the nutricline. Above this assemblage, a diatom assemblage(large diatoms) was blooming. Prior to the formation of thered tide, a subsurface chlorophyll maximum made up of smalldiatoms (Nilzschia f. seriaia, Chaeloceros socialis), smallflagellates (<30 µm) and small gymnodinid forms (<30µm) was observed. In the nutrient-depleted upper layer,several autotrophic and large heterotrophic dinoflagellatesdominated. It is suggested that the ratio between the velocityof upward water movement and the depth of the stratified upperlayer (flushing rate, day^–1) is the critical parameterwhich triggers active phytoplankton growth. It can be concludedthat upward water velocities of {small tilde}2.5 m day^–1and a stratified upper layer of 10 m depth (flushing rate 0.25day^–1) are the main physical constraints for red tidedevelopment.