Rates of microbial degradation of dissolved organic carbon from phytoplankton cultures

Dissolved organic carbon (DOC) decay was measured for samplesfrom cultures of the diatoms Chaetoceros gracilis and Phaeodactylumtricornutum, the flagellate Isochrysis galbana, the dinoflagellateAlexandrium tamarense, and a natural algal assemblage from theNorthwest Arm, Nova Scotia, Canada, by a high-temperature catalyticoxidation (HTCO) method. Decay rate constants were determinedusing first-order reaction kinetics in the multi-G model ofBerner (In Early Diagenesis, a Theoretical Approach, PrincetonUniversity Press, 1980). Decay rates as high as 0.37 day^–1wereobtained, which demonstrated that DOC released by phytoplanktonmight be highly labile to bacterial utilization and could bedegraded significantly within hours. Decay rates for most speciestested followed much the same pattern, with K₀₁ values around0.3–0.4, K₀₂ values around 0.03, and K₀₃ and K₀₄ valuesaround 10^–3 day^–1. DOC released by the senescentcells of A.tamarense was found to be essentially bacteria resistant,in contrast to that of the other species tested. The decay ofDOC was directly temperature dependent over the 10–20°Crange. Six methods for DOC preservation were tested. Acidificationwith HCl and refrigerated storage was demonstrated to be themost convenient and practical method. This method can be usedfor both short- and long-term preservation of DOC samples containinghighly labile organic compounds.     

Dr Han L. Golterman,a Limnologist: a tribute on the occasion of his 65th birthday and retirement

The green algae D. tertiolecta, the flagellate I. galbana and the diatom C. gracilis were grown in batch cultures. The organisms were analysed for lipid class composition at the logarithmic and stationary growth phases using the Chromarod-Iatroscan thin layer chromatography with flame ionization detection (TLC-FID) system.There were major differences in lipid class production among the organisms investigated, but few differences in lipid class distribution between log phase and stationary phase cultures of D. tertiolecta and I. galbana. C. gracilis displayed the general trend exhibited in diatom metabolism, which can be characterized by an increase in triacylglycerol synthesis in situations of stress.     

Bacterial response to extracellular dissolved organic carbon released from healthy and senescent Fragilaria crotonensis (Bacillariophyceae) in experimental systems

Responses of bacteria to dissolved organic carbon (DOC) released from healthy and senescent Fragilaria crotonensis (Bacillariophyceae) were examined in experimental systems. The alga released DOC actively, although the concentration fluctuated greatly in both the axenic (the alga alone) and the mixed (the alga plus the enriched bacteria) cultures. In the control (the bacteria alone) cultures, both DOC concentration and bacterial density were low and almost constant throughout the experiment: 5.0 mg C 1^–1 and 1.1 × 10⁵ cells ml^–1, respectively. In the mixed cultures, bacterial growth was negligible during the exponential growth phase of the alga, but rapid proliferation of the bacteria occurred after the onset of the stationary growth phase. As the bacterial population grew, the density of senescent algal cells also increased. When the bacteria were fed on the DOC from healthy algae, their growth rate was relatively low (0.44 d^–1), but the maximum cell density was high (6.4 × 10⁵ cells ml^–1). Conversely, when the bacteria fed on the DOC of senescent algae, they grew at a relatively high rate (0.51 d^–1), but the maximum cell density was low (2.8 × 10⁵ cells ml^–1). These results suggest that DOCs released from dominant phytoplankton species in different physiological states affect the biomass and activity of bacteria.     

CELL-ASSOCIATED PROTEOLYTIC ENZYMES FROM MARINE PHYTOPLANKTON1

Despite their central importance in cell metabolism, little is known about proteases in marine phytoplankton. We surveyed caseinolytic and leucine aminopeptidase (LAP) activities in log-phase cultures of the chlorophyte Dunaliella tertiolecta Butcher, the diatom Thalassiosira weissflogii (Gru.) Fryxell et Hasle, the chrysophyte Isochrysis galbana Parke, the coccolithophorid Emiliania huxleyi (Lohm.) Hay et Mohler, and the cyanobacterium Synechococcus sp. (WH 5701). LAP activity was very low at pH < 6 and peaked between pH 7.5 and 8.5 in all species, whereas caseinolytic activity in most species showed only minor peaks in the pH 4–5 range and broad maxima above pH 8. Thus, acidic vacuolar proteases apparently represented only a small fraction of total protease activity. Attempts to classify proteases using selective inhibitors were inconclusive. Neither the serine/cysteine protease inhibitor leupeptin nor the aspartic protease inhibitor pepstatin. A inhibited caseinolytic or LAP activity in any species. The metalloprotease inhibitor EDTA was only effective against LAP activity in some species, causing average decreases of 30–50%, whereas the cysteine/serine protease inhibitor phenyl methyl sulfonylfluoride achieved at best a 30–60% decrease in caseinolytic activity. Caseinolytic activities were remarkably stable. At pH 7.5 and 25°C, extracts of D. tertiolecta, E. huxleyi, and Synechococcus showed no changes in activity after 24 h, whereas activity declined by less than 50% in the other species. Incubation of cell extracts for 1 h at 25°C in pH 7.5 buffer did not alter patterns of cell proteins, suggesting that endogenous proteases did not effectively degrade endogenous proteins. Casein zymograms were used to identify >200-and <20-kDa proteases in homogenates of log-phase T. weissflogii; only the smaller protease was found in D. tertiolecta. Antibodies to the ATPase subunit (C) of the conserved, chloroplastic Clp protease from Pisum cross-reacted with proteins in Synechococcus, D. tertiolecta, and I. galbana, but no cross-reactions were found for any species with antibodies against the ClpP subunit from either E. coli or Nicotiana. Our results show that phytoplankton contain a diverse complement of proteases with novel characteristics.     

Bias in satellite-derived pigment measurements due to coccolithophores and dinoflagellates

Satellite-derived estimates of phytoplankton pigments are thoughtto be affected by the phytoplankton species composition. Measurementsof surface algal chlorophyll and satellite-derived pigment werecompared for waters containing coccolithophores and dinoflagellates.Satellite-derived chlorophyll concentration was underestimatedby a factor of 2–3 in a patch of the large coccolithophore,Umbilicosphaera sibogae, and also in a bloom of the dinoflagellate,Gonyaulax polyedra. Overall abundance and species-specific propertiessuch as light scatter and vertical migration probably causedthese results.     

Reactive oxygen species as causative agents in the ichthyotoxicity of the red tide dinoflagellate Cochlodinium polykrikoides

The underlying toxic mechanisms of the red tide dinoflagellate,Cochlodinium polykrikoides, were studied with respect to thereactive oxygen species-mediated toxic effect. Cochlodiniumpolykrikoides generates superoxide anion (O₂^–) and hydrogenperoxide (H₂O₂), as measured by the cytochrome c reduction methodand scopoletin–peroxidase method, respectively. The capabilityof C.polykrikoides to generate these oxygen radicals was relatedto the growth phase: the highest rate in the exponential phaseand a gradual decrease in the stationary phase. Other phytoplankton,such as Eutreptiella gymnastica, Heterosigma akashiwo, Prorocentrummicans, Gymnodinium sanguineum and Alexandrium tamarense, alsoproduce H₂O₂; the rate of H₂O₂ generation by these species waslower than that of C.polykrikoides. The exposure of liposomalsamples to intact or ruptured individuals of C.polykrikoidesresulted in severe membrane damage, such as liposomal lipidperoxidation. Cochlodinium polykrikoides-induced lipid peroxidationwas significantly reduced by oxygen radical scavengers, superoxidedismutase, benzoquinone, catalase and mannitol. In addition,lipid peroxidation of gill tissue of flatfish exposed to C.polykrikoidesincreased with increasing algal cell density. These resultssuggest that reactive oxygen species generated from C.polykrikoidesare responsible for oxidative damage leading to fish kills.     

Spatial and temporal patterns of phytoplankton composition in subtropical coastal lagoon, the Indian River Lagoon, Florida, USA

A 2 year study of the phytoplankton community was carried outin the Indian River Lagoon, USA. In terms of biovolume, thephytoplankton community was generally dominated by dinoflagellates,diatoms or cyanobacteria. Mean phytoplankton standing cropswere highest in the most flow-restricted regions of the lagoon,which had the lowest mean salinity values and comparativelyhigh total nitrogen:total phosphorus ratios. In this region,blooms of dinoflagellates were common in the first year of thestudy, which was characterized by an El Niño event thatyielded exceptionally high rainfall levels and freshwater outflow.Picoplanktonic cyanobacteria blooms became more prominent inthe second year of the study, which was characterized by belowaverage rainfall conditions. In unrestricted flow regions ofthe lagoon, located near inlets to the Atlantic Ocean, diatomswere most often the dominant taxa. Regions of intermediate waterturnover rates and high external loading of phosphorus had aprevalence of diatom blooms. However, the average phytoplanktonstanding crops in the latter regions did not reach the levelsexperienced in the flow-restricted parts of the lagoon. In termsof individual phytoplankton taxa, the most common bloom-formingdiatoms in the Indian River Lagoon system included: Skeletonemacostatum, Dactyliosolen fragilissimus, Skeletonema menzelii,Cerataulina pelagica, Odontella regia, Chaetoceros lorenzianus,Rhizosolenia setigera and Thalassionema nitzschioides. The majorbloom-forming dinoflagellate species included: Pheopolykrikoshartmannii, Akashiwo sanguinea, Prorocentrum micans, the potentiallytoxic species Pyrodinium bahamense var. bahamense and Prorocentrumminimum. Several picoplanktonic cyanobacteria were also prominentmembers of the phytoplankton community, including Synechococcuselongates. The spatial and temporal patterns observed in someof these dominant species were attributable to patterns in keyenvironmental variables, including salinity, temperature andnutrient concentrations.     

Weak 'top-down' control of dinoflagellate growth in the coastal Skagerrak

Effects of planktivorous fish (Sprattus sprartus), copepods(mainly Oithona sp.) and benthic filter feeders (Mytilus edulis)on the biomass and species composition of a natural marine planktoncommunity, dominated by dinoflagellates, was studied experimentallyin September 1988. Plastic 300 I cylinders were filled withSkagerrak surface water, filtered through a 90 µm nylonnet in order to remove mesozooplankton. Copepods were addedin three different concentrations (0, 1x and 6x the ambientdensity) with and without nutrient additions (nitrate, silicateand phosphate). In two nutrient-enriched cylinders with addedcopepods (1x and 6x), 5 cm sprats were also added (10 per cylinder).In two nutrient-enriched cylinders without added copepods. bluemussels (20 per cylinder. 3 cm length) were introduced. Chlorophylla. inorganic nutrients and densities of phytoplankton, ciliatesand copepods were measured throughout the experimental periodof 10 days. Gyrodinium aureolum increased in cell numbers inall but the mussel cylinders, while the other dominating dinoflagellate,Ceratium furca, decreased. This decrease was not due to grazing,but probably a container artefact. Diatoms, Rhizosolenia fragilissinia,Leptocylindrus danicus and Chaetoceros spp., increased slowlyin treatments without fish. In the fish treatments, diatomshad appreciably higher growth rates and cell numbers, probablydue to predation by fish on the copepods. Gyrodiniun aureolunalso had a somewhat higher growth rate in the presence of fish.although this was probably not due to reduction of copepod grazing.The results show that planktivorous fish can affect the biomassand species composition of natural phytoplankton communitiesin marine waters, but that the effect on the late summer-autumndinoflagellate dominated community is weak. Blue mussels areefficient grazers of the whole phytoplankton community and arenot particularly selective with respect to either size or species.     

Roles of mixotrophy in blooms of different dinoflagellates: Implications from the growth experiment

Studies over the last two decades suggested that mixotrophy could be an important adaptive strategy for some bloom-forming dinoflagellates. In the coastal waters adjacent to the Changjiang River estuary in the East China Sea, recurrent blooms of dinoflagellates Prorocentrum donghaiense, Karenia mikimotoi and Alexandrium catenella started to appear from the beginning of the 21 century, but roles of mixotrophy in the formation of dinoflagellate blooms were not well understood. In the current study, mixotrophy-based growth of four selected bloom-causative dinoflagellate species, i.e. K. mikimotoi, A. catenella, P. donghaiense and Prorocentrum micans, were studied. Dinoflagellates were co-cultured with different prey organisms, including bacterium Marinobacter sp., microalgae Isochrysis galbana and Hemiselmis virescens, under a variant of nutrient conditions. It was found that growth of dinoflagellate K. mikimotoi was significantly promoted with the presence of prey organisms. Growth of P. donghaiense and P. micans was only slightly improved. For A. catenella, the addition of prey organisms has no effects on the growth, while both of the two prey microalgae I. galbana and H. virescens were killed, probably by allelochemicals released from A. catenella. There was no apparent relationship between nutrient conditions and the mixotrophy-based growth of the tested dinoflagellates. Based on the results of the growth experiment, it is implicated that mixotrophy may play different roles in the growth and bloom of the four dinoflagellate species. It can be an important competitive strategy for K. mikimotoi. For the two Prorocentrum species and A. catenella, however, the role of mixotrophy is much limited. They may depend more on other competitive strategies, such as phototrophy-based growth and allelopathic effect, to prevail in the phytoplankton community and form blooms.     

Colloidal organic carbon and phytoplankton speciation during a coastal bloom

During the 1995 spring bloom in Bedford Basin, Nova Scotia,dissolved organic carbon (DOC) in the photic zone was separatedinto low-molecular-weight and colloidal size fractions by cross-flowultrafiltration. DOC, colloidal organic carbon (COC) and low-molecular-weightorganic carbon (LOC) were then analyzed by high-temperaturecatalytic oxidation. COC (associated with the production ofphytoplankton exudates) did not follow the concentration ofbulk chlorophyll a (chi a) or the total number of phytoplanktoncells. Instead, surface-active COC (that adhered to the ultrafiltrationsystem) was produced early during the bloom when the diatomSkeletonema costatum was at a maximum. Later on, as the bloombegan to decline, less surface-active COC (that remained largelyfree of the ultrafiltration surfaces) was produced and was associatedmore with variations in cell number of Chaetoceros socialis,the predominant diatom for most of the bloom. These resultssuggest that chl a or the total number of phytoplankton cellsmay not be reliable indices of the production of COC. On thecontrary, the results suggest that relatively high COC concentrationswere associated with specific diatom species. In addition, themaximum amount of COC was associated during the early stagesof the bloom with a diatom (S.costatum) that was a small fraction(<5.6%) of total phytoplankton cell number. This finding,that relatively large amounts of colloids were associated withexopolymer production during the onset and development of abloom, does not agree with reports suggesting that the productionof exopolymers by diatoms is primarily an end-of-bloom occurrence.     

Growth and bioluminescence of Noctiluca scintillans on varying algal diets

The effects of food concentration and food quality on the growthrate and bioluminescence potential of the heterotrophic dinoflagellateNoctiluca scintillans were examined. The growth rate of N. scinullansvaried greatly with the phytoplankton food it was provided,and those foods yielding higher growth rates also produced cellsthat were smaller in diameter, but with a greater bioluminescencepotential per unit volume. Small phytoplankton species, includingIsochrysis galbana and an unidentified chrysophyte responsiblefor the Texas brown tide, supported the lowest growth rates.Other small flagellates (Dunaliella tertiolecta) and dinoflagellates(Gyrodinium dorsum, Prorocentrum minimum) supported moderategrowth rates. The highest growth rates were supported by diatomsand prasinophytes. Maximum growth rates (0.5 day^-1) were obtainedwith the diatom Thalassiosira sp. at concentrations     

Oil production from five marine microalgae for the production of biodiesel

Marine microalgae were studied as potential resources for the production of biodiesel. Five marine microalgae, Tetraselmis suecica, Phaeodactylum tricornutum, Chaetoceros calcitrans, Isochrysis galbana, and Nannochloropsis oculata were cultured in f/2 media, 12:12 L:D cycle at 20 ± 1°C with a light intensity of 36.3 μmol/m²/sec using a 15-L circular cylindrical photobioreactor. The dry cell weight, specific growth rate, biomass productivity, oil content and fatty acid composition of palmitic acid, stearic acid, oleic acid, linoleic acid, and linolenic acid of microalgae were determined. T. suecica, I. galbana, and N. oculata showed high dry cell weights of 0.58, 0.57, and 0.57 g/L, respectively. The culture period of T. suecica to reach the stationary phase was 9 days. On the other hand, N. oculata showed the longest culture period of 28 days to reach the stationary phase. T. suecica absorbed nitrate at the initial stages of cell growth, decreasing the nitrate concentration to 0.5 mg/L on day-7 of the culture. The highest oil contents were observed in P. tricornutum with a 25.31% dry cell weight and I. galbana with a 23.15% dry cell weight on day-9 after the stationary phase. I. galbana showed 417.33 mg of palmitic acid per g oil and T. suecica showed 235.61 mg of oleic acid per g oil. Stearic acid, linoleic acid, and linolenic acid did not exceed 30.02 mg/g oil in any of the microalgae. T. suecica showed the shortest culture period of 9 days to reach the stationary phase. Therefore, the highest biomass production of 0.58 g/L was obtained and I. galbana showed high biomass production of 0.57 g/ L and oil content of 23.15% of dry cell weight. Therefore, T. suecica and I. galbana can be selected as a potential candidate for the production of biodiesel.     

The Early Jurassic palynostratigraphy of the Lusitanian Basin,western Portugal

A comprehensive investigation of the Early Jurassic stratigraphical palynology of the Lusitanian Basin in western Portugal was undertaken, with most emphasis placed on dinoflagellate cysts. A total of 214 samples from an upper Sinemurian to upper Toarcian composite section based on six successions were examined. The Sinemurian material examined was barren of dinoflagellate cysts; however, the Pliensbachian and Toarcian successions are characterised by relatively low diversities where Luehndea spinosa, Mancodinium semitabulatum, Mendicodinium microscabratum, Nannoceratopsis gracilis, Nannoceratopsis senex, and Scriniocassis priscus are relatively common and biostratigraphically significant. Luehndea spinosa dominates the lowermost Toarcian (Dactylioceras polymorphum ammonite Biozone), and is an index species. At the base of the Hildaites levisoni ammonite Biozone, the effects of the Toarcian Oceanic Anoxic Event (T-OAE) caused Luehndea spinosa to become extinct. At the same time, dinoflagellate cyst abundance and diversity markedly decreased. After the T-OAE, during the middle and late Toarcian, phytoplankton recovery was prolonged and slow in the Lusitanian Basin. The Luehndea spinosa and Mendicodinium microscabratum dinoflagellate cyst biozones are defined, both of which are subdivided into two dinoflagellate cyst subbiozones.     

Growth inhibition of the eight species of microalgae by growth inhibitor from the culture of Isochrysis galbana and its isolation and identification

A type of growth inhibitor was successfully isolated and purified from cell-free filtrates of cultural medium at the death phase of Isochrysis galbana, and its chemical structure was confirmed by the methods of FABMS, UV, ¹H-NMR, ¹³C-NMR and 2D NMR, which was 1-[hydroxyl-diethyl malonate]-isopropyl dodecenoic acid, C₂₂H₃₈O₇. The results showed that the growth-inhibitor strongly inhibited the growth of Isochrysis galbana, and the growth of the eight species of microalgae (Dunaliella salina, Platymonas elliptica, Chlorella vugralis, Nitzschia closterium, Chaetoceros muelleri, Chaetoceros gracilis, Nitzschia closterium minutissima, Phaeodactylum tricornutum) also could be regulated by the growth-inhibitor in a concentration-dependent manner. The further investigation found that the synthesis process of chlorophyll and protein in the cells of all test microalgae could be inhibited by the growth inhibitor, and the content of chlorophyll and protein significantly decreased.     

Structural analysis of winter phytoplankton in the Gulf of Naples

Quantitative and qualitative distribution of surface phytoplankton,as related to hydrographic conditions, was studied in the Gulfof Naples in February 1979. Previous work has shown that the Gulf of Naples is a diversifiedecosystem, due to geographic and hydrographic features as wellas man made eutrophication, that can be subdivided into twomajor parts: a coastal subsystem and an open water one. Hydrographic analysis of the winter situation at the surfacefully confirms this picture, as it identifies two distinct watermasses corresponding respectively to surfaced Tyrrhenian IntermediateWater and to Coastal Surface Water. The structural analysisof phytoplankton reveals three assemblages of species characterizingdifferent water types: 1 - the Ischia and Procida channels affectedby the advection of Volturno river and Cuma outfall plumes;2 - the coastal area of the Gulf proper, namely the bays ofPozzuoli, Naples and Castellammare; 3 - the open waterhemislocated beyond the 100 m isobath. The channel area assemblage is dominated by diatoms, particularlyby fast growing species, such as Asterionella japonica, severalspecies of Chaetoceros and Rhizosolenia hebetata f. semispina.The coastal assemblage is identified, among others, by the diatomsCerataulina bergonii, Hemiaulus sinensis; the dinoflagellatesGlenodinium lenticula, Exuviaella compressa and Porella perforata.The open water assemblage is characterized by the diatoms Coscinodiscuscurvatulus and Hemidiscus cuneiformis, the dinoflagellate Amphidiniumacutissimum and the coccolithophore Coccolithus haeckelii.     

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.     

Changes in the structure of a zooplankton community during a Ceratium (dinoflagellate) bloom in a eutrophic fishless pond

The community structure of zooplankton was studied in a eutrophic,fishless Japanese pond. The ecosystem was dominated by a dinoflagellate,Ceratium hirundinella, two filter-feeding clado-cerans, Daphniarosea and Ceriodaphnia reticulata, and an invertebrate predator,the dipteran Chaoborus flavicans. The midsummer zooplanktoncommunity showed a large change in species composition (theDaphnia population crashed) when a heavy Ceratium bloom occurred.It is shown that (i) the rapid density decline of D.rosea inmid-May was mainly caused by a shortage of edible phytoplankton,which was facilitated by the rapid increase in Chirundinellaabundance; (ii) the low density of D.rosea in June-July wasconsidered to be mainly caused by the blooming of Ceratium hirundinella(which may inhibit the feeding process of D.rosea), while predationby Cflavicans larvae, the changing temperature, the interspecificcompetition and the scarcity of edible algae were not judgedto be important; (iii) the high summer biomass of the planktonicCflavicans larvae was maintained by the bloom of C.hirundinella,because >90% of the crop contents of C.flavicans larvae wereC.hirundinella during this period. The present study indicatesthat the large-sized cells or colonies of phytoplankton arenot only inedible by most cladocerans, but the selective effectof the blooming of these algae can also influence the compositionand dominance of the zooplankton community, especially for thefilter-feeding Cladocera, in a similar way as the selectivepredation by planktivorous fish. The large-sized phytoplanktoncan also be an important alternative food for ominivorous invertebratepredators such as Chaoborus larvae, and thus may affect theinteractions between these predators and their zooplanktonicprey. In this way, such phytoplankton may play a very importantrole in regulating the dynamics of the aquatic food web, andbecome a driving force in shaping the community structure ofzooplankton.     

Nutritional suitability of the dinoflagellate Ceratium furcoides for four copepod species

The nutritional suitability of Ceratium furcoides for Eudiaplomusgracilis, Mesocyclops leuckarti, Thermocyclops oithonoides andCyclops abyssorum was studied by observing ingestion and assimilation.The dinoflagellate was ingested by female adults of all species.The calanoid copepod E.gracilis could not utilize Ceratium;mortality was high and no egg production was observed when Ceratiumwas the only food source. Mortality was low for the adult cyclopoidson this food and reproduction indicated that Ceratium was assimilated.The first two copepodite instars of M.leuckarti were not ableto handle Ceratium, while older stages preyed on them. The dinoflagellatewas not ingested by female M.leuckarti when its densities werelow. Advanced copepodite stages of C.abyssorum developed intoadults on a diet of Ceratium only. Mesocyclops leuckarti femalesingested Ceratium when offered a mixed food source of Ceratiumand the rotifer Brachionus rubens, but the rotifer was positivelyselected, even if its density was low. The results show thatCeratium provides a suitable food source for advanced copepoditeinstars and adult cyclopoid copepods, although it is not a preferredfood source.     

Assimilation numbers in cultures of marine phytoplankton

During exponential growth in batch culture, assimilation numbersof eleven algal species ranged from 1.6–20.8, with a meanvalue of 5.3 g C/g Chlorophyll a/hr. The highest assimilationnumber of 20.8 g C/g Chlorophyll a/hr was observed in Coccolithuspelagicus, due to the relatively low concentration of chlorophylla/cell. The assimilation number declined from exponential tostationary phase in batch cultures for ten algal species, butincreased with age in batch culture in Amphiprora paludasa (abenthic diatom). The assimilation number declined with decreasinggrowth rate in nitrate-limited chemostat cultures of Phaeodactylumtricornutum and in iron-limited chemostat cultures of Phaeodactylumtricornutum and Isochrysis galbana.     

STOICHIOMETRIC RESPONSES OF PHYTOPLANKTON SPECIES TO THE INTERACTIVE EFFECT OF NUTRIENT SUPPLY RATIOS AND GROWTH RATES1

Three species of phytoplankton, Rhodomonas sp., Phaeodactylum tricornutum Bohlin, and Isochrysis galbana Parke, were cultivated in semicontinuous culture to analyze the response of carbon (C):nitrogen (N):phosphorus (P) stoichiometry to the interactive effect of five N:P supply ratios and four growth rates (dilution rates). The relationship between cellular N and P quotas and growth rates fits well to both the Droop and Ågren’s functions for all species. We observed excess uptake of both N and P in the three species. N:P biomass ratios showed a significant positive relationship with N:P supply ratios across the entire range of growth rates, and N:P biomass ratios converged to an intermediate value independent of N:P supply ratios at higher growth rates. The effect of growth rates on N:P biomass ratios was positive at lower N:P supply ratios, but negative at higher N:P supply ratios for both Rhodomonas sp. and I. galbana, while for P. tricornutum this effect was negative at all N:P supply ratios. A significant interactive effect of N:P supply ratios and growth rates on N:P biomass ratios was found in both Rhodomonas sp. and P. tricornutum, but not in I. galbana. Our results suggest that Ågren’s functions may explain the underlying biochemical principle for the Droop model. The parameters in the Droop and Ågren’s functions can be useful indications of algal succession in the phytoplankton community in changing oceans.