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  • 1
  • 2
    Type of Medium: Book
    Series Statement: ICES council meeting papers 1980(22)
    Language: Undetermined
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  • 3
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Microalgae -- Congresses. ; Biogeochemical cycles -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (327 pages)
    Edition: 1st ed.
    ISBN: 9781402062148
    DDC: 579.8
    Language: English
    Note: 978-1-4020-6214-8_Book_OnlinePDF.pdf -- BIOG_83_1-3_bookprelim1.pdf -- BIOG_83_1-3_bookprelim2.pdf -- BIOG_83_1-3_bookprelim3.pdf -- BIOG_83_1-3_bookprelim4.pdf -- biog_83_1_Prelim_v_vi.pdf -- Introduction -- A taxonomic review of the genus Phaeocystis -- Abstract -- Introduction -- Molecular analysis -- Molecular clock -- Formally described species -- Undescribed species -- Outlook -- References -- Methods used to reveal genetic diversity in the colony-forming prymnesiophytes Phaeocystis antarctica, P. globosa and P. pouchetii-preliminary results -- Abstract -- Introduction -- AmpliWed fragment length polymorphism -- Microsatellite markers -- References -- The life cycle of Phaeocystis: state of knowledge and presumptive role in ecology -- Abstract -- Introduction -- Morphotypes among Phaeocystis species -- Morphotypes of P. globosa -- Colonial cells -- Haploid Xagellates -- Diploid Xagellates -- Morphotypes of P. pouchetii -- Colonial cells -- Flagellates -- Morphotypes of P. antarctica -- Colonial cells -- Flagellates -- Morphotypes of P. jahnii -- Colonial cells -- Flagellates -- Morphotype of P. cordata -- Morphotype of P. scrobiculata -- Synthesis of the observed morphotypes -- The Phaeocystis life cycle -- The haploid-diploid life cycle of P. globosa -- Phaeocystis globosa colony blooms result from sexual processes -- Vegetative reproduction in P. globosa -- Factors inducing phase changes within the P. globosa life cycle -- The life cycle of the other Phaeocystis species -- The haploid-diploid life cycle of Prymnesiophytes -- The ecological relevance of the haploid-diploid life cycle of P. globosa -- The advantage of haploid-diploid life cycles -- The ecology of P. globosa morphotypes -- Conclusions -- References. , Phaeocystis colony distribution in the North Atlantic Ocean since 1948, and interpretation of long-term changes in the Phaeocystis hotspot in the North Sea -- Abstract -- Introduction -- Materials and methods -- The Continuous Plankton Recorder -- Rijkswaterstaat-RIKZ survey -- Data presentation -- Results -- Discussion -- References -- Photosynthetic responses in Phaeocystis antarctica towards varying light and iron conditions -- Abstract -- Introduction -- Methods -- Culture conditions -- Photosynthetic parameters -- Sampling strategy and statistical analyses -- Results -- Discussion -- Acknowledgements -- References -- Effects of iron concentration on pigment composition in Phaeocystis antarctica grown at low irradiance -- Abstract -- Introduction -- Methods and materials -- Isolation of Phaeocystis antarctica -- Laboratory iron-addition dose-response experiment -- Ross Sea pigment samples -- HPLC pigment analyses -- Results and discussion -- Hex:Chl a ratios -- Fuco:Chl a ratios -- Chl c3:Chl a ratios -- Hex:Chl c3 ratios -- Fuco:Hex ratios -- Physiological and ecological implications -- Acknowledgements -- References -- Evidence for high iron requirements of colonial Phaeocystis antarctica at low irradiance -- Abstract -- Introduction -- Methods -- Field collections -- Shipboard iron-light manipulation experiment -- Laboratory dose-response iron-addition experiment -- Analytical methods -- Interpretation of experimental results -- Results and discussion -- Shipboard iron-light manipulation experiment -- Laboratory dose-response iron-addition experiment -- Conclusions and directions for future research -- Acknowledgements -- References -- The carbohydrates of Phaeocystis and their degradation in the microbial food web -- Abstract -- Introduction -- Phaeocystis carbohydrates and their characteristics -- Structural polysaccharides. , Mono- and oligosaccharides -- Storage glucan -- Mucopolysaccharides -- Contribution of mucopolysaccharides-C to POC -- Extra-colonial DOM -- Mechanisms of DOM release during a Phaeocystis bloom -- Formation of hydrogels by Phaeocystis carbohydrates -- Microbial degradation -- Microbial degradation of Phaeocystis carbohydrates -- Microbial degradation of hydrogels -- Conclusions -- Acknowledgements -- References -- The role of iron in the bacterial degradation of organic matter derived from Phaeocystis antarctica -- Abstract -- Introduction -- Materials and methods -- Experimental procedure -- Phaeocystis cultures -- Bacteria cultures -- Regrowth experiments -- Analytical procedures -- Nutrients -- Chlorophyll a and Phaeocystis antarctica biomass -- Organic carbon -- Bacterial biomass and activities -- Statistical analysis -- Results -- Characteristics of LFe and HFe Phaeocystis cultures -- Bacterial regrowth experiments -- Time evolution of organic carbon -- Bacterial communities -- Bacterial activities -- Discussion -- Fe control on P. antarctica-derived organic matter concentration and quality -- Fe control on the bacterial community composition and activities -- Fe control on organic matter remineralization in a Phaeocystis-dominated ecosystem -- Conclusion -- Acknowledgments -- References -- The colonization of two Phaeocystis species (Prymnesiophyceae) by pennate diatoms and other protists: a signiWcant contribution to colony biomass -- Abstract -- Introduction -- Material and methods -- Results -- Discussion -- References -- Zooplankton grazing on Phaeocystis: a quantitative review and future challenges -- Abstract -- Introduction -- Grazing on Phaeocystis: quantitative patterns in published data -- Crustacean zooplankton grazing on Phaeocystis: is there a general pattern? -- Treatment of literature data -- Statistical methods. , Results from statistical analysis -- Quantitative results from data on crustacean grazing -- Grazing by protozooplankton and other microzooplankton -- Cell-type and life-stage-speciWc interactions with grazers -- Colony formation and its potential role in morphological defense -- Chemical defense -- Does DMS aVect grazing on Phaeocystis? -- Does nutritional value aVect grazing on Phaeocystis? -- Survival of gut passage? -- Conclusions and future challenges -- References -- The influence of Phaeocystis globosa on microscale spatial patterns of chlorophyll a and bulk-phase seawater viscosity -- Abstract -- Introduction -- Materials and methods -- Study site -- Microscale sampling device -- Chlorophyll a analysis -- Bulk-phase seawater viscosity measurements -- Potential biases and limitations -- Data analyses -- Identifying spatial structure -- Statistical analyses -- Results -- Environmental conditions -- Microscale spatial variability -- Microscale spatial correlation -- Microscale spatial structure -- Discussion -- Microscale spatial patterns and Phaeocystis globosa bloom dynamics -- Type of spatial patterns and patch sizes -- Small-scale versus microscale variability -- On the potential role of biologically increased seawater viscosity in P. globosa ecology -- Conclusions -- Acknowledgements -- References -- Haemolytic activity of live Phaeocystis pouchetii during mesocosm blooms -- Abstract -- Introduction -- Material and methods -- Mesocosm set up -- Sampling -- Phytoplankton analysis -- Erythrocyte lysis analysis (ELA) -- Data analysis -- Results -- Bloom description -- Haemolytic activity -- Correlation of haemolysis with phytoplankton groups -- Dose response curves at diVerent temperatures -- Light eVects -- Discussion -- References -- Phaeocystis and its interaction with viruses -- Abstract -- Introduction. , Isolation and characterization of viruses infecting Phaeocystis -- Occurrence and dynamics of Phaeocystis viruses -- Diversity of Phaeocystis viruses and its ecological role -- Resistance to viral infection -- Environmental factors inXuencing virus-host interactions -- Virally induced mortality of Phaeocystis -- Impact of viral lysis of Phaeocystis on the microbial food web and element cycling -- Future perspectives -- References -- Does Phaeocystis spp. contribute significantly to vertical export of organic carbon? -- Abstract -- Introduction -- Methods -- Sampling sites and sediment trap measurements -- Analysis and calculations -- Results and discussion -- How to define vertical export of Phaeocystis-derived matter? -- The morphological challenge: cells and colonies -- The relative importance of Phaeocystis spp. cell carbon to vertical POC export -- Does mucus contribute significantly to the vertical export of Phaeocystis spp-derived C? -- Mucus carbon estimates -- Estimated mucus contribution to carbon export -- Fate of Phaeocystis colonies visualised through TEP -- Mechanisms for vertical export -- Concluding remarks -- Acknowledgement -- References -- Vernal sedimentation trends in north Norwegian fjords: temporary anomaly in 234Th particulate fluxes related to Phaeocystis pouchetii proliferation -- Abstract -- Introduction -- Material and methods -- Study area -- Measurements -- Irreversible scavenging model of 234Th -- Results -- Hydrography, Phaeocystis and DMSP distribution in the three fjords -- Vertical distribution of 234Th -- Particulate fluxes of 234Th -- Discussion -- 234Th fluxes and trap collection efficiencies -- Impact of Phaeocystis proliferation on settling flux -- Conclusions -- Acknowledgments -- References. , Environmental constraints on the production and removal of the climatically active gas dimethylsulphide (DMS) and implications for ecosystem modelling.
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  • 4
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Journal of the American Chemical Society 100 (1978), S. 228-246 
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Short- and long-term, light-dark, time-course studies of radiocarbon accumulation in the major intracellular end-products of photosynthesis (proteins, polysaccharides, lipids, small metabolites) and extracellular monomers and polymers were conducted at natural light intensity in Belgian coastal waters and in the English Channel on Phaeocystis poucheti colonies growing under depleted and non-limited, inorganic nitrogen concentration. Evidence is given that the exopolymeric substances which compose the colony envelope, massively secreted during the photoperiod, are used during the dark, together with the intracellular reserve products, to cover the carbon and energetic needs of the colonies either for the maintenance or for pursuing protein synthesis, according to the external inorganic nitrogen level.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Short- and long-term time course studies of radiocarbon accumulation in the intracellular end-products of photosynthesis (proteins, polysaccharides, lipids, small metabolites) and extracellular monomers and polymers were conducted at natural light intensity during a 24-h period in Belgian coastal waters dominated by large diatoms species in September, 1983. It is shown that carbon losses observed during the long-term incubation are due to the catabolism of reserve products (polysaccharides and lipids), which occurs both during the light and dark periods and provides carbon and energy for pursuing protein synthesis during the dark. Catabolism rates, as calculated by means of a simple mathematical model, indicate reduced rates of lipid catabolism (1–2% h-1, respectively for the light and dark periods), although polysaccharide catabolism proceeds at much higher rates, namely 20% h-1 during the light and 8% h-1 during the dark period. Assuming that protein synthesis proceeds at a constant rate during the 24-h period and that β 1–3 glucan constitutes the main storage product of this diatom population, it is shown that at least 65% of the gross primary production is catabolized by the cells. From this, only 16% are mobilized for dark protein synthesis. The remaining is respired, especially during the light period.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Marine biology 107 (1990), S. 305-314 
    ISSN: 1432-1793
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Conversion factors for calculating carbon biomass ofPhaeocystis sp. colonies and free-living cells were determined from microscopic observations and chemical analysis conducted on cultured and naturalPhaeocystis sp. populations originating from the Southern Bight of the North Sea in 1986 and 1987. They allow calculation, in terms of carbon biomass, of the different forms ofPhaeocystis sp. that succeed each other when the population is growing, on the basis of microscopic observations. The latter include enumerations of free-living cells (flagellated and non-motile) and colonies, as well as colonial biovolume measurement. Specific application to natural populations from Dutch coastal waters during spring 1986 shows that more than 90% ofPhaeocystis sp. carbon biomass is under colonial form, most of it exceeding the grazing characteristics of current zooplankton at this period of the year. Detailed analysis of seasonal changes shows in addition that the size of the colonies greatly increases during the course ofPhaeocystis sp. flowering, reaching sizes as high as 1 mm diameter at the top of the bloom when nutrients are depleted. Physiologically this corresponds to an enhanced synthesis of mucilaginous substances, with the decrease of available nutrients leading to an increasing contribution of the matrix to the total colonial carbon during the course of the bloom. Carbon content ofPhaeocystis sp. colonies therefore greatly varies with their size, ranging from 0.3 to 1430 ngC colony−1.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Aquatic ecology 22 (1988), S. 43-55 
    ISSN: 1573-5125
    Keywords: Schelde ; estuary ; phytoplankton ; bacterioplankton ; ecological models
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Since about 10 years, studies have been conducted at the University of Brussels in modelling the microbiological processes affecting biogenic substances in the Schelde estuary and its watershed. The first model, a one dimensional redox model, simulated the longitudinal distribution of oxygen, nitrate, iron and manganese in relation to the observed bacterial heterotrophic activity. A model allowing calculation of bacterial activity from data on organic discharge was coupled to this model. It was completed by a model of phytoplanktonic development within the estuary. Finally, an idealized model of the hydrographical network, based on Horton analysis, is being established in order to calculate the quality of the water at the downward boundary of the estuary. Together, all these sub-models form a general model of the ecological working of the Schelde estuary, able to predict at least the general trends of the redox state, the organic carbon, mineral nitrogen, and chlorophyll-a concentrations as a function of distance to the sea, from the knowledge of geomorphological and meteorological data, along with informations concerning the distribution of anthropogenic discharges. This model therefore provides a powerfull tool for the rational management of the Schelde estuary.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-5117
    Keywords: Northwestern Black Sea ; eutrophication ; mixotrophy ; ciliate ; food web
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Biomass and activities of planktonicmicroorganisms (bacteria, nanoplankton andmicroplankton) were measured in the northwestern BlackSea during summer 1995. The method based on theuptake of fluorescently labeled prey was chosen todetermine the ingestion rate of bacteria andnanoplankton by phagotrophic microorganisms. Thismethod revealed the presence of mixotrophic organismssuch as ’plastid-retaining ciliates‘ in the wholecoastal area. Mixotrophic ciliates were dominated bymicro-sized forms and maximum biomasses were recorded inthe water masses characterised by low nutrientconcentrations but high food particle concentrations. Mixotrophic nanoflagellates were absentand mixotrophic dinoflagellates were observed at onestation only. Mixotrophic ciliates were shown to ingestpreferably bacteria while mixotrophic dinoflagellateswere grazing almost exclusively on nanoflagellates.Although the biomass of mixotrophic organisms weresignificantly lower than those of aplastidic protozoa,their feeding activity contributed to 14 and 24% ofthe ingestion of bacteria and nanoplankton, respectively.This is due to the high specificingestion rate of mixotrophic micro-sized ciliates anddinoflagellates, which were two and three times higher,respectively, than the specific ingestion rate ofbacteria and nanoplankton by aplastidic protozoa. Thissuggests a significant contribution of phagotrophicmixotrophs to the microbial network of thenorthwestern Black Sea.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2020-08-05
    Description: Observations are presented for stable carbon isotope abundance (δ13C) and organic carbon and nitrogen content of suspended organic matter from the Southern Ocean (Circumpolar Current and Polar Front) during spring and early summer. The Polar Front Zone was characterized by elevated plankton biomasses and phytoplankton activity, which also increased significantly over the one-month investigation period. From the beginning of the phytoplankton bloom δ13C values of suspended organic matter in the Polar Front were high, exceeding values predicted from the relationship with CO2(aq) concentration observed in other areas of the Southern Ocean. Later in the season δ13C of suspended organic matter in the Polar Front became more negative despite continued high biomass and productivity. Ambient CO2 concentration and cell growth rate, therefore, are not the only factors controlling the δ13C of phytoplankton. The possible additional impact of shifts in nitrogen uptake regime is discussed.
    Type: Article , PeerReviewed
    Format: text
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